New Yuomys rodents from southeastern Qinghai-Tibet Plateau indicate low elevation during the Middle Eocene
Xijun Ni1,2,3* 
Qiang Li1,2,3* 
Tao Deng1,2,3 
Limin Zhang1,2,3 
Hao Gong1,2 Chao Qin1,2 Jingsong Shi1 Fuqiao Shi1 Shubing Fu1- 1Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China
- 2University of Chinese Academy of Sciences, Beijing, China
- 3CAS Center for Excellence in Life and Paleoenvironment, Beijing, China
Yuomys are medium-sized Hystricomorpha rodents. They are known for coming from areas of low elevation in China during the middle and late Eocene. Two new Yuomys were discovered from a locality near Xueshuo village in Litang County, Sichuan Province. The locality lies in the Gemusi pull-apart basin formed in the Litang Fault System (LTFS) in the Hengduan Mountains. The current average elevation is about 4200 m. One of the two new Yuomys is larger and shows clear lophodont and unilateral hypsodont morphology, similar to Yuomys yunnanensis, which was discovered as being from the early middle Eocene (Irdinmanhan, Asian Land Mammal Ages) in the Chake Basin of Jianshui County, Yunnan Province. The Chake Basin is one of the small pull-apart basins formed in the Xianshuihe-Xiaojiang Fault system (XSH-XJF). The other new Yuomys rodent is smaller, brachydont, and less lophodont than the larger new species. The small new Yuomys is smaller than all known Yuomys except Yuomys huheboerhensis, which is from the early middle Eocene Irdinmanhan of Inner Mongolia in Northern China. Given their narrow biochronological distribution and presumably preferred living environment, the occurrence of Yuomys in the pull-apart basins in LTFS and XSH-XJF suggests that the two deep fault systems probably started strike-slip movement by the early middle Eocene, about 49–45 million years ago. Well-studied middle Eocene mammalian faunas from Henan and Inner Mongolia include Yuomys, primates, and other low elevation forest mammals. We suggest that the two new Yuomys species reported here probably also lived in a similar low elevation forest environment.
1 Introduction
Yuomys is a genus of rodents that existed in the middle and late Eocene in East Asia (Figure 1). Known species of Yuomys show a clear evolutionary tendency of developing lophodont and hypodont teeth and increasing body size. The evolutionary sequence of Yuomys clearly correlates with the biochronology sequence of Asia (Gong et al., 2021). Apart from the earliest species, Yuomys huheboerhensis, later Yuomys species are significantly large compared to contemporary rodents, such as ctenodactylids and myomorph rodents. Y. huheboerhensis is the oldest-known and the most primitive Yuomys. It was discovered from the early middle Eocene Irdin Manha Formation at the Huheboerhe locality in the Huheboerhe-Nuhetingboerhe area of the Erlian Basin of Inner Mongolia (Li and Meng, 2015). Y. huheboerhensis is only slightly larger than contemporary ctenodactylids and shows a tendency of developing lophodont teeth. Yuomys yunnanensis was discovered from the middle Eocene at the Chake locality near Jianshui County of Yunnan Province. Mammalian fauna correlation suggests that the Chake locality is also Irdinmanhan in age (Huang and Zhang, 1990), probably slightly younger than the fossil site of Y. huheboerhensis. Yuomys weijingensis was discovered in the Ulan Shireh area of Inner Mongolia. The locality was originally reported as late Eocene, but recent revision of the stratigraphic and mammalian fauna correlations suggest that Y. weijingensis should be middle Eocene Irdinmanhan in age (Li and Meng, 2015; Li, 2019; Gong et al., 2021). Yuomys minggangensis was discovered from the middle Eocene at the Tuanshan locality near the Xinji Village of Minggang Town, Xinyang City of Henan Province (Wang and Zhou, 1982). The age of the Tuanshan locality is probably also Irdinmanhan. The type species of Yuomys, Yuomys cavioides, came from the late middle Eocene Sharamurunian at the Rencun locality of Mianchi County, Henan Province (Li, 1975). Yuomys cf. Y. cavioides was present at the Ula Usu locality of Inner Mongolia (Li, 1975; Gong et al., 2021), which is Sharamurunian in age. Yuomys records of similar age are Y. eleganes, Y. huangzhuangensis, Y. altunensis, and Y. magnus from a locality near Dalishu village of Wucheng Town, Tongbai County of Henan Province (Wang, 1978), the Langtougou locality near Huangzhuang village of Qufu City of Shandong Province (Shi, 1989), the Altyn Tagh of Xinjiang Province (Wang, 2017), and the Erden Obo locality of Nomogeng, Siziwangqi County of Inner Mongolia (Li, 2019). The youngest known Yuomys, Y. robustus, was discovered from the late Eocene at a locality near the Bujiamiaozi village, Lingwu City of Ningxia Province. A specimen from the Zhanglizi Gou locality near Chengliu village of Jiyuan County, Henan Province was recently referred to Y. robustus (Gong et al., 2021).
FIGURE 1. Locality of the Gemusi pull-apart basin and the distribution of Yuomys.
Here we report two new species of Yuomys discovered from southeast Qinghai-Tibetan Plateau, where Paleogene mammalian fossils are very rare. Although the two new Yuomys species are represented by three specimens only, their morphology clearly distinguishes them from other Yuomys and fits in the evolutionary sequence of Yuomys. The discovery therefore provides solid evidence for biochronology correlation and paleoenvironmental reconstruction of Southeastern Qinghai-Tibet Plateau.
