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1 June 2014 Pleistocene Equid Brain Endocast from Shanxi Province, China
Ying Hu, Yaoxing Chen, Shuo Wang, Qingmin Sun
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Brain endocasts are rare in the fossil record because they are only preserved under exceptional conditions. An equid brain endocast from the early Pleistocene of Wanrong County, Shanxi Province, China, is reported in this paper. Measuring approximately 140 × 95.2 × 83 mm, the new specimen represents a relatively advanced adult horse brain. Comparisons indicate that it is more derived than those of Hyracotherium and Mesohippus in having an expanded neocortex, and more than those of Pliohippus and Hipparion in having an enlarged network of branching sulci; in most characters involving these sulci, the Shanxi brain conforms to the extant species Equus caballus. The sulcus diagonalis of the Equus brain appears to have evolved conservatively during the early Pleistocene, whereas the sulcus suprasylvius seems to have evolved rapidly. The specimen demonstrates that the development of a high degree of complexity predates the enlargement of the brain in the horse, which increased in length, breadth, and especially height during the late Cenozoic.


Knowledge of evolutionary change in the nervous system is indispensable for understanding vertebrate evolution as a whole. Yet, despite the abundance of well-preserved equid material in the fossil record, three-dimensionally preserved brains are rare, since soft brain tissue is preserved only under highly specific sedimentary conditions: most preserved brain endocasts are cemented by sand, and sometimes the organic ingredients of the brain are replaced by calcium compounds (Wang and Bao 1984). CT-scanning of the cranial cavity (Franzosa and Rowe 2005; Dong et al. 2006) offers a way to reconstruct cerebral morphology even when no brain fossil has been recovered as such, but usually fails to capture exact details of the brain sulci. Thus, although a natural brain endocast is unlikely to be preserved, it can provide more detailed information about the function and evolution of the vertebrate nervous system than CT scans. The past few decades have seen reports of natural endocasts from a variety of animals, such as birds (Kurochkin et al. 2007), dinosaurs (Jerison 2004), and mammals (Edinger 1948; Radinsky 1976; Wang and Bao 1984; Kear 2003; Takai et al. 2003), including humans (Jerison 1975). Here, we add to this record by describing a nearly complete equid brain endocast from early Pleistocene sediments exposed in Shanxi Province, China, and discuss its evolutionary implications.

Institutional abbreviations.—AMNH, American Museum of Natural History, New York, USA; CNHM, Carnegie Museum of Natural History, Pittsburgh, USA; LACM, Natural History Museum of Los Angeles County, Los Angeles, USA; TNU, Tianjin Normal University, Tianjin, China; USNM, United States National Museum, Washington, DC, USA.

Geological setting

The brain endocast reported here was recovered from the Sanmen Formation of Chenjiagou, Ronghe Town, Wanrong County (E 110°29′23″; N 35°18′39″), southwestern Shanxi Province, China (Fig. 1), which lies about 1.5 km south of Xizhuozi (Tang et al. 1983). A well-developed fluvial sedimentary sequence extending from the Pliocene to the Pleistocene is exposed in this area, and has yielded numerous fossils (Zhou and Zhou 1959, 1965; Tang et al. 1983; Huang and Ji 1984). The specimen was derived from a layer of cross-bedded fluvial sandstone (Supplementary Online Material, SOM at SOM 1; Tang et al. 1983), which has also yielded abundant fossils of Equus sanmeniensis, E. przewalskii, E. cf. huanghoensis, artiodactyls (Tang et al. 1983), carnivorans (Zhou and Zhou 1959, 1965; Tang et al. 1983; Huang and Ji 1984; Wang and Zhao 2006) and birds (Wang et al. 2006). Both E. sanmeniensis and E. huanghoensis appeared during the early Pleistocene (Deng and Xue 1999), with E. sanmeniensis becoming extinct at the start of the middle Pleistocene. The mammalian assemblage of Chenjiagou closely resembles the Linyi fauna, dated to the Nihewanian (early Pleistocene, or Calabrian-Gelasian, sensu Gradstein et al. [2012]) based on the occurrence of Megantereon, Euctenoceros boulei, and Hipparion (Proboscidipparion) sinense (SOM 2; Tong et al. 1995). Taken together, this suggests an early Pleistocene age (or Calabrian-Gelasian, about 0.8–2.6 Ma) for the fluvial sandstone of Chenjiagou (SOM 2; Zhou and Zhou 1959; Huang and Ji 1984; Tong et al. 1995; Wang and Zhao 2006; Gradstein et al. 2012).

