On the stratigraphic position of the Famennian and Tournaisian fossil vertebrate beds in Andreyevka, Tula Region, Central Russia
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Cited by (43)
Late Devonian and Early Carboniferous alpha diversity, ecospace occupation, vertebrate assemblages and bio-events of southeastern Morocco
2018, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :This is in accordance with the global fossil record of vertebrates. With a few exceptions (Alekseev et al., 1994), early Tournaisian vertebrates are globally rare and even the extremely diverse late Famennian gnathostome fauna of the Cleveland Shales vanished entirely (Hansen, 1996; Friedman and Sallan, 2012). Environmental perturbations during the late Famennian might have strongly affected the ecosystem but the environment in the Tournaisian itself was probably not suitable for a diverse gnathostome ecosystem.
Overview of the emergence of tetrapods
2009, Comptes Rendus - PalevolMississippian δ<sup>13</sup>C<inf>carb</inf> and conodont apatite δ<sup>18</sup>O records - Their relation to the Late Palaeozoic Glaciation
2008, Palaeogeography, Palaeoclimatology, PalaeoecologyGeochemical evidence for major environmental change at the Devonian-Carboniferous boundary in the Carnic Alps and the Rhenish Massif
2006, Palaeogeography, Palaeoclimatology, Palaeoecology
Copyright © 1994 The Geologists' Association. Published by Elsevier Ltd. All rights reserved.