Marine biodiversity was greater in the presence of ecosystem engineers throughout the Phanerozoic. [PDF]
Cribb AT, Darroch SAF, Gearty W.
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Persistent global marine euxinia in the early Silurian. [PDF]
Stockey RG +5 more
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Mass extinction triggered the early radiations of jawed vertebrates and their jawless relatives (gnathostomes). [PDF]
Hagiwara W, Sallan L.
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Mechanisms of global climate change during the five major mass extinctions. [PDF]
Kaiho K.
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Ocean temperatures through the Phanerozoic reassessed. [PDF]
Grossman EL, Joachimski MM.
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Transitions between persistent climate-carbon regimes coincide with elevated Phanerozoic biosphere vulnerability. [PDF]
Sudakow I +5 more
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Mercury Spikes Indicate a Volcanic Trigger for the Late Ordovician Mass Extinction Event: An Example from a Deep Shelf of the Peri-Baltic Region. [PDF]
Smolarek-Lach J +3 more
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Silurian Climatic Zonation of Cryptospore, Trilete Spore and Plant Megafossils, with Emphasis on the Přídolí Epoch. [PDF]
Bek J +3 more
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Abrupt global-ocean anoxia during the Late Ordovician-early Silurian detected using uranium isotopes of marine carbonates. [PDF]
Bartlett R +5 more
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Correction to 'The evolutionary dynamics of the Early Palaeozoic marine biodiversity accumulation'. [PDF]
Kröger B, Franeck F, Rasmussen CMØ.
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