A revision of Anhuichelys Yeh, 1979, the earliest known stem Testudinidae (Testudines: Cryptodira) from the Paleocene of China

TONG Hai-YanLI LuLI Ding-ShengCHEN Li-MinLI TaoYU Shu-HuaYU Guo-ShengCHENG Xiao-QingDI Ye-LiJulien CLAUDE

(1Palaeontological Research and Education Centre,Mahasarakham UniversityKantarawichai, Mahasarakham 44150, Thailand htong09@yahoo.fr)

(2Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences,Institute of Vertebrate Paleontology and Paleoanthropology,Chinese Academy of ScienceBeijing 100044, China)

(3Museum of Qianshan CountyQianshan 246300, Anhui, China)

(4Tianzhushan Global GeoparkQianshan 246300, Anhui, China)

(5Shanghai Natural History MuseumShanghai 200041, China)

(6Institut des Sciences de l’Evolution de MontpellierMontpellier Cedex 5, 34095, France)

A revision of Anhuichelys Yeh, 1979, the earliest known stem Testudinidae (Testudines: Cryptodira) from the Paleocene of China

TONG Hai-Yan1,2LI Lu2LI Ding-Sheng3CHEN Li-Min3LI Tao3YU Shu-Hua3YU Guo-Sheng4CHENG Xiao-Qing4DI Ye-Li5Julien CLAUDE6

(1Palaeontological Research and Education Centre,Mahasarakham UniversityKantarawichai, Mahasarakham 44150, Thailand htong09@yahoo.fr)

(2Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences,Institute of Vertebrate Paleontology and Paleoanthropology,Chinese Academy of ScienceBeijing 100044, China)

(3Museum of Qianshan CountyQianshan 246300, Anhui, China)

(4Tianzhushan Global GeoparkQianshan 246300, Anhui, China)

(5Shanghai Natural History MuseumShanghai 200041, China)

(6Institut des Sciences de l’Evolution de MontpellierMontpellier Cedex 5, 34095, France)

Our systematic revision ofAnhuichelysYeh, 1979, based on abundant new material from the Paleocene of Qianshan Basin, Anhui Province, China provides evidences for its assignment to the stem Testudinidae.Anhuichelyscontains three species in the Paleocene of Qianshan Basin:A. siaoshihensisYeh, 1979 from the Early Paleocene of wanghudun Formation,A. tsienshanensisYeh, 1979 from both wanghudun and Doumu formations andA. doumuensissp. nov. from the Middle Paleocene Doumu Formation.A. xinzhouensisChen, 1983 from the Paleocene of Xinzhou, Hubei Province is synonymized withA. tsienshanensis. Associated with a terrestrial vertebrate fauna,Anhuichelysis likely a land turtle and also the fi rst testudinoid to develop the hinge on the shell.

Qianshan Basin, China; Paleocene; turtle, Testudinidae

1 Introduction

In 1970-1971, the Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences (IVPP), has collected several turtle shells in the Paleocene deposits of the Qianshan Basin, Anhui Province, central-eastern China. On the basis of this material, Ye Xiangkui (Yeh, 1979a) erected the genusAnhuichelysand its two species:A. siaoshihensisandA. tsienshanensis. Yeh (1979a) assignedAnhuichelysto the family Emydidae, and consideredit as the oldest representative of that family. Brinkman and co-authors (2008) retained this classification, but noted that “Anhuichelysshares derived features of the carapace with the Testudinidae, and may be a sister-group to this family” (Brinkman et al., 2008:80). During the past decades, abundant additional specimens ofAnhuichelyshave been collected in the Qianshan Basin. The material, mainly consisting of shells, is housed in several museums in China. In this paper, we provide a systematic revision ofAnhuichelyswhich includes the type series of the known taxa and new material. The purpose of this study is to review the validity of the taxa and their phylogenetic relationships.

Fig. 1 Map showing the location of Qianshan Basin and turtle localities▲Anhuichelyssiaoshihensis(1. IVPP V 5598; 2. TZSGP QT2; 3. MQSC V 005); ■A. tsienshanesis(4. MQSC V 012; 5. MQSC V 023-2; 6. MQSC V 00133; 7. MQSC V 061; 8. TZSGP QT15); ◆A. doumuensis(9. IVPP V 5599; 10. MQSC V 009; 11. MQSC V 002; 12. MQSC V 065); ●Anhuichelyssp. (13. MQSC V 023-1; 14. MQSC V 011-2; 15. TZSGP QT19); Ar. Archean; E1d. Doumu Fm. (Middle Paleocene); E1w. wanghudun Fm. (Early Paleocene); K2w. wanghe Fm. (Late Cretaceous)

Qianshan Basin is located in the southwest part of Anhui Province, central-eastern China. According to Qiu et al. (1977), the redbeds in the Qianshan Basin are subdivided into three formations. They are, in ascending order, the Cretaceous wanghe Formation, and the Paleocene wanghudun and Doumu formations. The wanghudun Formation is further dividedinto the Lower, Middle and Upper members and Doumu Formation is further divided into the Lower and Upper members. Both wanghudun and Doumu formations are rich in vertebrate remains, and fossil mammals have been recorded from all members except the Middle Member of the wanghudun Formation. To date, more than fifty species of vertebrates have been reported, including reptiles, birds and mammals (Qiu et al., 1977; wang et al., 2016). Previously dated as Middle and Late Paleocene respectively (Qiu et al., 1977), the wanghudun and Doumu formations are now considered Early and Middle Paleocene in age, according to the recent correlation based on the mammalian faunas. For more geological and stratigraphical information see wang et al., 2016 (this volume).

Turtle remains have been collected from all members of the two Paleocene formations except the Middle Member of the wanghudun Formation. The specimens ofA. siaoshihensishave been collected from the Lower and Upper members of the wanghudun Formation;A. tsienshanensishas been collected from the Upper Member of the wanghudun and both members of the Doumu Formation; and the specimens ofA. doumuensishave been collected only from the Upper Member of the Doumu Formation (Fig. 1).

Institutional abbreviations AHM, Anhui Provincial Museum (Hefei, Anhui Province); HBGM, Hubei Geological Museum (wuhan); IVPP, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences (Beijing); MQSC, Museum of Qianshan County (Qianshan, Anhui Province); RGSTHB, Regional Geological Surveying Team of Hubei (Hubei Province); SHNHM, Shanghai Natural History Museum (Shanghai); TZSGP, Tianzhushan Global Geopark (Qianshan, Anhui Province).

