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1 June 2014 The Problematic Early Cambrian Fossil Tumulduria incomperta Represents the Detached Ventral Interarea of a Paterinid Brachiopod
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The organophosphatic early Cambrian (Terreneuvian, Cambrian Stage 2) fossil Tumulduria incomperta has been problematic ever since its original description in 1969. Comparison of abundant specimens from the Lower Cambrian of Siberia with co-occurring brachiopod valves show that T. incomperta represents the central portion of the ventral interarea of a paterinid brachiopod similar to Cryptotreta neguertchenensis, and that the domed central portion of typical Tumulduria specimens represents the ridge-like pseudodeltidium of the interarea.


Lower Cambrian successions from around the world have yielded a wealth of small plate-, cone-, and spine-shaped fossils, often collectively referred to as “Small Shelly Fossils” (often abbreviated SSF; Rozanov et al. 1969; Matthews and Missarzhevsky 1975; Missarzhevsky 1989; Qian and Bengtson 1989; Bengtson et al. 1990; Bengtson 2004). These fossils represent a significant portion of the known record of body fossils from the first half of the Cambrian Period and have long been considered problematic in terms of biological function and affinity (Bengtson et al. 1990), but during the last two decades many SSF taxa have been shown to belong to the stem, or even crown groups of modern phyla (Conway Morris and Peel 1995; Vinther and Nielsen 2005; Skovsted et al. 2008). However, some characteristic SSF taxa remain biologically problematic (Kouchinsky et al. 2012), and Tumulduria incomperta Missarzhevsky, in Rozanov et al. 1969 from the lower Cambrian of Siberia is one such problematic taxon.

As originally defined, Tumulduria incomperta consists of small, bilaterally symmetrical plates with a central ridge and very variable lateral fields, all ornamented by transverse folds or ridges. In the original description, Missarzhevsky (in Rozanov et al., 1969: 175) compared the bilaterally symmetrical plates of Tumulduria to chiton plates, but similar fossils were later interpreted as trilobite remains by Fedorov et al. (1979), causing considerable interest in the palaeontological community as the oldest known trilobites (Repina 1981; Glaessner 1984; Khomentovsky 1986). However, based on detailed study of new material from Siberia, Bengtson et al. (1987) were able to demonstrate unequivocally that Tumulduria is highly variable morphologically and that the plates grew by accretion. Consequently, any similarity of individual specimens to different parts of the trilobite carapace is superficial and Tumulduria has since been regarded as a problematic fossil (Rozanov et al. 2010; Maloof et al. 2010; Kouchinsky et al. 2012). Bengtson et al. (1987) compared the preservation of Tumulduria and co-occurring organophos phatic brachiopods, but herein we show that Tumulduria incomperta more specifically represents the detached central portion of the ventral interarea of a paterinid brachiopod.

The Order Paterinida is a problematic group of Cambrian to Ordovician phosphatic-shelled brachiopods that includes some of the oldest known members of the phylum (Laurie 2000). The oldest paterinids have been placed in the problematic Family Cryptotretidae, which include several poorly known genera that may not all be closely related (Topper et al. 2013). The generic name Cryptotreta was proposed by Pelman (1977) for brachiopods from the Tommotian Stage of the Siberian Platform exhibiting a strophic hinge and an orthocline ventral interarea with a narrow, convex, ridge-like pseudodeltidium but without clear evidence of an open delthyrium. Cryptotreta is very similar to the somewhat younger Salanygolina Ushatinskaya, 1987, from Mongolia. The better-known Salanygolina has been shown to possess both a narrow ridge-like pseudodeltidium as well as a large foramen anterior to the ventral umbo (Ushatinskaya 1987), partly closed by a colleplax (Holmer et al. 2009), and identical structures can be found in the enigmatic chileids (Popov and Tikhonov, 1990; Popov and Holmer 2000). A similar ventral umbonal foramen appears to be present also in Cryptotreta (Laurie 2000; Galina T. Ushatinskaya, personal communication 2012). However, all other genera commonly referred to the Cryptotretidae, including the well-studied Askepasma Laurie, 1986 from Australia (Laurie 1986; Topper et al. 2013) and the Siberian Aldanotreta Pelman, 1977, differ from Salanygolina and Cryptotreta by the absence of an orthocline ventral interarea and a foramen anterior to the ventral umbo.

