Small mammal assemblages from paleosols in Eastern Europe indicate evolutionary trends and predominantly warm and dry climates across Middle and Late Pleistocene Interglacials

IF 1.9 3区 地球科学 Q3 GEOGRAPHY, PHYSICAL
Journal of Quaternary Science Pub Date : 2026-04-13 Epub Date: 2026-02-18 DOI:10.1002/jqs.70056
Anastasia K. Markova, Andrey Yu. Puzachenko, Alexander I. Tsatskin
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引用次数: 0

Abstract

We studied nine local small mammal faunas directly recovered from interglacial (and one interstadial) paleosols of the Middle (seven) and Late (two) Pleistocene on the East European Plain. The oldest faunas, dated to the Muchkap (MIS 15) and Likhvin (MIS 11) interglacials, belonged to the Late Tiraspolian and Gun'ki small mammal complexes, respectively. Later faunas, corresponding to the Kamenka, Romny, and Mezin paleosols, included chronotaxa morphologically close to modern species. The youngest Middle Pleistocene fauna most likely correlates with the Romny interglacial (MIS 7). The youngest overall fauna dates to the Bryansk (=Denekamp) interstadial (late MIS 3). We performed the first comprehensive analysis of the quantitative composition of these faunas using multivariate analysis and inferred qualitative relationships among them. The main component of variation in faunal composition identified by non-metric multidimensional scaling (first NMDS axis) reflects evolutionary changes in the phyletic lineages of steppe lemmings (Lagurus) and narrow-headed voles (Stenocranius). The other two components correlated with the geographical position (longitude and latitude, respectively) of the sections, most likely reflecting a relatively stable pattern of variation in ecological conditions across the East European Plain. The faunal composition suggests that the animals inhabited semi-arid and arid steppe habitats, and that the paleosols formed during the warmest and driest phases of the interglacials in Eastern Europe. The non-analog Bryansk interstadial complex is associated with conditions of periglacial, mosaic steppe–tundra-like environments. Based on the analysis of the small mammal faunas, we also present a biostratigraphic scheme for the Middle and Late Pleistocene of the central and southern parts of the East European Plain (Eastern Europe).

来自东欧古土壤的小型哺乳动物组合表明了中更新世和晚更新世间冰期的进化趋势和主要的温暖和干燥气候
本文研究了东欧平原中更新世(7)和晚更新世(2)间冰期(1)古土壤中直接恢复的9种本地小型哺乳动物。最古老的动物群分别属于晚Tiraspolian和Gun’ki小型哺乳动物群,可追溯到Muchkap间冰期(MIS 15)和Likhvin间冰期(MIS 11)。后来的动物群,对应于Kamenka, Romny和Mezin古土壤,包括在形态上接近现代物种的时分类群。最年轻的中更新世动物群最有可能与罗姆尼间冰期相关(MIS 7)。最年轻的动物群可以追溯到Bryansk (=Denekamp)间冰期(MIS 3晚期)。我们首次利用多变量分析对这些动物群的定量组成进行了综合分析,并推断了它们之间的定性关系。由非度量多维尺度(第一NMDS轴)确定的区系组成变异的主要成分反映了草原旅鼠(Lagurus)和窄头田鼠(Stenocranius)种系的进化变化。另外两个分量与剖面的地理位置(分别为经度和纬度)相关,很可能反映了整个东欧平原生态条件相对稳定的变化模式。动物群组成表明,这些动物生活在半干旱和干旱的草原栖息地,而古土壤形成于东欧间冰期最温暖和最干燥的阶段。非模拟的布良斯克冰期间复合体与冰缘、马赛克草原-苔原样环境的条件有关。在对小型哺乳动物区系分析的基础上,提出了东欧平原中南部地区中、晚更新世生物地层方案。
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来源期刊
Journal of Quaternary Science
Journal of Quaternary Science 地学-地球科学综合
CiteScore
4.70
自引率
8.70%
发文量
82
审稿时长
6-12 weeks
期刊介绍: The Journal of Quaternary Science publishes original papers on any field of Quaternary research, and aims to promote a wider appreciation and deeper understanding of the earth''s history during the last 2.58 million years. Papers from a wide range of disciplines appear in JQS including, for example, Archaeology, Botany, Climatology, Geochemistry, Geochronology, Geology, Geomorphology, Geophysics, Glaciology, Limnology, Oceanography, Palaeoceanography, Palaeoclimatology, Palaeoecology, Palaeontology, Soil Science and Zoology. The journal particularly welcomes papers reporting the results of interdisciplinary or multidisciplinary research which are of wide international interest to Quaternary scientists. Short communications and correspondence relating to views and information contained in JQS may also be considered for publication.
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