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22 February 2019 Description of Two Species of Hoploscaphites (Ammonoidea: Ancyloceratina) from the Upper Cretaceous (Lower Maastrichtian) of the U.S. Western Interior
Neil H. Landman, W. James Kennedy, Neal L. Larson, Joyce C. Grier, James W. Grier, Tom Linn
Author Affiliations +
Abstract

Two species of scaphitid ammonites (Ammonoidea: Ancyloceratina) from the Upper Cretaceous (lower Maastrichtian) of the Western Interior of North America are described. Hoploscaphites macer, n. sp., is medium size, with coarse ribs on the phragmocone, which become finer on the body chamber, and closely spaced ventrolateral tubercles. It occurs in the upper part of the Baculites baculus Zone and lower part of the overlying B. grandis Zone in the Pierre Shale in Montana, Wyoming, and Colorado, and in the Bearpaw Shale in Montana. Hoploscaphites criptonodosus (Riccardi, 1983) is larger and more coarsely ornamented, including one or two rows of lateral tubercles on the flanks of the phragmocone. It occurs in the upper part of the Baculites baculus Zone and overlying B. grandis Zone in the Pierre Shale in Montana, Wyoming, Colorado, and possibly South Dakota, and in the Bearpaw Shale in Montana and Saskatchewan, Canada. Both species form part of an evolving lineage of Hoploscaphites that first appears in the Western Interior of North America in the middle Campanian.

INTRODUCTION

The Upper Cretaceous Western Interior of North America contains a rich assemblage of scaphitid ammonites (hereafter referred to as scaphites for short). Hoploscaphites appears in the Western Interior in the middle Campanian Baculites asperiformis Zone and persists to the upper Maastrichtian Hoploscaphites nebrascensis Zone (fig. 1). It is represented by approximately 15 species, many of which have yet to be described. All of them are endemic to North America, with closely related species in western Greenland (Birkelund, 1965). They have occasionally been reported from Western Europe, but only as fragments (Machalski et al., 2007). Such rare occurrences are probably due to postmortem drift. In contrast, Hoploscaphites constrictus Sowerby, 1817, which is present in the Maastrichtian of Europe, is absent in North America.

Many of the species of Hoploscaphites in the Western Interior are very well preserved, retaining their original shell material and buccal apparatus. Their excellent preservation is due to their rapid burial in muddy to silty sediments that are nearly impermeable to groundwater penetration during postdepositional history. In addition, the ammonites commonly occur in early diagenetic concretions that preserve their three-dimensional shape. The shell material is also preserved with its original mineralogy and microstructure and is, thus, suitable for carbon and oxygen isotope analyses. The results of these studies suggest that species of Hoploscaphites lived close to the bottom in well-oxygenated environments (Landman et al., 2012a).

GEOLOGIC SETTING

Williams and Stelck (1975) and Landman et al. (2016) reviewed the paleogeography of the Western Interior Seaway during the early Maastrichtian. The western margin of the Seaway was bordered by a north-south trending unstable cordillera, whereas the eastern margin was formed by the low-lying stable platform of the eastern part of the coterminous United States and Canada (Cobban et al., 1994). The shoreline cut across the eastern half of Montana (fig. 1), forming a peninsula at the southeastern corner of the state that is referred to as the Sheridan Delta (Reiskind, 1975). The delta extended along the Montana-Wyoming border as far east as the Black Hills and separated the Mosby Embayment to the west from the rest of the Western Interior Seaway to the east (fig. 1). This deposit may not have comprised a single delta, but rather multiple deltas, reflecting shedding of sediments from regional uplifts in the area of the Big Horn and Granite Mountains (Krystinik and DeJarnett, 1995). The shoreline continued southwestward as a series of embayments as far as the northwestern corner of Colorado, and then cut southeastward across the middle of the state.

FIGURE 1.

Overview of the Late Cretaceous Western Interior Seaway (left) and close-ups of the strandlines (right) during the deposition of the upper Campanian–lower Maastrichtian Baculites eliasiB. grandis zones (modified from Landman et al., 2016). The numbered dots indicate U.S. localities cited in the text, as listed in the appendix.

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The fossil localities in this study are close to the western margin of the Seaway, probably less than 100 km from shore, according to the paleogeographic maps produced by Cobban et al. (1994) and modified by Slattery et al. (2013). The depth of the Seaway during this time is difficult to precisely establish, but recent studies have suggested that it was less than 100 m deep (Gill and Cobban, 1966; Kauffman and Caldwell, 1993; Sageman and Arthur, 1994). Based on the fauna, sedimentology, and distance from shore on the Cedar Creek Anticline in east-central Montana, we estimate that the depth of deposition in this area was possibly even less, perhaps ≤⃒50 m.

The sedimentary record of the Seaway contains a rich molluscan fauna that is used to subdivide the Upper Cretaceous strata of this area into numerous biostratigraphic zones (fig. 2). This zonation has been integrated with radiometric dates derived from interbedded bentonites (Cobban et al., 2006). The Maastrichtian Stage in the Western Interior Basin has been subdivided into six ammonite zones (Gill and Cobban, 1966; Landman and Waage, 1993a; Larson et al., 1997). They are, from lowest to highest, the Baculites baculus, B. grandis, B. clinolobatus, Hoploscaphites birkelundae, H. nicolletii, and H. nebrascensis zones (fig. 2). Walaszczyk et al. (2001) further refined the zonation using inoceramids. The B. baculus Zone is subdivided into the Endocostea typica Zone below and the “Inoceramus” incurvus Zone above, and the B. grandis Zone coincides with the Trochoceramus radiosus Zone (fig. 2). The Campanian-Maastrichtian boundary is placed at the base of the B. baculus Zone coincident with the base of the E. typica Zone (Walaszcyk et al., 2001; Cobban et al., 2006).

Hoploscaphites macer, n. sp., occurs in the upper part of the Baculites baculus Zone and lower part of the B. grandis Zone in the Pierre Shale in Montana, Colorado, and Wyoming, and the Bearpaw Shale in Montana. Hoploscaphites criptonodosus (Riccardi, 1983) occurs in the upper part of the B. baculus Zone and overlying B. grandis Zone in the Pierre Shale in Montana, Colorado, Wyoming, and possibly South Dakota, and in the Bearpaw Shale in Montana. It has also been reported from the B. baculus Zone in the Belanger Member of the Bearpaw Shale in southwestern Saskatchewan, Canada (Riccardi, 1983). The presence of this species in both the United States and Canada testifies to the broad extent of the Western Interior Seaway during the deposition of the lower Maastrichtian B. baculus Zone. In contrast, no ammonites are known from Canada in the overlying B. grandis Zone, implying that the Seaway must have retreated from this area by the late early Maastrichtian (Riccardi, 1983; Landman et al., 2017).

FIGURE 2.

Biostratigraphic chart of the Upper Cretaceous (Campanian and Maastrichtian) of the Western Interior of North America showing ammonite and inoceramid zones (modified from Cobban et al., 2006).

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STRATIGRAPHY

Old Woman Anticline, Wyoming

Many of the specimens in this study are from the Old Woman Anticline at Red Bird, Niobrara County, Wyoming. This section has been extensively documented by Gill and Cobban (1966), Hicks et al. (1999), and Slattery et al. (2018), and we briefly review it here (fig. 3). The Baculites baculus and B. grandis zones occur in the upper unnamed member of the Pierre Shale. This unit conformably overlies the Kara Bentonitic Member. It is 207 m thick and consists of variably sandy and silty shale containing many layers of fossiliferous limestone concretions. Several beds of bentonite and bentonitic shale occur in the middle of the unit. The sediments become progressively sandier and siltier toward the top of the section. The contact with the overlying Fox Hills Formation is marked by a 0.37 m thick bentonite overlain by a 4 m thick bed of glauconitic sandstone (unit 112, Gill and Cobban, 1966) containing a few phosphatic nodules and phosphatized internal molds of Baculites (see Gill and Cobban, 1966: 37).

Cedar Creek Anticline, Montana

Most of the other specimens in this study are from the Cedar Creek Anticline in east-central Montana (figs. 4, 5). The geology of the Upper Cretaceous section on the anticline has been described by Calvert (1910), Coryell and Salmon (1934), Erdmann et al. (1936), DeWolf and West (1939), Gries (1954), Robinson et al. (1959), Bishop (1967, 1973), Gill and Cobban (1973), Clement (1986), Grier et al. (1992, 2007), Grier and Grier (1998), Walaszczyk et al. (2001), Vuke et al. (2003), Linn (2010), and Landman et al. (2015a, 2018b). As a result of renewed study of this section in the last several years, we present a modified version of the stratigraphic column originally published by Bishop (1967, 1973).

FIGURE 3.

Stratigraphic section of the Pierre Shale at Red Bird, Niobrara County, Wyoming (modified from Gill and Cobban, 1966), showing the ranges of three species of Hoploscaphites The D numbers refer to USGS Mesozoic localities cited in the text.

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The Cedar Creek Anticline occupies parts of Dawson, Wibaux, Prairie, and Fallon counties, Montana, and Bowman County, North Dakota (fig. 1). The Pierre Shale in this area consists of light to dark gray fissile, silty or sandy shale 60–65 m thick interbedded with bentonites and bentonitic shale. It contains iron manganese (Fe-Mn), limestone, and sandy-bedded concretions, some of which are abundantly fossiliferous. The Pierre Shale becomes progressively siltier up section and is overlain by the Fox Hills Formation (fig. 5A), which is overlain in turn by the Hell Creek Formation. The Pierre Shale is late Campanian to early Maastrichtian in age and contains the upper part of the Baculites eliasi, B. baculus, and lower part of the B. grandis zones (fig. 4). The section is equivalent in age to the lower one-half of the upper unnamed shale member of the Pierre Shale at Red Bird, Wyoming, as described by Gill and Cobban (1966).

The lower part of the Pierre Shale in the northern area of the Cedar Creek Anticline is 10 m thick and consists of dark gray shale with seven thin bentonite layers and several layers of Fe-Mn concretions (Bishop, 1967, 1973; Linn, 2010). It is overlain by approximately 11 m of gray shale with additional Fe-Mn concretions and relatively abundant specimens of Baculites eliasi Cobban, 1958. Approximately 15 m above this interval are two layers of brownish-tan to yellowish sandy-bedded concretions (fig. 5E, F), commonly coated with cone-in-cone structure, which Bishop (1967, 1973) referred to as the “bedded concretions.” The upper layer is more persistent than the lower layer and is a reliable stratigraphic marker in this area.

Small, white, spherical to flat, sparsely fossiliferous carbonate concretions occur just below, in between, and just above the sandy-bedded concretions. Specimens of Baculites eliasi occasionally occur up to 2 m below the bedded concretions. Both the bedded and small white concretions occur in light gray sandy shale. A few large specimens of B. baculus Meek and Hayden, 1861, appear in the same horizon as the upper layer of sandy-bedded concretions (fig. 5F) in association with Endocostea typica (Whitfield, 1877) (fig. 6A) and Eurysalenia minima Kier, 1966 (7B). A cold methane seep deposit also occurs at this horizon and represents the highest occurrence of such deposits in the U.S. Western Interior (Delaney et al., 2018). The top layer of sandy-bedded concretions marks the base of the B. baculus and E. typica zones, which represents the Campanian-Maastrichtian boundary in this area.

An interval of gray septarian concretions occurs approximately 2 m above the upper layer of sandy-bedded concretions. Many of these septarian concretions contain barite crystals and invertebrate fossils including species of Hoploscaphites and Endocostea typica (fig. 6A). Another layer of concretions occurs approximately 1 m above the septarian concretions. They contain a diverse fauna with several species of Hoploscaphites, which Bishop (1967, 1973) aptly called the “scaphite concretions.” This is the source of the concretion studied in detail by Landman et al. (2015a). The septarian and scaphite concretions occur in gray fissile shale. The scaphite concretions are overlain, in turn, by a 2 m thick interval of bentonitic shale capped by a 7–8 cm thick bentonite (fig. 5C, D). On fresh exposures, the bentonite is pale yellow in color, but upon weathering, it turns light gray and develops a popcorn texture, with scattered gypsum crystals on top (fig. 5D). A few concretions occur within the bentonitic shale and contain species of Hoploscaphites and Endocostea typica. The top of the bentonite is approximately 8 m above the top of the upper layer of andy-bedded concretions (fig. 4).

FIGURE 4.

Stratigraphic section of the Pierre Shale and Fox Hills Formation on the Cedar Creek Anticline, east-central Montana (modified from Bishop, 1967, 1973; Landman et al., 2018b), showing the ranges of three species of Hoploscaphites.

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Immediately above the bentonite are approximately 15 m of medium gray fissile shale with intermittent gray limestone concretions 0.3–1.0 m in diameter. The lowest layer of concretions above the bentonite contains “Inoceramusincurvus Meek and Hayden, 1856, marking the base of the “I.” incurvus Zone (= upper Baculites baculus Zone) (fig. 7A, C). Because the concretions in this zone contain numerous inoceramids, we refer to them as inoceramid concretions. However, they also contain a wide variety of other faunal elements including other bivalves, gastropods, and scaphites. The species of Baculites in this interval appear to be intermediate between B. baculus and B. grandis (see Bishop, 1967; Linn, 2010).

