在过去的25000年里,小型哺乳动物群落的变化显示了组成、特征和干旱之间的复杂关系

Julia A. Schap, J. Meachen, Jenny L. McGuire
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摘要

今天,许多生态系统面临着日益频繁和极端的干旱。小型哺乳动物可能是更大的生态变化的先兆,使它们成为保护的关键组成部分。我们利用化石记录来探索小型哺乳动物群落如何应对干旱变化。最近,短期干旱导致小型哺乳动物的均匀性增加,因为优势的多面手物种遭受严重的种群波动。还有一种假设是,随着干旱的增加,食草动物的牙冠高度会增加,以对抗磨损。在这里,我们研究了一系列干旱-半干旱周期中社区水平的变化,包括均匀性、睡眠不足和饮食。我们比较了两个洞穴:自然陷阱洞穴(NTC)是开放的和干旱的,Samwell洞穴(SC)是封闭的和有森林的。从晚更新世到晚全新世,两个洞穴的均匀度都有所下降。在NTC,饮食通用型在更新世更为常见(61%),食草动物在中期(62%)和晚全新世(57%)占主导地位。然而,在SC,一般分类群增加到全新世。NTC更新世群落中,低齿冠高度的类群在全新世减半的比例最高(42%)。从更新世到最近,NTC的低密度变化和从多面手到草食性类群的转变与预期的干旱反应不一致。这些社区与干旱的功能关系可能比以前认为的更微妙。NTC的水的生物利用度和当地植被类型可以帮助分析这些趋势。更新世降水主要在冬季积累,不利于植物生长。因此,能够以稀少的、适应干旱的植物和无脊椎动物为食的多面手哺乳动物占据了主导地位。全新世的降水转向夏季积累,使得植物(如草)得以殖民,草食性类群的丰度增加,相应的向高冠群落转移。
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Changes in Small Mammal Communities Over the Last 25,000 Years Show a Complex Relationship Between Composition, Traits, and Aridity
Many ecosystems today face increasingly frequent and extreme droughts. Small mammals can be harbingers of larger ecological changes, making them critical components for conservation. We use the fossil record to explore how small mammal communities respond to aridity changes. Recent, short-term droughts caused small mammals to increase in evenness, as dominant generalist species suffer severe population fluctuations. It has also been hypothesized that with increasing aridity, herbivore tooth crown heights increase to combat wear. Here, we examine community-level changes, including evenness, hypsodonty, and diet across a series of arid-semiarid cycles. We compare two caves: Natural Trap Cave (NTC), which is open and arid, and Samwell Cave (SC), which is closed and forested. Evenness decreased at both caves from the Late Pleistocene to the Late Holocene. At NTC, dietary generalists were more common in the Pleistocene (61%) with herbivores dominating in the Middle (62%) and Late Holocene (57%). However, at SC generalist taxa increased into the Holocene. The Pleistocene community at NTC had the highest percentage of taxa with low tooth crown heights (42%) halving into the Holocene. Changes in hypsodonty and a shift from generalist to herbivorous taxa at NTC do not align with anticipated responses to aridity, which decreased from the Pleistocene to the recent. Functional relationships of these communities to aridity may be more nuanced than previously thought. Bioavailability of water and local vegetation types at NTC can help parse out these trends. Pleistocene precipitation mostly accumulated during the winter, not aiding plant growth. Thus, generalist mammals who could survive on scant, arid-adapted plants and invertebrates dominated. Precipitation through the Holocene shifted to summer accumulation, allowing plants, like grasses, to colonize and herbivorous taxa to increase in abundance with corresponding shifts to high crowned communities.
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