Modeling Dragons: Using linked mechanistic physiological and microclimate models to explore environmental, physiological, and morphological constraints on the early evolution of dinosaurs
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 withi...
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| creator | Lovelace, David M Hartman, Scott A Mathewson, Paul D Linzmeier, Benjamin J Porter, Warren P |
| description | 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. |
| doi_str_mv | 10.1371/journal.pone.0223872 |
| format | Article |
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This is in agreement with the Late Triassic fossil record and may have contributed to the latitudinal gap in the Triassic prosauropod record.</description><identifier>ISSN: 1932-6203</identifier><identifier>EISSN: 1932-6203</identifier><identifier>DOI: 10.1371/journal.pone.0223872</identifier><identifier>PMID: 32469936</identifier><language>eng</language><publisher>United States: Public Library of Science</publisher><subject>Biological research ; Biology ; Biology and Life Sciences ; Body temperature ; Boundary conditions ; Computer simulation ; Dinosaurs ; Earth science ; Earth Sciences ; Ecology and Environmental Sciences ; Environment models ; Extinction ; Heat ; Heat tolerance ; Humidity ; Hypotheses ; Insulation ; Medicine and Health Sciences ; Metabolic rate ; Metabolism ; Microclimate ; Microclimate models ; Morphology ; Natural history ; Niches ; Organisms ; Paleobiogeography ; Paleolatitude ; Phylogenetics ; Physical Sciences ; Physics ; Physiological aspects ; Physiology ; Precipitation ; Sensitivity analysis ; Temperate environments ; Temperature range ; Triassic ; Triassic period</subject><ispartof>PloS one, 2020-05, Vol.15 (5), p.e0223872-e0223872</ispartof><rights>COPYRIGHT 2020 Public Library of Science</rights><rights>2020 Lovelace et al. This is an open access article distributed under the terms of the Creative Commons Attribution License: http://creativecommons.org/licenses/by/4.0/ (the “License”), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. 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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.</description><subject>Biological research</subject><subject>Biology</subject><subject>Biology and Life Sciences</subject><subject>Body temperature</subject><subject>Boundary conditions</subject><subject>Computer simulation</subject><subject>Dinosaurs</subject><subject>Earth science</subject><subject>Earth Sciences</subject><subject>Ecology and Environmental Sciences</subject><subject>Environment models</subject><subject>Extinction</subject><subject>Heat</subject><subject>Heat tolerance</subject><subject>Humidity</subject><subject>Hypotheses</subject><subject>Insulation</subject><subject>Medicine and Health Sciences</subject><subject>Metabolic rate</subject><subject>Metabolism</subject><subject>Microclimate</subject><subject>Microclimate models</subject><subject>Morphology</subject><subject>Natural 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| subjects | Biological research Biology Biology and Life Sciences Body temperature Boundary conditions Computer simulation Dinosaurs Earth science Earth Sciences Ecology and Environmental Sciences Environment models Extinction Heat Heat tolerance Humidity Hypotheses Insulation Medicine and Health Sciences Metabolic rate Metabolism Microclimate Microclimate models Morphology Natural history Niches Organisms Paleobiogeography Paleolatitude Phylogenetics Physical Sciences Physics Physiological aspects Physiology Precipitation Sensitivity analysis Temperate environments Temperature range Triassic Triassic period |
| title | Modeling Dragons: Using linked mechanistic physiological and microclimate models to explore environmental, physiological, and morphological constraints on the early evolution of dinosaurs |
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