2 Materials and methods
The Yuomys fossils reported here were discovered from the middle Eocene Gemusi Formation near Xueshuo Village of Litang County, Sichuan Province (Figure 1). The Gemusi Formation sedimentation was developed in the Gemusi pull-apart basin in the Litang Fault System (LTFS). The Gemusi Basin is about 150 km south of Litang city, near the headstream of the Shuiluo river, which is a branch of the Jinsha river. The average elevation of the Gemusi Basin is about 4200 m.
The Gemusi Formation is a set of brownish red-purplish fluvial and lacustrine sediments unconformably overlaying the black Triassic slates (Zong et al., 1996). The remaining thickness of the Gemusi Formation is over 300 m. The lower third of the Gemusi Formation includes conglomerates and coarse sandstones, imbedded with thin layers of mudstones. The middle and upper parts of the Gemusi Formation are dominated by mudstones and sandstone, imbedded with conglomerate layers. There is a thin layer of freshwater limestone in the middle part. There are two mammalian fossil layers. The lower fossil layer only includes some fossil fragments. The upper mammalian fossil layer is within a bed of siltstone enriched with calcareous nodules. The mammalian fossils from this layer include Anthracokeryx litangensis Bothriodon sp., Sianodon sp., Caenolophus proficiens, Brontotheriidae gen. & sp. indet., and the new Yuomys species reported here.
The dental morphology terminology used for description and comparison (Figure 2) was modified from Marivaux et al. (2019). Maps were generated at the Conservation Biology Institute Data Basin online mapping system (https://databasin.org/datasets/366a1bef53344c02bcd7d7611d5f61f7/).
FIGURE 2. Dental terminology used for description and comparison.
3 Systematic paleontology
Class Mammalia Linnaeus, (1758). Order Rodentia Bowdich, (1821). Suborder Hystricomorpha Brandt. (1855). Infraorder Hystricognathi Tullberg, 1899. Family Yuomyidae Dawson et al. (1984). Genus Yuomys Li, 1975. Yuomys dawai nov. sp. Ni and Li. LSID urn:lsid:zoobank.org:act:7E3D50A6-A92E-4205-B7C2-A8AF0513A8F9. (Figure 3, Table 1).
FIGURE 3. New Yuomys from the Gemusi pull-apart basin. (A–C), Yuomys dawai sp. nov., IVPP V 31415, holotype, in occlusal, lingual, and buccal views; (D–F), Yuomys gemuensis sp. nov., IVPP V 31417, in occlusal, lingual, and buccal views; (G–I), Y. gemuensis sp. nov., IVPP V 31416, holotype, in occlusal, lingual, and buccal views.
TABLE 1. Measurements of Yuomys jaws discovered from the Gemusi Basin (in mm).
Holotype—Specimen IVPP V 31,415, a left lower jaw fragment preserving dp4, m1, and m2.
Type locality—Locality GMS20201010LQ02 (29° 21′ 28.628″N, 100° 28′ 9.665″E), near Xueshuo village, Gemusi Basin, Litang County, Sichuan Province (Figure 1).
Referred specimen—The holotype only.
Age—Early middle Eocene, early Irdinmanhan of Asian Land Mammal Ages, about 49–45 Ma.
Etymology—The species name is dedicated to Dr. Jian’an Dawa, who is a doctor in the Community Hospital at the Xueshuo Village. Dr. Jian’an helped us in the field.
Diagnosis—Small Yuomys, brachydont, weakly lophodont. Dp4 mesial cingulid strong, preprotolophid, and postprotolophid enclosing trigonid basin; Dp4-m2 ectolophid oblique, joining the protoconid near buccal side, talonid basin and hyposinusid broad, mesoconid present, mesial arm of hypoconid long; dp4-m1 hypoconulid larger and more projecting than hypoconid; m1 mesolophid present.
Description—Only the holotype is available for description. The jaw preserves a part of the incisor, dp4, m1, and m2. The mental foramen is small and located at a point mesial to the dp4. The inferior masseter ridge is strong. It starts from the lateral side of the m1 and extends inferiorly and posteriorly, and entirely lateral to the incisor alveolar. The inferior masseter ridge extends to the angular process. Origin of the angular process distinctly buccal to the plane of the incisor alveolus is traditionally defined as hystricognathous jaw (Tullberg, 1899). The ventral side of the incisor has a weak longitudinal enamel stripe.
The buccal side of the check teeth is higher than the lingual size. The overall crown height is low. The dp4 is smaller than the m1 and m2. Its trigonid includes two main cusps, protoconid and metaconid. The two cusps are equal in size, but the metaconid is more mesially positioned. The preprotolophid is short. The buccal and lingual parts of the preprotolophid form a V-shaped notch. The postprotolophid connects the metaconid. The preprotolophid and postprotolophid enclose the trigonid basin. Mesial to the protoconid and metaconid, the mesial cingulid is strong. The dp4 talonid is wider than the trigonid. The talonid basin is broad. The hypoconid is mesial-distally compressed. The entoconid is smoothly fused with the hypolophid. The ectolophid is thin and oblique. It connects the protoconid near the buccal side. A small mesoconid is present in the middle of the ectolophid. The hypolophid connects the ectolophid at a position mesial to the hypoconid. A short mesial arm of the hypoconid is present. The hypoconulid is larger than the hypoconid and strongly posterior projecting. The hyposinusid is large and deep. A fovea is present buccal and distal to the hypoconid-hypoconulid junction.