Institutional abbreviations.—GIN, Geological Institute of the Russian Academy of Sciences, Moscow, Russia; NRM, Swedish Museum of Natural History, Stockholm, Sweden.

Material and methods

The bulk of the available material is derived from samples collected by Anatoly K. Val'kov from the lowermost part of the Pestrotsvet Formation, Nochoroicyathus sunnaginicus Zone, Tommotian Stage, southeastern Siberian Platform. The geological setting and stratigraphical context of the sampled area were recently summarized by Khomentovsky and Karlova (2005), Varlamov et al. (2008), and Rozanov et al. (2010). Sample 449 was collected from the left bank of the Aldan River, 1–2 km upstream of the mouth of the Ennyues River (= section M403 in Rozanov et al. 1969). Sample 525 was collected from the left bank of the Aldan River, 7 km upstream the Ulakhan-Sulugur Brook. Sample 1793 was collected from the left bank of the Aldan River, at the Byukteleekh Brook, 25 km downstream of the “Dvortsy” section (= section M407 in Rozanov et al. 1969). Samples 1825 and 1832 were collected from the Mount Konus section on the right bank of the Uchur River, upper reaches of the Kholobolokh (1825) and Malyj Chajdakh (1832) rivulets (see Khomentovsky et al. 1990).

In addition, several hundred small specimens, including Tumulduria plates, incomplete dorsal valves and indeterminable shell fragments were derived from samples collected in 1990 by John S. Peel (JSP 1990 27/1) from about 30 cm above the base of the Pestrotsvet Formation (bed 15; Nochoroicyathus sunnaginicus Zone, early Tommotian Stage) at the reference section at “Dvortsy” on the Aldan River, Siberia.

All samples were prepared by dissolution in buffered acetic acid (7–10%) and the resulting residues sieved and scanned for microfossils using a stereomicroscope. Selected fossils were mounted and coated by gold prior to SEM study at the Swedish Museum of Natural History in Stockholm.

Tumulduria as a brachiopod

The lateral fields of the broadly triangular plates of Tumulduria incomperta are highly variable in shape and size relative to specimen length, and lateral margins are usually uneven (Fig. 1). The median ridge is very similar in morphology to the ridge-like pseudodeltidium of the ventral interarea of Cryptotreta and the lateral flanks are reminiscent of the flat, orthocline ventral interarea itself (Pelman 1977; Laurie 2000). In width, the convex pseudodeltidium of T. incomperta typically varies from 200 to 500 µm, which is comparable to the pseudodeltidium found on complete ventral valves of Cryptotreta neguertchenensis (see Laurie 2000). The variable transverse lineation of the plates often shows a distinct deflection towards the oldest part of the plate (as indicated by the overlapping shell layers) across the ridge, which is also the case in the pseudodeltidium of C. neguertchenensis and presumably reflects the small embayment of this part of the ventral interarea (Laurie 2000: fig. 85A). Comparison could also be made with the ventral interarea of Salanygolina obliqua Ushatinskaya, 1987 from the lower Cambrian of Mongolia, where a narrow and convex pseudodeltidium of similar morphology divides the flat, triangular interarea (Holmer et al. 2009: text-fig. 4A).

