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The Latitudinal Diversity Gradient of Tetrapods Across the Permo-Triassic Mass Extinction and Recovery Interval

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The Latitudinal Diversity Gradient of Tetrapods Across the Permo-Triassic Mass Extinction and Recovery Interval This is a repository copy of The latitudinal diversity gradient of tetrapods across the Permo-Triassic mass extinction and recovery interval. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/161099/ Version: Supplemental Material Article: Allen, BJ orcid.org/0000-0003-0282-6407, Wignall, PB orcid.org/0000-0003-0074-9129, Hill, DJ orcid.org/0000-0001-5492-3925 et al. (2 more authors) (2020) The latitudinal diversity gradient of tetrapods across the Permo-Triassic mass extinction and recovery interval. Proceedings of the Royal Society B: Biological Sciences, 287 (1929). 20201125. ISSN 0962-8452 https://doi.org/10.1098/rspb.2020.1125 © 2020 The Author(s). Published by the Royal Society. All rights reserved. This is an author produced version of an article published in Proceedings of the Royal Society B: Biological Sciences. Uploaded in accordance with the publisher's self-archiving policy. Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ S A BJ T PT P R S B DOI T N T 80°S 60°S 40°S 20°S 0° 20°N 40°N 60°N 80°N T Middle Ladinian 54 1 76 21 3 Triassic Anisian 11 150 7 2 35 74 86 Early Olenekian 6 35 13 6 48 95 1 Triassic Induan 21 76 1 2 38 Late Changhsingian 37 6 30 79 Permian Wuchiapingian 497 3 32 55 M 80°S 60°S 40°S 20°S 0° 20°N 40°N 60°N 80°N T Middle Ladinian 1 4 4 108 1 Triassic Anisian 7 24 93 2 Early Olenekian 1 25 9 Triassic Induan F 80°S 60°S 40°S 20°S 0° 20°N 40°N 60°N 80°N T Middle Ladinian 1 19 Triassic Anisian 5 22 13 Early Olenekian 1 12 13 Triassic Induan 1 1 Late Changhsingian 1 Permian Wuchiapingian S A BJ T PT P R S B DOI T M T 80°S 60°S 40°S 20°S 0° 20°N 40°N 60°N 80°N M Middle Ladinian 1.77 1 2.25 3.13 3 Triassic Anisian 3 2.04 1.43 1 1.61 1.49 2.69 Early Olenekian 1.5 1.6 1.27 1.17 1.96 1.83 1 Triassic Induan 2.09 2.87 1 1 1.35 Late Changhsingian 2.5 2.67 5 3.16 Permian Wuchiapingian 3.17 2 1.79 3.24 M 80°S 60°S 40°S 20°S 0° 20°N 40°N 60°N 80°N M Middle Ladinian 1 2.67 2 2.67 1 Triassic Anisian 2.75 1.14 1.68 1 Early Olenekian 1 1.35 1.13 Triassic Induan F 80°S 60°S 40°S 20°S 0° 20°N 40°N 60°N 80°N M Middle Ladinian 1 1.17 Triassic Anisian 2.5 1.95 2.83 Early Olenekian 1 3 2.67 Triassic Induan 1 1 Late Changhsingian 1 Permian Wuchiapingian S A BJ T PT P R S B DOI T N T 80°S 60°S 40°S 20°S 0° 20°N 40°N 60°N 80°N T Middle Ladinian 5 1 15 5 1 Triassic Anisian 3 22 3 3 11 20 14 Early Olenekian 4 11 5 3 15 29 1 Triassic Induan 7 17 1 2 18 Late Changhsingian 9 2 6 17 Permian Wuchiapingian 32 1 5 11 M 80°S 60°S 40°S 20°S 0° 20°N 40°N 60°N 80°N T Middle Ladinian 1 2 3 30 2 Triassic Anisian 1 12 26 2 Early Olenekian 1 12 4 Triassic Induan F 80°S 60°S 40°S 20°S 0° 20°N 40°N 60°N 80°N T Middle Ladinian 2 6 Triassic Anisian 1 9 5 Early Olenekian 1 5 5 Triassic Induan 1 1 Late Changhsingian 1 Permian Wuchiapingian.
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