The m1 is similar to the dp4, but without mesial cingulid. The preprotolophid is high. The postprotolophid is short. It reaches the metaconid but does not close the trigonid basin completely. The talonid basin is even broader. A weak mesolophid is present. The hypoconulid is even more distally projecting than in the dp4. The hyposinusid almost as broad as the talonid basin.
The m2 is much larger than the m1. Its metaconid is higher and more mesially positioned than the protoconid. The preprotolophid is fused with the metaconid and is relatively higher and stronger than in the m1. The postprotolophid of the m2 is short and does not connect the metaconid. As a result, the distal side of the trigonid is open to the talonid. The talonid is slightly wider than the trigonid. The talonid basin is broad and shallow. The ectolophid is thin and oblique, meeting the protoconid near the buccal margin, as in the dp4 and m1. The mesoconid is weak but visible. There is no mesolophid in the talonid basin. The hypoconid is more mesial-distally compressed than in the dp4 and m1. The mesial arm of the hypoconid is long. The entoconid and hypolophid are fused into a curved ridge. The middle part of the hypolophid is swollen, forming a small cusp. The hypoconulid is smaller and lower than the hypoconid. The hyposinusid is as broad as that of the m1.
Comparison—Yuomys huheboerhensis is smaller than all other Yuomys. It is characterized by round and low cusps and a relatively square occlusal surface of lower molars. Different from Y. dawai, protoconid in Y. huheboerhensis has a stronger and higher but relatively shorter buccal part of the preprotolophid and a relatively shorter and weaker postprotolophid. This ridge runs towards the metaconid but does not join the latter cusp. The metaconid of Y. huheboerhensis is more mesial-distally compressed. Its buccal part is transformed into the lingual part of the preprotolophid. The buccal and lingual parts of preprotolophid are separated by a shallow notch. In Y. huheboerhensis, the lingual preprotolophid is much longer than the buccal preprotolophid. In Y. dawai, the metaconid is more conical, and the two parts of the preprotolophid are equally developed. The postprotolophid in Y. dawai runs more transversely and joins the base of the metaconid. Y. huheboerhensis lacks the mesial cingulid. The hypoconid in Y. huheboerhensis is more distal-lingually expanding. In the m1 of Y. huheboerhensis, the distal-lingual part of hypoconid is almost fused with the hypoconulid, which is more buccally positioned. There is a sulcus separating the distal-buccal parts of hypoconulid and hypoconid. In Y. dawai, the hypoconid is more conical and widely separated from the similarly conical hypoconulid. A longer ridge than that in Y. huheboerhensis connects the tips of hypoconid and hypoconulid. The hypoconulid in Y. dawai projects distally and is positioned near the middle line. The ectolophid in Y. huheboerhensis is short and straight, while it is long and oblique in Y. dawai. The mesoconid in Y. huheboerhensis is very weak, present as a small swelling on the ectolophid. In Y. dawai, the mesoconid is large. In both Y. huheboerhensis and Y. dawai, the entoconid and hypolophid are fused together. In Y. huheboerhensis, the hypolophid is low, and has a weaker connection at the mesial arm of the hypoconid. In Y. dawai, the hypolophid is higher and stronger, connecting the distal lingual part of the ectolophid. The talonid basin and ectosinusid buccal to the ectolophid are broader in Y. dawai than in Y. huheboerhensis.
Yuomys yunnanensis includes a jaw preserving the dp4-m2. The specimen is much larger and has higher crown and stronger cristids than Y. dawai. The dp4 of Y. yunnanensis has a parastylid and a weak protostylid, two small cusps mesial to the metaconid and protoconid, respectively, but lacks the mesial cingulid. The hypoconulid in Y. yunnanensis is less projecting and more buccally positioned than in Y. dawai. The buccal end of the hypolophid in Y. yunnanensis has a distal turn, which makes the lophid joining the distolophid at the junction between hypoconid and hypoconulid. As a result, the hyposinusid enclosed by the hypolophid and distolophid is much narrower than in Y. dawai. In Y. dawai, the hypolophid joins the ectolophid at a place mesial to the hypoconid. The m1-2 of Y. yunnanensis have squarer occlusal surfaces compared with those of Y. dawai. In Y. yunnanensis, the preprotolophid is proportionally much higher than that in Y. dawai. The m1 postprotolophid in Y. yunnanensis runs more distally, therefore the distal side of the trigonid is open. In Y. dawai, the m1 postprotolophid extends to the metaconid and closes the trigonid. The ectolophid in Y. yunnanensis extends to the tip of metaconid, completely separating the talonid basin and the ectosinusid. The mesolophid and mesoconid are absent. In Y. dawai, the ectolophid joins the middle part of the metaconid. The hypolophid in Y. yunnanensis joins the ectolophid near the hypoconid, while in Y. dawai, the junction is more mesially positioned. In Y. yunnanensis, the hyposinusid between the hypolophid and distolophid is narrower than in Y. dawai. The hypoconulid in Y. dawai is more projecting than in Y. yunnanensis.
The Irdinmanhan Yuomys weijingensis is probably of similar age to Y. yunnanensis. Unfortunately, the specimens of this species were all lost. Available figures and description of the species show that it is less lophodont and about the size of Y. cavioides but with more conical cusps.
