, 2013 The Late Ordovician mass extinction was linked to climate cooling and glaciation of Gondwana during the terminal Ordovician Hirnantian Age (444.7–443.4 Ma).
Fischer, Woodward +4 more
core
Recurring marine phosphorus spikes during major palaeozoic mass extinctions and climate change. [PDF]
Nat CommunDodd MS +14 more
europepmc +1 more source
Ocean temperatures through the Phanerozoic reassessed. [PDF]
Sci Rep, 2022 Grossman EL, Joachimski MM.
europepmc +1 more source
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.
europepmc +1 more source
Late Ordovician Mass Extinction: Earth, fire and ice. [PDF]
Natl Sci RevHarper DAT.
europepmc +1 more source
Preservation bias obscures gradual Ordovician reef evolution. [PDF]
Proc Natl Acad Sci U S AJeon J, Li QJ, Lee JH.
europepmc +1 more source
Clay minerals evidences for cold-warm fluctuations in the Early Silurian. [PDF]
PLoS OneZhang Z +5 more
europepmc +1 more source
On the enigma of Palaenigma wrangeli (Schmidt), a conulariid with a partly non-mineralized skeleton. [PDF]
PeerJ, 2021 Kröger B +5 more
europepmc +1 more source
Reconstruction of Phanerozoic climate using carbonate clumped isotopes and implications for the oxygen isotopic composition of seawater. [PDF]
Proc Natl Acad Sci U S AThiagarajan N +6 more
europepmc +1 more source
Selectivity and the effect of mass extinctions on disparity and functional ecology. [PDF]
Sci Adv, 2021 Cole SR, Hopkins MJ.
europepmc +1 more source