The sediment coarsens toward the top of the Pierre Shale and consists of a 3 m thick interval of gray to light olive-gray, silty shale (fig. 4). Gray limestone concretions contain Baculites grandis Hall and Meek, 1855, and, very rarely, Trochoceramus radiosus (Quaas, 1902) (fig. 6B). The lowest occurrence of B. grandis and T. radiosus marks the base of the B. grandis and T. radiosus zones, respectively. Hoploscaphites macer, n sp., is relatively abundant in this interval, along with fewer specimens of H. criptonodosus and H. sargklofak Landman et al., 2015b.

The Pierre Shale is conformably overlain by the Fox Hills Formation (figs. 4, 5A). The base of this formation is marked by a layer of yelloworange jarosite nodules (Bishop, 1967, 1973; Linn, 2010) (fig. 5B). Occasionally this layer contains rare phosphatized internal molds of Baculites (fig. 6C–K). Because of the compressed shape of these internal molds, we attribute them to B. clinolobatus Elias, 1933. The presence of these phosphatized specimens indicates a lag deposit possibly associated with a transgression post-dating the deposition of the B. clinolobatus Zone and prior to the final retreat of the Western Interior Seaway (Gill and Cobban, 1966). The Fox Hills Formation is as much as 32 m thick and consists of yellowish gray silty, sandy shale in the lower part and yellowish-gray shale alternating with sandy shale and sandstone in the upper part. The top of the Fox Hills Formation culminates in a light-colored, nearshore sandstone called the Colgate Member that is up to 40 m thick (Vuke et al., 2003). The Hell Creek Formation, where present, conformably overlies the Fox Hills Formation.

MODE OF LIFE AND HABITAT OF SCAPHITES

The mode of life and habitat of scaphites, principally species of Hoploscaphites, has been reviewed by Landman et al. (2012a). The adult stage is indicated by the uncoiling of the body chamber and consists of a shaft and hook, which recurves backward. The uncoiling of the body chamber can be viewed as a morphogenetic countdown reflecting the growth of the reproductive organs and the attainment of maturity. The countdown begins at the point at which the shell departs from the spiral coil and develops into the shaft. This marks the beginning of an essentially irreversible process, unless a fatal injury intervenes, culminating in the formation of the adult shell. It involves a sequence of morphogenetic events that proceed step by step and terminate with the cessation of growth. Internally, the initiation of the morphogenetic countdown is indicated by closer spacing of the last two or three septa.

The shape of the aperture at maturity is an important clue to the mode of life of scaphites. The apertural opening is reduced in size relative to the whorl section at the point of recurvature. The shape of the aperture is visible in specimens in which the body chamber is broken in half. The aperture is kidney shaped with an elongate, broadly rounded projection along the dorsum (fig. 8C, D). This projection probably impeded unrestricted movement of the soft body outside of the aperture. Therefore, it is unlikely that scaphites were equipped with long arms or tentacles. In addition, the ventral and lateral sides of the aperture are bordered by a deep constriction that ends in a thin lip (fig. 9), further reducing the size of the aperture.

FIGURE 5.

Outcrops of the Pierre Shale and Fox Hills Formation on the Cedar Creek Anticline, east-central Montana. A. Overview of the contact between the Pierre Shale and Fox Hills Formation. The contact is marked by a color change from gray silty shale to yellowish gray silty sandy shale. The sagebrush in the foreground is 0.5 m high. B. Circular yellowish-orange jarosite nodules (arrow), approximately 14 × 16 cm in diameter, mark the base of the Fox Hills Formation. C. Photo from the top of the 2 m thick bentonitic shale, foreground, looking out over an adjacent part of the same outcrop. (The outcrop was cut through to make way for an oilfield transmission line.) The top of the bentonite coincides with the boundary between the upper and lower parts of the Baculites baculus Zone. D. The surface of the bentonite (pale yellow when freshly exposed) weathers to a light-gray popcornlike texture with irregular polygons, each approximately 4 cm × 4 cm in size. E. Upper layer of sandy-bedded concretions, which coincides with the boundary between the B. eliasi Zone below and the B. baculus Zone above, locally demarcating the Campanian-Maastrichtian boundary (length of hammer = 27 cm). F. Rare specimen (one of only four recovered from this interval) of B. baculus Meek and Hayden, 1861, from a light gray/tan concretion in the upper layer of sandy-bedded concretions (length of hammer = 32.5 cm).

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Because of the uncoiling of the body chamber, adult scaphites are poorly designed for swimming. Jacobs et al. (1994) investigated swimming efficiency in Scaphites whitfieldi Cobban, 1952, from the Turonian Carlile Shale of South Dakota. They did flow tank experiments on models of actual juvenile and adult specimens. They plotted the coefficient of drag versus Reynolds number (a proxy for the rate of flow). They demonstrated that the coefficient of drag is higher in adults than in juveniles during horizontal swimming. Thus, the uncoiling of the body chamber at maturity increases the coefficient of drag and decreases the hydrodynamic efficiency. In addition, scaphites lack a midventral sinus, implying that they could not have easily recurved their hyponome backward. As a result, they were probably limited to backward or downward swimming.

The musculature in scaphites also provides some insights into the swimming ability of these animals. Only two types of muscle scars are present in scaphites. The unpaired midventral scar appears a few millimeters adoral of the midventral saddle in the external lobe (fig. 8A, B). It is small and oval in shape. The dorsal muscle scar is wedge shaped and drapes over the umbilical shoulder on either side of the midline just adoral of the last suture. No lateral muscle scars are present. If Nautilus is used as a model for swimming in scaphites, the lack of large retractor muscles implies that little propulsive power was available for strong swimming.

Scaphites probably lived in well-oxygenated environments near the bottom. Sessa et al. (2015) studied the isotopic composition of species of Discoscaphites from the upper Maastrichtian Owl Creek Formation of Mississippi. The isotopic values of the scaphites at this site are more similar to those of benthic rather than planktic foraminifera, suggesting that the scaphites lived close to the bottom. Slattery et al. (2018) recently investigated the record of faunal communities, including scaphites, along the western margin of the Western Interior Seaway during the early Maastrichtian. They demonstrated that changes in faunal communities during this time interval reflected a number of environmental factors such as distance from shore, level of oxygen, and water depth. Scaphites are more common in the more nearshore, better oxygenated settings. In addition, observations of the kind and incidence of shell injuries suggest that scaphites were sometimes attacked by animals that lived close to the bottom, indicating that scaphites probably lived in the same habitat as these predators (Landman et al., 2010).

FIGURE 6.

A. Endocostea typica (Whitfield, 1877), AMNH 72834, Pierre Shale, 7 m below the crest of the 2 m-thick bentonitic shale, AMNH loc. 3921, Cedar Creek Anticline, east-central Montana. B. Trochoceramus radiosus (Quaas, 1902), AMNH 106046, Pierre Shale, highest layer of concretions below the base of the Fox Hills Formation, AMNH loc. 3921, Cedar Creek Anticline, east-central Montana. C–K. Phosphatized fragments of Baculites at the base of the Fox Hills Formation, Cedar Creek Anticline, east-central Montana. Because of their compressed whorl section, they are attributed to Baculites clinolobatus Elias, 1933. C, D. AMNH 106139, AMNH loc. 3921. C, Right lateral; D, whorl cross section at adapical end. E, F. USNM 723200, USGS Mesozoic loc. D14195. E, Right lateral; F, whorl cross section at adapical end. G-K. AMNH 106133, AMNH loc. 3921. G, Right lateral; H, dorsal; I, ventral; J, left lateral; K, whorl cross section at adapical end. Specimens ×1.

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The limited swimming ability of scaphites, especially as adults, may have prevented them from migrating over long distances. Instead, they may have exploited a low-energy lifestyle, remaining at a single site for an extended period of time. The discovery of scaphites and other ammonites in cold methane seep deposits in the Upper Cretaceous Western Interior is consistent with this hypothesis (Landman et al., 2012b, 2018a). The scaphites at some of these sites are very well preserved and permit analysis of the carbon and oxygen isotopic composition of the shell material. The carbon isotopic composition of specimens in seep deposits is statistically lower than that of specimens at age equivalent nonseep sites, implying that some scaphites may have spent part or all of their lives at a single seep.

EVOLUTIONARY PATTERNS

Landman et al. (2010) redescribed species of Hoploscaphites from the Upper Cretaceous (upper Campanian) Western Interior of North America. They noted a high degree of variation within and between species. They compared H. nodosus (Owen, 1852) and H. brevis (Meek, 1876), which occur in the same ammonite zones (Baculites compressusB. cuneatus zones). Although they treated these two species as separate, they noted that H. nodosus and H. brevis could be interpreted as representing the coarsely and finely ornamented end members, respectively, of the same species. Landman et al. (2010: 72–73) concluded that “it is entirely possible that all of the scaphites in the Baculites compressusB. cuneatus zones represent a single very variable species” and argued that “the differences in size, degree of compression, and coarseness of ornament [among specimens] may simply reflect differences in the rate of growth and age at maturity, keyed to changes in the environment.

A similar argument could be made for Hoploscaphites criptonodosus and H. sargklofak (fig. 10). Both species occur in the same ammonite zone (Baculites grandis Zone). The pattern of ornamentation is the same in both forms, including the presence of lateral tubercles on the exposed phragmocone, but the ribs and tubercles are coarser in H. criptonodosus than in H. sargklofak. In addition, the size and degree of compression differ between the two species, with H. criptonodosus being larger and more robust than H. sargklofak. Thus, in theory, the two forms could represent the coarsely and finely ornamented end members, respectively, of the same species. However, because the two forms can be easily distinguished (perhaps owing to the lack of transitional specimens in our collections), and in deference to historical precedence, we maintain them as separate species.

One of the conspicuous trends in the evolution of scaphites in the Western Interior Seaway during the Maastrichtian is the directional change over time in whorl shape and tuberculation (Landman and Waage, 1993a, 1993b). The flanks of the body chamber are flatter and the incidence of tubercles on the exposed phragmocone is higher in geologically younger species. This is apparent in a comparison between older species from the lower part of the Baculites baculus Zone with younger species from the upper part of the B. baculus Zone and overlying B. grandis Zone. These patterns are further played out in the overlying B. clinolobatus Zone that contains two undescribed species in which the flanks of the body chamber are even flatter and the exposed whorls are covered with even more tubercles.

FIGURE 7.

A, C. “ Inoceramusincurvus Meek and Hayden, 1856, AMNH 10659, AMNH loc. 3921, Pierre Shale, Cedar Creek Anticline, east-central Montana. B. Close-up of Eurysalenia minima Kier, 1966, AMNH 106132, in a small white concretion from the sandy-bedded concretionary interval, AMNH loc. 3921, Cedar Creek Anticline, east-central Montana.

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FIGURE 8.

A, B. Unpaired ventral muscle scar (arrow) just adoral of the last suture, Hoploscaphites macer, microconch, AMNH 69736, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. C. Apertural view of dorsal projection (arrow), Hoploscaphites criptonodosus (Riccardi, 1983), AMNH 108459, AMNH loc. 3278, Baculites grandis Zone, Pierre Shale, Weston County, Wyoming. The hook of the body chamber has broken off exposing the dorsal projection, which is plastered against the venter of the phragmocone. D. Kidney-shaped apertural opening showing the dorsal projection, Hoploscaphites criptonodosus (Riccardi, 1983), macroconch, AMNH 71830, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana.

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FIGURE 9.

Cross section of the shell wall at the apertural margin of a mature macroconch of Hoploscaphites criptonodosus (Riccardi, 1983), AMNH 94676, AMNH loc. 3728, Baculites grandis Zone, Pierre Shale, Weston County, Wyoming. A. Overview of part of the apertural margin. The exterior direction is toward the right and the adoral direction is toward the top. The shell wall bends sharply inward at nearly a right angle forming a thick varix and then reflects outward terminating in a flared lip. During fossilization, sediments usually accumulate in the narrow gap behind the flared lip (for a rare example in which epizoans colonized this gap during the lifetime of the ammonite, see Landman et al., 2016). B, C. Close-ups of the shell wall showing the recurved layers of shell.

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These changes in whorl shape and tuberculation can be captured in 3-D surface scans of ammonite specimens. We scanned six specimens with the help of Carolyn Merrill (AMNH) using an Arctec Space Spider scanner equipped with Artec Studio 12 software. The results of some of these scans are shown in figure 11. These images can be examined and manipulated in MeshLab and Geomagic. In collaboration with William Harcourt-Smith (AMNH), we are developing techniques to quantify the degree of tuberculation using spiral and radial transects that intersect the ribs and tubercles. Our preliminary results indicate that the “ridge and swale” topography produced by ribs can be distinguished from the “cinder cone” topography produced by tubercles, thus providing quantitative measures of the degree and kind of ornamentation.

FIGURE 10.

Hoploscaphites sargklofak Landman et al., 2015b, macroconchs. A, B. AMNH 108324, AMNH loc. 3264, lower Baculites grandis Zone, Pierre Shale, Weston County, Wyoming. A, Right lateral; B, ventral. C, D. AMNH 77027, Baculites grandis Zone, Pierre Shale, locality unknown. C, Right lateral; D, ventral. Arrows indicate the base of the body chamber. Specimens ×1.

