Results 111 to 120 of about 893 (201)
Hydrological control of river and seawater lithium isotopes. [PDF]
Zhang F +7 more
europepmc +1 more source
Rocks in the Late Ordovician paleotropics commonly exhibit the now well-known, positive Hirnantian Isotopic Carbon Excursion (HICE). This event is coincident with both continental scale glaciation in Gondwana and dramatic extinction across the marine ...
Holmden, C. +4 more
core
<p>Climatic simulation conducted using the general circulation model FOAM for the Late Ordovician (440 Ma; Hirnantian); using the same model setup as [<a href="https://doi.org/10.1038/s41467-023-41685-w">10.1038/s41467-023-41685-w</a>],
Pohl, Alexandre
core +1 more source
Hirnantian Trilobites and Brachiopods in Space and Time
A W Owen, D A T Harper, R Jia-yu
openaire +1 more source
Dynamic redox-promoted iron and nutrient cycling drove graptolite evolution across the Ordovician-Silurian transition. [PDF]
Qiu Z +10 more
europepmc +1 more source
Persistent global marine euxinia in the early Silurian. [PDF]
Stockey RG +5 more
europepmc +1 more source
Tempo of the Late Ordovician mass extinction controlled by the rate of climate change. [PDF]
Zhang Z +10 more
europepmc +1 more source
Mass extinction triggered the early radiations of jawed vertebrates and their jawless relatives (gnathostomes). [PDF]
Hagiwara W, Sallan L.
europepmc +1 more source
Mechanisms of global climate change during the five major mass extinctions. [PDF]
Kaiho K.
europepmc +1 more source
Large mass-independent sulphur isotope anomalies link stratospheric volcanism to the Late Ordovician mass extinction. [PDF]
Hu D +5 more
europepmc +1 more source

