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Palaeoecological and biostratigraphical implications of the microvertebrates of Qesem Cave in Israel

机译:以色列Qesem洞穴微脊椎动物的古生态学和生物地层学意义

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Microvertebrates are generally well suited for drawing inferences on past environmental conditions because they are closely bound to the areas in which they lived. In this paper, we discuss palaeoecological implications of two microvertebrate concentrations in the Middle Pleistocene site Qesem Cave in Israel. The ecological preferences of the nearest living relatives of the microvertebrate taxa recorded in Concentration 1 (squares L-N/13-15) and 2 (squares G-H/16-17) at Qesem Cave allow us to infer a mosaic of open palaeoenvironment with sparse vegetation, shrubland, Mediterranean Forest, rocky areas and riverbanks. Additionally, we infer palaeoclimate from the bioclimatic distribution of extant species using the Coexistence Approach. To our knowledge, this is the first time the approach has been applied to microfaunal assemblages. These data suggest cooler and slightly drier winters and somewhat lower seasonality than at present around Qesem Cave; the differences are more pronounced for the time covered by Concentration 2 than Concentration 1.
机译:微脊椎动物通常非常适合根据过去的环境条件进行推断,因为它们与它们所居住的区域紧密相连。在本文中,我们讨论了以色列中更新世遗址Qesem Cave中两个微脊椎动物浓度的古生态意义。在Qesem洞穴的浓度1(LN / 13-15正方形)和2(GH / 16-17正方形)中记录的最近生的微脊椎动物类群的生态偏好使我们可以推断出植被稀疏的开放古环境的镶嵌,灌木丛,地中海森林,多石地区和河岸。此外,我们使用共存方法从现存物种的生物气候分布推断古气候。据我们所知,这是该方法首次应用于微动物群。这些数据表明,比现在Qesem Cave周围的冬天更凉爽,干燥一些,季节性也有所降低。与浓度1相比,浓度2所涵盖的时间差异更为明显。

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