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中国山阳寨晚更新世地点 2 的大型化石仓鼠及 和 (啮齿目:仓鼠科)有效性的讨论。

Large-sized fossil hamsters from the late Middle Pleistocene Locality 2 of Shanyangzhai, China, and discussion on the validity of and (Rodentia: Cricetidae).

机构信息

State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an, Shaanxi Province, China.

出版信息

PeerJ. 2023 Jul 28;11:e15604. doi: 10.7717/peerj.15604. eCollection 2023.

Abstract

A detailed morphological description and comparative study were conducted on numerous large-sized hamster remains collected from the late Middle Pleistocene Locality 2 of Shanyangzhai (Syz 2), Hebei Province, China. The comparisons reveal that these fossils are highly similar to the extant in size and morphology, including the small degree of alternating between the main opposite cusps on M1-3, the presence of axioloph on M3, and mesolophids on m1-2 that are present but seldom reach the lingual margin of the teeth, among other features. However, minor differences between the two still exist. Consequently, all these fossils are designated as a chronosubspecies of the extant species, comb. nov. The skull and molar morphologies of and were meticulously compared to resolve the long-standing debate regarding the validity of Zdansky, 1928 and Zdansky, 1928. The findings indicate that the differences between the two are slight; as a result, can only be considered a chronosubspecies of , ., comb. nov., and should be recognized as a junior synonym of . We tentatively propose that, among the seven species once referred to , , , , and should be reassigned to , while should be transferred to , and to . Excluding . from the Late Pliocene Youhe fauna, there are no reliable fossils in China earlier than the Middle Pleistocene. Based on the current evidence, may have originated from during the Early Pliocene in Europe and subsequently spread to Asia. is its sole surviving representative, which now exclusively inhabits East Asia.

摘要

对来自中国河北省山阳寨(Syz 2)晚更新世地点 2 的大量大型仓鼠遗骸进行了详细的形态描述和比较研究。这些化石在大小和形态上与现生种 极为相似,包括 M1-3 上主对尖高度交替的程度、M3 上的轴脊以及 m1-2 上存在但很少到达牙齿舌侧缘的中脊等特征。然而,两者之间仍存在一些微小的差异。因此,所有这些化石都被指定为现生物种的一个年代亚种, 组合新种。对 和 的头骨和臼齿形态进行了仔细比较,以解决关于 和 的有效性的长期争论。研究结果表明,两者之间的差异很小;因此, 只能被视为 的一个年代亚种,.,., 组合新种,而 应该被认为是 的一个次同物异名。我们初步提出,在曾经归入 的七个种中, 、 、 、 和 应归入 ,而 应归入 , 应归入 。将 从晚更新世榆社动物群中排除,中国早于中更新世就没有可靠的 化石了。根据目前的证据, 可能起源于欧洲早更新世的 ,随后传播到亚洲。 是其唯一现存的代表,现在仅栖息于东亚。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/855d/10389077/a6ac194bf8f7/peerj-11-15604-g001.jpg

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