Complete specimens of ventral valves are lacking in our collections, mirroring the absence of complete ventral valves in most collections of Cryptotreta and Salanygolina. In the case of Cryptotreta and Salanygolina, the lack of complete ventral valves is presumably a consequence of fragmentation due to structural weakness caused by the large umbonal foramen (see also Pelman 1977 and Holmer et al. 2009) and a similar umbonal foramen was probably present also in Tumulduria. However, one specimen exhibits the central ridge and one complete lateral half of the triangular interarea (Fig. 2A), effectively bridging the morphological gap between typical specimens of T. incomperta and complete ventral valves of other cryptotretid brachiopods. Although incomplete, this specimen shows that the interarea originally was a flat, obtusely triangular plate (the specimen is broken parallel to the pseudodeltidium and thus represents only the left lateral half of the interarea; Fig. 2A1, A2) with a well marked pseudodeltidium (Fig. 2A3). The plate exhibits uneven transverse growth lines and an oblique, centrally placed flexure-line. The flexure line presumably represents a zone of weakness, and its inclination (about 30°) corresponds roughly to the slope of the lateral margins in typical Tumulduria plates (around 25–40°in larger specimens in our collections; Fig. 1A–D). A similar specimen was illustrated together with other specimens of Tumulduria as “Skeletal Problematicum 1” by Meshkova (1974: pl. 26: 3). The specimen illustrated by Meshkova (1974) appears to be more complete and preserves part of both lateral fields of the interarea, complete with flexure lines, pseudodeltidium and the posterior margin with a central embayment. Other fragmentary specimens in our collections preserve an acute linear fold which probably represents the lateral junction of the interarea and general shell surface and support the interpretation of the interarea as a flat, triangular plate separated from the rest of the shell by a sharp fold (Fig. 2B).

Fig. 1.

Paterinid brachiopod Tumulduria incomperta Missarzhevsky in Rozanov et al, 1969. Typical Tumulduria plates with pseudodeltidium and partially preserved lateral flanks representing ventral interarea. Aldan and Uchur River area, Nochoroicyathus sunnaginicus Zone, Siberia. A. NRM Br141128, sample 1825; A1, view from above; A2, oblique posterior view. B. NRM Br141129, sample 1825; B1, view from above; B2, oblique posterior view. C. NRM Br141130, sample 1825; C1, view from above; C2, oblique posterior view. D. NRM Br141131, sample 1825; D1, view from above; D2, oblique lateral view. E. NRM Br141132, sample JSP 1990 27/1; E1, view from above; E2, oblique posterior view. F. NRM Br141133, sample JSP 1990 27/1; F1, view from above; F2, oblique posterior view. G. NRM Br141134, sample JSP 1990 27/1; G1, view from above; G2, oblique posterior view. H. NRM Br141135, sample 1825; H1, internal view; H2, detail of internal surface with botryoidal structures.


In most samples investigated by us, we find an association of the problematic fossil Tumulduria incomperta with indeterminable brachiopod shell fragments and flat to gently convex and weakly sulcate brachiopod valves (Fig. 3). The associated shells are strongly reminiscent of the dorsal valves of cryptotretid brachiopods, including the genera Cryptotreta and Aldanotreta which are known to occur in the Tommotian of the Siberian Platform (Pelman 1977, 1979). Although isolated dorsal valves of cryptotretids may be difficult to separate morphologically, the valves occurring with Tumulduria in the Pestrotsvet Formation differ from the dorsal valves of all described cryptotretids in having an extremely small interarea divided by an open triangular notothyrium.

In addition to the co-occurrence and morphological similarities of Tumulduria plates and associated cryptotretid dorsal valves, the apparent botryoidal shell structure is very similar between typical specimens of T. incomperta and co-occurring flat brachiopod valves (compare Figs. 1H2 and 3D2). The botryoidal structure is observable on the internal surface of all available specimens, but is not apparent on external surfaces. This similarity in preservation of the shell structure was also noted by Bengtson et al. (1987: 368) although the illustrated brachiopod valves were identified as belonging to Aldanotreta sunnaginensis (Bengtson et al. 1987: fig. 7). Although the botryoidal structure is most likely of diagenetic origin, the close similarity in preservation provide a strong indication that the original composition and shell structure of typical Tumulduria plates and co-occurring cryptotretid brachiopod valves were identical or, at least, very similar.

Fig. 2.

