Department of Palaeontology, University of Vienna
Tuesday 25 March - 4.00 pm
Earth Sciences Seminar Room
(Basement, WEB 05, the previous Mineralogy Seminar Room)
Oldest records of many modern north-temperate woody angiosperm genera are from the Eocene. However, the precise time and place of origin of individual tree genera that play important roles in modern temperate forest ecosystems has largely remained unresolved. One hypothesis about the origin of modern temperate woody elements in the northern hemisphere was proposed in the late 19th century by Adolf Engler, who suggested that many modern temperate tree genera originated in Arctic areas and migrated southwards in the course of the Cenozoic when global climate cooled.
The final objective of the present study is to test the validity of Engler’s (1882) concept of the “arctotertiary element”, that is, to determine whether early Cenozoic high latitude floras were the cradle of a number of tree genera that now dominate north-temperate mid-latitude forests. To achieve this, the systematic affinities of pollen from Paleocene and Eocene sediments of western Greenland and the Faröe Islands are being assessed using combined light and scanning electron microscopy. Macrofossils from the same areas housed in existing museum and university collections are also under study, and new material has been collected in the field. By combining evidence from the palynofloras and the revised macrofloras, the phylogenetic affinities of the recognized plant taxa are being established in order to determine the proportion of extinct lineages and co-occurring extant genera, representing the “arctotertiary element” in the fossil floras.
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