Yuomys minggangensis includes a jaw fragment preserving the p4-m1. It is much larger than Y. dawai, has a squarer occlusal surface, and shows a strong unilateral hypsodonty. In Y. minggangensis, the buccal cusps (protoconid and hypoconid) are much larger than the lingual cusps (metaconid and entoconid). The preprotolophid is higher and forms a stronger ridge than in Y. dawai. The postprotolophid in Y. minggangensis is short and does not close the trigonid. The ectolophid is straighter and shorter than in Y. dawai, resulting in a deeper and narrower ectosinusid. The talonid basin in Y. minggangensis is narrower than in Y. dawai. The mesoconid and mesolophid is absent in Y. minggangensis. The hypolophid is proportionally weaker and joins the joint point between ectolophid and hypoconid. The hypoconulid is less projecting, and the hyposinusid between the hypolophid and distolophid is narrower than in Y. dawai.
Yuomys eleganes is represented by a pair of lower jaws and some postcranial fragments. Y. eleganes is larger than Y. dawai. The occlusal surface of Y. elegans is squarer than in Y. dawai. Like in other Yuomys, the preprotolophid is higher and postprotolophid is shorter in Y. eleganes than in Y. dawai. The ectolophid in Y. eleganes is straighter and shorter. The mesoconid and mesolophid are absent. The talonid basin is narrower than in Y. dawai. Being similar to Y. dawai, the hypolophid joins the distal part of the ectolophid in Y. eleganes. The hypoconulid in Y. elegans is present as a swelling of the distolophid. The cusp is not separated from the hypoconid but present as a lingual extension of the hypoconid arm.
Yuomys cavioides is represented by a pair of almost complete lower jaws and two skull fragments preserving the complete upper dentation. Y. cavioides is much larger and has higher crown and stronger lophid than Y. dawai. In the m1-2 of Y. cavioides, the metaconid forms a high lophid and is fused with the buccal part of the preprotolophid. In Y. dawai, the metaconid is more conical. The buccal and lingual parts of the preprotolophid are weaker and separated by a notch. The postprotolophid in Y. dawai joins the metaconid. In Y. cavioides, the postprotolophid is present as a distal-lingual spur of the protoconid. The ectolophid is a high ridge connecting the tips of hypoconid and protoconid in Y. cavioides. The ectosinusid and talonid basin are all narrow and deep. No mesolophid and mesoconid are present. In Y. dawai, the ectolophid is low and does not extend to the tip of the protoconid. The ectosinusid and talonid basin are broad. A weak mesoconid and a weak mesolophid are present. The hypolophid in Y. cavioides is much higher and thicker than that in Y. dawai. The hyposinusid enclosed by hypolophid and distolophid is broader and deeper in Y. dawai.
Yuomys magnus is much larger than Y. dawai. The lower m2s of the two species are the available teeth for comparison. Both have a relatively long occlusal surface. Y. magnus has higher tooth crown and stronger lophids. Its hypolophid is stronger but does not connect the ectolophid or hypoconid. The hypoconulid of Y. magnus is more conical than in Y. dawai.
Yuomys robustus and Yuomys huangzhuangensis are known from upper teeth only. They are much larger than Y. dawai and have higher tooth crown than Y. dawai does.
Yuomys gemuensis nov. sp. Ni and Li. LSID urn:lsid:zoobank.org:act:8670E4D0-3DA8-4F67-A306-EA93CF785AD1. (Figure 3, Table 1).
Holotype—Specimen IVPP V 31416, a right lower jaw fragment preserving dp4 and m1-3.
Type locality—Locality GMS20201011SJS01 (29° 21′ 22.000″N, 100° 28′ 25.000″E), near Xueshuo village, Gemusi Basin, Litang County, Sichuan Province (Figure 1).
Referred specimen—IVPP V 31417, a right lower jaw fragment preserving incisor, dp4 and partially erupted m1. From Locality GMS20201011LQ02 (29° 20′ 43.955″N, 100° 28′ 35.899″E), near the Xueshuo Village, Gemusi Basin, Litang County, Sichuan Province (Figure 1).
Age—Early middle Eocene, early Irdinmanhan of Asian Land Mammal Ages, about 49–45 Ma.
Etymology—The specific epithet is from Gemusi, the name of a local lama temple, and the name of the Gemusi Basin.
Diagnosis—Brachydont; Dp4 present mesial and buccal cingulid, mesial metastylid large; Dp4-m2 present buccal arm of hypoconulid; hypolophid thin but well-developed, hypoconulid distally projecting and larger than hypoconid, distal buccal sulcus between hypoconid and hypoconulid deep; m1-3 ectolophid straight, attaching to protoconid distal wall, ectosinusid deep and narrow, hyposinusid broad.
Description—The holotype is a right lower jaw fragment. The preserved inferior masseter ridge root is strong and positioned buccal to the plane of the incisor. The ascending ramus of mandible is vertical and shields the posterior part of the m3. The specimen referred to is a jaw fragment preserving incisor, dp4, and m1. The diastema is thin and long. The mental foramen is mesial to the dp4 and near the incisor. The incisor is gently curved. The enamel is thin. There is a weak longitudinal enamel strip along the ventral side of the incisor. The dp4 is fully erupted but has no wear facet. The m1 is fully developed but still in eruption.