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FIGURE 11.

Surface scans showing the lateral and apertural views of macroconchs of three species of Hoploscaphites spanning the Baculites baculus to B. grandis zones. A, B. Hoploscaphites criptonodosus, AMNH 108313, AMNH loc. 3269, B. grandis Zone, Pierre Shale, Weston County, Wyoming. C, D. Hoploscaphites macer, BHI 4306, AMNH loc. 3921, upper B. baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, eastcentral Montana. E, F. Hoploscaphites sp., AMNH 108443, AMNH loc. 3921, lower B. baculus Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana.

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The evolutionary changes in tuberculation and whorl shape are associated with changes in the environment in which the ammonites lived. As shown in the section on the Cedar Creek Anticline in east-central Montana, the sediments become siltier upsection from the Baculites baculus to the B. grandis zones (fig. 4). This trend is also apparent in the section on the Old Woman Anticline in northeast Wyoming, where it persists into the B. clinolobatus Zone (fig. 3). This change in lithology reflects the overall progradation of the shoreline eastward during the early Maastrichtian (although a brief transgression occurs during the deposition of the upper part of the B. grandis and lower part of the B. clinolobatus zones; see Slattery et al., 2018: fig. 13). Thus, both sites represent progressively more nearshore environments over time.

The increase in the number of tubercles may be related to an increase in the number and kinds of predators in these shallower water environments. Many studies have documented a relationship between ornamentation and predation in ammonites and other molluscs (Kroger, 2002; Larson, 2003; Keupp, 2006; Landman et al., 2010; Takeda et al., 2016). In Hoploscaphites criptonodosus and H. sargklofak, tubercles effectively increased the size of the shell, making it appear larger and less attractive to possible predators. The tubercles are also sharp and pointy, although in most specimens, the tips of the tubercles are now missing due to taphonomic factors. These conical projections probably made the shell more difficult to grasp by predators. Thus, the tubercles may have helped these scaphites elude predators or, in the event of an attack, may have limited the size of the damage to the shell.

This hypothesis is supported by an examination of injuries in other species of Hoploscaphites from the Western Interior Seaway. Landman and Waage (1986, 1993a, 1993b) studied the incidence of nonlethal injuries in two species of Hoploscaphites from the upper Maastrichtian Fox Hills Formation. They compared H. spedeni Landman and Waage, 1993a, from the Trail City Member with H. nebrascensis (Owen, 1852) from the overlying Timber Lake Member. The number of tubercle rows is higher in H. nebrascensis than in H. spedeni (nine versus seven rows of tubercles, respectively). The environment of these two species also changes from a more offshore to a more nearshore setting during this interval in response to the retreat of the Seaway during the Maastrichtian. At the same time, the incidence of injuries (number of injured specimens versus the total number of specimens in the sample) increased from 11.2% in H. spedeni to 25.8% in H. nebrascensis. One interpretation of these results is that H. nebrascensis became more successful at surviving attacks (Landman and Waage, 1986), possibly due to the presence of additional tubercles on the shell.

The change in whorl shape over time can also be interpreted in terms of an adaptation to shallower water environments. For example, the whorl section at midshaft is more compressed in Hoplocaphites sargklofak than in H. macer. The average value of WS/HS is 0.70 in H. sargklofak, as reported in Landman et al. (2015b), versus 0.77 in H. macer (table 1). This difference is consistent with hydrodynamic expectations. At higher Reynolds numbers (approximately equivalent to higher rates of flow) characteristic of higher energy environments, the coefficient of drag is lower in more compressed forms due to their smaller cross-sectional area. Jacobs et al. (1994) previously investigated this relationship in their study of scaphites from the Carlile Shale of South Dakota in which they utilized a flow tank to measure coefficient of drag versus Reynolds number with casts of actual specimens.

FIGURE 12.

Scaphite terminology (after Landman et al., 2013: 9, fig. 3). A. Macroconch, right lateral view. Abbreviations: HH = whorl height at the point of recurvature; HP1 = whorl height at the adapical end of the phragmocone; HP2 = whorl height at the adoral end of the phragmocone; HS = whorl height at midshaft; LMAX= maximum length along the long axis; apt. <) = apertural angle. B. Microconch, right lateral view. C. Close-up of the umbilicus of the macroconch showing the umbilical diameter measured parallel to the long axis (UD). D. View of the venter of the body chamber at midshaft, with the adoral direction toward the top, showing the width of the venter (VS), as measured between the ventrolateral margins.

f12_01.jpg

TERMS, METHODS, AND REPOSITORIES

Most of the terms used to describe scaphites are reviewed by Landman et al. (2010). The adult shell consists of a closely coiled phragmocone and a slightly to strongly uncoiled body chamber (fig. 12). The adult phragmocone is the part of the phragmocone that is exposed in the adult shell, as compared to the part that is concealed inside. The point of exposure is the most adapical point of the adult phragmocone. The body chamber consists of the shaft, beginning near the last septum, and a hook terminating at the aperture. The point of recurvature is the point at which the hook curves backward.

Measurements of the adult shell are illustrated in figure 12. The maximum length of the adult shell (LMAX) was measured from the venter of the adult phragmocone to the venter of the hook. The umbilical diameter of the adult shell (UD) was measured through the center of the umbilicus parallel to the line of maximum length. Whorl width (W) and whorl height (H) were measured at four points on the adult shell: (1) the adapical end of the phragmocone 90° adapical of the line of maximum length (WP1, HP1), (2) the adoral end of the phragmocone along the line of maximum length (WP2, HP2), (3) the body chamber at midshaft (WS, HS), and (4) the hook at the point of recurvature (WH, HH). The width of the venter at midshaft (VS) was measured between ventrolateral margins on opposite sides of the venter. All measurements were made using electronic calipers on actual specimens, rather than on photos. We calculated several ratios to describe the shape of the adult shell and facilitate comparisons among specimens. The ratios of whorl width to whorl height were calculated at four points on the shell (WP1/HP1, WP2/HP2, WS/HS, WH/HH), as described above, and provide a measure of the degree of whorl compression. The ratio of ventral width to whorl height at midshaft (VS/HS) provides an additional measure of the degree of whorl compression. The ratio of maximum length to whorl height of the phragmocone along the line of maximum length (LMAX/ HP2) is a measure of the degree of uncoiling. The ratio of maximum length to whorl height at midshaft (LMAX/HS) is a measure of the degree of curvature of the body chamber in lateral view. If the outline of the body chamber in lateral view is a semicircle, the ratio of LMAX/HSequals 2. This ratio applies only to macroconchs because the umbilical seam of the body chamber usually coincides with the line of maximum length in these forms, and thus the whorl height is the distance from the line of maximum length to the venter of the body chamber (equivalent to the radius in the case of a semicircle). The apertural angle, as defined by Landman and Waage (1993a) and Machalski (2005), was measured on photographs of specimens in lateral view. A line was drawn along the umbilical shoulder and another line was drawn along the apertural margin. The apertural angle is the angle of intersection between these two lines, extending from approximately the point of recurvature to the aperture. We restricted this measurement to macroconchs, but even in these forms, it is sometimes difficult to know where to draw the line along the umbilical shoulder because the shoulder occasionally shows a bulge or sag.

A number of terms describe ornamentation. Primary ribs originate near the umbilicus, whereas secondary ribs originate on the flanks or venter, either by branching or intercalation. The density of ribs is measured by counting the number of ribs/cm on the venter at four points on the adult shell: (1) the adapical end of the phragmocone, (2) the adoral end of the phragmocone, (3) the midshaft, and (4) the hook. In addition to ribs, the ornamentation includes tubercles, which are small conical swellings. Umbilicolateral tubercles occur near the umbilicolateral margin, ventrolateral tubercles occur near the ventrolateral margin, and lateral tubercles occur on the flanks (fig. 12). The number of ventrolateral and umbilicolateral tubercles on the phragmocone and body chamber of the adult shell were counted. We recorded the distance between tubercles following the curvature of the shell, for example, along the umbilicolateral margin for umbilicolateral tubercles and along the ventrolateral margin for ventrolateral tubercles. We also recorded the number of ribs that loop between ventrolateral tubercles on opposite sides of the venter.

The repository of specimens described in the text is indicated by a prefix, as follows: Division of Paleontology (Invertebrates), American Museum of Natural History (AMNH), New York; Black Hills Institute of Geological Research (BHI), Hill City, South Dakota; Denver Museum of Nature and Science (DMNH), Denver; the Field Museum (FM), Chicago; Geological Survey of Canada (GSC), Ottawa; Mississippi Museum of Natural Science (MMNS), Jackson, Mississippi; Yale Peabody Museum (YPM), New Haven, Connecticut; and U.S. National Museum (USNM), Washington, D.C. The localities of the specimens are listed in the appendix.

SYSTEMATIC PALEONTOLOGY

Class Cephalopoda Cuvier, 1797
Order Ammonoidea Zittel, 1884
Suborder Ancyloceratina Wiedmann, 1966
Superfamily Scaphitoidea Gill, 1871
Family Scaphitidae Gill, 1871
Subfamily Scaphitinae Gill, 1871
Genus Hoploscaphites Nowak, 1911
[= Mesoscaphites Atabekian, 1979: 523 (nomen nudum) fide Kennedy, 1986; Wright, 1996; Jeletzkytes Riccardi, 1983: 14].

  • Type Species: Ammonites constrictus J. Sowerby (1817: 189, pl. A, fig. 1), by original designation.

  • Diagnosis: “Small to large scaphites, strongly dimorphic, with broad variation in degree of whorl compression ranging from slender to robust, with involute phragmocone, short to long shaft, and weakly recurved hook; apertural angle ranging from approximately 35° to 85°; aperture constricted with dorsal projection; ribs straight to flexuous, increasing by branching and intercalation, with weak to strong adoral projection on venter; adult shell with or without umbilicolateral, flank, and ventrolateral tubercles; suture fairly indented, with symmetrically to slightly asymmetrically bifid first lateral lobe” (Landman et al., 2010: 93).

  • Discussion: In their monograph on the scaphites of the “nodosus group,” Landman et al. (2010) treated Jeletzkytes Riccardi, 1983, as a junior subjective synonym of Hoploscaphites. They argued that the shape of the shell, the pattern of ornamentation, and the complexity of the suture are the same in both genera, the only differences being the degree of compression and, as a result, the flexuosity of the ribs and the size of the tubercles. They noted that such variation already exists within the genus Hoploscaphites, as previously defined, and exemplified by the type species H. constrictus. Wright (1996: 261–262) cited the same reason for synonymizing the two genera: “Separation of the large and inflated species of the nodosus group as Jeletzkytes seems unnecessary, given the great variation within most scaphitid species.” Later, Cooper (1994) erected the new subgenus Karlwaageites for derived members of Jeletzkytes from North America that bear lateral tubercles. However, the number and distribution of lateral tubercles can vary even within a single species, casting doubt on the utility of this character for subgeneric separation. Until a thorough phylogenetic revision of all scaphitid genera and subgenera is undertaken, we prefer to follow a more conservative approach and treat all these species in the genus Hoploscaphites.

  • Hoploscaphites macer, n. sp.
    Figures 8A, B, 11C, D, 13–22, 23A–C, 24, 25

  • Diagnosis: Macroconchs oval to nearly circular in lateral view; cross section of shaft compressed subovoid with high whorls consisting of broadly rounded flanks and nearly flat venter; maximum width at adoral part of shaft; small umbilicus commonly with umbilical bulge; ribs coarse on phragmocone at the point of exposure, subsequently becoming finer; small, moderately closely spaced ventrolateral tubercles; small umbilicolateral tubercles on body chamber; occasional lateral tubercles on adapical part of phragmocone; apertural angle averaging 56°; microconchs oval in lateral view; cross section of shaft subovoid with broadly rounded flanks converging toward ventrolateral shoulder; large umbilicus exposing earlier whorls; closely spaced ventrolateral tubercles; relatively prominent umbilicolateral tubercles on body chamber; suture with broad, asymmetrically bifid first lateral saddle and narrow, symmetrically to asymmetrically bifid first lateral lobe.

  • Etymology: The name is derived from the Latin word macer, “thin,” which is one's first impression of this species relative to other species in the same biostratigraphic zones. Upon inspection, however, the shell is slightly inflated. Nevertheless, this name has been used informally for the last 20 years, and for the sake of stability, we decided to retain the name for this species.

  • Types: The holotype is AMNH 71839 (figs. 19E–H, 23A), a macroconch, from the lower part of the B. grandis Zone of the Pierre Shale on the Cedar Creek Anticline, Montana. It is a steinkern with some attached shell 54.2 mm in diameter with a small umbilicus. The macroconch paratypes are AMNH 113323 (fig. 20D–F) and 113324 (fig. 20G–I), both from the upper part of the B. baculus Zone or the lower part of the B. grandis Zone of the Pierre Shale on the Cedar Creek Anticline, Montana, and USNM 713612 (fig. 17A–C) from the B. grandis Zone of the Bearpaw Shale in Roosevelt County, Montana. The microconch paratypes are AMNH 72634 (fig. 24M–P) and 108314 (fig. 24E–H) from the upper part of the B. baculus Zone or the lower part of the B. grandis Zone of the Pierre Shale on the Cedar Creek Anticline, Montana.