2 Systematic paleontology

Type speciesA. siaoshihensisYeh, 1979.

Emended diagnosis Carapace oval and relatively high domed; wide nuchal; elongate hexagonal neurals with short anterolateral sides and a neural formula of 4＞6＞6＞6＞6＞6＞6＞6; alternate costals (costals 2, 4, and 6 with short medial end and expanded lateral end; while costals 3 and 5 with expanded medial end and short lateral end); narrow vertebrals, vaseshaped vertebral 1 with its anterior part restricted to the nuchal; well developed plastron with large and sub-rectangular anterior and posterior lobes; anterior rim of the plastron concave, extending up to or beyond the anterior margin of the carapace; epiplastra forming a pair of strong and upturned horn-shaped lateral processes; anal notch extremely shallow or absent; xiphiplastra expanded, with the hypoplastron/xiphiplastron suture straight and situated close to the base of the posterior lobe; intergular absent, femoral scute short at the midline.

Included speciesA.tsienshanensisYeh, 1979 andA.doumuensissp. nov.

Distribution Early-Middle Paleocene of Qianshan Basin, Anhui Province and Paleocene of Xinzhou, Hubei Province, China.

(Figs. 2-3)

Holotype IVPP V 5598 (Field number: 71080), a complete shell with articulated carapace and plastron.

Referred specimens TZSGP QT2 (150 m east to Zhangjiawu, Qianshan; Upper Member of wanghudun Fm.) and MQSC V 005 (Zhangchong, wufan, Huangpu; lower part of the Upper member of wanghudun Fm.).

Type locality and horizon Dinghuawu, Mao’an, Xiaoshi Town, Huaining County, Anhui Province, China; Lower Member of wanghudun Formation (Early Paleocene).

Fig. 2 Shell ofAnhuichelys siaoshihensis(IVPP V 5598, holotype) A-B. dorsal view; C-D. ventral view; E-F. left lateral view

Fig. 3 Shell ofAnhuichelys siaoshihensis(TZSGP QT2) A-B. dorsal view; C-D. ventral view; E-F. anterior view; G-H. left lateral view

Emended diagnosis A species ofAnhuichelys; different fromA. tsienshanensisin having a hinge between the epiplastra/entoplastron and hyoplastra; the entohyoplastral suture and epihyoplastral suture together forming a straight line situated posterior to the entoplastron; and the humeropectoral sulcus matching or close to the entohyoplastral and epihyoplastral sutures. It further differs fromA. tsienshanensisandA. doumuensisin having a long midline contact of the epiplastra; a half circle-shaped entoplastron; long gulars which extend onto the entoplastron; the humeropectoral sulcus matching the posterior margin of the entoplastron; a short pectoral scutes and a straight pectoroabdominal sulcus.

Distribution Early Paleocene (wanghudun Formation) of Qianshan Basin.

(Figs. 4-5, 6E-F)

SynonymyAnhuichelys xinzhouensisChen, 1983.

Holotype AHM V 71079-3 (Field number: 71079), anterior 4/5 of a shell with articulated carapace and plastron; the middle portion of the carapace is damaged, as well as the anterior part of the right bridge region of the plastron.

Paratype AHM V 71079-1, a shell exposed dorsally with worn surface so that the structure is obscure (from the type locality (Yeh, 1979a)).

Fig. 4 Shell ofAnhuichelys tsienshanensis(AHM V 71079-3, holotype) A. dorsal view; B-C. ventral view; D-E. anterior view

Fig. 5 Shell ofAnhuichelys tsienshanensis(TZSGP QT15) A-B. dorsal view; C-D. ventral view; E-F. anterior view; G-H. right lateral view

Referred specimens AHM V 71079-2, fragments of a carapace (from the type locality (Yeh, 1979a)); TZSGP QT15 (Xudawu, Qianshan; Lower Member of Doumu Fm.), MQSC V 001 (Yangxiaowu, wangling, Huangpu, Qianshan; Upper Member of Doumu Fm.), MQSC V 061 (Hanjiashanbao, Qipan Village, Pailou Township, Qianshan; Lower Member of Doumu Fm. or the base of the Upper Member of Doumu Fm.), MQSC V 023-2 (Jinshi Village, Qinglou Township, Qianshan; upper part of the Upper Member of wanghudun Fm. or Lower Member of Doumu Fm.), MQSC V 012 (hillside southeast of wangjiazha, Qianshan; Upper Member of wanghudun Fm.?), MQSC V 010 (South of Lianhuatang, Huangpu, Qianshan; Upper Memberof wanghudun Fm.?) and MQSC V 066 (Yangxiaowu, Huangpu, Qianshan; Upper Member of Doumu Fm.), RGSTHB V.H751, RGSTHB V.H753 and HBGM V.H752 (Zhaigang, Jiujie, Xinzhou County, Hubei Province), ten shells; IVPP V 23137, anterior portion of a plastron (Fujiashanzui, Qianshan; upper part of Upper Member of wanghudun Fm.).

Type locality and horizon Hanhuawu, Huangpu Township, Qianshan County, Anhui Province, China; Lower Member of Doumu Formation (Middle Paleocene).

Emended diagnosis A species ofAnhuichelys, different fromA. siaoshihensisandA. doumuensisin the absence of a hinge at the base of the anterior lobe of the plastron; in having the epihyoplastral suture situated lateral to entoplastron, the humeropectoral sulcus posterior to the epihyoplastral suture; a short midline contact of epiplastra; a diamond-shaped entoplastron which is roughly as long as wide; wide gulars which do not or barely extend onto the entoplastron; a long pectoral scute and the pectoroabdominal sulcus convex backward.

Distribution Early-Middle Paleocene (Upper Member of the wanghudun Formation and Doumu Formation) of Qianshan Basin and Paleocene of Xinzhou Basin.

Fig. 6 Shell ofAnhuichelys doumuensis(A-D, IVPP V 5599, holotype) andA.tsienshanensis(E-F, IVPP V 23137) A-B. dorsal view; C-D. ventral view; E-F. anterior portion of the plastron showing the epiplastral lips in ventral (E) and dorsal (F) views

(Figs. 6A-D, 7)

Holotype IVPP V 5599 (Field number: 71071), a shell with damaged carapace and complete plastron.

