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LATE CAINOZOIC VEGETATION HISTORY OF NORTH-WESTERN AUSTRALIA, FROM THE PALYNOLOGY OF A DEEP-SEA CORE (ODP-SITE-765)
In the late Miocene, casuarinaceous forests were predominant in north-western Australia. Through the Pliocene and Pleistocene, Casuarinaceae declined and Poaceae increased, until grasslands predominated. Acacia and some other shrub species were present, suggesting possible shrublands. Surprisingly, however, there were very few Myrtaceae; hence, eucalypt dominated vegetation was never present in this part of Australia. The present vegetation of Acacia shrublands and tussock/hummock grasslands developed, therefore, from casuarinaceous forests. The late Cainozoic palaeovegetation is compared with others of equivalent age elsewhere in Australia. © 1994 CSIRO. All rights reserved.
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- Article
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AUSTRALIAN JOURNAL OF BOTANYVolume
42Issue
1Pagination
95-102:8eISSN
1444-9862ISSN
0067-1924Publisher
CSIRO PUBLICATIONSPublication status
- Published
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University of Tasmania, HOBART, TAS, 7001, AUSTRALIARights statement
Copyright 1994 CSIROUsage metrics
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