The cheek teeth are brachydont, and weakly lophodont. The buccal side of the cheek teeth is higher than the lingual side. The dp4 has an oval occlusal shape. Its trigonid is narrower than the talonid. The metaconid is buccal-lingually compressed. The tip of metaconid is higher and more mesially positioned than the protoconid. The distal arm of the metaconid is strong. The buccal and lingual parts of the preprotolophid is separated by a deep V-shaped notch. The postprotolophid is short and does not connect the metaconid, therefore the distal wall of the trigonid (postvallid) is open. The mesial cingulid is strong. It extends from the mesial side of the metaconid to the protoconid and becomes a weak buccal cingulid and ends at the mesial side of the hypoconid. A small parastylid is present at the lingual end of the mesial cingulid. There is also an incipient protostylid mesial to the protoconid. The talonid has a broad basin. Its lingual border has a low rim. The hypoconid is conical. Its mesial arm is very short. The entoconid is also conical, but its buccal side is fused into the hypolophid. The hypolophid buccally joins the distal arm of the hypoconid, instead of ectolophid. The ectolophid is thin and oblique. Its mesial part ends in the distobuccal side of the protoconid but does not extends to the tip of the protoconid. The ectosinusid is deep and narrow. The hypoconulid is large and higher than the hypoconid. A strong and blunt buccal arm of hypoconulid is present. There is a deep and broad sulcus enclosed by the hypoconid, hypoconulid, and the buccal arm of the hypoconulid. The hyposinusid is broad.
The m1 has a rectangular occlusal shape. The trigonid and talonid are similar in width. The protoconid is robust and conical. The metaconid is mesial-distally compressed and fused with the preprotolophid. The postprotolophid is short and does not connect the metaconid. The talonid basin is broad. The hypoconid is mesial-distally compressed. Its mesial arm is very short. The entoconid is also mesial-distally compressed. It is fully fused with the hypolophid. The entoconid, hypolophid, and hypoconid form a transverse ridge. The ectolophid is straight. It connects the distal wall of the protoconid but does not extend to the protoconid tip. The ectosinusid between the protoconid and hypoconid is deep and narrow. The hypoconulid is much larger than the hypoconid. The buccal arm of the hypoconulid is strong. The sulcus buccal-distal to the joint of hypoconid and hypoconulid is relatively shallower and narrower than that of dp4. The m2 is smaller than the m1 and has a squarer occlusal shape than the m1. The cusp shape and ridge arrangement are similar to those of the m1. Because the tooth is relatively short, the talonid basin, ectosinusid, and hyposinusid of the m2 are all narrower than those of the m1. Between the metaconid and entoconid, the talonid basin border has a thicker rim and develops an incipient metastylid. The ectosinusid has a low buccal rim. There is an incipient hypostylid on the rim. The m3 is much larger than the m1 and m2. The m3 talonid is narrower than the trigonid, and the distal side of the tooth is rounded. Different from the m1 and m2, the protoconid and hypoconid of the m3 are more conical, and the ridges are thicker. The hypoconulid is less projecting and smaller than the hypoconid. There is a cusp-like swelling on the hypolophid. The metastylid and hypostylid are large.
Comparison—Yuomys gemuensis is more similar to Y. yunnanensis than to other Yuomys species. The dp4 of Y. gemuensis has a mesial cingulid and a buccal cingulid. The two cingulids are absent in Y. yunnanensis. The paratylid in Y. gemuensis is relatively smaller than that in Y. yunnanensis, and the protostylid is present as a nodule on the mesial cingulid. The hypoconid in Y. yunnanensis is more buccally expanded than in Y. gemuensis. The hypoconulid is less distally projecting. As a result, the distal valley enclosed by hypoconulid and hypolophid is narrower than in Y. gemuensis. A buccal arm rises from the buccal side of the hypoconulid in Y. gemuensis. The m1s of Y. gemuensis and Y. yunnanensis are similar in size and morphology. Slightly different from Y. gemuensis, the hypolophid in Y. yunnanensis is weaker, and the distal buccal sulcus between the hypoconid and hypoconulid is shallower. The m2 of Y. yunnanensis is proportionally larger than the m2 of Y. gemuensis. As in the m1, the m2 hypolophid in Y. yunnanensis is weaker and the distal buccal sulcus between the hypoconid and hypoconulid is shallower than in Y. gemuensis. The ectolophid extends to the tip of protoconid in Y. yunnanensis. In Y. gemuensis, the ectolophid does not extend to the tip of protoconid.
Yuomys huheboerhensis is much smaller and has more conical cusps than Y. gemuensis. The lingual and buccal preprotolophid of molars are separated by a notch in Y. huheboerhensis. In Y. gemuensis, the lingual and buccal preprotolophid are fused into a strong ridge connecting the protoconid and metaconid. As in Y. gemuensis, the ectolophid in Y. huheboerhensis does not extend to the tip of protoconid. A rudimentary mesoconid is present in some individuals in Y. huheboerhensis, but it is totally absent in Y. gemuensis. The talonid basin in Y. huheboerhensis is relatively broader than in Y. gemuensis. The hypolophid in Y. huheboerhensis is very weak. Its buccal end does not join the ectolophid, or has only a weak connection. Similar to Y. gemuensis, but different from most other Yuomys, the hypoconulid is more buccally positioned, and usually has a deep distal buccal notch separating it from the hypoconid in the m1-2. Different from Y. gemuensis, the m1-2 hypoconulid in Y. huheboerhensis barely projects above the hypoconid.