  • Material: The collection consists of approximately 100 specimens of which 75 comprise the measured set (40 macroconchs and 35 microconchs) (tables 1, 2). All the specimens in our collection are from the upper part of the Baculites baculus Zone or lower part of the B. grandis Zone of the Pierre Shale in Wyoming, Colorado, and Montana and the Bearpaw Shale in Montana.

  • Macroconch Description: In the measured sample, LMAX averages 61.4 mm and ranges from 45.2 to 76.0 mm (table 1). The ratio of the size of the largest specimen to that of the smallest is 1.68. The specimens form a broad size distribution, with a peak at 50–55 mm (fig. 13). Adults are slender with an oval to circular outline in side view. LMAX/HSaverages 2.05 and ranges from 1.86 to 2.25 (1.94 in the holotype). BHI 4346 (fig. 14A–D) is an example of a specimen with an oval outline (LMAX/HS= 2.17) and AMNH 108487 (fig. 19A–D) is an example of a specimen with a more rounded, nearly perfectly circular outline (LMAX/HS= 1.98).

    The umbilicus is small and deep. The umbilical diameter averages 3.8 mm and ranges from 1.9 to 6.5 mm. UD/LMAX averages 0.06 and ranges from 0.04 to 0.12. In lateral view, the umbilical wall is straight and usually exhibits a pronounced umbilical bulge, so that part of the umbilicus of the phragmocone is concealed. All specimens are tightly coiled with little or no gap between the phragmocone and hook. LMAX/HP2averages 2.78 and ranges from 2.55 to 2.98 (2.70 in the holotype). AMNH 76388 (fig. 18A–C) is an example of a tightly coiled specimen (LMAX/HP2= 2.75) and BHI 4346 (fig. 14A–D) is an example of a more loosely coiled specimen (LMAX/HP2= 2.89).

    The exposed phragmocone occupies approximately one-half whorl and usually terminates just below the line of maximum length. AMNH 76367 (not figured) is an exception in which the phragmocone terminates just adapical of midshaft. An unpaired muscle scar appears on the venter just adoral of the end of the phragmocone (fig. 8A, B). The body chamber consists of a short shaft and recurved hook totaling slightly more than one-half whorl. The apertural lip is flexuous with a deep constriction, as in other scaphites (fig. 9). The apertural angle averages 55.9° and ranges from to 36.0° to 69.0° (44.5° in the holotype).

    The whorl section of the phragmocone near the point of exposure is compressed subovoid with maximum whorl width at one-third whorl height. WP1/HP1averages 0.98 and ranges from 0.82 to 1.16 (0.99 in the holotype). The umbilical wall is steep and subvertical and the umbilical shoulder is sharply rounded. The flanks are broadly rounded and converge toward the venter starting at two-thirds whorl height. The ventrolateral shoulder is sharply rounded and the venter is broadly rounded. The whorl section of the phragmocone at the line of maximum length is more compressed than that at the point of exposure, reflecting a marked increase in whorl height. WP2/HP2averages 0.88 and ranges from 0.74 to 0.98 (0.84 in the holotype). In addition, the flanks are very broadly rounded and the venter is nearly flat.

    As the shell passes from the phragmocone into the body chamber, the whorl width increases and reaches its maximum value on the adoral part of the shaft and, as a result, the shell forms a bulge in this area. Whorl height increases even more markedly during this transition and reaches its maximum value at midshaft. Thereafter, it diminishes to the point of recurvature and remains nearly the same up to the aperture. Because of these changes in whorl width and height, the whorl section at midshaft is only slightly more compressed than that along the line of maximum length (table 1). WS/HSaverages 0.81 and ranges from 0.67 to 0.95 (0.80 in the holotype). The whorl section is subovoid with maximum whorl width at one-quarter whorl height. The umbilical wall is steep and subvertical and the umbilical shoulder is sharply rounded. The whorls are very high and broadly rounded and gently converge to the venter. The ventrolateral shoulder is sharply rounded and the venter is nearly flat. VS/HSaverages 0.40 and ranges from 0.30 to 0.51 (0.38 in the holotype).

    The whorl section at the point of recurvature is less compressed than that at midshaft, mainly due to a decrease in whorl height. WH/HHaverages 1.06 and ranges from 0.94 to 1.19 (1.11 in the holotype). The whorl section at the point of recurvature is subovoid with maximum whorl width at one-half whorl height. The umbilical wall is slightly concave and the umbilical shoulder is sharply rounded. The flanks are broadly rounded and gently converge toward the venter.

    At the adapical end of the exposed phragmocone, ribs emerge at the umbilical seam and strengthen across the umbilical wall and shoulder. They attain their maximum strength at onethird whorl height and in some specimens, such as AMNH 113324 (fig. 20G–I) develop into small umbilicolateral tubercles at this point. Ribs are rectiradiate to slightly prorsiradiate and weakly flexuous, bending slightly backward on the inner flanks, slightly forward on the midflanks, and slightly backward again on the outer flanks. They are widely spaced, with intercalation and branching occurring at one-third and two-thirds whorl height, so that the outer flanks are more densely covered with ribs than the inner flanks. Ribs are uniformly strong on the venter, which they cross with a slight adoral projection. The rib density on the venter on the adapical end of the phragmocone ranges from 6 to 8 ribs/cm in our measured sample (7 ribs/cm in the holotype).

    The same pattern of ribbing persists onto the adoral part of the phragmocone. However, because the whorl section is more compressed at this point than on the adapical part of the phragmocone due to an increase in whorl height and a flattening of the flanks, the ribs on the adoral part of the phragmocone are relatively longer and more closely spaced. The rib density on the venter on the adoral end of the phragmocone ranges from 6 to 9 ribs/cm in our measured sample (9 ribs/cm in the holotype).

    On the body chamber, ribs arise at the umbilical seam and are rursiradiate on the umbilical wall and shoulder. They are adorally concave at one-third whorl height and in many specimens form small umbilicolateral tubercles at this point. The tubercles are evenly spaced and usually extend to the aperture. In the holotype, the distance between consecutive umbilicolateral tubercles at midshaft is 5 mm. Ribs are straight and prorsiradiate on the middle and outer flanks, with branching and intercalation occurring at two-thirds whorl height. As a result, the outer flanks are more densely covered with ribs than the inner flanks. Ribs cross the venter with a strong adoral projection. They become more closely spaced toward the aperture. In our measured sample, the rib density ranges from 7 to 10 ribs/cm on the midshaft versus 8 to 13 ribs/cm on the hook (10 versus 13 ribs/cm, respectively, in the holotype).

    Ventrolateral tubercles develop early in ontogeny at a diameter of approximately 6 mm and persist onto the exposed phragmocone (fig. 22). Because the venter is broadly rounded, the tubercles occur slightly below the ventrolateral shoulder. The tubercles are widely and unevenly spaced on the adapical end of the exposed phragmocone, but become more closely and uniformly spaced toward the adoral end. In the holotype, the distance between consecutive tubercles on the exposed phragmocone, starting at the point of exposure, is 7, 6.5, 4.5, 3, 5, 3, 5, 3, 4, and 4 mm (fig. 19E–H). The total number of ventrolateral tubercles on the exposed phragmocone ranges from 6 to 13 in our measured sample (11 tubercles in the holotype). The tubercles are conical in shape and change from slightly radially elongate at the point of exposure to slightly clavate at the adoral end of the phragmocone.

    Ventrolateral tubercles persist onto the body chamber. They gradually become more widely spaced, attaining their maximum spacing on the adoral end of the shaft, and become more closely spaced again on the hook. In the holotype, the distance between consecutive ventrolateral tubercles is 6 mm at midshaft, 7.5 mm on the adoral end of the shaft, and 4.5 mm on the hook (fig. 19E–H). Three or four ribs loop between tubercles on opposite sides of the venter at midshaft, with an equal number of ribs intercalating between them. Because the venter is broadly rounded to nearly flat, the tubercles appear at or just below the ventrolateral shoulder. The number of ventrolateral tubercles on the body chamber ranges from 10 to 25 in our measured sample (16 in the holotype). The tubercles are clavate on the adoral end of the shaft where they attain their maximum height. They become smaller on the hook and, in some instances, slightly radially elongate.

    In a few specimens, small lateral tubercles occur on the adapical end of the exposed phragmocone. They form a single row at two-thirds whorl height and persist for as much as onequarter whorl. For example, in USNM 713623 (not figured), a single row of five lateral tubercles is present beginning at the point of exposure. They occur on every rib and are evenly spaced at intervals of 2.5 mm. Similarly, in AMNH 113323 (fig. 20D–F), a single row of five lateral tubercles appears on the adapical end of the phragmocone and persists for one-eighth whorl.

    The suture is deeply incised, with a broad, asymmetrically bifid first lateral saddle (E/L) and a narrow, symmetrically to asymmetrically bifid first lateral lobe (L) (fig. 23A, B).

  • Microconch Description: In comparison with macroconchs, microconchs are characterized by a more openly coiled shell with a larger umbilicus. In addition, the umbilical shoulder is concave in lateral view and the umbilicolateral tubercles are more prominent. LMAX averages 45.1 mm and ranges from 35.4 to 56.6 mm (table 2). The ratio of the average size of microconchs to that of macroconchs is 0.73. The size distribution is unimodal with a peak at 35–40 mm (fig. 13).

    Microconchs are oval in lateral view. The phragmocone usually terminates at or below the line of maximum length. Microconchs are less tightly coiled than macroconchs with a gap between the phragmocone and hook. LMAX/HP2averages 2.90 and ranges from 2.56 to 3.22. AMNH 72624 (fig. 25E–G) is an example of an openly coiled specimen (LMAX/ HP2= 3.19) and AMNH 76383 (fig. 24I–L) is an example of a more tightly coiled specimen (LMAX/HP2= 2.90). The body chamber occupies slightly more than one-half whorl. The umbilicus is relatively large. UD/LMAX averages 0.08 and ranges from 0.06 to 0.11. The average value of UD/LMAX is significantly higher in microconchs than it is in macroconchs (UD/LMAX = 0.06).

    The whorl section of the exposed phragmocone is compressed subquadrate. WP1/HP1averages 0.89 and ranges from 0.64 to 1.16; WP2/HP2averages 0.86 and ranges from 0.70 to 1.01. The umbilical wall is steep and nearly vertical, the umbilical shoulder is sharply rounded, and the flanks are broadly rounded and gently converge to the ventrolateral shoulder. The ventrolateral shoulder is sharply rounded and the venter is broadly rounded.

    Whorl width gradually increases from the phragmocone into the body chamber, attaining its maximum value on the hook. Whorl height also increases gradually from the phragmocone into the body chamber, but reaches its maximum value at midshaft and remains nearly the same thereafter. The whorl section at midshaft is compressed subquadrate with maximum width at one-quarter whorl height. WS/HSaverages 0.86 and ranges from 0.75 to 0.99 (table 2). The umbilical wall is steep and slopes outward at an acute angle. The flanks are broadly rounded and converge gently toward the ventrolateral shoulder. The ventrolateral shoulder is sharply rounded and the venter is nearly flat. VS/HSaverages 0.41 and ranges from 0.31 to 0.54. The whorl section at the hook is more ovate than that at midshaft. WH/HHaverages 0.99 and ranges from 0.82 to 1.17. The venter is broadly rounded, which is accentuated by the disappearance of the ventrolateral tubercles.

    On the exposed phragmocone, ribs emerge at the umbilical seam and are slightly rursiradiate on the umbilical wall. They are weakly flexuous on the flanks, swinging gently backward on the inner flanks, gently forward on the midflanks, and gently backward again on the outer flanks. Ribs are uniformly strong on the venter, which they cross with a weak adoral projection. They are relatively closely spaced with an average of 8 ribs/cm on both the adapical and adoral portions of the phragmocone.

    Ribs are long and prorsiradiate on the shaft, swinging gently forward on the midflanks and backward again on the outer flanks. In general, ribs are much weaker on the shaft than on the phragmocone. Intercalation and branching occur at two-thirds whorl height. Ribs cross the venter with a strong adoral projection and become more closely spaced on the hook. For example, in AMNH 108314 (fig. 24E–H), the rib density increases from 9 to 11 ribs/cm in passing from the midshaft to the hook.

    Umbilicolateral tubercles are absent on the adapical end of the phragmocone, and usually appear on the adoral end, and continue onto the body chamber up to the aperture. They are perched on the umbilical shoulder, which constitutes one of the distinctive features of microconchs. The tubercles are small, radially elongate, and evenly spaced. The distance between consecutive tubercles at midshaft is 4.6 mm in AMNH 108314 (fig. 24E–H) and 4.2 mm in AMNH 72634 (fig. 24M–P). The number of umbilicolateral tubercles on the body chamber ranges from 5 to 8 in our measured sample, e.g., 5 in AMNH 108314 (fig. 24E–H) and 7 in AMNH 72634 (fig. 24M–P).

