在更新世末期生态系统崩溃中,土狼揭示了基线氮的下降

L. Desantis, J. Meachen, Joshua H. Miller, R. Dunn, E. Lindsey, M. Pardi, J. Southon, W. Binder, J. Cohen, F. O’Keefe, Elsa Muller, Elizabeth Hall, Solathus Johnson, Benjamin Fuller, A. Farrell, G. Takeuchi
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引用次数: 0

摘要

更新世末期是一个生态动荡的时期,与环境变化、物种灭绝和人类对景观的影响同时发生。作为更新世为数不多的持续存在的掠食者之一,拉布雷亚的土狼(Canis latrans)的特殊记录为阐明最近记录的生态系统状态转变如何影响幸存者提供了一个独特的机会。通过对过去5万年至今兰乔拉布雷亚土狼的多代理分析,我们分析了100多个个体的放射性碳年代学、稳定同位素、牙齿微磨损和形态,以评估大型动物灭绝对这些食肉动物的影响。最值得注意的是,土狼的δ15Nbone胶原蛋白值在巨型动物灭绝后立即显著下降。虽然这种下降表明饮食从更多肉类到更少肉类的变化,但来自一小部分样本的氨基酸稳定同位素提供了氮基线变化的证据,表明营养资源的可获得性发生了大规模变化。根据牙釉质稳定碳同位素和牙齿微磨损结构分析推断,土狼的饮食在灭绝边界上没有明显变化,但δ18牙釉质和δ13Cbone胶原蛋白稳定氧同位素的显著变化表明潜在猎物资源发生了更细微的变化。土狼也表现出体型的线性下降,这种下降开始于当地巨型动物灭绝之前(约2万年前),可能是为了应对与大型犬科动物的竞争,大型猎物的减少,以及/或在此期间同时干旱的增加。在过去的一个世纪里,森林猎物(如鹿)的食腐性急剧增加,与过去5万年中所占据的饮食生态位明显不同,这意味着人类行为对土狼的巨大影响,它们的生态角色最近发生了转变,以及这些食肉动物的高度适应性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Coyotes Reveal Baseline Nitrogen Decline Across End-Pleistocene Ecosystem Collapse
The end Pleistocene was a time of ecological turmoil, coincident with environmental change, extinctions, and anthropogenic impacts on the landscape. As one of the few persisting predators from the Pleistocene, La Brea’s exceptional record of coyotes (Canis latrans) provides a unique opportunity to clarify how a recently documented ecosystem state-shift impacted survivors. Through a multiproxy analysis of Rancho La Brea coyotes from the past 50,000 years to present, we analyzed over 100 individuals for radiocarbon chronologies, stable isotopes, dental microwear, and morphology to assess the consequences of megafaunal extirpation on these predators. Most notably, coyotes demonstrate a significant decline in δ15Nbone collagen values immediately after the extirpation of megafauna. While this decline is suggestive of a change in diet from more to less meat, stable isotopes of amino acids from a subset of samples instead provide evidence of a baseline shift in nitrogen—indicating large scale changes in the availability of nutritional resources. While coyotes do not demonstrate notable changes in diet across the extirpation boundary, as inferred from stable carbon isotopes in tooth enamel and dental microwear texture analysis, significant shifts in stable oxygen isotopes in δ18Oenamel and δ13Cbone collagen indicate more nuanced changes in potential prey-resources. Coyotes also demonstrate a linear decline in body size that begins prior to the local extirpation of megafauna (~20,000 years ago) and may be in response to competition with larger canids, the decline in large prey, and/or concurrent increases in aridity during this interval. A dramatic increase in scavenging of forested prey (e.g., deer) during the past century stands out as significantly distinct from the dietary niches occupied over the past 50,000 years—implying dramatic impacts of human behavior on coyotes, a recent shift in their ecological role, and the highly adaptable nature of these carnivores.
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