Paterinid brachiopod Tumulduria incomperta Missarzhevsky in Rozanov et al, 1969. Fragmentary valves. Aldan and Uchur River area, Nochoroicyathus sunnaginicus Zone, Siberia. A. NRM Br141136, sample 449, left lateral half of ventral interarea; A1, view from above; A2, oblique posterior view; A3, detail of pseudodeltidium in oblique view. B. NRM Br141137, sample 1832, fragment preserving junction of ventral interarea and ventral shell surface; B1, view from posterior; B2, oblique posterolateral view. C. NRM Br141138, sample 525, fragment of shell surface with fila and nick points.


Based on the observed occurrence patterns as well as morphological and ultrastructural similarities we conclude that Tumulduria incomperta is likely to represent the detached central portion of the ventral interarea of a cryptotretid brachiopod and that the associated brachiopod valves represent the dorsal valve of the same taxon.

Systematic palaeontology

Phylum Brachiopoda Duméril, 1806
Class Paterinata Williams, Carlson, Brunton, Holmer, and Popov, 1996
Order Paterinida Rowell, 1965
Superfamily Paterinoidea Schuchert, 1893
Family Cryptotretidae Pelman, 1979
Genus Tumulduria Missarzhevsky in Rozanov et al., 1969

  • Type species: Tumulduria incomperta Missarzhevsky in Rozanov et al., 1969 from the Nochoroicyathus sunnaginicus Zone, Tommotian Stage, Cambrian Series 2, of the Aldan River area, southeastern Siberian Platform.

  • Emeded diagnosis.—Ventral valve with orthocline, flat, triangular interarea with a narrow pseudodeltidium. Interarea with low, transverse ribs and furrows and oblique, poorly developed flexure lines. Dorsal valve flat or slightly convex and gently sulcate. Catacline dorsal interarea reduced and developed as a low elongate ridge along the posterior margin; dorsal triangular notothyrium open.

    Tumulduria differs from Aldanotreta Pelman, 1977, Dzunarzina Ushatinskaya, 1993, and Askepasma Laurie, 1986 in having an orthocline, triangular ventral interarea with a narrow pseudodeltidium and a low ridge-like dorsal interarea. It differs from Cryptotreta Pelman, 1977 in having more irregular transverse ornament on the ventral interarea and an open triangular notothyrium lacking a chilidium. It differs from Salanygolina Ushatinskaya, 1987 in its more strongly sulcate dorsal shell, small dorsal interarea with open notothyrium and in lacking the pustulose adult microornament.

  • Discussion.—The rationale behind the reinterpretation of Tumulduria incomperta as a paterinid brachiopod is outlined above. Based on the shared presence of an orthocline ventral interarea with a pseudodeltidium and an inferred foramen anterior to the umbo, Tumulduria is likely to be closely related to Cryptotreta from the Siberian Platform and Salanygolina from the lower Cambrian of Mongolia. The relationship of Tumulduria to other genera included in the Cryptotretidae is less clear.

  • Geographic and stratigraphic range.—Tumulduria is known from the Nochoroicyathus sunnaginicus Zone, Tommotian Stage (Terreneuvian Series, Cambrian Stage 2), southeastern Siberian Platform, from sections along the Aldan River and from the Uchur-Maya region representing the transitional facies belt (Rozanov et al. 1969; Khomentovsky et al. 1990; Rozanov and Zhuravlev 1992; Khomentovsky and Karlova 2005).

  • Fig. 3.

    Paterinid brachiopod Tumulduria incomperta Missarzhevsky in Rozanov et al, 1969. Dorsal valves. Aldan and Uchur River area, Nochoroicyathus sunnaginicus Zone, Siberia. A. NRM Br141139, sample 1793; A1, dorsal view; A2, oblique anterior view; A3, oblique posterior view; A4, detail of cardinal area in oblique posterior view; A5, oblique anterolateral view of internal surface. B. NRM Br141140, sample 1825; B1, dorsal view; B2, oblique posterior view. C. NRM Br141141, sample 1832; C1, dorsal view; C2, oblique posterior view; C3, oblique anterior view of internal surface. D. NRM Br141142, sample 1832; D1, internal view; D2, detail of internal surface with botryoidal structures.


    Tumulduria incomperta Missarzhevsky in Rozanov et al., 1969
    Figs. 13.

