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Anne-Laure Decombeix (CNRS)21.09.26, 09:25Invited keynote
The plant fossil record is, by its very nature, fragmentary, but some pieces of this puzzle preserve morphological and/or anatomical characters that provide direct insights into the ecology and physiology of extinct taxa. This "functional approach" allows paleobotanists to study plant evolution in a way that complements systematics, seeing fossil plants as once-living organisms that interacted...
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Chris Mays (Naturhistorisches Museum Wien)21.09.26, 10:05Invited keynote
The greatest diversity losses in Earth’s history occurred at the end of the Paleozoic Era, during the end-Permian extinction event (EPE). For life on land, plants are unparalleled archivists of the EPE, preserving evidence of ecosystem dynamics, biodiversity and biogeography changes, climatic instability, and carbon cycle (dys)function.
The EPE is characterized by the largest climate-state...
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Fridgeir Grímsson (University of Vienna, Department of Botany and Biodiversity Research)21.09.26, 11:15Invited keynote
Direct evidence of animal–flower interactions in the fossil record is rare, but pollen preserved on or inside fossil animals provides unique insight into the evolution of pollination systems through time. In recent years, there has been accumulating evidence of flower visitation from the Cenozoic fossil record, and fossil flies, beetles, bees, birds, and bats bearing pollen have been...
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Julia Gravendyck (Bonn Institute for Organismic Biology (BIOB), Department of Biology, University of Bonn, Germany)21.09.26, 11:55Invited keynote
This keynote addresses the changing reality of palynology and palaeobotany through a historical lens. Drawing on examples from conference records, institutional structures, and personal accounts from the 1900s onward, it highlights a period in which both fields flourished. In contrast, the present landscape is increasingly characterised by fragmentation, specialisation, and reduced...
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