Newly integrated approaches towards understanding Late Triassic terrestrial ecosystems
Newly integrated approaches towards understanding Late Triassic terrestrial ecosystems
The Late Triassic (~235–201.3 Ma) is one of the critical intervals of Phanerozoic earth history. Against a backdrop of marked climatic differences across Pangea (Sellwood and Valdes, 2006) and changing global atmospheric conditions (e.g., Berner, 2006), the Late Triassic saw the final recovery from the Permo–Triassic mass extinction, just before the end-Triassic mass extinction, and was punctuated by at least one major extraterrestrial bolide impact (Hodych and Dunning, 1992; Ramezani et al., 2005). Late Triassic terrestrial ecosystems are of particular interest, because they saw the origin of many modern vertebrate groups (e.g., Hugall et al., 2007), including the origin and early diversification of dinosaurs, while continents drifted through distinctly different climate zones (Kent and Tauxe, 2005). A variety of recent research examining the terrestrial realm with new analytical tools has dramatically changed our understanding of this time interval on land.
689-691
Irmis, Randall B.
1490574b-4ad6-4896-a1d7-b66933a7e12e
Whiteside, Jessica H.
5d9ad7aa-eba3-4ad9-9f6f-81be71b6829b
November 2010
Irmis, Randall B.
1490574b-4ad6-4896-a1d7-b66933a7e12e
Whiteside, Jessica H.
5d9ad7aa-eba3-4ad9-9f6f-81be71b6829b
Irmis, Randall B. and Whiteside, Jessica H.
(2010)
Newly integrated approaches towards understanding Late Triassic terrestrial ecosystems.
Palaios, 25 (11), .
(doi:10.2110/palo.2010.S06).
Abstract
The Late Triassic (~235–201.3 Ma) is one of the critical intervals of Phanerozoic earth history. Against a backdrop of marked climatic differences across Pangea (Sellwood and Valdes, 2006) and changing global atmospheric conditions (e.g., Berner, 2006), the Late Triassic saw the final recovery from the Permo–Triassic mass extinction, just before the end-Triassic mass extinction, and was punctuated by at least one major extraterrestrial bolide impact (Hodych and Dunning, 1992; Ramezani et al., 2005). Late Triassic terrestrial ecosystems are of particular interest, because they saw the origin of many modern vertebrate groups (e.g., Hugall et al., 2007), including the origin and early diversification of dinosaurs, while continents drifted through distinctly different climate zones (Kent and Tauxe, 2005). A variety of recent research examining the terrestrial realm with new analytical tools has dramatically changed our understanding of this time interval on land.
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Published date: November 2010
Organisations:
Paleooceanography & Palaeoclimate
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Local EPrints ID: 354769
URI: http://eprints.soton.ac.uk/id/eprint/354769
ISSN: 0883-0351
PURE UUID: b61d8685-2bdc-4d5f-8dbe-975e786f3935
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Date deposited: 19 Jul 2013 10:22
Last modified: 14 Mar 2024 14:24
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Author:
Randall B. Irmis
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