Yuomys minggangensis is much bigger than Y. gemuensis and shows stronger unilateral hyposodonty. The protoconid, metaconid, and hypoconid of Y. minggangensis are more conical and robust than those of Y. gemuensis. The entoconid and the hypolophid of Y. minggangensis are relatively weaker. The ectolophid in Y. minggangensis is short and straight, proportionally stronger than in Y. gemuensis. The hypoconulid of the m1 in Y. minggangensis is smaller than the hypoconid, whereas in Y. gemuensis, the hypoconulid is larger than hypoconid. The distal buccal side of the hypoconulid in Y. minggangensis lacks a buccal arm as in Y. gemuensis. In Y. minggangensis, the hyposinusid enclosed by the distolophid and hypolophid is also proportionally smaller.
Yuomys eleganes is of roughly the same size as Y. gemuensis. The cusps and ridges of both taxa are also equally developed. The m1-2 of Y. eleganes are deeply worn. Detailed morphology is not available for comparison. However, it is obvious that the hypolophid in Y. eleganes is more mesially positioned, and the talonid basin is narrower than in Y. gemuensis. The hypoconulid in Y. eleganes is probably fused with the hypoconid and present as an extension of the distal arm of hypoconid. No trace of sulcus is present between the hypoconid and hypoconulid. A small hypostylid in the ectosinusid mesial to the hypoconid is present in both taxa. The m3 of Y. gemuensis is of slightly bigger size. In both taxa, the preprotolophid is high, and the postprotolophid is a short spur. The m3 hypolophid connects the middle of the ectolophid in Y. eleganes, whereas the lophid joins the ectolophid near hypoconid in Y. gemuensis. As a result, the m3 talonid basin in Y. eleganes is narrower. There is a small metastylid mesial to the entoconids on the lingual edge of the talonid basin in Y. eleganes. This small cusp almost closes the lingual side of the talonid basin. Similarly in Y. gemuensis, the lingual side of the talonid basis has a low and blunt rim, and the metastylid is also present. In the ectosinusid and mesial to the hypoconid, there is a small hypostylid in both taxa. The m3 hypoconulid in Y. eleganes is present as a swelling of the hypoconid distal lingual arm (distal lophid). There is no sulcus defining the border between hypoconid and hypoconulid, and probably no projection from the arm. In Y. gemuensis, the hypoconulid clearly projects above the distal lophid and is separated from the hypoconid by a shallow sulcus distal lingual to the junction between hypoconid and hypoconulid.
Yuomys cavioides is larger, more hypsodont and lophodont than Y. gemuensis. The postprotolophid is longer in Y. cavioides than in Y. gemuensis. The m3 postprotolophid in Y. cavioides is particularly longer, which reaches the lingual side of the hypolophid. The m1-3 ectolophids in Y. cavioides all extend to the tips of protoconid. The hypolophids are more mesially positioned and proportionally higher than in Y. gemuensis. The talonid basin and ectosinusid in Y. cavioides are narrower and deeper. The small hypostylid mesial to the hypoconid as that in Y. gemuensis is absent in Y. cavioides. A small metastylid mesial to the entoconid along the lingual tooth border of the m2-3 is present in Y. cavioides but is weaker in Y. gemuensis. The hypoconulid of the m1-2 is slightly smaller than hypoconid in Y. cavioides, whereas it is bigger than hypoconid in Y. gemuensis. The sulcus distal buccal to the junction between hypoconid and hypoconulid of the m1-2 in Y. gemuensis is deeper than that in Y. cavioides. The buccal ridge-like arm from hypoconulid is present in the m1-2 of Y. gemuensis but absent in Y. cavioides. The lingual extension of the distolophid is longer in Y. gemuensis than in Y. cavioides. The m3 hypoconulids and distolophids are equally developed in both taxa. Both have a shallow sulcus distal buccal to the junction between hypoconid and hypoconulid. This sulcus is absent in other Yuomys.
Yuomys magnus is larger than Y. gemuensis. The tooth crown of Y. magnus is higher than Y. gemuensis. The m2-3 ectolophid of Y. magnus is oblique and connects the protoconid near the buccal side. As a result, the m2-3 ectosinusid of Y. magnus is shallower and oblique. The m2 hypolophid of Y. magnus does not connect the ectolophid or hypoconid. The m3 hypolophid of Y. magnus has a weaker connection to the ectolophid than in Y. gemuensis. In Y. gemuensis, the m2 hypoconulid has a buccal arm that forms a transverse ridge from hypoconulid. The sulcus between this buccal arm and hypoconid is deep. In Y. magnus, the m2 hypoconid is conical and lacks a buccal extension.
Yuomys robustus is known from upper teeth only. It is much larger than Y. gemuensis and has higher tooth crown. Yuomys huangzhuangensis is also known from the upper teeth only. Its size matches that of Y. gemuensis. Relatively thicker ridges of Y. huangzhuangensis upper teeth suggest that the lower teeth of this species should also have thicker ridges than Y. gemuensis.
