Uppermost Ordovician (upper Katian-Hirnantian) graptolites of north-central Nevada, U.S.A. [PDF]
P. Štorch +3 more
openaire +1 more source
Conodont and graptolites from the Oberbuchach I and Oberbuchach Ib sections (Katian-Lochkovian)
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Schönlaub, H. P., CORRADINI, CARLO
openaire +2 more sources
Volcanism and basalt weathering drove Ordovician climatic cooling. [PDF]
Zhao H +5 more
europepmc +1 more source
Dynamics of Silurian Plants as Response to Climate Changes. [PDF]
Pšenička J +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
Tempo of the Late Ordovician mass extinction controlled by the rate of climate change. [PDF]
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]
Paz M +7 more
europepmc +1 more source
Cold low-latitude Ordovician paleotemperatures may be in hot water. [PDF]
Grossman EL +5 more
europepmc +1 more source
Changes in palaeoclimate and palaeoenvironment in the Upper Yangtze area (South China) during the Ordovician-Silurian transition. [PDF]
Men X, Mou C, Ge X.
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