Material and methods

Our observations and descriptions are based on a relatively complete natural brain endocast housed at Tianjin Normal University (TNU V44). For comparisons, we relied largely on descriptions of brain endocasts of Hyracotherium, Miohippus, Mesohippus, Neohipparion, Pliohippus, and Hipparion (Tilney 1933; Edinger 1948; Radinsky 1976), as well as the brain of the extant horse Equus caballus (Edinger 1948, and a specimen housed at the China Agricultural University). We measured the new material following the protocols of Edinger (1948). The endocast was first measured with calipers, and then modeled in resin at a 1:1 scale. The volume of the brain was estimated by submerging the model and measuring the volume of water displaced. Relative brain size taking into account body size was assessed by calculating the encephalization quotient (EQ), following the methodology of Jerison (1970) (see SOM 3 for details).


Description.—The brain endocast was cemented by sand and clay. The cerebral hemispheres are nearly complete, and many details are visible on the dorsal, lateral and ventral surfaces in particular (Figs. 2, 3). The endocast is 140 mm long and 95.2 mm wide, and has a maximum height of 83 mm. Judging from its comparatively large volume of 465 ml, it represents a relatively advanced adult horse brain. The symmetrical cerebral hemispheres bear a complicated network of branched sulci, resembling the general pattern of neocortical fissures seen in modern horses.

Fig. 1.

Map showing the position of Wanrong County, Shanxi Province, China.


The longitudinal fissure is discernible, and the olfactory bulbs can be seen on the lower halves of the anterior faces of the cerebral hemispheres. The anterior portions of both olfactory bulbs are broken away, with the fractured surfaces measuring 24 mm (right) and around 20 mm (left) in diameter, respectively. The anterodorsal part of the right frontal lobe is missing. The sulci of the occipital lobe are shallow on both sides, making it difficult to distinguish particular features. The morphology of the right occipital region is particularly obscure, owing to some fragments of bony tissue that remain attached to the endocast. Most of the sulci of the frontal, temporal and apical lobes can be identified in left lateral view, while in the right hemisphere only the temporal and frontal lobes can be distinguished. In ventral view, only the optic tract, hypophysis and ventral surface of the cerebellum can be recognized, with the optic tract being distinctly larger than in the modern Equus specimen housed at the China Agricultural University.

Owing to the shallowness of the sulci, many characters relating to the pattern of fissuration are difficult to assess. The praesylvian and suprasylvian sulci are recognizable on both sides, although the suprasylvian sulcus is clearer on the left. The suprasylvian sulcus is located close to the longitudinal fissure and forms anterior, middle and posterior branches, with the middle branch being the deepest of the three. The left coronal sulcus is shallow, while the right one is not preserved. The left ectomarginal sulcus is deep and well developed, extending forwards and curving towards the longitudinal fissure. By contrast, the right ectomarginal sulcus is poorly defined. The ectosylvian sulcus and the fossa sylvii can be clearly distinguished in left lateral view. Similarly, the interorbital sulcus and the frontal part of the praesylvian sulcus are well developed in the right hemisphere.

Fig. 2.

Fossil equid brain endocast (TNU V44) from Shanxi Province, China (early Pleistocene) and associated bones in left lateral (A) and right lateral (B) views. Photographs (A1, B1) and sketches (A2, B2).


Comparisons.—The oldest evidence of equid brain morphology consists of a natural endocast of Eocene age, originally referred to Hyracotherium by Edinger (1948). Radinsky (1976) subsequently challenged this assignment, and instead produced three artificial endocasts from a series of confidently identified Hyracotherium skulls. The latter have comparatively featureless surfaces, with only the sulcus suprasylvius, sulcus lateralis, and sulcus rhinalis being clearly distinguishable (Radinsky 1976). After Hyracotherium, the next reliable record comes from an endocast of Mesohippus, a 30-million-year-old taxon thought to be close to the ancestral line of modern horses (Edinger 1948). The frontal and occipital lobes of this taxon are significantly expanded and their lateral sulci visibly more elongated than in Hyracotherium (Radinsky 1976). Compared with both Hyracotherium and Mesohippus, TNU V44 clearly has a more expanded neocortex.

