PB McQUILLAN - Biological Journal of the Linnean Society, 1993 - academic.oup.com
The invertebrates directly associated with the southern hemisphere tree genus Nothofagus are described and discussed in terms of their organization into guilds and attributes of their …
Until recently, few people would have associated rainforest with Australia. The present-day distribution of Australian rainforest is limited but it was formerly more widespread and was …
The phytogeographic distribution of Cainozoic ferns is reported based upon a critical re- appraisal of the macrofossil and mesofossil record also taking account of evidence from a …
DR Greenwood, SK Donovan - The processes of fossilization, 1991 - academia.edu
Taphonomy is defined as the study of the transition of organic remains from the living organism to fossil assemblages (Efremov, 1940). As such, plant taphonomy incorporates the …
RS Hill, TJ Brodribb - Australian Journal of Botany, 1999 - CSIRO Publishing
The three southern conifer families, Araucariaceae, Cupressaceae and Podocarpaceae, have a long history and continue to be an important part of the vegetation today. The …
M Gtari, JO Dawson - Functional Plant Biology, 2011 - CSIRO Publishing
A compilation and synthesis of information derived from plant databases and other sources on the occurrence, diversity and geographic distribution of actinorhizal plants in Africa is …
TC Chambers, AN Drinnan… - International Journal of …, 1998 - journals.uchicago.edu
Morphological details of Wollemia nobilis (Wollemi pine) are described and illustrated, and compared with the extant genera Agathis and Araucaria and with selected araucarian fossils …
A new mid-latitude terrestrial climate proxy record is presented for southeastern Australia. The Middle Eocene to Middle Miocene palynofloral and δ 13 C record of the Latrobe Group …
EA Colhoun - Quaternary Research, 1985 - cambridge.org
Geomorphic, stratigraphic, palynologic and 14C evidence indicates that the West Coast Range, Tasmania, was glaciated at least three times during the late Cenozoic. The last or …