about
Sulfur record of rising and falling marine oxygen and sulfate levels during the Lomagundi event.Sulfur isotopes track the global extent and dynamics of euxinia during Cretaceous Oceanic Anoxic Event 2.Evidence for rapid weathering response to climatic warming during the Toarcian Oceanic Anoxic Event.Oceanic oxygenation events in the anoxic Ediacaran ocean.Constraining the rate of oceanic deoxygenation leading up to a Cretaceous Oceanic Anoxic Event (OAE-2: ~94 Ma).Thallium isotopes reveal protracted anoxia during the Toarcian (Early Jurassic) associated with volcanism, carbon burial, and mass extinctionRapid recovery of life at ground zero of the end-Cretaceous mass extinctionTracking the rise of eukaryotes to ecological dominance with zinc isotopesFully oxygenated water columns over continental shelves before the Great Oxidation EventAbsence of biomarker evidence for early eukaryotic life from the Mesoproterozoic Roper Group: Searching across a marine redox gradient in mid-Proterozoic habitability
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description
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Jeremy D Owens
@ast
Jeremy D Owens
@en
Jeremy D Owens
@es
Jeremy D Owens
@nl
type
label
Jeremy D Owens
@ast
Jeremy D Owens
@en
Jeremy D Owens
@es
Jeremy D Owens
@nl
prefLabel
Jeremy D Owens
@ast
Jeremy D Owens
@en
Jeremy D Owens
@es
Jeremy D Owens
@nl
P108
P106
P31
P496
0000-0002-0530-2177