Results 111 to 120 of about 1,129 (198)

Uppermost Ordovician (upper Katian-Hirnantian) graptolites of north-central Nevada, U.S.A. [PDF]

open access: yesBulletin of Geosciences, 2011
P. Štorch   +3 more
openaire   +1 more source

Volcanism and basalt weathering drove Ordovician climatic cooling. [PDF]

open access: yesNat Commun
Zhao H   +5 more
europepmc   +1 more source

Dynamics of Silurian Plants as Response to Climate Changes. [PDF]

open access: yesLife (Basel), 2021
Pšenička J   +5 more
europepmc   +1 more source

Dynamic redox-promoted iron and nutrient cycling drove graptolite evolution across the Ordovician-Silurian transition. [PDF]

open access: yesSci Adv
Qiu Z   +10 more
europepmc   +1 more source

Tempo of the Late Ordovician mass extinction controlled by the rate of climate change. [PDF]

open access: yesSci Adv
Zhang Z   +10 more
europepmc   +1 more source

Deep-sea Ordovician lingulide brachiopods and their associated burrows suggest an early colonization of proximal turbidite systems. [PDF]

open access: yesSci Rep, 2023
Paz M   +7 more
europepmc   +1 more source

Cold low-latitude Ordovician paleotemperatures may be in hot water. [PDF]

open access: yesProc Natl Acad Sci U S A
Grossman EL   +5 more
europepmc   +1 more source

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