Published July 26, 2010
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Figure 1 in Do extraordinarily high growth rates in Permo-Triassic dicynodonts (Therapsida, Anomodontia) explain their success before and after the end-Permian extinction?
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Figure 1. Stratigraphical ranges of the anomodonts used in this study. Modified from Angielczyk & Kurkin (2003) and Angielczyk & Walsh (2008). Oudenodon range updated from Botha & Angielczyk (2007). Kingoria is now referred to as Dicynodontoides following Angielczyk et al. (2009). Vertical solid bars and open bars indicate ranges and ghost lineages, respectively. Abbreviations: Chsn, Changhsingian; Ciste., Cistecephalus Assemblage Zone; Eodicyn., Eodicynodon Assemblage Zone; Ind., Induan; Lystro., Lystrosaurus; Olen., Olenekian; Prist., Pristerognathus Assemblage Zone; PTB, Permo-Triassic boundary; Tap., Tapinocephalus Assemblage Zone; Tropid. Tropidostoma Assemblage Zone; Wn, Wordian. Numbers indicate million years ago. Stratigraphical chart follows Catuneanu et al. (2005).
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Published as part of Botha-Brink, Jennifer & Angielczyk, Kenneth D., 2010, Do extraordinarily high growth rates in Permo-Triassic dicynodonts (Therapsida, Anomodontia) explain their success before and after the end-Permian extinction?, pp. 341-365 in Zoological Journal of the Linnean Society 160 (2) on page 343, DOI: 10.1111/j.1096-3642.2009.00601.x, http://zenodo.org/record/5439764
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- Journal article: 10.1111/j.1096-3642.2009.00601.x (DOI)
- Journal article: urn:lsid:plazi.org:pub:FFD6FFA1AB20F06CFFA9FFFB2758FFC7 (LSID)
- Journal article: http://publication.plazi.org/id/FFD6FFA1AB20F06CFFA9FFFB2758FFC7 (URL)
- Journal article: https://zenodo.org/record/5439764 (URL)