Etymology From Doumu Formation, where the specimens of this species come from.

Referred specimens MQSC V 002 and MQSC V 007 (Yangxiaowu, wangling, Huangpu, Qianshan; Upper Member of Doumu Fm.), MQSC V 009 (Yanglaowu,wenliang Village, Lingtou Township, Qianshan; Upper Member of Doumu Fm.), MQSC V 065 (Meiyuan, Doumu Township; Upper Member of Doumu Fm.), SHNHM 1945 (Qianshan Basin (?), Anqing; Paleocene), fi ve shells.

Type locality and horizon Yangxinwu, Qianshan; Upper Member of the Doumu Formation.

Diagnosis A species ofAnhuichelyswhich has a hinge on the base of the anterior lobe between the epiplastra/entoplastron and the hyoplastra. It differs fromA. siaoshihensisandA. tsienshanensisin having a sub-oval to oval shaped and longer than wide entoplastron; a moderate epiplastral midline contact. In addition, it differs fromA. siaoshihensisin having wide gulars, a long pectoral scute and a backward convex pectoroabdominal sulcus; and fromA. tsienshanensisin the gulars extending onto the entoplastron in most specimens.

Distribution Middle Paleocene (Doumu Formation) of Qianshan Basin.

Fig. 7 Shell ofAnhuichelys doumuensis(SHNHM 1945) A-B. dorsal view; C-D. ventral view; E-F. right lateral view; G-H. anterior view

Referred specimens Three shells: TZSGP QT19 (Fujiashanzui, Qianshan; upper part of Upper Member of wanghudun Fm.); MQSC V 011-2 (East to Niuxing Reservoir, wanfeng, Yujing, Qianshan; base of Doumu Fm. or top of wanghudun Fm.); MQSC V 023-1 (Jinshi Village, Qinglou Township, Qianshan; upper part of Upper Member of wanghudun Fm. or Lower Member of Doumu Fm.); and IVPP V 18674, an internal mold of a juvenile shell (location and horizon unknown).

Measurements See Table 1.

Table 1 Measurements ofAnhuichelys(cm)

Description The description is based on three species ofAnhuichelyswith a total of more than twenty shells, including juveniles and adult individuals.

The carapace size ranges from 9.3 cm (juvenile) to 30 cm (adult) in length. One of the largest specimens is the holotype ofA. siaoshihensis(IVPP V 5598), with a carapace length of 29 cm. The shell is thick. The carapace is moderate to high domed with a height/length ratio ranging from 30% to 42% (see Table 2); in most specimens this ratio is about 40%. Thecarapace outline is sub-rectangular rather than oval, with somewhat parallel lateral borders. The cervical notch is deep. The posterolateral margin of the carapace is fl ared and serrated. The pygal is sub-vertical. A caudal notch is present, formed entirely by pygal (SHNHM 1945, TZSGP QT5 and TZSGP QT2) or by both pygal and peripherals 11 (MQSC V 002).

The complete nuchal and neural series are preserved in two specimen ofA. siaoshihensis(IVPP V 5598 and TZSGP QT2), one specimen ofA. doumuensis(SHNHM 1945), and one specimen ofA. tsienshanensis(TZSGP QT15). The nuchal is trapezoid in shape and wider than long. The complete neural series includes eight neurals with a neural formula of 4＞6＞6＞6＞6＞6＞6＞6. The neurals 1-5 are elongate, while the more posterior neurals are shorter. SHNHM 1945 has an additional small neural between the neural 8 and the suprapygal 1. The suprapygals, two in number, are preserved in IVPP V 5598, MQSC V 005 and TZSGP QT2 (A. siaoshihensis), MQSC V 002, MQSC V 009 and SHNHM 1945 (A. doumuensis) and TZSGP QT15 (A. tsienshanensis). Their morphology is variable and may be grouped in two morphotypes. Morphotype 1, represented by SHNHM 1945 and MQSC V 009, has a suprapygal 1 clearly smaller and narrower than the suprapygal 2. Morphotype 2 is well represented in MQSC V 002, and also includes IVPP V 5598, TZSGP QT2 and TZSGP QT15. It has a large suprapygal 1 that bounds posteriorly the oval-shaped suprapygal 2 which is wider than long but narrower than the suprapygal 1. The pygal, well preserved in MQSC V 002, is high, almost vertical and trapezoid, with backward convergent lateral borders and a deep caudal notch. This morphology is also present in IVPP V 5598 (A.siaoshihensis), MQSC V 009 (A. doumuensis), TZSGP QT19 and MQSC V 011-2 (Anhuichelyssp.). In TZSGP QT2 (A. siaoshihensis), SHNHM 1945 (A. doumuensis) and TZSGP QT15 (A. tsienshanensis), the pygal is low, wider than high with rather parallel lateral borders. There are eight costals. Costal 1 is much longer than costal 2 and contacts the peripherals 1 to 4. Costals 2 to 6 alternate in length in nearly all specimens, with costals 2, 4 and 6 being longer laterally than medially, while costal 3 and 5 are longer medially than laterally. However the degree of the alternation is variable, from strongly alternate in IVPP V 5598 and TZSGP QT15 to slightly alternate (TZSGP QT2 and SHNHM 1945). In one specimen (MQSC V 009) the costals have almost parallel anterior and posterior borders. There are eleven pairs of peripherals. The anterior peripherals are relatively short. The bridge peripherals are high with a wide angle between the dorsal sheet and the ventral sheet. The posterolateral peripherals are fl ared. The peripherals 11 are expanded posteriorly when the pygal is narrowed posteriorly.

