, 2006 Vertebrate micro-remains of jawless vertebrates (psammosteid heterostracans) and gnathostomes (acanthodians and sarcopterygians) occur in a residue collected from the Late Devonian Kap Graah Group sandstones of East Greenland.
Carlsson, A., Marshall, J.E.A., Blom, H.
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Reconstruction of feeding behaviour and diet in Devonian ctenacanth chondrichthyans using dental microwear texture and finite element analyses. [PDF]
R Soc Open SciGreif M +5 more
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The early diversification of ray-finned fishes (Actinopterygii): hypotheses, challenges and future prospects. [PDF]
Biol Rev Camb Philos Soc, 2023 Henderson S +3 more
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New ovulate cupule further informs the relationships among early seed plants and their adaptation to wind pollination. [PDF]
Proc Biol SciLi BX +6 more
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Marine biodiversity was greater in the presence of ecosystem engineers throughout the Phanerozoic. [PDF]
Nat CommunCribb AT, Darroch SAF, Gearty W.
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Mechanisms of global climate change during the five major mass extinctions. [PDF]
Sci RepKaiho K.
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Significant fluctuation in the global sulfate reservoir and oceanic redox state during the Late Devonian event. [PDF]
PNAS Nexus, 2022 Cai C, Xu C, Fakhraee M, Chen D, Peng Y.
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Fern-like Plants Establishing the Understory of the Late Devonian Xinhang Lycopsid Forest. [PDF]
Life (Basel)Yang J, Wang D, Liu L, Zhou Y.
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Niche conservatism and ecological change during the Late Devonian mass extinction. [PDF]
Proc Biol Sci, 2023 Brisson SK +4 more
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In situ forest with lycopsid trees bearing lobed rhizomorphs from the Upper Devonian of Lincheng, China. [PDF]
PNAS NexusQin M, Wang D, Liu L, Liu L, Zhou Y.
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