Table 1.

Brain, body size estimates, and encephalization quotients (EQ) of fossil and modern horses.


Fig. 3.

Fossil equid brain endocast (TNU V44) from Shanxi Province, China (early Pleistocene) and associated bones in dorsal (A) and ventral (B) views. Photographs (A1 B1) and sketches (A2, B2).


Two endocasts of Pliohippus (AMNH 10844 and CNHM P15870) and a further one belonging to Hipparion (AMNH 10732a) are only slightly smaller than TNU V44 (Edinger 1948). However, the maximum length to width ratio of the Hipparion endocast is about 1.3, in contrast to 1.47 in TNU V44, reflecting the more slender shape of the brain of Hipparion. In addition, while the sulcus diagonalis is similar in TNU V44 and Pliohippus, the sulcus suprasylvius of the former is longer and more sinuous, thus indicating that the sulcus diagonalis was relatively conservative in the transition from Pliohippus to more derived equids, whereas the sulcus suprasylvius was more progressive. Furthermore, in accordance with its large optic tract, TNU V44 has a much broader and higher occipital lobe, indicating more advanced visual abilities. Finally, although the anterior portions of the olfactory bulbs are missing, they are located much closer to the cerebrum and do not project as far rostrally as in Pliohippus.

While the brain endocast of Hipparion resembles TNU V44 in terms of its complexity, some obvious differences also exist, including a straight middle part of the sulcus suprasylvius and a sulcus lateralis running parallel to the longitudinal fissure (Edinger 1948). By contrast, both of these sulci are sinuous in TNU V44. Neither an artificial endocast nor a detailed description of the olfactory bulbs of Hipparion was available to us, thus preventing their comparison with those of TNU V44.

In Equus, the sulcus suprasylvius extends anterodorsally in the anterior part of the cerebrum, before curving and running caudally further posteriorly. By contrast, the left lateral sulcus continues anteriorly across the cruciate and ansate sulci, forming a long, anteroposteriorly oriented, undulating, multi-branched line (Edinger 1948). In general, the morphology of TNU V44 closely resembles that of the brain of an extant horse, with the exception of a somewhat shallow er frontal lobe and a sulcus suprasylvius located much closer to the longitudinal fissure (Sisson 1956; Georg 2005), although the latter may well be reflective of the high degree of intraspecific variation found in extant Equus (Edinger 1948). Detailed morphological variation aside, the gross volume of TNU V44 appears slightly smaller than is typical for Equus caballus. According to Edinger (1948) and our own measurements, the brain capacity of Equus caballus is around 580–750 ml, compared to 465 ml in TNU V44. It is thus possible that TNU V44 may represent an early type of Equus brain.

Taking body size into account (SOM 3; Table 1), the brain volume of Equus occidentalis is 3.2 times, and its body size 2.9 times, that of Pliohippus, indicating that both features evolved in synchrony. The EQ of TNU V44 is 0.83, meaning that its brain was about 83% the size one would expect in an average living mammal of similar body w eight. This value is smaller than that of Pleistocene Equus occidentalis and modern horses, but distinctly larger than that of Paleogene and Neogene equids, thus providing additional evidence that TNU V44 likely represents an early Pleistocene Equus brain.


While the brains of TNU V44 and Equus caballus are significantly larger than those of Neohipparion and Pliohippus, Pliohippus displays a pattern of sulci comparable in complexity to that of Equus, and more complex than that seen in Neohipparion. Taking into account their stratigraphic context (Fig. 4), this may indicate that the complex sulci characteristic of Equus appeared before the early Pleistocene, and that the subsequent evolution of the brain during the Pleistocene was primarily a matter of enlargement. However, the latter was likely not proportional: while, despite its overall smaller size, the brain of Neohipparion is about as high as that of Pliohippus, the brains of TNU V44 and Equus caballus are both significantly higher. This implies that, during the Pleistocene, the height of the cerebrum increased to a larger degree than its length and width, and is in agreement with the previous suggestion that, during the late stages of equid evolution, enlargement of the brain no longer occurred through increases in length alone, but rather through simultaneous increases in length, width and height (Edinger 1948).

