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Bank vole Myodes (=Clethrionomys) glareolus (Schreber, 1780): Rare species in the Late Pleistocene fauna of Croatia

机译:银行田鼠Myodes(= Clethrionomys)glareolus(Schreber,1780年):克罗地亚晚更新世动物区系中的稀有物种

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摘要

In comparison to other vole species, bank vole Myodes (=Clethrionomys) glareolus (Schreber, 1780) is a very rare fossil element in the Late Pleistocene fauna in Croatia. So far, it has been found in several Croatian localities, from which four are presented here. In the Vindija Cave (NW Croatia), 33 molars were found in the faunal assemblages from layers/complexes I to B (MIS 5 to MIS 1; dated at approximately 88 ka to Holocene). A very small sample (16 molars) has been discovered from the Romualdova Cave (W Istria; layer B? (Postglacial). Only one fragment of a mandible with M_(1and2) has been found in the fossil material from the Marlera I site (S Istria; MIS 3-2), and one molar originates from the Ljubiceva Cave (S Istria; MIS 2-1). This small sample of 52 teeth (M_1s, M_2s, M_3s, and M~3s) was determined as M. glareolus, a very good indicator of forest habitats. These molars have been morphometrically analysed, and the results have been compared to those of the contemporaneous fossil material from other European localities. Increase of the length values has been observed for the Vindija sample, in concordance to the Berg-mann's rule. A/L indices show higher values for the Holocene sample (layer B) than for the specimens which originated from the G and E + F complexes dated at >42-18.5 ka BP. The most frequent mor-photype is B in the Vindija and Romualdova Caves, respectively. Morphometric data for the present-day bank voles of Croatia have been also given. M. glareolus is for the first time determined from the Romualdova and Ljubiceva Caves. Both sites have been recently systematically excavated. It is expected that future investigations of the small mammal remains will yield new findings of the bank vole from the Late Pleistocene layers of these Croatian sites.
机译:与其他田鼠物种相比,河岸田鼠Myodes(= Clethrionomys)glareolus(Schreber,1780)是克罗地亚晚更新世动物群中非常罕见的化石元素。到目前为止,在克罗地亚的几个地方都可以找到它,这里有四个。在Vindija洞穴(克罗地亚西北部)中,从I / B层/复合体(MIS 5到MIS 1;距新世约88 ka)的动物群中发现了33颗臼齿。从Romualdova洞穴(W Istria; B?层(冰川后))中发现了一个非常小的样品(16磨牙)。在Marlera I遗址的化石材料中仅发现了M_(1and2)下颌骨的一个碎片( S Istria; MIS 3-2),其中一个磨牙起源于Ljubiceva洞穴(S Istria; MIS 2-1),该小样本的52颗牙齿(M_1s,M_2s,M_3s和M〜3s)被确定为M。 glareolus,非常好的森林生境指标,对这些臼齿进行了形态计量分析,并将结果与​​欧洲其他地区的同期化石材料进行了比较,结果发现Vindija样品的长度值有所增加根据Berg-mann法则,全新世样品(B层)的A / L指数值高于源自G和E + F络合物的标本,样品年龄大于> 42-18.5 ka BP。分别在Vindija和Romualdova洞穴中的B型。克罗地亚的新台币银行田鼠也已经给出。首次由Romualdova和Ljubiceva洞穴确定了M. glareolus。最近已系统地挖掘了两个地点。预计将来对这些小型哺乳动物遗骸的调查将在这些克罗地亚遗址的晚更新世层中产生新的岸田鼠发现。

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  • 来源
    《Quaternary International》 |2014年第10期|167-178|共12页
  • 作者

    Jadranka Mauch Lenardic;

  • 作者单位

    Institute for Quaternary Paleontology and Geology, Croatian Academy of Sciences and Arts, Ante Kovacica 5/Ⅱ, HR-10000 Zagreb, Croatia;

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