  • 1969 Tumulduria incomperta sp. nov. Missarzhevsky; Rozanov et al. 1969: 175, pl. 6: 5, 6.

  • 1974 Skeletal Problematica 1; Meshkova 1974: 193, pl. 26: 1–3, 6–7.

  • 1987 Tumulduria incomperta Missarzhevsky; Bengtson et al. 1987: 364, figs 1–6. (cum. syn.).

  • 1987 Aldanotreta sunnaginensis Pelman; Bengtson et al. 1987: fig. 7.

  • 1989 Tumulduria incomperta Missarzhevsky; Missarzhevsky 1989: 215, pl. 28: 6, 9.

  • 1992 Tumulduria incomperta Missarzhevsky; Rozanov and Zhuravlev in Lipps and Signor 1992: 257, fig. 9, panel 78.

  • 1998 Tumulduria incomperta Missarzhaevsky; Vasil'eva 1998: 115, pl. 44: 3, 7.

  • 2008 Tumulduria incomperta Missarzhevsky; Varlamov et al. 2008; pl. 13: 12, 13.

  • 2010 Tumulduria incomperta Missarzhevsky; Rozanov et al. 2010: 86, pl. 59: 5, 6.

  • Holotype: GIN 3593/138. Partial ventral interarea with narrow central pseudodeltidium and broken lateral margins. From Aldanocyathus sunnaginicus- Tiksitheca licis Zone, Aldan River.

  • Type locality: Aldan River, left bank, 7 km west of settlement Ugino (section M402 in Rozanov et al. 1969).

  • Type horizon: Tommotian Stage, Nochoroicyathus sunnaginicus Zone, Cambrian.

  • Diagnosis.—As for genus.

  • Material.—The available material consists of 34 partially complete ventral interareas, 15 dorsal valves and possible shell fragments collected from the Aldan and Uchur River regions (Pestrotsvet Formation, Nochoroicyathus sunnaginicus Zone, Tommotian Stage, southeastern Siberian Platform).

  • Description.—The morphology of both isolated Tumulduria interareas and associated ventral valve fragments (Figs. 1, 2) is described above. The dorsal valves are flat or very gently convex with a straight posterior margin and a weakly developed anterior sulcus (Fig. 3). Growth is hemiperipheral. Dorsal interarea is absent or vestigial in smaller specimens (Fig. 3B, C), but larger specimens exhibit a low, catacline interarea (Fig. 3A). Under the slightly elevated umbo the dorsal interarea is divided by a small, triangular notothyrium lined on both sides by weakly defined ribs (Fig. 3A4). The internal morphology is poorly preserved, but one large specimen shows a weakly defined pair of ridges radiating from the umbonal region (Fig. 3A5).

    The surface sculpture of the shell consists of fine concentric fila and variable, often slightly uneven, low ribs and furrows (transverse furrows on ventral interarea; Fig. 2A3). On some shell fragments from larger shells, the concentric ornament is complemented by fine transverse furrows and nick points (Fig. 2C).

  • Discussion.—As discussed above, no complete ventral valves of Tumulduria are known, but based on comparison with Cryptotreta and Salanygolina the ventral valve is assumed to have been strongly convex with an orthocline triangular interarea with a narrow pseudodeltidium. Anterior to the umbo the shells are assumed to have had a large foramen, possibly with a colleplax, and as in Cryptotreta and Salanygolina (where complete ventral valves are very rarely preserved) the structural weakness introduced by the umbonal foramen could account for the lack of preserved ventral valves.

    The ornament, particularly on the ventral interarea, is generally more chaotic than in other cryptotretid brachiopods, including the other Siberian taxa Aldanotreta and Cryptotreta, and there is no trace of a pustulose micro-ornament such as in Salanygolina.

  • Stratigraphic and geographic range.—Same as for genus by monotypy.