Fig. 4.

Evolutionary trends in equid brain morphology. Drawings of the brains of Pliohippus, Neohipparion, Miohippus, and Mesohippus are based on Edinger (1948); the drawing of the brain of Hyracotherium is based on Radinsky (1976); the brain of the extant horse Equus caballus is based on the specimen housed at the China Agricultural University. All specimens are shown to the same scale. Numerical ages are taken from Gradstein et al. (2012).


From the comparisons above, it is possible to identify two major morphological stages of brain evolution in the horse (Fig. 4, Table 1): the first stage, occurring from the Eocene through to the Pliocene, involved the evolution of increasingly complex patterns of sulci; by contrast, the second stage, occurring during the Pleistocene, mainly involved brain enlargement, as shown by Equus (but not the Pleistocene representatives of Hipparion). In connecting the two stages, the early Pleistocene marks a critical point in equid evolution, with the second stage possibly triggered by the migration of Equus out of its original habitat.

The genus Equus first appeared about 3.5 Ma ago in North America, before rapidly spreading into Eurasia via the land bridge connecting the two continents around 2.5 Ma (Deng and Xue 1999). Adaptation to this new environment, made even more variable by strong winter monsoons causing periodic fluctuations in the climate and vegetation patterns of East Asia (Liu and Ding 1992), possibly resulted in the evolution of improved visual (as reflected in the enlargement of the brain and optic tract) and auditory (as reflected in the higher cerebrum and temporal lobe) abilities, as well as an increase in body size (Xue et al. 2006). In turn, the enlargement of the brain likely had important consequences in terms of gregariousness, territorial establishment and defense, reproduction and rearing of the young, feeding, and social organization (Butler and Hodos 2005).


We thank Yu Chen (Tianjin, China) for drawing the figures; Lianbin Zheng (Tianjin Normal University, Tianjin, China) and Yue Wu (Tianjin Medical University, Tianjin, China) for discussion; we also express our thanks to Felix Marx (University of Otago, Dunedin, New Zealand), Jun Wang (Duke University, Durham, USA) and Corwin Sullivan (Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China), who revised the manuscript; and to Tuo Yang (Institute of Botany, Chinese Academy of Sciences, Beijing. China), Dan Chen (Institute of Zoology, Chinese Academy of Sciences, Beijing, China) and Shaokun Chen (Three Gorges Museum, Chongqing, China) for providing important references. This work was supported by the Key Laboratory of Evolutionary Systematics of Vertebrates, CAS (2010LESV007).



A.B. Butler and W. Hodos 2005. Comparative Vertebrate Neuroanatomy. Second edition. 744 pp. John Wiley and Sons, inc., New Jersey. Google Scholar


T. Deng and X.X. Xue 1999. Chinese Fossil Horses of Equus and Their Environment. 158 pp. China Ocean Press, Beijing. Google Scholar


W. Dong , J.Y. Liu , and Y.S. Fang 2006. Virtual reconstruction and comparative anatomy of 3D fossil endocranium, In : W. Dong (ed.), Proceedings of the Tenth Annual Meeting of the Chinese Society of Vertebrate Paleontology , 77–84. China Ocean Press, Beijing. Google Scholar


T. Edinger 1948. Evolution of the horse brain. The Geological Society of America Memoir 25: 1–187. Google Scholar


J. Franzosa and T. Rowe 2005. Cranial endocast of the Cretaceous theropod dinasaur Acrocanthosaurus atokensis. Journal of Vertebrate Paleontology 25: 859–864. Google Scholar


F.S. Georg 2005. Principles of Brain Evolution. 436 pp. Publishers Sunderland, Massachusetts. Google Scholar


F.M. Gradstein , J.G. Ogg , M.D. Schmitz , and G.M. Ogg 2012. The Geological Time Scale 2012. 1176 pp. Elsevier, Amsterdam. Google Scholar


W.B. Huang and H.X. Ji 1984. A brief of Quaternary mammalian fossils of the Sanmenxia district. Vertebrata PalAsiatica 22: 230–238. Google Scholar