    Ventrolateral tubercles are usually present at the point of exposure. They are initially closely spaced but become more widely spaced toward the adoral end of the phragmocone. In AMNH 72634 (fig. 24M–P), the distance between consecutive tubercles is 4.1 mm at the adapical end of the phragmocone and 6.3 mm at the adoral end of the phragmocone. The tubercles are small and conical. The number of ventrolateral tubercles on the phragmocone ranges from 4 to 8 in our measured sample, e.g., 4 in AMNH 108314 (fig. 24E–H) and 7 in AMNH 72634 (fig. 24M–P). Two ribs loop between ventrolateral tubercles on opposite sides of the venter with as many as three ribs intercalating between them.

    Ventrolateral tubercles persist onto the body chamber and become more widely spaced toward the adoral end of the shaft. The distance between ventrolateral tubercles at midshaft is 8.2 mm in AMNH 108314 (fig. 24E–H) and 7.2 mm in AMNH 72634 (fig. 24M–P). The number of ventrolateral tubercles on the body chamber ranges from 7 to 10 in our measured sample. The total number of ventrolateral tubercles on the adult shell ranges from 12 to 19, e.g., a total of 12 tubercles in AMNH 108314 (fig. 24E–H) and 15 tubercles in AMNH 72634 (fig. 24M–P). They are clavate on the midshaft, with steeply sloping adapical sides and more gently sloping adoral sides. In larger specimens, as many as four ribs loop between ventrolateral tubercles on opposites sides of the venter, with up to five ribs intercalating between them. In smaller specimens, as many as three ribs loop between tubercles on opposite sides of the venter, with up to five ribs intercalating between them. Tubercles disappear on the adoral end of the shaft.

    Two specimens (AMNH 72589 and 74354) in our measured set exhibit a single row of lateral tubercles on the adapical end of the phragmocone (not figured). The tubercles are closely and evenly spaced and nearly the same size as the ventrolateral tubercles. However, the ventrolateral tubercles persist onto the body chamber whereas the lateral tubercles disappear on the adoral end of the phragmocone.

  • Occurrence: This species occurs in the upper part of the Baculites baculus Zone and lower part of the B. grandis Zone in the Pierre Shale in Montana, Colorado, and Wyoming. Nearly all the specimens that were collected with precise biostratigraphic information (down to zone) are from the lower part the B. grandis Zone.

  • Discussion: Among older species from the Western Interior of North America, small specimens of Hoploscaphites macer most closely resemble small specimens of H. brevis from the Baculites compressus–B. cuneatus zones. However, H. macer differs from H. brevis in its more tightly coiled shell, with more inflated flanks, its less flexuous ribs, and its smaller, more numerous, and more closely spaced ventrolateral tubercles. Among younger species from the Western Interior, H. macer most closely resembles H. criptonodosus and H. sargklofak. It differs from H. criptonodosus in its finer ribbing and, in general, the absence of lateral tubercles on the exposed phragmocone. However, as noted above, in some specimens of H. macer such as USNM 713623 from the B. grandis Zone, a few lateral tubercles appear on the adapical end of the exposed phragmocone. It differs from H. sargklofak in its more inflated shell, with more broadly rounded flanks, and its fewer and more widely spaced ventrolateral tubercles. However, in some specimens of H. macer, such as BHI 4346 (fig. 14) from the B. grandis Zone, the spacing of the ventrolateral tubercles begins to approach that of H. sargklofak.

    Outside the Western Interior, Hoploscaphites macer most closely resembles H. youngi Larson, 2016, from the upper Campanian Coon Creek Member of the Ripley Formation, McNairy County, Tennessee (Larson, 2016: fig. 11F–I), and the Nacatoch Sand, Red River County, Texas (Stephenson, 1941: pl. 90, figs. 7, 8). However, it differs from this species in its more inflated whorl section with more broadly rounded flanks. Outside North America, H. macer most closely resembles H. constrictus from northern Europe (see Kennedy, 1986: pl. 13, figs. 13, 16–24; pl. 14, figs. 138; pl. 15, figs. 131; text-figs. 9, 11; Machalski, 2005: figs. 57, 10, 12), which ranges from the base of the Maastrichtian to the Cretaceous-Paleogene boundary and possibly into the lower Paleocene (Machalski and Heinberg, 2005). However, H. macer differs from H. constrictus in having more numerous ventrolateral tubercles on the exposed phragmocone. In addition, the distance between ventrolateral tubercles on opposite sides of the venter at midshaft is greater in H. macer than in H. constrictus.

  • FIGURE 13.

    Size-frequency histogram of Hoploscaphites macer, n. sp., based on the samples in tables 1 and 2.

    f13_01.jpg

    Table 1

    Measurements of Hoploscaphites macer, n. sp., macroconchs

    See figure 12 for description of measurements. All measurements are in mm except for apertural angle. * = close to H. sargklofak; ** = close to H. criptonodosus; b = B. baculus Zone; g= B. grandis Zone; b/g = Baculites baculus or B. grandis Zone; ub= upper B. baculus Zone; lg = lower B. grandis Zone; ub/lg= upper B. baculus or lower B. grandis Zone; 1 = suture; 2 = scanned.

    t01a_01.gif

    Continued

    t01b_01.gif

    Table 2

    Measurements of Hoploscaphites macer, n. sp., microconchs

    See figure 12 for description of measurements. All measurements are in mm. b = B. baculus Zone; g= B. grandis Zone; b/g = Baculites baculus or B. grandis Zone; ub= upper B. baculus Zone; lg = lower B. grandis Zone; ub/lg= upper B. baculus or lower B. grandis Zone; 1 = suture.

    t02a_01.gif

    Continued

    t02b_01.gif

    FIGURE 14.

    Hoploscaphites macer, macroconch. A–D. BHI 4346, AMNH loc. 3278, Baculites grandis Zone, Pierre Shale, Weston County, Wyoming. A, Right lateral; B, apertural; C, ventral; D, left lateral. Arrow indicates the base of the body chamber. Specimens ×1.

    f14_01.jpg

    FIGURE 15.

    Hoploscaphites macer, macroconch. A–D. AMNH 74335, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. A, Right lateral; B, apertural; C, ventral; D, left lateral. Part of the phragmocone is missing and is filled in with clay. Arrow indicates the base of the body chamber. Specimens ×1.

    f15_01.jpg

    FIGURE 16.

    Hoploscaphites macer, macroconch. A–D. BHI 4306, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. A, Right lateral; B, apertural; C, ventral; D, left lateral. Arrow indicates the base of the body chamber. Specimens ×1.

    f16_01.jpg

    FIGURE 17.

    Hoploscaphites macer, macroconchs. A–C. USNM 713612, paratype, USGS loc. 5440, Baculites grandis Zone, Bearpaw Shale, Roosevelt County, Montana. A, Right lateral; B, apertural; C, ventral. D–F. USNM 713624, USGS Mesozoic loc. D2118, lower Baculites grandis Zone, Pierre Shale, Niobrara County, Wyoming. D, Right lateral; E, apertural; F, ventral. Arrows indicate the base of the body chamber. Specimens ×1.

    f17_01.jpg

    FIGURE 18.

    Hoploscaphites macer, macroconchs. A–C. AMNH 76388, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. A, Right lateral; B, apertural; C, ventral. D–F. BHI 4786, AMNH loc. 3921, Baculites baculus or B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. D, Right lateral; E, apertural; F, ventral. G–I. AMNH 74328, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. G, Right lateral; H, apertural; I, ventral. Arrows indicate the base of the body chamber. Specimens ×1.

    f18_01.jpg

    FIGURE 19.

    Hoploscaphites macer, macroconchs. A–D. AMNH 108487, AMNH loc. 3278, Baculites baculus or B. grandis Zone, Pierre Shale, Weston County, Wyoming. A, Right lateral; B, apertural; C, ventral; D, left lateral. E–H. AMNH 71839, holotype, AMNH loc. 3921, lower Baculites grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. E, Right lateral; F, apertural; G, ventral; H, left lateral. I–K. AMNH 71931, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. I, Right lateral; J, ventral, K, left lateral. Arrows indicate the base of the body chamber. Specimens ×1.

    f19_01.jpg

    FIGURE 20.

    Hoploscaphites macer, macroconchs. A. AMNH 74331, right lateral, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana (used for ontogenetic breakdown). B, C. DMNH EPI 19920, DMNH loc. 1405, Baculites baculus or B. grandis Zone, Pierre Shale, Jefferson County, Colorado. B, Left lateral; C, ventral. D–F. AMNH 113323, paratype, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. D, Right lateral; E, apertural; F, ventral. G–I. AMNH 113324, paratype, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. G, Right lateral; H, apertural; I, ventral. Arrows indicate the base of the body chamber. Specimens ×1.

    f20_01.jpg

    FIGURE 21.

    Hoploscaphites macer, macroconchs. A. DMNH EPI 19946, left lateral, finely ribbed specimen with a lethal injury at the aperture, DMNH loc. 1405, Baculites baculus or B. grandis Zone, Pierre Shale, Jefferson County, Colorado. B, C. DMNH EPI 22915, DMNH loc. 1405, Baculites baculus or B. grandis Zone, Pierre Shale, Jefferson County, Colorado. B, Right lateral; C, ventral. D–G. DMNH EPI 36444, incomplete specimen, DMNH loc. 5751, Baculites baculus or B. grandis Zone, Pierre Shale, Jefferson County, Colorado. D, Right lateral; E, apertural; F, ventral; G, left lateral. Arrows indicate the base of the body chamber. Specimens ×1.

    f21_01.jpg

    FIGURE 22.

    Ontogenetic breakdown of Hoploscaphites macer, macroconch, AMNH 74331, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. A–L. Six sizes through ontogeny in lateral and ventral views showing The change in ornamentation from early ontogeny (K, L) to maturity (A, B). Arrow indicates the base of the body chamber. Scale bar = 1 cm.

    f22_01.jpg

    FIGURE 23.

    Sutures. A. Hoploscaphites macer, macroconch, AMNH 71839, holotype, third suture from the last, AMNH loc. 3921, lower Baculites grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. B. Hoploscaphites macer, macroconch, USNM 713624, third suture from the last, USGS Mesozoic loc. D2118, lower Baculites grandis Zone, Pierre Shale, Niobrara County, Wyoming. C. Hoploscaphites macer, microconch, AMNH 76381, third suture from the last, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. D. Hoploscaphites criptonodosus (Riccardi, 1983), macroconch, AMNH 95766, third suture from the last, AMNH loc. 3278, Baculites baculus or B. grandis Zone, Pierre Shale, Weston County, Wyoming. E. Hoploscaphites criptonodosus (Riccardi, 1983), macroconch, AMNH 82725, third suture from the last, AMNH loc. 3268, Baculites baculus Zone, Pierre Shale, Weston County, Wyoming. F. Hoploscaphites sp., AMNH 76187, macroconch, last suture of a closely related, undescribed species, AMNH loc. 3921, lower Baculites baculus Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana.

    f23_01.jpg

    FIGURE 24.

    Hoploscaphites macer, microconchs. A-D. YPM 35657, YPM loc. A4745, Baculites baculus or B. grandis Zone, Pierre Shale, Niobrara County, Wyoming. A, Right lateral; B, apertural; C, ventral; D, left lateral. E–H. AMNH 108314, paratype, AMNH loc. 3244, lower B. grandis Zone, Pierre Shale, Dawson County, Montana. E, Right lateral; F, apertural; G, ventral; H, left lateral. I–L. AMNH 76383, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. I, Right lateral; J, apertural; K, ventral; L, left lateral. M–P. AMNH 72634, paratype, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. M, Right lateral; N, apertural; O, ventral; P, left lateral. Arrows indicate the base of the body chamber. Specimens ×1.

    f24_01.jpg

    Hoploscaphites criptonodosus (Riccardi, 1983)
    igures 8C, D, 9, 11A, B, 23D, E, 26–38

  • 1983. Jeletzkytes criptonodosus. Riccardi, p. 28, pl. 6, fig. 10; pl. 7, figs. 1, 2; pl. 8, figs. 7–9; text-figs. 25–27.

    1983. Jeletzkytes cf. criptonodosus. Riccardi, p. 30, pl. 11, figs. 111, 1521; text-figs. 28, 29b, 30, 31.

    non 1983. Jeletzkytes cf. criptonodosus. Riccardi, p. 30, pl. 11, figs. 1214; text-fig. 29a (= Hoploscaphites sargklofak).

    1994. Jeletzkyites (Karlwaageites) criptonodosus Riccardi. Cooper, p. 181.

    1995. Jeletzkytes criptonodosus Riccardi, 1983. Cobban and Kennedy, p. 31, figs. 6.4, 6.5, 22.5–22.12, 23.1–23.5.

    1997. Jeletzkytes criptonodosus Riccardi, 1983. Larson et al., p. 81, fig. on bottom; p. 82. top (= Riccardi, 1983, pl. 6, fig. 10, pl. 7, fig. 1).