The scute sulci are deeply imprinted and wide. The cervical scute as preserved in TZSGP QT2 is large, wider than long with the lateral margins convergent forward. The vertebrals are narrow, with the vertebrals 1-3 clearly longer than wide. However, IVPP V 5598 and TZSGP QT2 (A. siaoshihensis), MQSC V 001, RGSTHB V.H751, RGSTHB V.753 and HBGM V.752 (A. tsienshanensis), and MQSC V 009 (A. doumuensis) appear to have narrower vertebral 2-3 compare to other specimens. Vertebral 1 is vase-shaped with a constriction at its anterior part. Vertebral 4 is roughly as wide as long. Vertebral 5 is trapezoid and wider thanthe vertebral 4. The pleural scutes are much wider than the vertebrals. The marginal scutes are all restricted to the peripherals. Marginals 1-2 are short, with their length less than half length of corresponding peripherals. Marginals 12 do not cover the suprapygal 2; they are lower than the pygal in IVPP V 5598 and TZSGP QT2 (A. siaoshihensis), MQSC V 002 (A. doumuensis) and TZSGP QT19 and MQSC V 011-2 (Anhuichelyssp.); while in TZSGP QT15 (A. tsienshanensis) and SHNHM 1945 (A. doumuensis), the vertebral 5/marginals 12 sulcus matches the suprapygal 2/pygal suture.

The plastron is sutured to the carapace. The plastron is wide, with a sub-rectangular outline. The anterior lobe of the plastron extends greatly forward, with its front margin up to the anterior edge of the carapace (A. tsienshanensis: TZSGP QT15, MQSC V 061;A. doumuensis: IVPP V 5599, SHNHM 1945) or extending beyond it (A. siaoshihensis: IVPP V 5598, TZSGP QT2;A. tsienshanensis: AHM V 71079-1, MQSC V 010;A. doumuensis: MQSC V 009). The anterior lobe is wide and sub-rectangular in ventral view, with a concave anterior border. The epiplastra form large, upturned horn-shaped processes on the anterolateral corner of the plastron, which are separated one from another by a rather fl at space. The lateral rim of the epiplastron is greatly convex laterally. The bridge is long and narrow, and is longer than the anterior or posterior lobes. The posterior lobe is wide, with convex lateral margins. The anal notch is very shallow (A. siaoshihensis: IVPP V 5598, TZSGP QT2;A. tsienshanensis: MQSC V 066;A. doumuensis: SHNHM 1945) or absent (A. siaoshihensis: MQSC V 005;A. tsienshanensis: TZSGP QT15;A. doumuensis: IVPP V 5599). The axillary and inguinal buttresses are short, contacting the posterior part of peripheral 3 and the anterior part of peripheral 7 respectively. On the internal mold of IVPP V 18674 (Anhuichelyssp.), the axillary buttresses reach half of the width of costal 1 and the inguinal buttresses insert at the mid length of the costal 5. The slender rib heads are remained in situ on the right side.

The epiplastron midline suture is short in most specimens, representing about 1/3 to 1/4 of the entoplastron length or even shorter. InA. siaoshihensis(IVPP V 5598, TZSGP QT2 and MQSC V 005), the midline suture of the epiplastra is longer, being almost as long as (IVPP V 5598 and TZSGP QT2) or even longer (MQSC V 005) than the entoplastron length. MQSC V 065 and SHNHM 1945 show the intermediate state, in which the epiplastra midline length is about half the length of the entoplastron. InA. siaoshihensisandA. doumuensis, there is a hinge at the base of the anterior lobe, situated between the epiplastra/entoplastron and the hyoplastra. In these species, the entohyoplastral suture is straight, and the epihyoplastral suture aligns with the entohyoplastral suture laterally, instead of being lateral to the entoplastron as in most other turtles. The shape of the entoplastron varies: it is a half circle inA. siaoshihensis(IVPP V 5598, TZSGP QT2 and MQSC V 005); but sub-rectangular to sub-oval and longer than wide in MQSC V 007, MQSC V 009, MQSC V 065 and IVPP V 5599 (A. doumuensis). In SHNHM 1945 (A. doumuensis), the entoplastron is a small oval that is separated from the hinge and anterior to it. InA. tsienshanensis, a hinge is absent on the base of the anterior lobe. In this species the entoplastron is diamond-shape, as long as wide, slightly wider than long orslightly longer than wide; and the epihyoplastral suture is lateral to the entoplastron.

The hyoplastron midline length is roughly equal to that of the hypoplastron. The xiphiplastron is expanded, which makes up nearly the entire posterior lobe, with the hypoxiphiplastral suture close to the base of the posterior lobe. The xiphiplastra are loosely connected to the hypoplastra in most specimens, with a hypoxiphiplastral suture which is more open compared to other sutures on the plastron, indicating some degree of mobility of the posterior lobe.

The gular is paired. The morphology of the gular is variable. InA. siaoshihensis(IVPP V 5598, TZSGP QT2 and MQSC V 005), each gular is longer than wide, triangular in shape and extending onto the entoplastron. In other specimens the gular is very short, much wider than long and entirely anterior to the entoplastron (A. tsienshanensis: AHM V 71079-3, MQSC V 061, MQSC V 010 and MQSC V 066) or covering the anterior end of the entoplastron (A. tsienshanensis: TZSGP QT15;A. doumuensis: SHNHM 1945 and IVPP V 5599) or barely reaching entoplastron (A. doumuensis: MQSC V 007). MQSC V 065 (A. doumuemsis) represents an intermediate morphology, with a wide but relatively long gular which covers the anterior end of the entoplastron.

InA. siaoshihensisandA. doumuensis, the humeropectoral sulcus matches the hinge (IVPP V 5598, TZSGP QT2, MQSC V 005, MQSC V 009 and MQSC V 065) or is slightly anterior to the latter at the middle portion (SHNHM 1945 and MQSC V 007). InA. tsienshanensis, the humeropectoral sulcus crosses the entoplastron in AHM V 71079-3 and MQSC V 023-2, or passing through the posterior edge of the entoplastron (TZSGP QT15 and MQSC V 061). The pectoral scute is very short inA. siaoshihensis(IVPP V 5598 and TZSGP QT2) with its length about half the length of the abdominal scute and a straight pectoroabdominal sulcus; while in other specimens this scute is much longer, being almost as long as the abdominal scute, with a straight or almost straight pectoroabdominal sulcus (A. doumuensis: MQSC V 009 and SHNHM 1945;A. tsienshanensis: MQSC V 061) or strongly backward convex pectoroabdominal sulcus (A. tsienshanensis: AHM V 71079-3, TZSGP QT15, MQSC V 012, MQSC V 023-2, MQSC V 010 and MQSC V 066;A. doumuensis: MQSC V 007, MQSC V 065 and IVPP V 5599). The abdominofemoral sulcus matches completely the hypoxiphiplastral suture (IVPP V 5598), or mostly except the lateral ends (MQSC V 011-2), or only in the middle portion in other specimens. The femoral scute is very short at the midline in all specimens. In SHNHM 1945, the vestige of inframarginals is visible as broken sucli around the carapace/ plastron suture on the right side.

