Volcanism and basalt weathering drove Ordovician climatic cooling. [PDF]
Zhao H +5 more
europepmc +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
Soft robotics informs how an early echinoderm moved. [PDF]
Desatnik R +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
Cold low-latitude Ordovician paleotemperatures may be in hot water. [PDF]
Grossman EL +5 more
europepmc +1 more source
Graptolites of the Králův Dvůr Formation (mid Katian to earliest Hirnantian, Czech Republic) [PDF]
P. Kraft, P. Štorch, C.E. Mitchell
openaire +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
Spore assemblages from Upper Ordovician and Lowermost Silurian sediments recovered from the Qusaiba-1 shallow core hole, Qasim region, central Saudi Arabia [PDF]
Miller, M.A. +2 more
core +1 more source
Odontopleurid trilobites of the Katian/Hirnantian boundary interval in the Prague Basin (Bohemia) [PDF]
openaire +1 more source
Evidence for cryptic molting behavior in the trilobite Toxochasmops vormsiensis from the Upper Ordovician Katian Kõrgessaare Formation, Estonia. [PDF]
Bicknell RDC +3 more
europepmc +1 more source

