20.–25. Sept. 2026
Münster
Europe/Berlin Zeitzone

Sitzung

Biotic interactions

S14
23.09.2026, 11:30
Münster

Münster

Fürstenberghaus, Domplatz 20–22, 48143 Münster

Beschreibung

This symposium will contain presentations focusing on plant-animal interactions, including herbivory, granivory, and coprolites as palynological archives.

Präsentationsmaterialien

Es gibt derzeit keine Materialien.

  1. Alexandru M.F. Tomescu (Department of Biological Sciences, California State Polytechnic University Humboldt, USA)
    23.09.26, 11:30
    Biotic interactions
    Talk

    Emsian fossil assemblages from Laurentia have yielded evidence for anti-herbivore defenses: secretory capitate glands and other glandular emergences (trichomes), spinescent emergences (spines, hereafter) with sclerified cortex and specialized morphology and wound response periderm for piercing-sucking and putative surface feeding wounds. Circumstantial evidence from the Emsian includes...

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  2. Tao Zhao (Yunnan University)
    23.09.26, 11:45
    Biotic interactions
    Talk

    Leaf mining is a specialized feeding strategy in which insect larvae inhabit and feed on the internal tissues of leaves. This strategy not only improves feeding efficiency but also provides natural protection against environmental stressors. For host plants, leaf mining can lead to increased water and nutrient loss and reduced photosynthetic efficiency. In response to these threats, plants...

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  3. Margaret Collinson (Royal Holloway University of London)
    23.09.26, 12:00
    Biotic interactions
    Talk

    A distinctive seed type is present in the stomach of two species of mammal and one unidentified small trogon-like bird from the late early to early middle Eocene oil shale (Cenozoic, Paleogene) of Messel, Germany. The bird contains several more or less intact seeds. Amongst the mammals two species of the rodent Masillamys contain numerous seed coat fragments. As revealed by SEM the surfaces...

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  4. Adam Sedlačko (Department of Botany and Biodiversity Research, University of Vienna, Vienna, Austria)
    23.09.26, 12:15
    Biotic interactions
    Talk

    The Gratkorn pit, comprising late Middle Miocene sediments and fossils, is well known for its diverse terrestrial vertebrate fauna. Vertebrate fossils and associated coprolites are found in a paleosol at the base of the pit, which is part of the Gratkorn Fm and is of late Serravallian age (c. 12.2 Ma). The paleosol is overlain by limnic sediments of the Gleisdorf Fm. Until now, paleoecological...

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