Limb bones: The proximal portion of the left humerus is exposed ventrally in IVPP V 5598. The large medial process is separated from the small lateral process by a deep intertubercular fossa. The shaft is strong and relatively straight.

The left foot is partly preserved in MQSC V 011-2, including the posterior half of the femur and some disarticulated phalanges, likely of middle digits. The femur, exposed in lateral view, has a robust and straight shaft. The phalanges are slender but relatively short. The mostlateral two elements seem to be the claws; they are stronger than other phalanges but exposed proximally and damaged; no details are visible.

3 Discussion

Anhuichelyshas axillary buttresses reaching costal 1 and inguinal buttresses contacting costal 5, which are the synapomorphies of Testudinoidea. In Lindholmemydidae, the contact of the inguinal buttresses is mainly with costal 5, but close to its posterior margin (e.g.GravemysbarsboldiandParamongolemyskhosatzkyi), or slightly overlapping costal 6 (e.g.Lindholmemysmartinsoni) (Danilov and Sukhanov, 2001, 2013; Danilov, 2003). Cadena et al. (2013) indicated some variation in the inguinal buttress/costals contact inMongolemys elegans: it is restricted to costal 5 in IGM 90/11; but in the holotype of the species, this contact is with costal 5 on the left side, and with both costal 5 and 6 on the right side. In modern testudinoids, the contact of the inguinal buttresses is restricted to costal 5 in Emydidae, and with costal 5 or costals 5 and 6 in Geoemydidae. In Testudinidae the inguinal buttresses contact both costals 5 and 6, or even the costal 6 only (e.g.,Geochelonepardalis). Inframarginal scutes are absent inAnhuichelys, a derived character found in modern testudinoids, different from primitive testudinoid lindholmemydids which retained a complete row of inframarginals. The vestige of the inframarginals present in SHNHM 1945 is considered as individual variation that occasionally occurs in the extant testudinoids (e.g., in one specimen of emydidChrysemys picta(Natural History Museum of Basel no 1863-c1108)).

3.1 Af fi nities with Testudinidae

Anhuichelyspresent a clear synapomorphic feature of Testudinidae: alternating costal pattern: the costals 2, 4 and 6 have the expanded distal end but narrow proximal end, inversely the costals 3 and 5 are shortened distally but expanded proximally. This character is present in nearly all specimens ofAnhuichelys, but the degree of the alternation varies from strong (e. g. IVPP V 5598 and TZSGP QT15) to slight (e. g. TZSGP QT2 and SHNHM 1945); only one specimen (MQSC V 009) has no alternating costals. The alternating costals 2 to 6 is characteristic of Testudinidae; while the geoemydids have parallel anterior and posterior margins of the costals (Auffenberg, 1974; Claude and Tong, 2004).

Some characters exhibited inAnhuichelysare polymorphic, with states being synapomorphies of Testudinidae or found only in that family:

(1) There are two morphotypes on the morphology of the suprapygals inAnhuichelys(Fig. 8). In morphotype 1, the suprapygal 1 is smaller and narrower than suprapygal 2, with some variations in the relative size of the suprapygals 1 and 2. This morphology is similar to the primitive condition found in Lindholmemydidae, Emydidae and Geoemydidae, and occurs in four specimens among nine (44% of total specimens observed) ofAnhuichelys. Morphotype2 has a large suprapygal 1 with a concave posterior border and an oval suprapygal 2 that is relatively short and slightly narrower than suprapygal 1. This morphology, present in 56% of specimens with well preserved suprapygals that were observed ( fi ve specimens among nine), is close to the condition found in some Testudinidae, such asIndotestudo, although suprapygal 1 is not fully bifurcated as in that taxon. InI. elongatathe suprapygal 1 is bifurcated and bounds laterally the suprapygal 2. It should be noted that variation in suprapygal morphology is present within the extant testudinid species. For example inGopherusorTestudograeca, the two morphotypes are observed in the same species (Auffenberg, 1976; Lapparent de Broin et al., 2006).

Fig. 8 Posterior part of the carapace showing the variations of the suprapygals and pygal inAnhuichelysA.Anhuichelyssp. (MQSC V 011-2); B, D.A. doumuensis(B. SHNHM 1945, D. MQSC V 002); C, F.A. siaoshihensis(C. TZSGP QT2, F. IVPP V 5598); E.A. tsienshanensis(TZSGP QT15). Not to scale

(2) The pygal (Fig. 8) is tall and sub-vertical, with the lateral margins convergent posteriorly in 75% of the specimens ofAnhuichelyswith preserved pygal (6 specimens among eight). This morphology is observed in Testudinidae, such asIndotestudo,AgrionemysorTestudograeca(Lapparent de Broin et al., 2006). Two specimens ofAnhuichelyshave a low and wide pygal with parallel lateral margins as in Lindholmemydidae, Emydidae and Geoemydidae, but different from the latters in that the pygal is still more vertical in comparison with the gently sloping pygal typical of Geoemydidae, such as is seen inSiebenrokiella crassicollis. In addition, the peripherals 11 ofAnhuichelysare expanded posteriorly with an oblique medial border when the pygal is narrowed posteriorly.

(3) Marginal 12 (Fig. 8) is lower than pygal in 5 specimens ofAnhuichelysamong 7 (morphotype 1), while 2 specimens have the vertebral 5/marginals 12 sulcus matching the suture between the suprapygal 2 and the pygal (morphotype 2). Morphotype 1 is primitive and found in most lindholmemydids (exceptGravemys) (Danilov, 2003; Danilov et al., 2012) and Emydidae, such asEmys orbicularisandTrachemys scripta; while morphotype 2 appears to bederived and found in Testudinidae. In Geoemydidae, marginal 12 is taller than pygal, covering the posterior part of the suprapygal 2.

(4) The pectoral scute is short, with its length about half the length of abdominal scute inA. siaoshihensis. In this species, a short pectoral is associated not only with a hinge, but also with a half circle-shaped entoplastron which is placed at the base of the anterior lobe.A. doumuensisandA. tsienshanensishave a longer pectoral which is as long as the abdominal scute. All testudinids have a short pectoral scute, while geoemydids have a longer pectoral scute with its length slightly shorter or equal to that of the abdominal scute.

