Late Quaternary communities of shrews, Soricidae, from Ural and Far East Regions of Russia: A protocol for the multifactorial morphospace building

L.L. Voyta, V.E. Omelko, E.P. Izvarin, Yu.E. Kropacheva, E.O. Eidinova, J.A. Shemyakina, V.S. Nikiforova, T.V. Strukova, N.G. Smirnov
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Abstract

The present paper is a preliminary attempt to develop a protocol for analyzing Late Pleistocene and Holocene paleocommunities of soricids using modern approaches for the morphological data analysis. First, we assessed the abilities of fossil soricid collections from Ural and Far East localities to provide a complex interregional analysis of the phenotype variation. Accordingly, for the first time in the general context, the study provides a species list and chronological position of Ural and Far East shrew fossil samples in terms of inter- and intraregional comparisons to reveal general and specific responses of paleocommunities to climatic fluctuations. Second, under the modern approaches, we prepared 182 three-dimensional models of hemimandibles or isolated m1 and built the morphospace of m1 shape for seven Sorex species from the Upper Pleistocene layer MKl-13 and Middle Holocene layer MKl-7 of Medvezhyi Klyk Cave (South Primorye, Russia). Recent samples from East Siberia (Yakutia) and the northern part of the Far East (Magadanskaya Oblast' and Khabarovsky Kray; “cold” habitats) and South Primorye (“warm” habitats) were included into morphospace to actualize potential responses of the fossil samples to Late Quaternary climate fluctuations. Our analysis revealed: (i) a weak reaction of m1 shape of almost all species to the “cold” and “warm” environmental conditions, except S. daphaenodon Thomas, 1907 and S. caecutiens Laxmann, 1788; (ii) two groups of species, namely “generalized” and “specialized” in m1 shape, in line with the idea of distribution of trophic niches among coexisted shrews; (iii) a diagnostic character for fossil samples of S. unguiculatus Dobson, 1890 and S. isodon Turov, 1924.
俄罗斯乌拉尔和远东地区鼩鼱科晚第四纪群落:多因子形态空间构建的协议
本文是利用现代形态学方法分析晚更新世和全新世水蛭古群落的初步尝试。首先,我们评估了来自乌拉尔和远东地区的固体化石收集的能力,以提供复杂的区域间表型变异分析。因此,本研究首次在一般背景下,从区域间和区域内比较的角度,提供了乌拉尔和远东鼩鼱化石样本的物种列表和年代位置,揭示了古群落对气候波动的一般和特定响应。其次,在现代方法下,对俄罗斯南滨海地区Medvezhyi Klyk洞穴上更新世MKl-13层和中全新世MKl-7层的7个Sorex物种,制备了182个半下颚动物或分离的m1三维模型,并建立了m1形态的形态空间。来自东西伯利亚(雅库特)和远东北部(马加丹斯卡州和哈巴罗夫斯基克雷)的最新样本;将“冷”生境和“暖”生境纳入形态空间,以实现化石样品对晚第四纪气候波动的潜在响应。结果表明:(1)除S. daphaenodon Thomas(1907)和S. caecutiens Laxmann(1788)外,几乎所有物种对“冷”和“暖”环境条件都有较弱的m1型反应;(ii)两组物种,即“广义”和“特化”,呈m1形,符合共存鼩鼱间营养生态位分布的概念;(iii) S. unguiculatus Dobson(1890)和S. isodon Turov(1924)化石样本的诊断特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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