Permo-Triassic tetrapods and their climate implications
Permo-Triassic tetrapods and their climate implications
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DOI:
10.1016/j.gloplacha.2021.103618
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发表时间:
2021-10
影响因子:
3.9
通讯作者:
Jun Liu;K. Angielczyk;F. Abdala
中科院分区:
文献类型:
--
作者:
Jun Liu;K. Angielczyk;F. Abdala
The narrow active temperature ranges of ectothermic tetrapods can be used as proxies for reconstructing paleoclimates. Here we deduce the climatic preferences of major Permo-Triassic tetrapod groups based on their known geographic distributions, the critical thermal limits of living tetrapods, and paleoclimate information from other sources. The resulting preferred temperature sequence of amniotes places most Triassic archosauromorphs at the high end of the spectrum, with preferred temperatures over 32 °C in some cases, followed by captorhinids, pareiasaurs, procolophonids, cynognathian cynodonts, dicynodonts (excludingLystrosaurus),Proterosuchus fergusi,and finallyLystrosaurusat the lowest preferred temperature. The poleward distribution of PermianLystrosaurusmarks the border of cool temperate climates, whereas TriassicLystrosaurusdelineates the border of the arid zone. Most temnospondyls indicate the availability of perennial water sources. Captorhinids and pareiasaurs preferred dry climates, whereas dicynodonts preferred wetter conditions. Based on current evidence, central Pangea transitioned from an arid zone to a tropical zone during the late Olenekian.