Associated with a terrestrial fauna composed mainly of mammals,Anhuichelyswere probably land turtles since their morphology is very close to the extant Testudinidae which are all terrestrial. The above mentioned testudinid characters inAnhuichelysseem not due to the convergence for the terrestrial habitat, since their combination is absent in terrestrial geoemydids (e. g.Geoemyda,Heosemys,Cuora) and emydids (e. g.Terrapene). It should be noted that these characters are observed only in some of the specimens ofAnhuichelysand the variation is found throughout the stratigraphical range ofAnhuichelysfrom the Qianshan Basin in the Early-Middle Paleocene, indicating that these testudinid synapomorphic features were still unstable at the beginning of their development.

On the other hand,Anhuichelysretains some primitive characters. The neurals in allAnhuichelysspecimens are elongated hexagonal in shape with short anterolateral sides and undifferentiated as in the basal testudinoid Lindholmemydidae. The neurals of Geoemydidae and Emydidae, as well as the primitive Testudinidae (e.g.Kansuchelys,HadrianusandStylemys) are hexagonal and undifferentiated, while those of advanced Testudinidae are highly differentiated with alternation of octagonal and tetragonal neurals (Hay, 1908; Yeh, 1963, 1979b; Auffenberg, 1974). In addition, the majority of modern members of Testudinoidea have wider neurals.

Anhuichelyslacks developed epiplastral lip, an important synapomorphy of Testudinidae (Auffenberg, 1974), although their epiplastra form a pair of strong and upturned lateral processes. Contrary to the epiplastral lip in Testunididae which is a continuous high bony bulge at the front border of the plastron, the left and right processes ofAnhuichelysare independent one from another, and the area between the processes are rather fl at as in geoemydids, such asPalaeoemys,Batagur,KachugaandPangshura(Fig. 6E-F).

3.2 Character variation inAnhuichelysand validity of the species

Anhuichelysfrom the Paleocene of Qianshan Basin show great variation in both derived and primitive characters. The distribution of characters is shown in Table 2.Anhuichelyscontains three species based on the combination of the characters:A. siaoshihensisYeh, 1979;A. tsienshanensisYeh, 1979 andA. doumuensissp. nov. BothA. siaoshihensisandA. doumuensishave a hinge on the base of the anterior lobe of the plastron, but differ one from another by a series of characters (see diagnoses and Table 2). Concerning the distribution of the species,so far as the stratigraphical information is available, the three specimens ofA. siaoshihensisare from the Early Paleocene wanghudun Formation;A. tsienshanensisis recorded from the Upper Member of wanghudun Formation and Doumu Formation; whileA. doumuensisis only recorded from the Upper Member of Doumu Formation. ThusA. tsienshanensiswas living in sympatry withA. siaoshihensisduring part of the Early Paleocene and withA. doumuensisduring the Middle Paleocene.

we exclude the possibility that the presence or absence of an anterior hinge as a sexual dimorphism because of its position. In some Testudinidae (e. g.Testudograeca), a hinge on the posterior lobe between the hypoplastra and xiphiplastra is present only in females, but such a hinge is incipient in males. The loose articulation of the posterior lobe facilitates oviposition. In the extant testudinidPyxis arachnoidesfrom Madagascar, a hinge at the base of the anterior lobe may be present as the geographical variation that characterizes a subspecies (Bonin et al., 2006).

Chen (1983) described three shells from the Paleocene of Xinzhou, Hubei Province and erectedAnhuichelys xinzhouensis. Chen (1983) noted the close resemblances between the Xinzhou specimens andA. siaoshihensison the carapace, and withA. tsienshanensison the plastron, since the carapace ofA. tsienshanensisis poorly preserved. Chen pointed out five differences which allow Xinzhou specimens to be distinguished fromA. tsienshanensis: 1) deeper cervical notch; 2) entoplastron wider than long; 3) the gularohumeral sulcus anterior to the entoplastron; 4) the pectoroabdominal sulcus close to the hyoplastra/hypoplastra suture or reaching the latter; and 5) the femoroanal sulcus curved, instead of V-shaped as inA. tisenshanensis. All these differences are contained in the intraspeci fi c variations inAnhuichelysfrom the Qianshan Basin.A. xinzhouensisis therefore synonymised withA. tsienshanensisbecause of the absence of a hinge on the plastron; the epihyoplastral suture situated lateral to entoplastron, the humeropectoral sulcus posterior to the epihyoplastral suture; a short midline contact of epiplstra; a diamond-shaped entoplastron roughly as long as wide; the wide gulars which does not or barely extend onto the entoplastron; a long pectoral scute and the pectoroabdominal sulcus convex posteriorly.

3.3 Development of the hinge

A. siaoshihensisandA. doumuensisdeveloped a hinge at the base of the anterior lobe between the epiplastra/entoplastron and the hyoplastra. The presence of the hinge is associated with a series of modification of the surrounding plastral elements: the entoplastron has a straight posterior edge to fit the hinge; the suture between the epiplastra and hyoplastra is moved posteriorly to align with the entoplastron/hyoplastra suture; and the humeropectoral sulcus matches, or is close to the hinge. On the posterior lobe of the plastron, the xiphiplastra are loosely connected to the hypoplastra in most specimens ofAnhuichelys. Among them, a hinge is clearly present at the base of the posterior lobe between the hypoplastra and the xiphiplastra in IVPP V 5598 (A. siaoshihensis) with the abdominofemoral sulcus matchingperfectly the hypoplatra/xiphiplastra suture. In other specimens, the hypoplastra/xiphiplastra suture is often more open compared with other sutures on the plastron, indicating some degree of mobility around this suture. Furthermore, the abdominofemoral sulcus is close to the hypoplastra/xiphiplastra suture, especially its middle portion which matches or almost matches the suture.

