EGU2020-2558
https://doi.org/10.5194/egusphere-egu2020-2558
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

The Devonian plant revolution and its role in multiple marine extinction crises

David Bond and Charlotte Stephenson
David Bond and Charlotte Stephenson
  • Department of Geography, Geology and Environment, University of Hull, Hull, United Kingdom (d.bond@hull.ac.uk)

The Devonian was one of the most dynamic periods in Earth history, with major changes on land and in the oceans that experienced at least two of the ten most severe biotic crises of the Phanerozoic. The Period saw the first extensive global floral record; prior to the Devonian, plant assemblages were low in diversity and abundance, and were restricted to areas close to water sources with little competition from co-existing taxa. By the end, plants were geographically widespread in diverse environments. Their colonisation of the land surface has been implicated in the Frasnian/Famennian marine crisis, but little is known of the effects of plants on the global biosphere during the rest of the Devonian. Synthesis of 389 publications reporting 294 Devonian plant genera has resulted in a database that we analyse at generic and stage level for trends in Devonian plant evolution and extinction. Our analysis reveals several key events within this dynamic phase of terrestrialisation: 1) an early Euramerican presence for all plant groups, suggesting this region may have been the site of origination for several higher taxa; 2) the origination of lycopsids in equatorial settings was followed by latitudinal migration northward and southward; 3) a major turnover in plants between the Late Givetian and Middle Frasnian, when significant diversity losses occurred in every palaeo-region in every extant plant group – this may be a hitherto unidentified terrestrial extinction event that coincided with one or both of the Taghanic and Frasne minor marine crises; 4) several Devonian marine black shale events coincide with major steps in terrestrialisation suggestive of a causal link and supporting the notion that plant evolution played a significant role in the Frasnian/Famennian mass extinction nexus.

How to cite: Bond, D. and Stephenson, C.: The Devonian plant revolution and its role in multiple marine extinction crises, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2558, https://doi.org/10.5194/egusphere-egu2020-2558, 2020

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Presentation version 1 – uploaded on 27 Apr 2020
  • CC1: Comment on EGU2020-2558, Sofie Lindström, 05 May 2020
    1. Your database shows that the generic diversity hit a low in the Eifelian. This more or less coincides with a shift from Zosterophyllophyte dominance to Lycopsid dominance. Is this an artefact due to sampling bias, or is this real do you think?
    2. It is interesting that most groups appear to have originated simultaneously in Euramerica and Gondwana. Yet you state that Euramerica was most likely the cradle of vascular plants. Can you differentiate these records in age? Just curious because this is not obvious from your presentation.
    3. The evolution of more complex and water efficient root systems must have decreased the amount of sediments transported to the ocean tremendously. I think this was also shown by D’Antonio et al. (2019 in Geology). How does this add up with what is going on in the ocean at that time?
  • CC2: Anoxia?, Emilia Jarochowska, 05 May 2020

    Hi David and Charlotte, could you explain a bit more how the link with marine anoxia would work? Are there any palynological records (e.g. spores) that would allow comparing terrestrial and marine records of plant diversity through the Devonian?