    2000. Jeletzkytes criptonodosus Riccardi, 1983. Kennedy et al., p. 26, fig. 12A, B.

    2016. Jeletzkytes criptonodosus Riccardi, 1983. Klein, p. 138.

  • Emended Diagnosis: Macroconchs oval in lateral view; robust, with compressed subquadrate whorl section of shaft consisting of broadly rounded flanks and nearly flat venter; small umbilicus commonly with umbilical bulge; apertural angle averaging approximately 60°; ribbing coarse on the adapical end of the phragmocone, becoming finer on the body chamber; moderately closely spaced, medium sized ventrolateral tubercles; small umbilicolateral tubercles on phragmocone and body chamber; one or two rows of lateral tubercles on the outer flanks on the adapical end of the phragmocone; microconchs oval in lateral view; whorl section of shaft subquadrate with broadly rounded flanks converging toward ventrolateral shoulder; large umbilicus exposing earlier whorls; moderately closely spaced, medium sized ventrolateral tubercles; relatively prominent umbilicolateral tubercles on body chamber; one or two rows of lateral tubercles on the adapical end of the phragmocone; suture deeply incised, with a broad, asymmetrically bifid first lateral saddle and a narrow, symmetrically to asymmetrically bifid first lateral lobe (slightly modified from Riccardi, 1983).

  • Types: The holotype and paratype are GSC 67104 and 67105, respectively, illustrated in Riccardi (1983: pl. 6, fig. 10; pl. 7, figs. 1, 2; pl. 8, figs. 7–9). They are both from GSC loc. 10374 from the Baculites baculus Zone of the Belanger Member of the Bearpaw Shale, on the north side of Frenchman River, sec. 14, T. 6, R. 25, W3rd Mer., Saskatchewan, Canada.

    Material: The collection consists of approximately 90 specimens of which 61 comprise the measured set (tables 3, 4) representing 43 macroconchs and 18 microconchs. The specimens in our collection are from the upper part of the Baculites baculus and B. grandis zones of the Pierre Shale in Wyoming, Colorado, Montana, and possibly South Dakota, and the Bearpaw Shale in Montana.

    Macroconch Description: In the measured sample, LMAX averages 79.2 mm and ranges from 60.9 to 102.4 mm (table 3). The ratio of the size of the largest specimen to that of the smallest is 1.68. The specimens form a broad size distribution, with a primary peak at 65–70 mm and a secondary peak at 75–80 mm (fig. 26). Adults are stout with an oval outline in side view. LMAX/HSaverages 2.09 and ranges from 1.86 to 2.32 (2.04 in the holotype). USNM 463215 (fig. 33) is an example of a specimen with an oval outline (LMAX/HS= 2.27) and AMNH 108445 (fig. 30) is an example of a specimen with a more rounded outline (LMAX/HS= 1.98).

    The umbilicus is small and deep. The umbilical diameter averages 5.0 mm and ranges from 3.7 to 7.6 mm. UD/LMAX averages 0.06 and ranges from 0.05 to 0.10. The umbilicus is unusually large (7.6 mm) in AMNH 108456 (fig. 31). In lateral view, the umbilical shoulder is straight and usually exhibits a pronounced umbilical bulge. Most specimens are tightly coiled with little or no gap between the phragmocone and hook. LMAX/HP2averages 2.83 and ranges from 2.59 to 3.04 (2.79 in the holotype). AMNH 95771 (fig. 32A–C) is an example of a tightly coiled specimen (LMAX/HP2= 2.76) and USNM 463215 (fig. 33) is an example of a more loosely coiled specimen (LMAX/HP2= 2.91). The exposed phragmocone occupies approximately one-half whorl and generally terminates just below the line of maximum length. The body chamber consists of a short shaft and recurved hook totaling slightly more than onehalf whorl. The apertural lip is flexuous with a dorsal projection (fig. 8C, D). The apertural angle averages 58.8° and ranges from 26.0 to 78.0° (47.5° in the holotype). AMNH 108456 (fig. 31) exhibits a very low apertural angle (26.0°) and is associated with a very large umbilicus (7.6 mm diameter).

    The whorl section of the phragmocone near the point of exposure is depressed subquadrate with maximum whorl width at one-third whorl height. WP1/HP1averages 1.08 and ranges from 0.91 to 1.23 (1.06 in the holotype). The umbilical wall is steep and subvertical and the umbilical shoulder is sharply rounded. The flanks are broadly rounded and converge toward the ventrolateral shoulder starting at two-thirds whorl height. The ventrolateral shoulder is sharply rounded and the venter is broadly rounded. The whorl section of the phragmocone at the line of maximum length is slightly more compressed than that at the point of exposure, reflecting a steep increase in whorl height. WP2/HP2averages 0.96 and ranges from 0.84 to 1.11 (0.94 in the holotype). The flanks are very broadly rounded and the venter is nearly flat.

    The whorl width increases as the shell passes from the phragmocone into the body chamber and reaches its maximum value on the adoral part of the shaft but does not produce a conspicuous bulge in this area. Whorl height increases much more markedly during this transition and reaches its maximum value at midshaft. Thereafter, it diminishes to the point of recurvature and remains nearly the same up to the aperture. These changes in whorl width and height result in a slightly more compressed whorl section at midshaft than at the adoral end of the phragmocone. WS/HSaverages 0.90 and ranges from 0.74 to 1.07 (0.88 in the holotype). The whorl section is subquadrate with maximum whorl width at one-quarter whorl height. The umbilical wall is steep and subvertical and the umbilical shoulder is sharply rounded. The whorls are very high and broadly rounded, and gently converge toward the venter. The ventrolateral shoulder is sharply rounded and the venter is broadly rounded. VS/ HSaverages 0.43 and ranges from 0.31 to 0.73 (0.44 in the holotype). In USNM 463215 (fig. 33), the value of VS/HSis very high (0.73) because the ventrolateral tubercles occur slightly below the ventrolateral shoulder, so that the distance between ventrolateral tubercles on opposite sides of the venter is unusually high.

    The whorl section at the point of recurvature is less compressed than that at midshaft, mainly due to a decrease in whorl height. WH/ HHaverages 1.14 and ranges from 0.93 to 1.33 (1.16 in the holotype). The whorl section at the point of recurvature is subovoid with maximum whorl width at one-third whorl height. The umbilical wall is slightly concave and the umbilical shoulder is sharply rounded. The flanks are broadly rounded and gently converge toward the venter.

    At the adapical end of the exposed phragmocone, ribs emerge at the umbilical seam. They are strong and widely spaced on the flanks and bend slightly forward at two-thirds whorl height. They attain their maximum strength at one-third whorl height and develop into small umbilicolateral tubercles at this point. Ribs are equally spaced on the venter, which they cross with a slight adoral projection. In the holotype, the rib density on the adapical end of the phragmocone is 4.5 ribs/cm. The rib density is nearly the same on the adoral end of the phragmocone (e.g., 5 ribs/cm in the holotype).

    On the body chamber, ribs arise at the umbilical seam and are rursiradiate on the umbilical wall and shoulder. They are long, broad, straight, and rectiradiate at midshaft, becoming more prorsiradiate toward the adoral end of the shaft. Umbilicolateral tubercles are usually present on the body chamber, but given the large size and robust cross section of the shell, they are surprisingly small. In the holotype, the distance between consecutive umbilicolateral tubercles at midshaft is 4.9 mm. Branching and intercalation occur at two-thirds whorl height, with the result that the outer flanks are more densely covered with ribs than the inner flanks. Ribs are usually not preserved on the venter of the shaft, but in AMNH 108313 (fig. 28) in which they are preserved, the rib density is 6 ribs/cm. Ribs are narrow and closely spaced on the venter of the hook, which they cross with a strong adoral projection. In AMNH 108313, the rib density on the hook is 9 ribs/cm (fig. 28).

    Ventrolateral tubercles appear early in ontogeny at a diameter of approximately 6 mm and continue onto the exposed phragmocone (fig. 36). They are closely and evenly spaced, occurring on every rib or every other rib. In the holotype, the distance between consecutive tubercles is 4.3 mm on the adapical end and 6.3 mm on the adoral end of the exposed phragmocone, yielding a total of 17 tubercles. The tubercles are conical in shape and change from slightly radially elongate at the point of exposure to slightly clavate on the adoral end of the phragmocone.

    Ventrolateral tubercles are closely and evenly spaced on the midshaft, becoming slightly more widely spaced on the adoral end of the shaft, and slightly more closely spaced again near the aperture. In the holotype, the distance between consecutive ventrolateral tubercles is 9.6 mm on the midshaft, 12.7 mm on the adoral end of the shaft, and 7.4 mm on the hook, yielding a total of 15 tubercles on the body chamber (32 tubercles on the whole exposed shell). In AMNH 108313 (fig. 28) in which the ribs are well preserved on the venter at midshaft, two or three ribs loop between ventrolateral tubercles on opposite sides of the venter with one or two ribs intercalating between them. The tubercles are slightly clavate on the adoral end of the shaft where they attain their maximum height.

    A single row of outer lateral tubercles appears early in ontogeny at approximately 10 mm diameter (fig. 36). It is joined by another row of inner lateral tubercles, both of which continue onto the exposed phragmocone for an additional oneeighth to one-half whorl. The tubercles are closely spaced and occur on every rib or every other rib. The tubercles in the outermost row are only slightly smaller than those in the ventrolateral row.

    The suture is deeply incised, with a broad, asymmetrically bifid first lateral saddle (E/L) and a narrow, symmetrically to asymmetrically bifid first lateral lobe (L) (fig. 23D, E).

  • Microconch Description: Microconchs are smaller than macroconchs. LMAX averages 51.0 mm and ranges from 43.2 to 68.2 mm (table 4). The size distribution is unimodal with a broad peak at 45–55 mm (fig. 26). The ratio of the average size of microconchs to that of macroconchs is 0.64. This is lower than that in most species of Hoploscaphites and may reflect the fact that the sample of microconchs is biased because of its small size.

    Microconchs are oval in lateral view with a large gap between the phragmocone and hook. LMAX/HP2averages 3.10 and ranges from 2.81 to 3.39. The average value of LMAX/HP2in microconchs is significantly higher than that in macroconchs (2.83). The phragmocone occupies slightly more than one-half whorl and terminates just below the line of maximum length. The umbilical diameter is relatively larger in microconchs than in macroconchs. UD/LMAX averages 0.10 in microconchs whereas it averages 0.06 in macroconchs. In addition, the umbilical seam in microconchs is concave in side view. The body chamber occupies slightly more than onehalf whorl and terminates in a constriction and accompanying varix.

    The whorl section at the adapical end of the phragmocone is robust and subquadrate with maximum whorl width at one-quarter whorl height. WP1/HP1averages 0.96 and ranges from 0.82 to 1.09. The umbilical wall is nearly vertical and the umbilical shoulder is sharply rounded. The flanks are broadly rounded and gently converge toward the ventrolateral shoulder. In costal cross section, the flanks flatten out between the inner lateral and ventrolateral tubercles. The venter is broadly rounded. The whorl section at the adoral end of the phragmocone is more quadrate than that at the adapical end of the phragmocone, with flatter flanks and more sharply rounded ventrolateral shoulder. However, the average value of WP2/HP2(0.95) is nearly the same as that of WP1/HP1(0.96).

    In passing from the phragmocone to the body chamber, both whorl width and height gradually increase, but the increase in whorl height is much less dramatic than in macroconchs. Whorl height attains its maximum value at midshaft and remains nearly the same thereafter, but whorl width attains its maximum value on the hook and decreases slightly thereafter. The whorl section at midshaft is compressed subquadrate, with maximum width at one-quarter whorl height. WS/HSaverages 0.92 and ranges from 0.77 to 1.01. The umbilical wall is broad and slopes gently outward culminating in the umbilicolateral tubercles. The flanks are nearly flat and converge toward the ventrolateral shoulder. The ventrolateral shoulder is abruptly rounded and the venter is nearly flat. The whorl section at the point of recurvature is compressed subovate. WH/HHaverages 1.01 and ranges from 0.85 to 1.10. The flanks are broadly rounded with maximum width at one-quarter whorl height. The venter is broadly rounded, which is accentuated in specimens without ventrolateral tubercles.

    On the adapical end of the phragmocone, ribs emerge at the umbilical seam and strengthen on the flanks. They are strong and widely spaced. In more finely ribbed specimens such as AMNH 74357 (fig. 38B–D), they bend slightly backward on the inner flanks, slightly forward on the midflanks, and slightly backward again on the outer flanks. However, in more coarsely ornamented specimens such as USNM 713635 (fig. 38E–H), the ribs are nearly straight and bend only slightly backward on the outer flanks. Ribs are uniformly strong on the venter, which they cross with a slight adoral projection. They are relatively closely spaced with an average of 7 ribs/cm. They are equally coarse on the adoral end of the phragmocone, with branching and interca lation occurring at one-third and two-thirds whorl height.

    Ribs are strong and prorsiradiate on the shaft and cross the flanks with a broad adoral convexity. Branching and intercalation occur at onethird whorl height (at and between the umbilicolateral tubercles) and, again, at twothirds whorl height. Ribs are generally not preserved on the venter. However, in USNM 713635 (fig. 38E–H) in which they are preserved, they are closely spaced (9 ribs/cm), with a strong adoral projection. Ribs are prorsiradiate on the hook, with branching and intercalation occurring at one-quarter whorl height (at and between the umbilicolateral tubercles) and at one-half whorl height. The outer flanks and venter are covered with fine, closely spaced ribs. The rib density ranges from 8 to 10 ribs/cm in our measured sample.