The hinge is an adaptive apomorphic feature in turtles that allows the shell to be closed for a better protection of the animal and/or for an easier oviposition (the latter case occurs only in females). It has evolved independently in various groups of turtles and occurs at various position of the shell. In Adocidae, a hinge is developed between the epiplastra and entoplastron/hyoplastra inShachemysfrom the Cretaceous of Asia (Lapparent de Broin, 2004; Danilov et al., 2007).In Kinosternidae, a hinge is present at the base of the anterior lobe, between the epiplastra/entoplastron and the hyoplastra inStaurotypus, whileKinosternonhas an additional hinge at the base of the posterior lobe. In Testudinoidea, a hinge is located between the hyoplastra and hypoplastra inCuora(Geoemydidae) andTerrapene(Emydidae), or on the posterior part of the carapace inKinixys(Testudinidae). In pleurodires, a hinge has evolved at the base of the anterior lobe inPelusios(Pelomedusidae).Anhuichelysis the fi rst Testudinoidea to develop hinges on the shell. The hinge on the base of the anterior lobe of the plastron inAnhuichelyscertainly acted as a protective structure.

3.4 Phylogenetic analysis

In order to determine the phylogenetic relationships ofAnhuichelys, a data matrix of 30 informative characters is gathered inAnhuichelys, 5 well known Cretaceous and Palaeocene Lindholmemydidae (Lindholmemys,Mongolemys,Gravemys,Elkemys, Pseudochrysemys), two testudinoid fossils known in the Early Eocene (PalaeoemysandAchilemys), and 12 living genera representing Chelydridae, Kinosternidae, Dermatemydidae, Platysternidae, Emydidae, Geoemydidae and Testudinidae.Ordosemysis included for rooting the tree.

Two analyses were run, one using only morphological characters and one constraining the relationship among living taxa using a molecular scaffold based on the phylogenies obtained by Crawford et al. (2015), Louren?o et al. (2012) and Guillon et al. (2012). Character description and distribution are given in Appendix 1 and 2. All characters except one were ordered, and all ordered multi-state characters were scaled so that those characters would not have a disproportionate effect above binary characters on phylogeny estimation. Parsimony analyses were performed in PAUP 4.0 b10 (Swofford, 1998) using random addition sequence, and the tree bisection-reconnection branch swapping algorithm across 10000 replicates.

The unconstrained analysis resulted in 8 equally parsimonious trees of 77.5 steps (Fig. 9, strict consensus 1). In this analysis,Anhuichelysis found in a clade withAchilemysrooting other Testudinidae.Gravemys,LindholmemysandMongolemysare rooting Emydidae, while the positions ofElkemysandPseudochrysemyswere variable. Contrary to the results obtained by molecular phylogenies, none of the hypothesis recordedPlatysternonwithin Testudinoidea.

The analysis constrained by a molecular scaffold resulted in a single tree of 84.5 steps (Fig. 9, Tree 1). As in the unconstrained analysis,Anhuichelysis found in a clade withAchilemysrooting other Testudinidae. In this analysis,Mongolemysis rooting Emydidae, whilePseudochrysemys,Elkemys,GravemysandLindholmemysform a grade to Testudinidae+ Geoemydidae. The topology is, however, not very robust. For instance, removing either character 24 (shape of vertebrals 2 to 4) or character 29 (shape of the epihyoplastral suture) resulted in the alternative topologies illustrated in Fig. 9 (Consensus 2). In these topologies,Anhuichelysforms a clade withPlatysternonwhich is the sister group ofLindholmemys+Mongolemys+emydids (a hypothesis formerly proposed by Claude and Tong, 2004); andElkemysandGravemysare sister groups of Testudinidae + Geoemydidae. The position ofPseudochrysemysis unstable. Removing character 24 resulted in two trees of 78 steps, while removing character 29 resulted in two trees of 80 steps. By removing other single character (data not shown), alternative topologies were obtained, butAnhuichelyswas always found within Testudinoidea. In conclusion,Anhuichelysis resolved as a testudinoid in all analyses; it is found as the sister taxon of modern Testudinidae when all characters are included but this position is not strongly supported by the data.

Fig. 9 Phylogenetic hypotheses from this study Left, single tree obtained by using a molecular scaffold; middle, consensus tree obtained when the molecular constrained is removed; right, consensus tree obtained using a molecular scaffold when either character 24 or 29 is removed

4 Conclusions

AnhuichelysYeh, 1979 from the Paleocene of Qianshan Basin represents the earliest known stem Testudinidae and is the fi rst Testudinoidea to develop a hinge. In Qianshan Basin,the genusAnhuichelyscontains three species:A. siaoshihensisYeh, 1979 from the Early Paleocene wanghudun Formation,A. tsienshanensisYeh, 1979 from the wanghudun and Doumu formations andA. doumuensissp. nov. from the Middle Paleocene Doumu Formation, which differ from one another by a combination of characters.A. xinzhouensisChen, 1983 is a junior synonymy ofA. tsienshanensis. The shell morphology and associated vertebrate fauna suggest thatAnhuichelysis likely a land turtle as are all other members of the family Testudinidae.

Acknowledgements we would like to thank wang Yuanqing (IVPP) for inviting Tong Haiyan to study turtle remains from Qianshan Basin and providing facilities for access to the new material; Liu Jun for his support; Zheng Longting (Anhui Provincial Museum), Zheng Fang (IVPP), and colleagues of the Geological Museum of Hubei Province for access to the specimens in their care. This study was supported by the Conservation Program of the Geological Heritage Sites of the Ministry of Finance and the Ministry of Land and Resources, China.

Auffenberg w, 1974. Checklist of fossil land tortoises (Testudinidae). Bull Florida State Mus, Biol Sci, 18: 121-251

Auffenberg w, 1976. The genusGopherus(Testudinidae): Pt I. Osteology and relationships of extant species. Bull Florida State Mus, Biol Sci, 20: 48-110

Bonin F, Devaux B, Dupré A, 2006. Toutes les tortues du monde. Paris: delachaux et niestlé. 1-415

Brinkman D, Li J L, Ye X K, 2008. Order Testudines. In: Li J L, wu X C, Zhang F C eds. The Chinese Fossil Reptiles and Their Kin. Beijing: Science Press. 35-102

Cadena E A, Ksepka D T, Norell M A, 2013. New material ofMongolemys elegansKhosatzky and Mlynarski,1971 (Testudines: Lindholmemydidae) from the Late Cretaceous of Mongolia with comments on bone histology and phylogeny. Am Mus Novit, 3766: 1-27

