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Late Pleistocene-Holocene paleobiogeography of the genus Apodemus in Central Europe

机译:中欧姬鼠属晚更新世-全新世古生物地理学

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摘要

Wood mice of the genus Apodemus are an essential component of small mammal communities throughout Europe. Molecular data suggest the postglacial colonization of current ranges from south European glacial refugia, different in particular species. Yet, details on the course of colonization and Holocene history of particular species are not available, partly because of a lack of reliable criteria for species identification in the fossil record. Using a sample of extant species, we analyzed variation patterns and between-species overlaps for a large set of metric and non-metric dental variables and established the criteria enabling the reliable species identification of fragmentary fossil material. The corresponding biometrical analyses were undertaken with fossil material of the genus (2528 items, 747 MNI) from 22 continuous sedimentary series in the Czech Republic and Slovakia, from LGM to Recent. In Central Europe, the genus is invariantly absent in LGM assemblages but regularly appears during the Late Vistulian. All the earliest records belong to A. flavicollis, the species clearly predominating in the fossil record until the Late Holocene. A. uralensis accompanied it in all regions until the late Boreal when disappeared from the fossil record (except for Pannonia). A few items identified as A. sylvaticus had already appeared in the early Holocene assemblages, first in the western part of the region, yet the regular appearance of the species is mostly in the post-Neolithic age. A. agrarius appeared sparsely from the Boreal with a maximum frequency during the post-Neolithic period. The results conform well to the picture suggested by molecular phylogeography but demonstrate considerable differences among particular species in dynamic of the range colonization. Further details concerning Holocene paleobiogeography of individual species in the medium latitude Europe are discussed.
机译:姬鼠属的木鼠是整个欧洲小型哺乳动物群落的重要组成部分。分子数据表明,冰川后的当前定居点来自南欧冰川避难所,在特定物种中有所不同。但是,尚无关于特定物种的定殖过程和全新世历史的详细信息,部分原因是化石记录中缺乏可靠的物种识别标准。我们使用一个现存物种的样本,分析了一组大量的公制和非公制牙科变量的变异模式和种间重叠,并建立了能够可靠地识别碎片化石材料的物种的标准。使用来自捷克共和国和斯洛伐克的22个连续沉积系列(从LGM到最近)的属化石材料(2528种,747 MNI)进行了相应的生物特征分析。在中欧,LGM组合中始终不存在该属,但在晚世的Vistulian时期经常出现。所有最早的记录都属于黄曲霉(A. flavicollis),该物种显然在化石记录中占主导地位,直到晚新世。乌regions在所有地区都伴随着它,直到北北方晚期从化石记录中消失(潘诺尼亚除外)。一些被识别为A. sylvaticus的物种已经出现在全新世早期的组合中,首先出现在该地区的西部,但是该物种的正常出现主要出现在新石器时代以后。在新石器时代以后,从北部稀疏出现了A. agrarius,出现频率最高。结果很好地符合了分子系统地理学所建议的图像,但是显示了特定物种之间在范围定殖动态方面的显着差异。讨论了有关中纬度欧洲各个物种的全新世古生物地理学的更多细节。

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