4 Discussion
Huchon et al. (2000) defined “Ctenohystrica” as a suborder of Rodentia based on molecular evidence. Initially Ctenohystrica was defined as a crown-group that includes the least-inclusive clade of all extant family Ctenodactylidae and infraorder Hystricognathi. Marivaux et al. (2004) and Flynn et al. (2019) redefined Ctenohystrica as a more inclusive group that includes stem and extant Hystricognathi, stem and extant sciurognathous Ctenodactylidae, and all extant or extinct groups more closely related to them than to other sciurognathous rodents. Blanga-Kanfi et al. (2009) revised the rodent phylogeny based on the combined nucleotide datasets and supported the monophyly of Ctenohystrica. It is not difficult to see that the main connotation of Ctenohystrica has no difference with the traditional Hystricomorpha. Here we follow the systematic of Wilson and Reeder (2005) by using suborder Hystricomorpha. Yuomys are moderately diverse Eocene rodents. The taxonomy and distribution of Yuomys have been revised recently (Gong et al., 2021). Previously, Yuomys was considered as a rodent with a hystricomorphous skull but with a hystricognathous jaw. For this reason, Yuomys was traditionally assigned in the “trash bin” high level taxon Ctenodactyloidea. Our re-observation on the lower jaw of the type specimen of Yuomys cavioides revealed that this specimen is actually hystricognathous (Figure 4). In living hystricognaths, the origin of the angular process is distinctly lateral to the plane of the incisor alveolus. The inferior margin of the angular process is generally wide, and the reflexa part of lateral masseter passes around the ventral surface of the angular process to insert on the medial side of the angular process (Tullberg, 1899; Wood, 1985). The angular process of the type specimen of Y. cavioides is well preserved. The plane of angular process is clearly lateral to the plane of the incisive alveolus (Figure 4). The ventral edge of the angular process is widened (Figure 4) in a form generally present in living hystricognaths. We therefore categorized Yuomys and Yuomyidae as the infraorder Hystricognathi.
FIGURE 4. The low jaw of the type specimen of Yuomys cavioides (IVPP V 4796.1-2), showing the hystricognathous form. (A), ventral view; (B), occlusal view: (C), yellow shadow indicating the plane of the incisive alveolus, red shadow indicating the plane of the angular process being distinctly lateral to the plane of the incisive alveolus, green shadow indicating expanded ventral edge of the angular process; (D), virtual section of the right half mandible in medial view, yellow shadow indicting the posterior extension of the incisor, red shadow indicating the angular process.
Yuomys dawai is much smaller with a lower tooth crown than other Yuomys species except Yuomys huheboerhensis. Compared to Y. huheboerhensis, Y. dawai shows more typical Yuomys features, suggesting that the sediments bearing Y. dawai is probably younger than that of Y. huheboerhensis, but it is still older than other Yuomys. Yuomys gemuensis and Yuomys yunnanensis from the Chake pull-apart basin closely resemble each other and both show similar development of tooth crown height and ridges. The similar evolutionary grade shared by these two species suggests that the fossil layers bearing the two Yuomys have the same mammalian age: early Irdinmanhan of Asian Land Mammal Age (about 49–45 Ma).
It has been demonstrated that about 1300–2500 km of the northward convergence between the Indian plate with the continent of Eurasia caused widespread crustal deformation, including mountain building, plate shortening, and plateau uplifting (Molnar and Stock, 2009; Copley et al., 2010; Cande and Stegman, 2011; van Hinsbergen et al., 2011; Tong et al., 2015; Yao et al., 2015; Ding et al., 2017; Wang and Shen, 2020). The most intriguing feature of this widespread crustal deformation is reflected by clockwise rotation of southeastern Qinghai-Tibet Plateau around the Eastern Himalayan Syntaxis (EHS) and lateral escape of crustal materials on the southeastern edge of the plateau relative to the rigid South China Block (Yin and Harrison, 2000; Tapponnier et al., 2001; Molnar and Stock, 2009; Copley et al., 2010; Cande and Stegman, 2011; van Hinsbergen et al., 2011; Tong et al., 2015). One theory is that the outward expansion along major strike-slip faults (such as Xianshuihe-Xiaojiang Fault, Litang Fault System, Three Rivers Faults, and Red River Fault) and clockwise strike-slip processes around EHS occur at the mantle scale (Tapponnier et al., 2001; Zhang et al., 2021). The development of the Cenozoic extensional intermountain basins in the southeast margin of Qinghai-Tibetan Plateau is kinematically linked with the strike-slip faults, and the sedimentation in these basins can provide important age constraints for the timing of fault development and orogenic processes (Li et al., 2015; Li et al., 2020).
The southeastern margin of Qinghai-Tibet Plateau was one of the most important accommodation zones during the India-Eurasia collision. The temporal and spatial evolution of the zone is tightly correlated with the crustal deformation and high topography evolution of Qinghai-Tibet Plateau (Figure 5). This accommodation zone comprises the Shan Thai Block (STB), Indochina Block (ICB), and Chuandian Terrane (CDT), which consists of fragments from the western part of South China Block (SCB) and the southern part of Songpan Ganzi fold belt (Wang et al., 1998; Wang et al., 2014; Tong et al., 2015). The CDT is separated from the relatively stable SCB in the north and northeast by the Xianshuihe-Xiaojiang Fault (XSH-XJF), and from the STB and ICB in the south and southwest by the Ailao Shan-Red River Fault (ASRRF) (Wang et al., 1998; Tong et al., 2015; Li et al., 2017; Li et al., 2020).