  • Acknowledgements

    John S. Peel (Uppsala University, Uppsala, Sweden) is thanked for access to specimens of Tumulduria from Dvortsy, Siberia. Galina T. Ushatinskaya (Paleontological Institute, Russian Academy of Sciences, Moscow, Russia), Timothy P. Topper (Museum of Geology, Copenhagen, Denmark) for valuable discussions on the taxonomy of Cambrian brachiopods. The work was supported financially by the Swedish Museum of Natural History and by grants to LEH and SB from the Swedish Research Council (VR 2009-4395, 2012-1658 and 2010-3929) and to SB from the Danish National Research Foundation (DNRF 53). Constructive comments by external reviewers, John R. Laurie (Geoscience Australia, Canberra, Australia) and John L. Moore (University of California, Santa Barbara, USA) greatly improved the final version of the manuscript.



    S. Bengtson 2004. Early skeletal fossils. In : J.H. Lipps and B.M. Waggoner (eds.), Neoproterozoic-Cambrian Biological Revolutions. The Paleontological Society Papers 10: 67–77. Google Scholar


    S. Bengtson , A.B. Fedorov , V.V. Missarzhevsky , A.Y. Rozanov , E.A. Zhegallo , and A.Yu. Zhuravlev 1987. Tumulduria incomperta and the case for Tommotian trilobites. Lethaia 20: 361–370. Google Scholar


    S. Bengtson , S. Conway Morris , B.J. Cooper , P.A. Jell , and B.N. Runnegar 1990. Early Cambrian fossils from South Australia. Memoirs of the Association of Australasian Palaeontologists 9: 1–364. Google Scholar


    S. Conway Morris and J.S. Peel 1995. Articulated halkieriids from the Lower Cambrian of North Greenland and their role in early protostome evolution. Philosophical Transactions of the Royal Society of London B 347: 305–358. Google Scholar


    A.M.C. Dumeril 1806. Zoologie analytique ou méthode naturelle de classification des animaux. 364 pp + xxiv. Allais, Paris. Google Scholar


    A.B. Fedorov , L.I. Egorova , and V.E. Savitsky [ V.E. Savickij ] 1979. The first find of ancient trilobites in the lower part of the stratotype of the Lower Cambrian Tommotian Stage (R. Aldan) [in Russian]. Doklady AN SSSR 249 (5): 1188–1190. Google Scholar


    M.F. Glaessner 1984. The Dawn of Animal Life. A Biohistorical Study. 244 pp. Cambridge University Press, Cambridge. Google Scholar


    L.E. Holmer , S. Pettersson Stolk , C.B. Skovsted , U. Balthasar , and L.E. Popov 2009. The enigmatic Early Cambrian Salanygolina—a stem group of rhynchonelliform chileate brachiopods? Palaeontology 52: 1–10. Google Scholar


    V.V. Khomentovsky 1986. The Vendian System of Siberia and a standard stratigraphic scale. Geological Magazine 123: 333–348. Google Scholar


    V.V. Khomentovsky and G.A. Karlova 2005. The Tommotian Stage base as the Cambrian lower boundary in Siberia. Stratigraphy and Geological Correlation 13: 21–34. Google Scholar


    V.V. Khomentovsky [V.V. Homentovskij ], A.K. Val'kov , and G.A. Karlova 1990. New data on the biostratigraphy of transitional Vendian- Cambrian strata in the middle reaches of the River Aldan [in Russian]. In : V.V. Homentovskij and A.S. Gibšer (eds.), Pozdnij dokembrij i rannij paleozoj Sibiri. Voprosy regional'noj stratigrafii , 3–57. Institut geologii i geofiziki SO AN SSSR, Novosibirsk. Google Scholar


    A. Kouchinsky , S. Bengtson , B. Runnegar , C.B. Skovsted , M. Steiner , and M. Vendrasco 2012. Chronology of early Cambrian biomineralisation. Geological Magazine 149: 221–251. Google Scholar


    J.R. Laurie 1986. Phosphatic fauna of the Early Cambrian Todd River Dolomite, Amadeus Basin, Central Australia. Alcheringa 10: 431–454. Google Scholar


    J.R. Laurie 2000. Class Paterinata. In : R.L. Kaesler (ed.), Treatise on Invertebrate Paleontology, Part H, Brachiopoda, Revised, Vol. 2 , 147– 157. Geological Society of America and University of Kansas Press, Boulder. Google Scholar