Chen G, 1983. Chelonian fossils from Xinzhou Basin of Hubei Province. Vert PalAsiat, 21: 42-48

Claude J, Tong H, 2004. Early Eocene testudinoid turtles from Saint-Papoul, France, with comments on the early evolution of modern Testudinoidea. Oryctos, 5: 3-45

Crawford N G, Parham J F, Bellas A B et al., 2015. A phylogenomic analysis of turtles. Mol Phylogenet Evol, 83: 250-257

Danilov I, 2003.GravemysSukhanov and Narmandakh, 1983 (Testudinoidea: Lindholmemydidae) from the Late Cretaceous of Asia: new data. Paleo Bios, 23: 9-19

Danilov I, Sukhanov V B, 2001. New data on lindholmemydid turtleLindholmemysfrom the Late Cretaceous of Mongolia. Acta Palaeont Pol, 46: 125-131

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Danilov I, Claude J, Sukhanov V B, 2012. A redescription ofElkemys australis(Yeh, 1974), a poorly known basal testudinoid turtle from the Paleocene of China. Proc Zool Inst RAS, 316: 223-238

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Appendix 1 Character states

1. Alternating costal plates: 0 no, 1 polymorphic or intermediate, 2 yes.

2. Inguinal and axillary buttresses contacting costals: 0 no, 1 yes.

3. Second suprapygal larger than fi rst: 0 no, 1 polymorphic or intermediate, 2 yes.

4. Longer than wide pygal plate: 0 no, 1 polymorphic or intermediate, 2 yes.

5. Marginal 12 relative to pygal: 0 marginals 12 higher than pygal, 1 marginals 12 = pygal, 2 marginals 12 lower than pygal.

6. Neurals: all hexagonal with shortest sides facing anterolaterally: 0 yes, 1 no.

7. Costal 1 reaching peripheral 4: 0 yes, 1 polymorphic, 2 no.

8. Lateral epiplastral lip present: 0 yes, 1 no.

9. Epiplastral lip present in the middle: 0 yes, forming an elevated bulge, 1 yes but forming a fl at bulge, 2 no.

10. Gular reaching entoplastron: 0 no, 1 polymorphic, 2 yes.

11. Humeropectoral sulcus behind entoplastron: 0 yes, 1 polymorphic, 2 no.

12. Presence of a strong central carina in juvenile: 0 no, 1 yes.

13. Cervical scute: 0 as long as wide or wider than long, 1 narrow, 2 absent.

14. Coalescent trochanters on the femur: 0 no, 1 yes.

15. Bony bridge: 0 no, 1 yes.

16. Anal midline length relative to that of femoral: 0 anal longer than femoral, 1 anal equal to femoral, 2 anal shorter than femoral.

17. Midline length of xiphiplastron greater than that of the hypoplastron: 0 no, 1 yes.

18. Anal notch: 0 absent, 1 small, 2 clearly present.

19. Inframarginal row complete: 0 yes, 1 polymorphic, 2 no.

20. wide entoplastron: 0 yes, 1 polymorphic or intermediate, 2 no.

21. Lateral carina in juveniles: 0 no, 1 yes.

22. Pairs of musk duct: 0 no, 1 yes.

23. Nuchal emargination: 0 absent, 1 small or variable, 2 well developed.

24. Vertebrals 2-4: 0 wider than long, 1 longer than wide.

25. Vertebral 1: 0 wide, 1 narrow (included in nuchal plate).

26. Contact between nuchal plate and fi rst peripheral: 0 nearly parallel to body axis, 1 convergent forward.

27. Gular notch: 0 absent, 1 present.

28. Inguinal buttresses: 0 do not reach costal or reach costal 5 only, 1 reaches costal 6.

29. Suture between epiplastron and hyoplastron: 0 nearly perpendicular to body axis or backward laterally, 1 forward laterally.

30. Disappearance of pectoral scutes: 0 no, 1 yes.

Appendix 2 Data matrix

最早的基干陸龜——安徽龜(Anhuichelys Yeh, 1979)的再研究

佟海燕1,2李 錄2李丁生3陳立民3李 騊3余淑華3余國(guó)盛4程小青4底野力5Julien CLAUDE6

(1 泰國(guó)馬哈薩拉坎大學(xué)古生物研究與教育中心 馬哈薩拉坎 44150)
(2 中國(guó)科學(xué)院古脊椎動(dòng)物與古人類研究所，中國(guó)科學(xué)院脊椎動(dòng)物演化與人類起源重點(diǎn)實(shí)驗(yàn)室 北京 100044)
(3 潛山縣博物館 安徽潛山 246300)
(4 天柱山世界地質(zhì)公園 安徽潛山 246300)
(5 上海自然博物館 上海 200041)
(6 法國(guó)蒙彼利埃進(jìn)化科學(xué)院 蒙彼利埃 34095)

基于安徽省潛山盆地大量新材料，對(duì)安徽龜屬(AnhuichelysYeh, 1979)進(jìn)行了系統(tǒng)再研究，將其歸入了陸龜科基干類型(Testudinidae)。安徽龜屬包含了潛山盆地古新統(tǒng)地層中的三個(gè)種：產(chǎn)自下古新統(tǒng)望虎墩組的小市安徽龜(A. siaoshihensisYeh, 1979), 望虎墩組和痘姆組的潛山安徽龜(A.tsienshanensisYeh, 1979)以及中古新統(tǒng)痘姆組的新種痘姆安徽龜(A.doumuensissp. nov.)。產(chǎn)自湖北新洲古新統(tǒng)的新洲安徽龜(A.xinzhouensisChen, 1983)為潛山安徽龜?shù)耐沓鐾锂惷?。作為陸相脊椎?dòng)物群的成員，安徽龜很可能是一種陸生龜類并且是第一個(gè)甲殼具有鉸鏈的陸龜超科成員。

潛山盆地，古新世，龜鱉類，陸龜科

Q915.864

A

1000-3118(2016)02-0156-24

2016-01-14

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Tong H, Li L, Li D S et al., 2016. A revision ofAnhuichelysYeh, 1979, the earliest known stem Testudinidae (Testudines: Cryptodira) from the Paleocene of China. Vertebrata PalAsiatica, 54(2): 156-179

財(cái)政部和國(guó)土資源部國(guó)家地質(zhì)遺跡保護(hù)項(xiàng)目資助。