Whitney MR, Sidor CA. Evidence of torpor in the tusks of Lystrosaurus from the Early Triassic of Antarctica.
Commun Biol 2020;
3:471. [PMID:
32855434 PMCID:
PMC7453012 DOI:
10.1038/s42003-020-01207-6]
[Citation(s) in RCA: 13] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/05/2020] [Accepted: 08/01/2020] [Indexed: 11/16/2022] Open
Abstract
Antarctica has hosted a wide range of ecosystems over the past 500-million years. Early in the Mesozoic, the Antarctic portion of southern Pangaea had a more habitable climate, but its position within the polar circle imposed extreme photoperiod seasonality on its resident flora and fauna. It remains unclear to what degree physiological adaptations underpinned the ability of tetrapods to establish the terrestrial communities captured in the fossil record. Here we use regular and stressful growth marks preserved in the dentine of ever-growing tusks of the Early Triassic mammalian predecessor, Lystrosaurus, to test for adaptations specific to this polar inhabitant. We find evidence of prolonged stress indicative of torpor when compared to tusk samples from non-polar populations of Lystrosaurus. These preliminary findings are to our knowledge the oldest instance of torpor yet reported in the fossil record and demonstrate unexpected physiological flexibility in Lystrosaurus that may have contributed its survivorship through the Permo-Triassic mass extinction.
Whitney and Sidor examine the growth marks on Lystrosaurus tusks from the Early Triassic, and demonstrate evidence of torpor in polar specimens. These preliminary findings give insight into physiological adaptations that could have aided in survival and recovery from the Permo-Triassic mass extinction.
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