Puzachenko Andrei Yurievich, Markova Anastasia Konstantinovna
Institute of Geography, Russian Academy of Sciences, Moscow, Russia.
Integr Zool. 2014 Aug;9(4):461-70. doi: 10.1111/1749-4877.12059.
Fossil record data on the mammal diversity and species richness are of importance for the reconstruction of the evolution of terrestrial ecosystems during the Late Pleistocene-Holocene transition. In Eastern Europe, the transformations during the Pleistocene-Holocene transition consisted mainly in changes in zonal structure and local fauna composition (Markova & Kolfschoten 2008). We investigated the species richness and the analogues of the α, β diversity indexes (in the sense of Whittaker 1972) of large and medium size mammals for 13 climate-stratigraphic units dating to the Late Pleistocene and the Holocene, from the Hasselo Stadial (44-39 kBP) to the Subatlantic period and the present day. The biological diversity of the Last Glacial Maximum (LGM) and the Holocene thermal optimum was investigated in more detail using information about all mammalian taxa (PALEOFAUNA database; Markova 1995). One of our results show that the α, β diversity values show only a negative correlation with the temperature conditions during the Late Pleistocene, the period that is characterized by the so-called 'Mammoth Fauna' complex. For the Holocene faunas the diversity indexes are nearly independent from physical conditions; the α diversity index decreased and the β diversity index increased. The relatively low α diversity and high β diversity indexes for the present-day faunas are referred to the decrease of the population number of some forest species in historical time and the increase of the dominance of unspecialized species or the species connected with intra-zonal ecosystems. The study shows furthermore the occurrence of several East European 'centers' with a high mammal diversity, which are relatively stable during the Pleistocene-Holocene transition. The orientation of the boundaries between the large geographical mammal assemblages depended, particularly in the northwestern part of Eastern Europe, on the expansion of the Scandinavian ice sheet.
哺乳动物多样性和物种丰富度的化石记录数据对于重建晚更新世 - 全新世过渡时期陆地生态系统的演化至关重要。在东欧,更新世 - 全新世过渡期间的转变主要体现在地带性结构和当地动物群组成的变化上(马尔科娃和科尔夫肖滕,2008年)。我们研究了13个可追溯到晚更新世和全新世的气候地层单位中大中型哺乳动物的物种丰富度以及α、β多样性指数类似物(按照惠特克1972年的定义),这些单位从哈塞洛冰期(44 - 39千年前)到亚大西洋期直至现今。利用所有哺乳动物类群的信息(古动物数据库;马尔科娃,1995年),对末次盛冰期(LGM)和全新世高温期的生物多样性进行了更详细的研究。我们的一项结果表明,α、β多样性值在晚更新世期间与温度条件仅呈现负相关,该时期以所谓的“猛犸象动物群”复合体为特征。对于全新世动物群,多样性指数几乎与物理条件无关;α多样性指数下降,β多样性指数上升。现今动物群相对较低的α多样性和较高的β多样性指数归因于历史时期一些森林物种数量的减少以及非特化物种或与区域内生态系统相关物种优势度的增加。此外,该研究还表明存在几个哺乳动物多样性高的东欧“中心”,它们在更新世 - 全新世过渡期间相对稳定。大型地理哺乳动物组合之间边界的走向,特别是在东欧西北部,取决于斯堪的纳维亚冰盖的扩张。