    J.H. Lipps and P.H. Signor (eds.) 1992. Origin and Early Evolution of the Metazoa. 570 p. Plenum Press, New York. Google Scholar


    A.C. Maloof , S.M. Porter , J.L. Moore , F. Ö. Dudás , S.A. Bowring , J.A. Higgins , D.A. Fike , and M.P. Eddy 2010. The earliest Cambrian record of animals and ocean geochemical change. Geological Society of America Bulletin 122: 1731–1774. Google Scholar


    S.C. Matthews and V.V. Missarzhevsky 1975. Small shelly fossils of late Precambrian and early Cambrian age: a review of recent work. Journal of the Geological Society 131: 289–304. Google Scholar


    N.P. Meshkova [N.P. Meškova ] 1974. Cambroscleritida insertae sedis—a new order of Cambrian fossils [in Russian]. In : I.T. Žuravleva and A.Û. Rozanov (eds.), Biostratigrafiâ i paleontologiâ nižnego kembriâ Evropy i Severnoj Azji , 190–193. Nauka, Moskva. Google Scholar


    V.V. Missarzhevsky [V.V. Missarževskij ] 1989. The oldest skeletal fossils and stratigraphy of the Precambrian-Cambrian boundary beds fossils [in Russian]. Trudy Geologiceskogo Instituta AN SSSR 443: 1–237. Google Scholar


    Yu.L. Pelman [Û.L. Pelman ] 1977. Early and Middle Cambrian inarticulate brachiopods of the Siberian Platform fossils [in Russian]. Trudy Instituta Geologii i Geofiziki AN SSSR, Sibirskoe Otdelenie 316: 1–168. Google Scholar


    Yu.L. Pelman [Û.L. Pelman ] 1979. The oldest complexes of brachiopods (Class Inarticulata) fossils [in Russian]. Trudy Instituta Geologii i Geofiziki AN SSSR, Sibirskoe Otdelenie 406: 34–39. Google Scholar


    L.E. Popov and Yu.A. Tikhonov [Û.A. Tihonov]1990. Early Cambrian brachiopods from southern Kirgizia fossils [in Russian]. Paleontologiceskij žurnal 3: 33–46. Google Scholar


    L.E. Popov and L.E. Holmer 2000. Class Chileata. In : R. Kaesler (ed.), Treatise on Invertebrate Paleontology. Part H Brachiopoda (Revised) 2, 193–196. Geological Society of America and University of Kansas Press, Boulder. Google Scholar


    Y. Qian and S. Bengtson 1989 Palaeontology and biostratigraphy of the Early Cambrian Meishucunian Stage in Yunnan Province, South China. Fossils and Strata 24: 1–156. Google Scholar


    L.N. Repina 1981. Trilobite biostratigraphy of the Lower Cambrian Stages of Siberia. In : M.E. Taylor (ed.), Short Papers for the Second International Symposium on the Cambrian System. U.S. Geological Survey Open-File Report 81–743: 173–180. Google Scholar


    A.J. Rowell 1965. Inarticulata. In : R.C. Moore (ed.), Treatise on Invertebrate Paleontology. Part H. Brachiopoda , H260–H296. Geological Society of America and University of Kansas Press, Lawrence. Google Scholar


    A.Yu. Rozanov and A.Yu. Zhuravlev 1992. The Lower Cambrian fossil record of the Soviet Union. In : J.H. Lipps and P.W. Signor (eds.), Origin and Early Evolution of the Metazoa, 205-82. Plenum, New York. Google Scholar


    A.Yu Rozanov . [A.Û. Rozanov], V.V. Missarzhevsky [V.V. Missarževskij ], N.A. Volkova , L.C. Voronova , I.N. Krylov , B.M. Keller , I.K. Korolyuk [I.K. Korolûk ], K. Lendzion , R. Michniak , N.G. Pykhova [N.G. Pykova ], and A.D. Sidorov 1969. The Tommotian Stage and the Cambrian lower boundary problem [in Russian]. Trudy Geologiceskogo instituta AN SSSR 206: 1–380. (English edition: 1981, 359 pp. Amerind Publishing Co., New Delhi) Google Scholar


