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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Large mass-independent sulphur isotope anomalies link stratospheric volcanism to the Late Ordovician mass extinction. [PDF]
Hu D +5 more
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Ocean temperatures through the Phanerozoic reassessed. [PDF]
Grossman EL, Joachimski MM.
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Episodic body size variations of early Paleozoic trilobites associated with marine redox changes. [PDF]
Sun Z, Zhao F, Zeng H, Erwin DH, Zhu M.
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Late Ordovician Mass Extinction: Earth, fire and ice. [PDF]
Harper DAT.
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Preservation bias obscures gradual Ordovician reef evolution. [PDF]
Jeon J, Li QJ, Lee JH.
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On the enigma of Palaenigma wrangeli (Schmidt), a conulariid with a partly non-mineralized skeleton. [PDF]
Kröger B +5 more
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Clay minerals evidences for cold-warm fluctuations in the Early Silurian. [PDF]
Zhang Z +5 more
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Reconstruction of Phanerozoic climate using carbonate clumped isotopes and implications for the oxygen isotopic composition of seawater. [PDF]
Thiagarajan N +6 more
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