FIGURE 5. Chuandian Terrane and the major faults in the accommodation zone in the southeastern margin of Qinghai-Tibet Plateau. Hollow arrows indicating modern GPS velocity field (based on Wang and Shen 2020).
The Yuomys fossils reported here were discovered from the Gemusi pull-apart basin, which was formed within the northwest striking LTFS. This fault system is located between the XSH-XJF to the north and ASRRF to the south. Its activity is controlled by the two latter faults (Chevalier et al., 2016). The Yuomys fossil from the Chake was discovered from a locality in the Chake pull-apart basin, which was formed within the southern end of the XSH-XJF. Similarities shared by the Yuomys from Gemusi and Chake suggest that they lived during the same geological epoch and similar adaptive environment, and consequently suggest that the Gemusi Basin and Chake Basin were formed roughly in the same period (about 49–45 Ma).
In a recent study, the mammalian fossil localities in the Gemusi Basin, which were reported in Zong et al. (1996), were wrongly pinned, and the fossil layer of Gemusi Formation was wrongly correlated to the upper part of the Relu Formation of the nearby Relu Basin (He et al., 2022). Our field tracing and previous stratigraphic correlations (Chen et al., 1983; Guo, 1986; Zong et al., 1996) indicate that the mammalian fossil layer of the Gemusi Formation should be correlated with the lower part of the Relu Formation (equivalent to the Changzong Formation in He et al., 2022), below the plant fossil strata of the Relu Formation. U-Pb dating of the zircons from the volcanic tuffs imbedded in the plant fossil layers of the Relu Formation showed an age of 42–40 Ma, and U-Pd dating of the zircons from the sandstone of the lower part of the Relu Formation indicated that the maximum depositional age is about 50 Ma (He et al., 2022). These dating results are consistent with our biochronological estimation.
Present-day CDT is characterized by clockwise rotation around EHS as revealed by GPS velocities (Figure 5, Zhang et al., 2004; Wang and Shen, 2020; Xu et al., 2022). A maximum shear strain rate of 40–60 nanostrain/yr is found along the XSH-XJF (Wang and Shen, 2020). The initiation timing of the strike-slip movement of XSH-XJF and ASRRF and the formation of the CDT is controversial. It was suggested that the CDT remained relatively stable and did not begin rotational extrusion movement before 17 Ma (Tong et al., 2015), while some other research suggested that the crustal deformation of the CDT began at ∼ 35 Ma (Li et al., 2020). The Yuomys fossils from CDT constrain the timing of sedimentation within the Gemusi pull-apart basin and Chake pull-apart basin. Our paleontological evidence suggests that the initiation of CDT crustal movement could be earlier than 49 Ma.
The occurrence of Yuomys in CDT may suggest that the area had a lowland tropical environment during the middle Eocene. It is known that Yuomys occurred with small-sized stem anthropoid and tarsiiform primates, in, for example, the Mianchi-Yuanqu Basin in Henan Province and Erlian Basin in Inner Mongolia (Beard, 1998; Beard and Wang, 2004; Ni, 2010; Wang et al., 2018). Living and fossilized small primates are known to occur only in lowland tropical forest or jungle environments (Fleagle, 2013; Li and Ni, 2016; Ni et al., 2016). Plant fossils from the nearby Relu Formation indicate a lowland tropical environment (Chen et al., 1983; Guo, 1986; Su et al., 2009; He et al., 2022). It is therefore likely that the uplift of CDT and the strike-slip movement of XSH-XJF and ASRRF were not synchronous.
Data availability statement
The original contributions presented in the study are included in the article/supplementary material, further inquiries can be directed to the corresponding authors.
Author contributions
XN analyzed the data and wrote the manuscript. QL analyzed the data and edited the manuscript. TD analyzed the data. LZ, HG, and CQ CT-scanned the fossil. JS, FS, and SF collected data.
Funding
This project was supported by the Second Tibetan Plateau Scientific Expedition and Research Program (2019QZKK705), the National Natural Science Foundation of China (41988101, 41888101, 41625005), the Strategic Priority Research Program of Chinese Academy of Sciences (CAS XDB26030300, XDA20070203, XDA19050100).
Acknowledgments
We thank T. Stidham for comments and English-language editing. We thank Qian Li, Lawrence J. Flynn, and Olivier Maridet for comments and discussion.
Conflict of interest
The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
Publisher’s note
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Keywords: Yuomys, Chuandian terrane, accommodation zone, strike-slip movement, plateau uplifting
Citation: Ni X, Li Q, Deng T, Zhang L, Gong H, Qin C, Shi J, Shi F and Fu S (2023) New Yuomys rodents from southeastern Qinghai-Tibet Plateau indicate low elevation during the Middle Eocene. Front. Earth Sci. 10:1018675. doi: 10.3389/feart.2022.1018675
Received: 13 August 2022; Accepted: 25 November 2022;
Published: 23 January 2023.
Edited by:
Lucja A. Fostowicz-Frelik, Institute of Paleobiology (PAN), PolandReviewed by:
Olivier Maridet, JURASSICA Museum, SwitzerlandLawrence John Flynn, Harvard University, United States
Copyright © 2023 Ni, Li, Deng, Zhang, Gong, Qin, Shi, Shi and Fu. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
*Correspondence: Xijun Ni, nixijun@ivpp.ac.cn; Qiang Li, liqiang@ivpp.ac.cn