H.J. Jerison 1970. Brain evolution: new light on old principles. Science 170: 1224–1225. Google Scholar


H.J. Jerison 1973. Evolution of the Brain and Intelligence. 482 pp. Academic Press, New York. Google Scholar


H.J. Jerison 1975. Fossil evidence of the evolution of the human brain. Annual Review of Anthropology A : 27–58. Google Scholar


H.J. Jerison 2004. Dinosaur brains. In : G. Adelman and B.H. Smith (ed.), Encyclopedia of Neuroscience. 3rd Edition. CD Edition. Elsevier, Amsterdam. Google Scholar


B.P. Kear 2003. Macropodoid endocranial casts from the early Miocene of Riversleigh, northestern Queensland. Alcheringa 27: 295–302. Google Scholar


E.N. Kurochkin , G.J. Dyke , S.V. Saveliev , E.M. Pervushov , and E.V. Popov 2007. A fossil brain from the Cretaceous of European Russia and avian sensory evolution. Biology Letters 3: 309–313. Google Scholar


D.S. Liu and Z.L. Ding 1992. The stage coupling process of the monsoon conditions and the change of the ice volume in 2.50 Ma. Quaternary Sciences 12 (1): 12–23. Google Scholar


L. Radinsky 1976. Oldest horse brains: more advanced than previously realized. Science 194: 626–627. Google Scholar


S. Sisson 1956. The Anatomy of the Domestic Animals. Fourth Edition, revised. 265 pp. W.B. Saunders Company, Moscow. Google Scholar


M. Takai , N. Shigehara , and N. Egi 2003. Endocranial cast and morphology of the olfactory bulb of Amphipithecus mogaungensis (lastest middle Eocene of Myanmar). Primates 44: 137–144. Google Scholar


Y.J. Tang , G.F. Zong , and Q.Q. Xu 1983. Mammalian fossils and stratigraphy of Linyi, Shanxi. Vertebrata PalAsiatica. 21: 77–86. Google Scholar


F. Tilney 1933. Fossil Brains of Some Early Tertiary Mammals of North America. Bulletin of the Neurological Institute of New York 1933: 430–505. Google Scholar


Y.S. Tong , C.K. Li , and Z.D. Qiu 1995. Cenozoic mammal ages of China. Vertebrata PalAsiatica 33: 290–314. Google Scholar


J.W. Wang and Y.C. Bao 1984. A fossil brain of the large Felid from North Xizang. Vertebrata PalAsiatica 22: 134–137. Google Scholar


S. Wang and S.N. Zhao 2006. Additional note on the Cuon from Linyi, Shanxi province, China. In : W. Dong (ed.), Proceedings of the Tenth Annual Meeting of the Chinese Society of Vertebrate Paleontology , 63–68. China Ocean Press, Beijing. Google Scholar


S. Wang , S.N. Zhao , X.S. Hu , and Q.M. Sun 2006. Anew genus of early Pleistocene Galliformes in the lower reaches of Fenhe river, Shanxi, China. Geological Bulletin of China 25: 858–861. Google Scholar


X.X. Xue , Y.X. Zhang , and L.P. Yue 2006. Paleoenvironments indicated by the fossil mammalian assemblages from red clay-loess sequence in the Chinese Loess Plateau since 8.0 Ma B.P. Science China, Earth Sciences 49: 518–530. Google Scholar


M.Z. Zhou and B.X. Zhou 1959. Mammalian fossils from early Pleistocene of Linyi, Shanxi. Acta Palaeontologica Sinica 7: 89–97. Google Scholar


M.Z. Zhou and B.X. Zhou 1965. Notes on Villafranchian mammals of Linyi, Shanxi. Vertebrata PalAsiatica 9: 223–229. Google Scholar
© 2014 Y. Hu 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.
Ying Hu, Yaoxing Chen, Shuo Wang, and Qingmin Sun "Pleistocene Equid Brain Endocast from Shanxi Province, China," Acta Palaeontologica Polonica 59(2), 253-258, (1 June 2014).
Received: 11 October 2011; Accepted: 5 July 2012; Published: 1 June 2014
equid brain
Shanxi Province
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