Describing a Newly Excavated Packrat Midden Near Natural Trap Cave, Wyoming to Help Assess Biases in Fossil Microfaunal Accumulation

Michael Sketel, Jenny L. McGuire, Julia A. Schap, Rachel A. Short
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Abstract

Microfauna communities resulting from packrat accumulation provide crucial information about how natural communities respond to environmental changes. However, fossil accumulation mechanisms can be complex, making it difficult to interpret these community responses. Natural Trap Cave (NTC) is an open-mouth cave with an 85-foot drop that often lies unseen by passing animals, making it a major location for fossil accumulation. NTC, located in the Bighorn Mountains of Wyoming, has accumulated a paleontological record of the local community’s biota dating back to the Late Pleistocene, 25,000 years ago. The rim of the cave’s mouth is home to packrat middens located directly above the major deposits of microvertebrate (<5 kg) fossils. It is hypothesized that middens along the rim have accumulated seeds, bones, teeth, and bird pellets from the local communities over time and have periodically washed into the cave below. We seek to assess the bias in microvertebrate community composition introduced by packrat accumulation. We identified bones and teeth collected from a 9-section grid of a modern midden located adjacent to the cave, which allow us to see which species dominate the NTC environment. We calculate species evenness, richness, and relative abundances using MNI. To assess local bias resulting from packrat accumulation, we compare the modern midden with live-and camera-trap data of small mammal communities. To assess which NTC fossils result from packrat accumulation, we compare the modern midden with fossil material from within the cave, ranging in age from 2 to 20 ka. Once we understand these biases present in the fossil accumulation, we can associate species’ relative abundances with changes in climate, such as drought, increasing temperatures, and flooding. By knowing how climate has affected NTC species’ abundances through time, we will be prepared to aid in conservation efforts by predicting how species numbers will be affected by future climate change.
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描述怀俄明州自然陷阱洞附近新挖掘的背包鼠巢穴,以帮助评估化石微动物积累的偏见
由鼠群积累形成的小动物群落提供了关于自然群落如何响应环境变化的重要信息。然而,化石积累机制可能很复杂,因此很难解释这些群落的反应。天然陷阱洞穴(NTC)是一个开口的洞穴,有85英尺的落差,经常被路过的动物看不见,使其成为化石堆积的主要地点。NTC位于怀俄明州的大角山,已经积累了当地社区生物群的古生物学记录,可以追溯到25000年前的晚更新世。洞穴口的边缘是包鼠的巢穴,位于主要的微脊椎动物(小于5公斤)化石沉积物的正上方。据推测,随着时间的推移,沿着边缘的丘堆积累了当地社区的种子、骨头、牙齿和鸟丸,并定期被冲入下面的洞穴。我们试图评估小脊椎动物群落组成的偏差,这是由背包鼠积累引起的。我们鉴定了从靠近洞穴的现代洞穴的9段网格中收集的骨骼和牙齿,这使我们能够看到哪些物种主导了NTC环境。我们使用MNI计算物种均匀度、丰富度和相对丰度。为了评估鼠群聚集造成的局部偏差,我们将现代鼠穴与小型哺乳动物群落的现场数据和相机陷阱数据进行了比较。为了评估哪些NTC化石是由背包鼠堆积形成的,我们将现代midden与洞穴内的化石材料进行了比较,这些化石的年龄从2到20 ka不等。一旦我们了解了化石积累中存在的这些偏差,我们就可以将物种的相对丰度与气候变化联系起来,比如干旱、气温升高和洪水。通过了解气候如何随着时间的推移影响NTC物种的丰度,我们将准备通过预测物种数量如何受到未来气候变化的影响来帮助保护工作。
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