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Mesozoic and Cenozoic palaeogeography, palaeoclimate and palaeoecology in theeastern Tethys
Nanjing Institute of Geology and Palaeontology.
Nanjing Institute of Geology and Palaeontology.
Naturhistoriska riksmuseet, Enheten för paleobiologi.ORCID-id: 0000-0001-6723-239X
Natural History Museum of Los Angeles County.
2019 (engelsk)Inngår i: Palaeogeography, Palaeoclimatology, Palaeoecology, ISSN 0031-0182, E-ISSN 1872-616X, Vol. 515, s. 1-5Artikkel i tidsskrift, Editorial material (Fagfellevurdert) Published
Abstract [en]

It is now more than 100years since Suess advanced the concept of the Tethys Ocean in 1893. Since the 1960s when the theory of plate tectonics became established, the Tethys region has attracted the attention of many geologists because it has experienced a complex evolution involving numerous continental fragments drifting in several discrete stages from the Gondwanan margin in the Southern Hemisphere northward to amalgamate with Eurasia in the Northern Hemisphere. The subsequent orogenies associated with consecutive microplate collisions caused great changes to the regional topography and environments, which researchers now realize had global impacts on climate, biotic evolution, and biogeography.

sted, utgiver, år, opplag, sider
Amsterdam: Elsevier, 2019. Vol. 515, s. 1-5
Emneord [en]
Tethyan faunas, biogeography, palaeoclimate, tectonics, Gondwana
HSV kategori
Forskningsprogram
Den föränderliga jorden
Identifikatorer
URN: urn:nbn:se:nrm:diva-3425DOI: 10.1016/j.palaeo.2018.11.014OAI: oai:DiVA.org:nrm-3425DiVA, id: diva2:1372956
Forskningsfinansiär
Swedish Research Council, 2014-5234
Merknad

Additional funding by Strategic Priority Research Program of the Chinese Academy of Sciences (grant numbers XDA20070202, XDB26000000 and XDB03010103), the National Natural Science Foundation of China (grant number 41872004), and UNESCO -IUGS project IGCP 632.

Tilgjengelig fra: 2019-10-01 Laget: 2019-11-25bibliografisk kontrollert

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Forlagets fullteksthttps://doi.org/10.1016/j.palaeo.2018.11.014

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