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Ecomorphological characterization of murines and non-arvicoline cricetids (Rodentia) from south-western Europe since the latest Middle Miocene to the Mio-Pliocene boundary (MN 7/8–MN13)

机译:自最近的中新世至密奥上新世边界(MN 7 / 8–MN13)以来来自欧洲西南部的鼠类和非arvicoline ice足类(啮齿类)的生态形态特征

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摘要

Rodents are the most speciose group of mammals and display a great ecological diversity. Despite the greater amount of ecomorphological information compiled for extant rodent species, studies usually lack of morphological data on dentition, which has led to difficulty in directly utilizing existing ecomorphological data of extant rodents for paleoecological reconstruction because teeth are the most common or often the only micromammal fossils. Here, we infer the environmental ranges of extinct rodent genera by extracting habitat information from extant relatives and linking it to extinct taxa based on the phenogram of the cluster analysis, in which variables are derived from the principal component analysis on outline shape of the upper first molars. This phenotypic “bracketing” approach is particularly useful in the study of the fossil record of small mammals, which is mostly represented by isolated teeth. As a case study, we utilize extinct genera of murines and non-arvicoline cricetids, ranging from the Iberoccitanian latest middle Miocene to the Mio-Pliocene boundary, and compare our results thoroughly with previous paleoecological reconstructions inferred by different methods. The resultant phenogram shows a predominance of ubiquitous genera among the Miocene taxa, and the presence of a few forest specialists in the two rodent groups (Murinae and Cricetidae), along with the absence of open environment specialists in either group of rodents. This appears to be related to the absence of enduring grassland biomes in the Iberian Peninsula during the late Miocene. High consistency between our result and previous studies suggests that this phenotypic “bracketing” approach is a very useful tool.
机译:啮齿动物是最特殊的哺乳动物群体,并表现出极大的生态多样性。尽管针对现存啮齿动物物种收集了大量的生态形态学信息,但研究通常缺乏有关牙列的形态学数据,这导致难以直接利用现存啮齿动物的现有生态形态学数据进行古生态重建,因为牙齿是最常见的或通常是唯一的微型哺乳动物化石。在这里,我们根据聚类分析的象形图,通过从现存亲戚中提取栖息地信息并将其与灭绝的生物分类相关联,从而推断灭绝的啮齿类动物的环境范围,其中变量是根据上部第一个轮廓形状的主成分分析得出的磨牙。这种表型“包围”方法在研究小型哺乳动物的化石记录时特别有用,该化石记录主要由孤立的牙齿代表。作为一个案例研究,我们利用了灭绝的鼠类和非arcoclineline cricetids的种类,从伊比洛西坦最新的中新世中期到密奥上新世边界,并将我们的结果与以前通过不同方法推断的古生态重建进行了比较。生成的象形图显示,中新世分类群中普遍存在属,并且在两个啮齿动物类群(Murinae和Cricetidae)中都有一些森林专家,而在任何啮齿动物类群中都没有开放环境专家。这似乎与中新世晚期伊比利亚半岛没有持久的草地生物群落有关。我们的结果与以前的研究之间的高度一致性表明,这种表型“包围”方法是非常有用的工具。

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