    A.Yu. Rozanov [A. Û. Rozanov], P.Yu. Parkhaev [P. Û Parhaev], Yu.E. Demidenko [Û.E. Demidenko], G.A. Karlova , I.V. Korovnikov , Yu.Ya. Shabanov [Û. Šabanov ]., A.Yu. Ivancov [A. Û. Ivancov], V.A. Luchinina [V.A. Lucinina ], Ya.E. Malakhovskaya [Â.E. Malahovskaâ], L.M. Melnikova , E.B. Naimark , A.G. Ponomarenko , N.A. Skorlotova , V.M. Sundukov , D.A. Tokarev , G.T. Ushatinskaya [G.T. Ušatinskaâ] and L.D. Kipriyanova [L.D. Kipriânova ]. 2010. Iskopaeme stratotipov ârusov nižnego kembriâ. 226 pp. PIN RAN, Moskva. Google Scholar


    C. Schuchert 1893. A classification of the Brachiopoda. American Geologist 11: 141–167. Google Scholar


    C.B. Skovsted , G.A. Brock , J.R. Paterson , L.E. Holmer , and G.E. Budd 2008. The scleritome of Eccentrotheca from the Lower Cambrian of South Australia: lophophorate affinities and implications for tommotiid phylogeny. Geology 36: 171–174 Google Scholar


    T.P. Topper , L.E. Holmer , C.B. Skovsted , G.A. Brock , U. Balthasar , C.M. Larsson , S. Petterson Stolk , and D.A.T. Harper 2013. The oldest brachiopods from the lower Cambrian of South Australia. Acta Palaeontologica Polonica 58: 93–109. Google Scholar


    G.T. Ushatinskaya [G.T. Ušatinskaâ ] 1987. Unusual inarticulate brachiopods from the Lower Cambrian of Mongolia [in Russian]. Paleontologiceskij žurnal 2: 62–68. Google Scholar


    G.T. Ushatinskaya [G.T. Ušatinskaâ ] 1993. Early and Middle Cambrian lingulids of the Siberian Platform [in Russian]. Paleontologiceskij žurnal 2: 133–136. Google Scholar


    A.I. Varlamov , A.Yu. Rozanov , V.V. Khomentovsky , Yu.Ya. Shabanov , G.P. Abaimova , Yu.E. Demidenko , G.A. Karlova , I.V. Korovnikov , V.A. Luchinina , Ya.E. Malakhovskaya , P.Yu. Parkhaev , T.V. Pegel , N.A. Skorlotova , V.M. Sundukov , S.S. Sukhov , A.B. Fedorov , and L.D. Kipriyanova 2008. The Cambrian System of the Siberian Platform. Part 1: The Aldan-Lena Region . 300 pp. PIN RAS, Moscow. Google Scholar


    N.I. Vasil'eva 1998. Small shelly fauna and biostratigraphy of the Lower Cambrian of Siberian Platform [in Russian]. In : A.I. Kirichkova (ed.), Trudy VNIGRI 1998: 1–139. Google Scholar


    J. Vinther and C. Nielsen 2005. The Early Cambrian Halkieria is a mollusk. Zoologica Scripta 34: 81–89. Google Scholar


    A. Williams , S.J. Carlson , C.H.C. Brunton , L.E. Holmer , and L.E. Popov 1996. A supra-ordinal classification of the Brachiopoda. Philosophical Transactions of the Royal Society of London, Series B 351: 1171–1193. Google Scholar
    © 2014 C.B. Skovsted et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
    Christian B. Skovsted, Artem Kouchinsky, Stefan Bengtson, and Lars E. Holmer "The Problematic Early Cambrian Fossil Tumulduria incomperta Represents the Detached Ventral Interarea of a Paterinid Brachiopod," Acta Palaeontologica Polonica 59(2), 359-365, (1 June 2014).
    Received: 8 June 2012; Accepted: 17 September 2012; Published: 1 June 2014
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