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Flora of The Late T...
Flora of The Late Triassic
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- Kustatscher, Evelyn (författare)
- Museum of Nature South Tyrol, Bindergasse 1, 39100 Bozen/Bolzano, Italy
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- Ash, Sidney (författare)
- Department of Earth and Planetary Sciences, Northrop Hall, University of New Mexico, Albuquerque, NM 87131, USA
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- Karasev, Eugeny (författare)
- Borissiak Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya 123, Moscow 117647, Russia
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- Pott, Christian (författare)
- Naturhistoriska riksmuseet,Enheten för paleobiologi
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- Vajda, Vivi (författare)
- Naturhistoriska riksmuseet,Enheten för paleobiologi,Department of Geology, Lund University, Sweden
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- Yu, Jianxin (författare)
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, P.O.Box 430074, P.R. China
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- McLoughlin, Stephen, 1964- (författare)
- Naturhistoriska riksmuseet,Enheten för paleobiologi
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(creator_code:org_t)
- 1
- 2017-11-17
- 2017
- Engelska.
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Ingår i: The Late Triassic World: Earth in a Time of Transition. - New York : Springer International Publishing. - 9783319680088 ; , s. 545-622
- Relaterad länk:
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http://www.springer....
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https://urn.kb.se/re...
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https://doi.org/10.1...
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Abstract
Ämnesord
Stäng
- The Triassic was a crucial period of botanical evolutionary innovations and plant diversification. Key plant groups (Bennettitales, Czekanowskiales, Gnetales and several modern fern and conifer families) originated during this span of time, together with some taxa putatively related to angiosperms. The composition of the various plant assemblages shows a more homogeneous flora globally than during the Permian. Nonetheless two major floristic provinces are distinguishable during the Late Triassic (Gondwana and Laurussia) together with several subprovinces (two within Gondwana, nine within Laurussia), based on palyno- and macro-floras.The latter are differentiated by contrasting taxonomic composition and group abundances related to different climatic and regional environmental conditions. Many plant families and genera are widely distributed in the Late Triassic, at least in the respective hemispheres. Based on the array of preserved damage types on leaves and wood, insect faunas appear to have recovered from the end-Permian mass extinction by the Late Triassic, with a major expansion of herbivory in Gondwana. All modern functional feeding groups (FFG) were present by the Triassic, including external foliage feeding, piercing-and-sucking, galling, leaf mining and seed predation, with some evidence for the development of very specialized feeding traits and egg-laying strategies.
Ämnesord
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Annan geovetenskap och miljövetenskap (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Other Earth and Related Environmental Sciences (hsv//eng)
Nyckelord
- Non-marine ecosystems
- Palaeoclimate
- Plant fossils
- Palynomorphs
- Palaeo-provinces
- Mass-extinction
- Plant-animal interactions
- Ecosystems and species history
- Ekosystem och arthistoria
Publikations- och innehållstyp
- ref (ämneskategori)
- kap (ämneskategori)
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