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<i>Prototaxites</i> fossils are structurally and chemically distinct from extinct and extant Fungi. [PDF]
Sci AdvLoron CC +13 more
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Mechanisms of global climate change during the five major mass extinctions. [PDF]
Sci RepKaiho K.
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Episodic body size variations of early Paleozoic trilobites associated with marine redox changes. [PDF]
Sci AdvSun Z, Zhao F, Zeng H, Erwin DH, Zhu M.
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The possible adaption of the human respiratory system to past atmospheres. [PDF]
Exp PhysiolCannell A.
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Marine ostracod faunas through the Late Devonian extinction events. Part II: the Hangenberg event
Earth-Science ReviewsGuillam, Elvis, Forel, Marie-Béatrice
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Role of volcanism and impact heating in mass extinction climate shifts. [PDF]
Sci RepKaiho K.
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Distinct causes underlie double-peaked trilobite morphological disparity
Drage HB, Pates S.
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Rapid canalisation of mandible structure in Tetrapoda
Watt EC, Felice RN, Goswami A.
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Basin-scale reconstruction of euxinia and Late Devonian mass extinctions
Nature, 2023The Devonian-Carboniferous transition marks a fundamental shift in the surface environment primarily related to changes in ocean-atmosphere oxidation states1,2, resulting from the continued proliferation of vascular land plants that stimulated the hydrological cycle and continental weathering3,4, glacioeustasy5,6, eutrophication and anoxic expansion in
Swapan K. Sahoo +8 more
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