Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Geology Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Geology; April 2006; v. 34; no. 4; p. 265-268; DOI: 10.1130/G22187.1
© 2006 Geological Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Kerp, H.
Right arrow Articles by Bandel, K.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Typical Triassic Gondwanan floral elements in the Upper Permian of the paleotropics

Hans Kerp1, Abdalla Abu Hamad*,1, Birgit Vörding1 and Klaus Bandel2

1 Forschungsstelle für Paläobotanik, Universität Münster, Hindenburgplatz 57, 48143 Münster, Germany
2 Geologisch-Paläontologisches Institut, Universität Hamburg, Bundesstrasse 55, 20146 Hamburg, Germany

Permian floras of the Middle East often show a mixture of Euramerican, Cathaysian, and Gondwanan elements. We report several species of Dicroidium, a seed fern typical for the Triassic of Gondwana, from the Upper Permian of the Dead Sea region. This is the earliest unequivocal record and the most northerly occurrence of this genus, suggesting that it may have evolved during the Permian in the paleotropics. With the decline and eventual extinction of the typical Permian Glossopteris flora, Dicroidium may have migrated southward. As the climate ameliorated in the Triassic, Dicroidium could have spread farther, eventually colonizing all of Gondwana, where it became one of the dominant floral elements.

Key Words: floral provinces • Permian-Triassic transition • migration • pteridosperms




This article has been cited by other articles:


Home page
Proc R Soc BHome page
J. Wang and H. W. Pfefferkorn
Nystroemiaceae, a new family of Permian gymnosperms from China with an unusual combination of features
Proc R Soc B, August 5, 2009; (2009) rspb.2009.0913v1.
[Abstract] [Full Text] [PDF]


Home page
Am. J. Bot.Home page
E. L. Taylor and T. N. Taylor
Seed ferns from the late Paleozoic and Mesozoic: Any angiosperm ancestors lurking there?
Am. J. Botany, January 1, 2009; 96(1): 237 - 251.
[Abstract] [Full Text] [PDF]


Home page
Proc. Natl. Acad. Sci. USAHome page
D. Jablonski
Colloquium Paper: Extinction and the spatial dynamics of biodiversity
PNAS, August 12, 2008; 105(Supplement_1): 11528 - 11535.
[Abstract] [Full Text] [PDF]


Home page
PaleobiologyHome page
J. C. McElwain, M. E. Popa, S. P. Hesselbo, M. Haworth, and F. Surlyk
Macroecological responses of terrestrial vegetation to climatic and atmospheric change across the Triassic/Jurassic boundary in East Greenland
Paleobiology, December 1, 2007; 33(4): 547 - 573.
[Abstract] [Full Text] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
S. G. Lucas, J. W. Schneider, and G. Cassinis
Non-marine Permian biostratigraphy and biochronology: an introduction
Geological Society, London, Special Publications, January 1, 2006; 265(1): 1 - 14.
[Abstract] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Geological Society of America