Results 121 to 130 of about 1,784 (228)

An Upper Ordovician (Katian) trilobite fauna from the Lower Ktaoua Formation, Morocco [PDF]

Bulletin of Geosciences, 2017
R.A. Fortey, G.D. Edgecombe
openaire   +1 more source

Conodont and graptolites from the Oberbuchach I and Oberbuchach Ib sections (Katian-Lochkovian)

, 2017
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Schönlaub, H. P., CORRADINI, CARLO
openaire   +2 more sources

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

Nat Commun
Zhao H, Zhang L, Algeo TJ, Lyu Z, Wang X, Hao F.   +5 more
europepmc   +1 more source

Changes in palaeoclimate and palaeoenvironment in the Upper Yangtze area (South China) during the Ordovician-Silurian transition. [PDF]

Sci Rep, 2022
Men X, Mou C, Ge X.
europepmc   +1 more source

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

Sci Adv
Qiu Z, Zou C, Zhang J, Dong A, Kong W, Xiong Y, Wignall PB, Li M, Wang Z, Zhu X, Poulton SW.   +10 more
europepmc   +1 more source

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

Sci Adv
Zhang Z, Yang C, Sahy D, Zhan RB, Wu RC, Li Y, Deng Y, Huang B, Condon DJ, Rong J, Li XH.   +10 more
europepmc   +1 more source

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

Proc Natl Acad Sci U S A
Grossman EL, Barney BB, Sun Z, Henkes GA, Gao Y, Joachimski MM.   +5 more
europepmc   +1 more source

Graptolites of the Králův Dvůr Formation (mid Katian to earliest Hirnantian, Czech Republic) [PDF]

Bulletin of Geosciences, 2015
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]

Sci Adv
Hagiwara W, Sallan L.
europepmc   +1 more source

Soft robotics informs how an early echinoderm moved. [PDF]

Proc Natl Acad Sci U S A, 2023
Desatnik R, Patterson ZJ, Gorzelak P, Zamora S, LeDuc P, Majidi C.   +5 more
europepmc   +1 more source