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建模恐龙:利用链接的机械生理和微气候模型来探索环境、生理和形态对恐龙早期进化的限制。

Modeling Dragons: Using linked mechanistic physiological and microclimate models to explore environmental, physiological, and morphological constraints on the early evolution of dinosaurs.

机构信息

University of Wisconsin Geology Museum, Department of Geosciences, University of Wisconsin-Madison, Madison, Wisconsin, United States of America.

Department of Geoscience, University of Wisconsin-Madison, Madison, Wisconsin, United States of America.

出版信息

PLoS One. 2020 May 29;15(5):e0223872. doi: 10.1371/journal.pone.0223872. eCollection 2020.

Abstract

We employed the widely-tested biophysiological modeling software, Niche Mapper™ to investigate the metabolic function of the Late Triassic dinosaurs Plateosaurus and Coelophysis during global greenhouse conditions. We tested a variety of assumptions about resting metabolic rate, each evaluated within six microclimate models that bound paleoenvironmental conditions at 12° N paleolatitude, as determined by sedimentological and isotopic proxies for climate within the Chinle Formation of the southwestern United States. Sensitivity testing of metabolic variables and simulated "metabolic chamber" analyses support elevated "ratite-like" metabolic rates and intermediate "monotreme-like" core temperature ranges in these species of early saurischian dinosaur. Our results suggest small theropods may have needed partial to full epidermal insulation in temperate environments, while fully grown prosauropods would have likely been heat stressed in open, hot environments and should have been restricted to cooler microclimates such as dense forests or higher latitudes and elevations. This is in agreement with the Late Triassic fossil record and may have contributed to the latitudinal gap in the Triassic prosauropod record.

摘要

我们使用了经过广泛测试的生物生理建模软件 Niche Mapper™ 来研究晚三叠世恐龙板龙和腔骨龙在全球温室条件下的代谢功能。我们测试了关于静息代谢率的各种假设,每个假设都在六个微气候模型中进行了评估,这些模型的边界条件是美国西南部奇尔岩层的古环境条件,由沉积物学和气候同位素示踪剂确定。代谢变量的敏感性测试和模拟的“代谢室”分析支持这些早期蜥脚形亚目恐龙具有升高的“似平胸鸟类”代谢率和中等的“似单孔类动物”核心温度范围。我们的结果表明,小型兽脚类恐龙在温带环境中可能需要部分到完全的表皮隔热,而完全生长的蜥脚类恐龙在开阔、炎热的环境中可能会受到热压力,并且应该局限于较凉爽的微气候,如茂密的森林或更高的纬度和海拔。这与晚三叠世的化石记录一致,可能导致了三叠纪蜥脚形亚目恐龙记录中的纬度差距。

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