    Umbilicolateral tubercles appear on the adoral end of the phragmocone and continue uninterruptedly to the aperture. They become slightly more widely spaced adorally, attaining their maximum spacing on the adoral end of the shaft, e.g., 6 mm in USNM 713635 (fig. 38E–H), 7 mm in AMNH 74357 (fig. 38B–D), and 8 mm in USNM 713626 (fig. 38I–K). The tubercles are radially elongate on the adoral end of the phragmocone, conical on the midshaft, and clavate on the adoral end of the shaft and hook.

    Ventrolateral tubercles are present at the point of exposure. They are initially closely and evenly spaced, becoming slightly more widely spaced on the adoral end of the phragmocone. For example, in USNM 713635 (fig. 38E–H), the distance between consecutive tubercles is 2.5 mm and 4.5 mm on the adapical and adoral ends of the phragmocone, respectively. In contrast, in AMNH 74346 (fig. 37E–H), the tubercles are uniformly spaced at distances of 3–4 mm, except for two gaps of 5–6 mm each on the adapical end of the phragmocone. One or two ribs loop between tubercles on opposite sides of the venter, with up to three ribs intercalating between them. The number of ventrolateral tubercles on the phragmocone ranges from 9 to 13 in our measured sample.

    Ventrolateral tubercles continue onto the body chamber and gradually become more widely spaced until the adoral end of the shaft, after which they disappear. The distance between consecutive tubercles on the adoral end of the shaft is 7.5 mm in smaller specimens such as AMNH 74357 (fig. 38B–D) and 11.5 mm in larger specimens such as USNM 713626 (fig. 38I–K). The number of ventrolateral tubercles on the body chamber ranges from 6 to 10 in our measured sample, so that the total number of ventrolateral tubercles on the adult shell ranges from 17 to 24. In specimens in which the ribs are well preserved on the venter of the shaft such as USNM 713635 (fig. 38E–H), as many as four ribs loop between ventrolateral tubercles on opposite sides of the venter, with two or three nontuberculate ribs intercalating between them. The tubercles become progressively larger and more clavate toward the adoral end of the shaft. They are asymmetric in profile. with steeply sloping adapical faces and more gently sloping adoral faces.

    One or two lateral rows of tubercles are usually present at the point of exposure. As a result, most of the surface of the shell in this area is covered with tubercles (umbilicolateral, lateral, and ventrolateral tubercles). The lateral tubercles persist to the middle of the phragmocone, but if two rows are present, the inner lateral row usually dies out first. The lateral and ventrolateral tubercles occur on the same rib, with the height of the rib dipping between tubercles. The lateral tubercles are more or less evenly spaced; for example, in USNM 713635 (fig. 38E–H), the distance between consecutive outer lateral tubercles is 5 mm.

  • Occurrence: This species occurs in the upper part of the Baculites baculus Zone and B. grandis Zone in the Pierre Shale of Montana, Colorado, and Wyoming and in the Bearpaw Shale of Montana. It is also possible that it occurs in the Pierre Shale of South Dakota but our only specimen from this area (BHI 4345) is from a gravel pit, and its provenance is unknown (fig. 37M, N). Riccardi (1983) also recorded it from the B. baculus Zone in the Bearpaw Shale of Saskatchewan, Canada. On the U.S. Gulf Coastal Plain, it occurs in the Coon Creek Member of the Ripley Formation of Mississippi, in the Prairie Bluff Chalk of Alabama (Cobban and Kennedy, 1995), and possibly in the Nacatoch Sand of Arkansas. On the U.S. Atlantic Coastal Plain, it occurs in the Navesink Formation of New Jersey (Kennedy et al., 2000).

  • Discussion: Most of the microconchs in our measured sample are small. The largest microconch is USNM 713626 (fig. 38I–K), which presumably corresponds to one of the larger macroconchs in our sample, for example, AMNH 108445 (fig. 30). All the microconchs illustrated by Riccardi (1983: pl. 11, figs. 1–21) are equally small and, in this context, it is worth noting that the illustrations of some of his specimens are magnified and, in reality, the specimens are much smaller than they appear (Riccardi, 1983: pl. 11, figs. 711). The absence of larger microconchs in both collections may be a preservational bias. We also illustrate a pathologic specimen (AMNH 108325), which is very openly coiled even for a microconch (fig. 37O, P).

    The specimens illustrated by Riccardi (1983) are from the Baculites baculus Zone, but most of the specimens that we describe are from the B. grandis Zone. We also illustrate two specimens of this species from the U.S. Gulf Coastal Plain. FM 10689 (fig. 35A–C) is a macroconch erroneously labelled as coming from the Pierre Shale, Arkadelphia, Clark County, Arkansas, but probably from the Nacatoch Sand. MMNS-IP 7881.3 (fig. 35D–F) and 8825.1 (fig. 38A) are a macroconch and microconch, respectively, from the Coon Creek Member of the Ripley Formation, Union County, Mississippi. Cobban and Kennedy (1995: fig. 22.5–12) illustrated fragments of similar material from the Prairie Bluff Chalk, Wilcox County, Alabama.

    Among older species in the Western Interior, Hoploscaphites criptonodosus is most closely similar to large specimens of H. brevis from the Baculites compressusB. cuneatus Zones. It differs, however, in its more closely coiled shell and, notably, multituberculate phragmocone, the character from which its name is derived (Riccardi, 1983). As noted above, H. criptonodosus is also similar to H. sargklofak (fig. 10), which occurs in the same biostratigraphic zone. Indeed, lateral tubercles appear on the adapical end of the exposed phragmocone in both species. However, H. criptonodosus is larger and more coarsely ornamented than H. sargklofak, although it is possible that the two forms represent the coarsely and finely ornamented end members of a single species.

  • FIGURE 25.

    Hoploscaphites macer, microconchs. A–D. DMNH EPI 22907, DMNH loc. 1405, Baculites baculus or B. grandis Zone, Pierre Shale, Jefferson County, Colorado. A, Right lateral; B, apertural; C, ventral; D, left lateral. E–G. AMNH 72624, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. E, Right lateral; F, apertural; G, ventral. H–J. USNM 713625, ?AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. H, Right lateral; I, apertural; J, ventral. Arrows indicate the base of the body chamber. Specimens ×1.

    f25_01.jpg

    TABLE 3

    Hoploscaphites criptonodosus (Riccardi, 1983), macroconchs

    See figure 12 for description of measurements. All measurements are in mm, except for apertural angle. * = close to H. macer; b = B. baculus Zone; g= B. grandis Zone; b/g = Baculites baculus or B. grandis Zone; ub= upper B. baculus Zone; lg = lower B. grandis Zone; ug = upper B. grandis Zone; ub/lg= upper B. baculus or lower B. grandis Zone; C = illustrated in Cobban and Kennedy (1995); 1 = suture; 2 = scanned; 3 = locality details appear in the appendix.

    t03a_01.gif

    Continued

    t03b_01.gif

    Table 4

    Hoploscaphites criptonodosus (Riccardi, 1983), microconchs

    See Figure 12 for description of measurements. All measurements are in mm. b = B. baculus Zone; g= B. grandis Zone; b/g = Baculites baculus or B. grandis Zone; ub= upper B. baculus Zone; lg = lower B. grandis Zone; ub/lg= upper B. baculus or lower B. grandis Zone; 1 = found in gravel pit.

    t04_01.gif

    FIGURE 26.

    Size frequency histogram of Hoploscaphites criptonodosus (Riccardi, 1983) based on the sample in tables 3 and 4.

    f26_01.jpg

    FIGURE 27.

    Hoploscaphites criptonodosus (Riccardi, 1983), macroconch. A–D. AMNH 95773, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, Montana. A, Right lateral; B, apertural; C, ventral; D, left lateral. Arrow indicates the base of the body chamber. Specimens ×1.

    f27_01.jpg

    FIGURE 28.

    Hoploscaphites criptonodosus (Riccardi, 1983), macroconch. A–D. AMNH 108313, AMNH loc. 3269, Baculites grandis Zone, Pierre Shale, Weston County, Wyoming. A, Right lateral; B, apertural; C, ventral; D, left lateral. Arrow indicates the base of the body chamber. Specimens ×1.

    f28_01.jpg

    FIGURE 29.

    Hoploscaphites criptonodosus (Riccardi, 1983), macroconch. A-D. AMNH 108312, AMNH loc. 3265, Baculites baculusB. grandis zones, Pierre Shale, Weston County, Wyoming. A, Right lateral; B, apertural; C, ventral; D, left lateral. Arrow indicates the base of the body chamber. Specimens ×1.

    f29_01.jpg

    FIGURE 30.

    Hoploscaphites criptonodosus (Riccardi, 1983), macroconch. A–D. AMNH 108445, AMNH loc. 3730, Baculites baculus Zone, Pierre Shale, Niobrara County, Wyoming. A, Right lateral; B, apertural; C, ventral; D, left lateral. Arrow indicates the base of the body chamber. Specimens ×1.

    f30_01.jpg

    FIGURE 31.

    Hoploscaphites criptonodosus (Riccardi, 1983), macroconch. A–D. AMNH 108456, AMNH loc. 3269, Baculites grandis Zone, Pierre Shale, Niobrara County, Wyoming. A, Right lateral; B, apertural; C, ventral; D, left lateral. Arrow indicates the base of the body chamber. Specimens ×1.

    f31_01.jpg

    FIGURE 32.

    Hoploscaphites criptonodosus (Riccardi, 1983), macroconchs. A–C. AMNH 95771, AMNH loc. 3278, Baculites baculusB. grandis zones, Pierre Shale, Weston County, Wyoming. A, Right lateral; B, apertural; C, ventral. D–F. BHI 4300, AMNH loc. 3278, Baculites grandis Zone, Pierre Shale, Weston County, Wyoming. D, Right lateral; E, apertural; F, ventral. Arrows indicate the base of the body chamber. Specimens ×1.

    f32_01.jpg

    FIGURE 33.

    Hoploscaphites criptonodosus (Riccardi, 1983), macroconch. A–D. USNM 463215, USGS loc. 12700, Baculites grandis Zone, Pierre Shale, Campbell County, Wyoming. A, Right lateral; B, apertural; C, ventral; D, left lateral. Arrow indicates the base of the body chamber. Specimens ×1.

    f33_01.jpg

    FIGURE 34.

    Hoploscaphites criptonodosus (Riccardi, 1983), macroconch. A–D. USNM 713617, USGS loc. 12757, Baculites grandis Zone, Pierre Shale, Weston County, Wyoming. A, Right lateral; B, apertural; C, ventral, D, left lateral. Arrow indicates the base of the body chamber. Specimens ×1.

    f34_01.jpg

    FIGURE 35.

    Hoploscaphites criptonodosus (Riccardi, 1983), macroconchs. A–C. FM 10689, erroneously labeled Pierre Shale, but probably Nacatoch Sand, Clark County, Arkansas. A, Apertural; B, ventral; C, left lateral. D–F. MSNS-IP 7881.3, ?Baculites grandis Zone, Coon Creek Member of the Ripley Formation, Union County, Mississippi. D, Apertural; E, ventral; F, left lateral. Arrows indicate the base of the body chamber. Specimens ×1.

    f35_01.jpg

    FIGURE 36.

    Ontogenetic breakdown of Hoploscaphites criptonodosus (Riccardi, 1983), macroconch, AMNH 94607, AMNH loc. 3729, Baculites grandis Zone, Pierre Shale, Niobrara County, Wyoming. A–N. Seven sizes through ontogeny in lateral and ventral views showing the change in ornamentation from the early whorls (M, N) to the adult phragmocone (A, B). Scale bar = 1 cm.

    f36_01.jpg

    FIGURE 37.

    Hoploscaphites criptonodosus (Riccardi, 1983), microconchs. A–D. AMNH 108316, AMNH loc. 3278, Baculites baculus or B. grandis Zone, Pierre Shale, Weston County, Wyoming. A, Right lateral; B, apertural; C, ventral; D, left lateral. E–H. AMNH 74346, AMNH loc. 3921, B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. E, Right lateral; F, apertural; G, ventral; H, left lateral. I–L. AMNH 74355, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. I, Right lateral; J, apertural; K, ventral; L, left lateral. M, N. BHI 4345, Baculites grandis Zone, Pierre Shale, Fall River County, South Dakota (found in gravel pit). M, Right lateral; N, apertural. O, P. AMNH 108325, pathologic specimen with unusually openly coiled whorls, Baculites grandis Zone, Pierre Shale, Weston County, Wyoming. Gift of Jordan K. Sawdo, Northglen, Colorado, O, Right lateral; P, apertural. Arrows indicate the base of the body chamber. Specimens ×1.

    f37_01.jpg

    FIGURE 38.

