Phytogeography and Paleoecology in Western Europe and Eastern Greenland Near the Triassic-Jurassic Boundary

Other| April 01, 2000 Phytogeography and Paleoecology in Western Europe and Eastern Greenland Near the Triassic-Jurassic Boundary RICHARD N.L.B. HUBBARD; RICHARD N.L.B. HUBBARD 1Palaeobiology Research Unit, University of East London, London E15 4LZ, UK Search for other works by this author on: GSW Google Scholar MICHAEL C. BOULTER MICHAEL C. BOULTER 1Palaeobiology Research Unit, University of East London, London E15 4LZ, UK Search for other works by this author on: GSW Google Scholar Author and Article Information RICHARD N.L.B. HUBBARD 1Palaeobiology Research Unit, University of East London, London E15 4LZ, UK MICHAEL C. BOULTER 1Palaeobiology Research Unit, University of East London, London E15 4LZ, UK Publisher: SEPM Society for Sedimentary Geology Accepted: 22 Dec 1999 First Online: 03 Mar 2017 Online ISSN: 1938-5323 Print ISSN: 0883-1351 Society for Sedimentary Geology PALAIOS (2000) 15 (2): 120–131. https://doi.org/10.1669/0883-1351(2000)015<0120:PAPIWE>2.0.CO;2 Article history Accepted: 22 Dec 1999 First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation RICHARD N.L.B. HUBBARD, MICHAEL C. BOULTER; Phytogeography and Paleoecology in Western Europe and Eastern Greenland Near the Triassic-Jurassic Boundary. PALAIOS 2000;; 15 (2): 120–131. doi: https://doi.org/10.1669/0883-1351(2000)015<0120:PAPIWE>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyPALAIOS Search Advanced Search Abstract Previous multivariate statistical analyses identified at least seven associations of sporomorphs within a major vegetational group of late Triassic-earliest Jurassic times identified as corresponding to arctic or cool-temperate climatic conditions. Detailed examination of how these associations responded to the climatic changes near the Triassic-Jurassic boundary allows them to be classified in terms of their thermophily and drought tolerance. These deductions also give rise to a fairly detailed reconstruction of climatic changes at the time. Consideration of the presumed family affinities of the various sporomorphs gives some support to the climatic interpretations; and allows tentative reconstructions of some of the vegetation. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.