Herbivory in Antarctic fossil forests: evolutionary and palaeoclimatic

Summary Many collections of Eocene Fossil leaves from Antarctica contain a rich store of insect trace fossils, indicating that insects were an important component of the unique forests that grew in polar regions. However, insect body fossils themselves are rare and so insect traces provide an excell...

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Bibliographic Details
Main Author: J. Smellie
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.511.7607
http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea059.pdf
Description
Summary:Summary Many collections of Eocene Fossil leaves from Antarctica contain a rich store of insect trace fossils, indicating that insects were an important component of the unique forests that grew in polar regions. However, insect body fossils themselves are rare and so insect traces provide an excellent opportunity to examine both the palaeoentomology and the palaeoclimate of Antarctica. The fossils studied include Eocene leaves from both Seymour Island and King George Island on the Antarctic Peninsula. A database of all insect traces on the Antarctic fossil leaves was compiled and analysed in terms of the diversity of palaeoherbivory. The fossil leaves are diverse with several different plant species present such as Nothofagaceae and Cunoniaceae. The range of traces found includes leaf mines, galls and general leaf chewing, of which both marginal and non-marginal examples are present. The preliminary results of the comparison with modern day environments in South America will be shown