    Hoploscaphites criptonodosus (Riccardi, 1983), microconchs. A. MSNS-IP 8825.1, right lateral, ?Baculites grandis Zone, Coon Creek Member of the Ripley Formation, Union County, Mississippi. B–D. AMNH 74357, AMNH loc. 3921, upper Baculites baculus or lower B. grandis Zone, Pierre Shale, Cedar Creek Anticline, Montana. B, apertural; C, ventral; D, left lateral. E–H. USNM 713635, USGS Mesozoic loc. D2118, lower Baculites grandis Zone, Pierre Shale, Niobrara County, Wyoming. E, Right lateral; F, apertural; G, ventral; H, left lateral. I–K. USNM 713626, USGS Mesozoic loc. D12208, ?B. baculus Zone, Bearpaw Shale, Garfield County, Montana. I, Apertural; J, ventral; K, left lateral. Arrows indicate the base of the body chamber. Specimens ×1.

    f38_01.jpg

    ACKNOWLEDGMENTS

    At the American Museum of Natural History, we thank Bushra Hussaini, Mary Conway, Kathleen Sarg, and Marion Savas for accessioning material and assigning AMNH numbers, Mariah Slovacek for collecting fossils in the field and preparing specimens, Carolyn Merril for surfacescanning several specimens, William Harcourt- Smith for interpreting these scans, Mary Knight for editing the manuscript for publication, and Stephen Thurston for photographing specimens and preparing figures. We thank the landowners Donley and Nancy Darnell and Bobbie Blackenship for permission to collect on their property and Barbara A. Beasley for arranging permits to collect on the Buffalo Gap National Grassland, South Dakota. Many students, colleagues, and family members have helped us collect in the field and interpret the results, and we wish to express our thanks to Jamie Brezina, Barry and Aimee Brown, J. Kirk Cochran, Matthew P. Garb, Kate F. Grier, Isabella Kruta, Ekaterina Larina, Luke Larson, Kimberly C. Meehan, Corinne Myers, Jack Petersen, Kristin Polizzotto, Anastasia Rashkova, Isabelle Rouget, Remy Rovelli, Al Rowe, Joshua Slattery, Kazushige Tanabe, and James Witts. We thank K.C. McKinney for facilitating use of the USGS collections and for hunting down locality data. We thank Susan H. Butts and Jessica Utrup (YPM), George Phillips (MMNS), Kristen MacKenzie (DMNH), and Kathy Hollis (USNM) for arranging loans of specimens from their institutions. An earlier version of this manuscript was reviewed by Margaret (Peg) M. Yacobucci (Bowling Green State University) and Royal H. Mapes (Ohio University), both of whom made very helpful suggestions that improved the quality of the manuscript. This research was supported by the N.D. Newell Fund (AMNH) and personal funds of J.C. and J.W. Grier, T. Linn, and N.L. Larson.

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    Appendices

    APPENDIX

    List of Localities

    Localities are from the American Museum of Natural History (AMNH), the Denver Museum of Nature and Science (DMNH), the Geological Survey of Canada (GSC), the U.S. Geological Survey (USGS), and the Yale Peabody Museum (YPM). Several localities specify a range of biozones, but some specimens from these localities were collected with more precise information (within a single biozone or part thereof). The biostratigraphic information is listed in a column next to the specimens in tables 14. The names of collectors and dates of collection are indicated at the end of each entry, where known. In the USGS numbers, the prefix D refers to Denver locality numbers and the others refer to Washington, D.C., locality numbers.

    AMNH Localities

    • 1. 3244. Baculites baculusB. grandis zones, Pierre Shale, secs. 2, 34, and 35 T. 14 N., R. 55 E. and sec. 1, T. 13 N., R. 55 E., approximately 10 km south of Glendive, Dawson County, Montana.

    • 2. 3264. Upper Baculites baculus–lower B. grandis zones, Pierre Shale, W¼ sec. 15, T. 42 N., R. 62 W., west of Newcastle, Weston County, Wyoming. July 8, 1998.

    • 3. 3265. Baculites baculusB. grandis zones, Pierre Shale, SE¼ sec. 15, T. 42 N., R. 62 W., west of Newcastle, Weston County, Wyoming.

    • 4. 3268. Baculites baculusB. grandis zones, Pierre Shale, S½ sec.19, T. 43N., R. 62W., west of Newcastle, Weston County, Wyoming.

    • 5. 3269. Baculites baculusB. grandis zones, Pierre Shale, SE¼ sec. 30, SW¼ sec. 29, NE. sec. 31 and NW¼ sec. 32, T. 43 N., R. 62 W., west of Newcastle, Weston County, Wyoming.

    • 6. 3278. Baculites baculusB. grandis zones, Pierre Shale, near Newcastle, Weston County, Wyoming.

    • 7. 3487. Baculites grandis Zone, upper part of Pierre Shale, 43° 35′ 36″ N, -104° 16′ 42″ W, Weston County, Wyoming.

    • 8. 3727 (= G71188). Baculites grandisB. clinolobatus zones, mostly in and below 8 ft (2.4 m) thick bentonite noted by Gill and Cobban (1966), upper unnamed shale member, Pierre Shale, SW¼ to NW¼NE¼NE¼ sec. 14, T. 38 N., R. 62 W., in an area trending northeast across Brewster Draw, 2.1–2.5 mi (3.4–4.0 km) north-northeast of Red Bird, Niobrara County, Wyoming. N. H. Landman and K. M. Waage, July11, 1988.

    • 9. 3728 (= G71288). Baculites grandisB. clinolobatus zones, mostly in and below 8 ft (2.4 m) thick bentonite noted by Gill and Cobban (1966), upper unnamed shale member, Pierre Shale, SW¼ to NW¼NE¼NE¼ sec. 14, T. 38 N., R. 62 W., in an area trending northeast across Brewster Draw, 2.1–2.5 mi (3.4–4.0 km) north-northeast of Red Bird, Niobrara County, Wyoming. N. H. Landman and K. M. Waage, July 12, 1988.

    • 10. 3730 (= G71488). Baculites baculusB. grandis zones, mostly in and below 8 ft (2.4 m) thick bentonite noted by Gill and Cobban (1966), upper unnamed shale member, Pierre Shale, SW¼ to NW¼NE¼NE¼ sec. 14, T. 38 N., R. 62 W., in an area trending northeast across Brewster Draw, 2.1–2.5 mi (3.4–4.0 km) north-northeast of Red Bird, Niobrara County, Wyoming. N. H. Landman and K. M. Waage, July 14, 1988.

    • 11. 3732 (= G71688). Baculites baculusB. clinolobatus zones, mostly in and below 8 ft (2.4 m) thick bentonite noted by Gill and Cobban (1966), upper unnamed shale member, Pierre Shale, SW¼ to NW¼NE¼NE¼ sec. 14, T. 38 N., R. 62 W., in an area trending northeast across Brewster Draw, 2.1–2.5 mi (3.4–4.0 km) north-northeast of Red Bird, Niobrara County, Wyoming. N. H. Landman, July 16, 1988.

    • 12. 3921. Baculites eliasiB. grandis zones, Pierre Shale, Cedar Creek Anticline, Wibaux, Dawson, Fallon, and Prairie counties, Montana.

    Denver Museum of Nature and Science Localities

    • 13. 1405. Baculites baculusB. grandis zones, Pierre Shale, Western Aggregate Pit, near Golden, Jefferson County, Colorado. W. D. Bateman, 1998 (approximately the same site as below).

    • 14. 5751. Baculites baculusB. grandis zones, Pierre Shale, TXI Clay Quarry, near Golden, Jefferson County, Colorado. W. D. Bateman, 1995 (approximately the same site as above).

    GSC Localities

    • 15. 10374. Baculites baculus Zone, Bearpaw Shale, north side of Frenchman River, just west of road from Caton's Ranch to Robsart, sec. 14, T. 6, R. 25, W 3rd Mer., Saskatchewan. G.M Furnival, 1940.

    USGS Localities

    • 16. 5440. Bearpaw Shale, near Poplar, Roosevelt County, Montana.

    • 17. 6528. Baculites grandis Zone, Pierre Shale, 3 mi (4.8 km) southeast of Moorcroft, Crook County, Wyoming. T. W. Stanton, 1910.

    • 18. 10189. Upper part of Pierre Shale, SW¼ sec. 32, T. 36 N., R. 63 W., Niobrara County, Wyoming.

    • 19. 10764. Bearpaw Shale, 200 ft (71 m) below top, sec. 30, T. 21 N., R. 34 E., drainage of Seven Blackfoot Creek, breaks of Missouri River, Garfield County, Montana. Dobbin, Thom, and Stanton, 1921.

    • 20. 12700. Baculites grandis Zone, Pierre Shale, NE¼ T. 56 N., R. 69 W., Campbell County, Wyoming.

    • 21. 12757. Upper 100 ft (30.5 m) of Pierre Shale, 43.8540882° N., -104.4027328° W., 10 mi (16 km) west of Newcastle, Weston County, Wyoming. C.E. Dobbin and J. B. Reeside, 1924.

    • 22. 23628. Bearpaw Shale, SW¼SW¼ sec. 6, T. 27 N., R. 52 E., Roosevelt County, Montana.

    • 23. 24312. Bearpaw Shale, 38 ft (11.6 m) below top, E¼NW¼ sec. 2, T. 26 N., R. 50 E., 5 mi (8 km) south-southwest of Poplar, on west side of Redwater Creek Valley, Roosevelt County, Montana. W.A. Cobban, 1951.

    • 24. D771. Baculites grandis Zone, Pierre Shale, NE¼NE¼sec. 9, T. 3 S., R. 70 W., north of Golden, Jefferson County, Colorado.

    • 25. D1018. Baculites baculus Zone, Pierre Shale, brownish calcareous concretions about 412–422 ft (125.6–128.6 m) below top, SE . NW . sec. 24, T. 39 N., R. 62 W., south side of U.S. Highway 85, 2.1 mi (3.4 km) southwest of bridge over Mule Creek, Niobrara County, Wyoming. W.A. Cobban, 1956.

    • 26. D1033. Baculites grandis Zone, Pierre Shale, brown and gray calcareous concretions 364–394 ft (110.9–120.1 m) below top, NW¼ sec. 25, T. 39 N., R. 62 W., about 1 mi (1.6 km) southeast of U. S. Highway 85, Niobrara County, Wyoming. W.A. Cobban, September 29, 1956.

    • 27. D1047. Baculites baculus Zone, Pierre Shale, gray calcareous concretions 77–87 ft (23.5–26.5 m) below top, E¼ E¼ sec. 27 T. 14 N., R. 55 E., approximately 10 mi (16.1 km) south of Glendive, Dawson County, Montana.

    • 28. D1984. Baculites baculus Zone, Pierre Shale, 150 ft (45.7 m) below top of uppermost bentonitic unit, SW¼SE¼SE¼ SW¼ sec. 14, T. 38 N., R. 62 W., Niobrara County, Wyoming. J.R. Gill, W.J. Mapel, C.S. Robinson, and H. A. Tourtelot, 1958.

    • 29. D1985. Baculites grandis Zone, Pierre Shale, 110 ft (33.5 m) below top of uppermost bentonitic unit, NW¼SE¼ sec. 14, T. 38 N., R. 62 W., Niobrara County, Wyoming. J.R. Gill, W.J. Mapel, C.S. Robinson, H. A. Tourtelot, and W.A. Cobban, 1958.

    • 30. D1986. Upper part of Baculites grandis Zone, upper unnamed shale member, Pierre Shale, NW¼SE¼ sec. 14, T. 38 N., R. 62 W., Niobrara County, Wyoming.

    • 31. D2118. Lower part of Baculites grandis Zone, brown limestone concretions, upper unnamed shale member, Pierre Shale, NW¼SE¼ sec. 14, T. 38 N., R. 62 W., Niobrara County,Wyoming.

    • 32. D12208. Bearpaw Shale, NW¼ sec. 32, T. 24 N., R. 42 E., south side of peninsula on Big Dry Creek arm of Ft. Peck Reservoir, Garfield County, Montana. R. J. Sutton, 1971.

    • 33. D14195. Base of Fox Hills Formation, NE¼ sec. 11, T.12 N., R. 56 E., Dawson County, Montana.

    YPM Localities

    • 34. A4745. Baculites baculusB. grandis zones, upper part of Pierre Shale, in gulleys from 0.3 mi (0.5 km) south of old road from Lance Creek to U.S. Rt. 85, and 0.5 mi (0.8 km) east of East Fork Buck Creek, and 8.3 mi (13.4 km) east-northeast of Lance Creek, Wyoming. K. M. Waage.

    • 35. A4768. Lower part of Baculites grandis Zone, in and below 8 ft (2.4 m)-thick bentonite noted by Gill and Cobban (1966), upper unnamed shale member, Pierre Shale, SW¼ to NW¼ NE¼NE¼ sec.14, T. 38 N., R. 62 W., in an area trending northeast across Brewster Drawer, 2.1–2.5 mi (3.4–4.0 km) north-northeast of Red Bird, Niobrara County, Wyoming.

    © American Museum of Natural History 2019
    Neil H. Landman, W. James Kennedy, Neal L. Larson, Joyce C. Grier, James W. Grier, and Tom Linn "Description of Two Species of Hoploscaphites (Ammonoidea: Ancyloceratina) from the Upper Cretaceous (Lower Maastrichtian) of the U.S. Western Interior," Bulletin of the American Museum of Natural History 2019(427), 1-72, (22 February 2019). https://doi.org/10.1206/0003-0090.427.1.1
    Published: 22 February 2019
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