Small Mammal Hypsodonty Ratios Do Not Track Precipitation Changes at Natural Trap Cave, Wyoming

Lily Turner, Julia A. Schap, Jenny L. McGuire
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Abstract

With future climate change, drought events are expected to increase. Hypsodonty is an adaptation in herbivorous mammals for higher crowned teeth, which are better able to process coarse foods. Typically, animals with highly hypsodont teeth are found in arid places. This trait is considered an adaptation to aridity and drought. Many studies examined the spatial distribution of hypsodonty with respect to climate in both ungulates and Glires (rodents and lagomorphs). However, few studies have examined whether spatial trends play out across known climate shifts at a single location. Glires evolved hypsodonty millions of years before ungulates, adapt readily due to short generation times, and have relatively small home ranges, so they may provide more accurate climate predictions. Here, we use Glires from Natural Trap Cave, WY to examine whether community-level changes in hypsodonty reflect known precipitation changes. Additionally, this study investigates the effects of measurement techniques (teeth in-jaw versus out-of-jaw) and tooth wear on hypsodonty measurements. Currently, most hypsodonty studies try to use only completely unworn teeth, which are difficult to find in the fossil record. We find that community-level hypsodonty did change over time, but not in ways that corresponded with established precipitation values at Natural Trap Cave. There were likely other factors driving hypsodonty levels within this community, such as an increasing abundance of grasses with increases in temperature and precipitation. Tooth wear did not seem to have significant effects on hypsodonty measurements across time, and tooth wear only sometimes significantly affected hypsodonty measurements across taxa. With further analysis, it might be conclusively decided that samples can be expanded to somewhat worn teeth. This analysis of hypsodonty as a climate proxy can help shape both its use in future studies and our understanding of how species will respond to future climate changes.
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在怀俄明州的天然陷阱洞穴,小型哺乳动物的假说比率不能追踪降水变化
随着未来的气候变化,干旱事件预计会增加。低齿畸形是食草哺乳动物对高冠牙齿的一种适应,因为高冠牙齿能更好地处理粗糙的食物。通常,长着高度下尖牙的动物生活在干旱地区。这一特性被认为是对干旱的适应。许多研究都考察了有蹄类动物和Glires(啮齿动物和足形动物)中关于气候的假说的空间分布。然而,很少有研究考察空间趋势是否在单一地点的已知气候变化中发挥作用。Glires比有蹄类动物早进化了几百万年,由于一代时间短,适应能力强,而且生活范围相对较小,因此它们可以提供更准确的气候预测。在这里,我们使用来自WY自然陷阱洞穴的Glires来研究群落水平的变化是否反映了已知的降水变化。此外,本研究还调查了测量技术(牙齿在颌内与下颌外)和牙齿磨损对下颌缺损测量的影响。目前,大多数假牙研究试图只使用完全未磨损的牙齿,这在化石记录中很难找到。我们发现,随着时间的推移,群落水平的假说确实发生了变化,但与自然陷阱洞的既定降水值不一致。可能还有其他因素推动了这个群落的低密度水平,比如随着温度和降水的增加,草的丰度也在增加。牙齿磨损似乎对不同时间的下颌测量没有显着影响,并且牙齿磨损只是有时显着影响不同分类群的下颌测量。通过进一步的分析,可能会最终确定样本可以扩展到有些磨损的牙齿。对假说作为气候代用物的分析有助于塑造其在未来研究中的应用,以及我们对物种如何应对未来气候变化的理解。
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