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1. chinaXiv:201708.00333 [pdf]

Cranial and dental material of Gomphotherium wimani (Gomphotheriidae, Proboscidea) from the Middle Miocene of the Linxia Basin, northwestern China

YANG Xiang Wen; LI Yu ; WANG Shi-Qi
Subjects: Geosciences >> Geology

嵌齿象是真象的基干类群,其研究历来受到重视,同时也存在很多争议。维曼嵌齿象(Gomphotherium wimani)是中国的一个特有种,之前仅有一些牙齿和破碎下颌的报道,研究者对其形态特征和演化地位的认识一直比较模糊。本文报道了发现于甘肃省临夏盆地的维曼嵌齿象的新材料,包括上沟地点一件未成年头骨和倒黑沟地点属于同一个体的部分颊齿。通过研究对比,认为维曼嵌齿象是嵌齿象中一个比较进步的种,具有如下独有特征:颊齿的主齿柱前后中心小尖分裂并成嵴状,副齿柱趋向于分裂,发育有弱的副齿柱中心小尖,齿谷中等开阔,齿冠相对较高。对过去发现的维曼嵌齿象材料的厘定表明,该种最初建立时产于泉头沟地点的一颗m3实际上是葛氏铲齿象(Platybelodon grangeri)的M3; 而西宁吊沟地点发现的维曼嵌齿象的一件M3极有可能属于铲齿象类(amebelodontids)。对厘定后的维曼嵌齿象地点的研究表明,维曼嵌齿象分布于中国甘肃、青海的几个中中新统地点,其时代基本上可以与MN6−MN7/8早期相对比,时代跨度估计为15~13 Ma。

submitted time 2017-08-24 From cooperative journals:《古脊椎动物学报》 Hits1107Downloads485 Comment 0

2. chinaXiv:201708.00332 [pdf]

Paleoecology of Cenozoic rhinos from northwest China: a stable isotope perspective

Dana BIASATTI; WANG Yang; DENG Tao
Subjects: Geosciences >> Geology

The diets and environments of fossil rhinocerotoids from the Linxia Basin, Gansu, China, ranging in age from 25 to 2.5 Ma, were reconstructed based on bulk and serial carbon (C) and oxygen (O) isotope analyses of tooth enamel. The results support many previous hypotheses inferred from dentition and cranial and limb morphology and offer new insight on the paleoecology of some genera. The isotopic results support the following previous hypotheses: the Late Oligocene rhino Paraceratherium inhabited a forested environment, and the coexisting rhino Allacerops lived in a relatively open habitat and had a less specialized diet; the Middle Miocene Hispanotherium grazed in open territory, whereas the contemporaneous Alicornops had a more generalized diet in a forested environment; and the Late Miocene rhino Parelasmotherium grazed in an open steppe habitat. The isotope data indicate that the rhinos Acerorhinus and Dicerorhinus inhabited open steppe environments, inconsistent with previous inferences that these two rhinos dwelled in forested environments. The isotopic results are not conclusive concerning the habitat of Iranotherium, but support previous hypotheses that this rhino was a specialized C3 grazer. The results also suggest that Chilotherium was a forest-dweller throughout much of the Late Miocene, but occupied a more open environment by the end of the Late Miocene. Additionally, the results are consistent with previous hypotheses that the Pliocene rhino Shansirhinus and the Pleistocene rhino Coelodonta were grazers in open habitats. Finally, the C isotope data support that all rhinos in this study were pure C3 feeders, confirming that C4 grasses were not an important component of the plant biomass in the Linxia Basin from 25 to 2.5 Ma. 根据牙齿釉质的全样和系列碳、氧同位素分析,重建了甘肃临夏盆地25~2.5Ma期间犀牛的食性和环境。其结果支持先前根据牙齿和头骨-肢骨形态做出的一些推断,并对部分属的古生态提出了新的看法。同位素结果支持如下的推断:晚渐新世的巨犀Paraceratherium生活于森林环境,而与其共生的异角犀Allacerops栖息地相对开阔,食性特化程度低;中中新世的西班牙犀Hispanotherium在开阔领地上取食草本植物,而同时代的奇角犀Alicornops在森林环境中具有更特化的食性;晚中新世的副板齿犀Parelasmotherium在开阔的稀树草原上取食草本植物。与先前认为无鼻角犀Acerorhinus和额鼻角犀Dicerorhinus生活于森林化环境的推断不同,数据指示这两种犀牛也生活于开阔的稀树草原环境。同位素结果未能得出伊朗犀Iranotherium的确切生活环境,但支持先前认为它特化为C3草本植物取食者的推断。研究结果也显示大唇犀Chilotherium在晚中新世的大多数时间内是森林生活者,但其在晚中新世末期占据了更开阔的环境。此外,分析结果与先前的推断一致,即上新世的山西犀Shansirhinus和更新世的披毛犀Coelodonta是开阔生活环境中的食草者。最后,碳同位素数据支持在此项研究中的所有犀牛都是纯C3取食者,确认C4植物不是临夏盆地从25Ma到2.5Ma期间植被的重要成分。

submitted time 2017-08-24 From cooperative journals:《古脊椎动物学报》 Hits1430Downloads461 Comment 0

3. chinaXiv:201708.00170 [pdf]

Early Mammut from the Upper Miocene of northern China, and its implications for the evolution and differentiation of Mammutidae

WANG Shi-Qi; LI Yu; Jaroon DUANGKRAYOM; CHEN Shao-Kun; HE Wen; CHEN Shan-Qin
Subjects: Geosciences >> Geology

Mammut is the terminal taxon of the proboscidean group Mammutidae, which survived to the Late Pleistocene. Although this genus was widely distributed in the Pliocene of Eurasia and the Pleistocene of North America, little is known about its early evolution. Here, we report on Mammut cf. M. obliquelophus from the Upper Miocene of northern China based on new fossil material, including an almost complete juvenile cranium and other remains, which show many primitive features within Mammutidae and clearly demonstrate the morphological evolution of Mammut. The strongly laterally expanded lateral wing of the occiput and the presence of basal constriction of the incisive fossa display cranial similarity between Mammut cf. M. obliquelophus and both Eozygodon morotoensis and Choerolophodon guangheensis, early representatives of the Mammutidae and Choerolophodontidae, respectively, indicating the close relationship between these two groups: both of them are located at the basal phylogenetic positions in Elephantimorpha.This result is further confrmed by a cladistic analysis.

submitted time 2017-08-08 From cooperative journals:《古脊椎动物学报》 Hits499Downloads300 Comment 0

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