Abstract
There are four symbiotic associations involving corals known from the Late Devonian. Corals formed at least six symbiotic associations in the Mississippian, most of which involved crinoids. There was an escalation in the abundance and complexity of coral symbiosis from the Ordovician into the Devonian, and no decline in the Carboniferous. Coral symbiosis after the Kellwasser biotic crises was impoverished and presumably did not recover to Middle Devonian levels in the early Carboniferous. Recovery of symbiotic associations after the Hangenberg Event was due to the re-establishment of associations known from earlier Palaeozoic times and appearance of new symbiotic associations. The lack of various worm bioclaustrations and endobiotic tentaculitoid tubeworms in Carboniferous corals is the main difference from the Ordovician, Silurian, and Devonian coral symbiosis. Late Devonian symbiotic associations involving corals are different from early Carboniferous associations.
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Acknowledgements
Financial support was provided by a Palaeontological Association Research Grant and Estonian Research Council projects ETF9064 and IUT20-34. I am grateful to Sergio Rodríguez, Julien Denayer, and Victor Ogar for the comments on coral symbiosis in the Carboniferous. I am grateful to Markus Aretz and Mark A. Wilson for the constructive reviews.
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Vinn, O. Symbiosis in Late Devonian-Mississippian corals: a review. Palaeobio Palaeoenv 97, 723–729 (2017). https://doi.org/10.1007/s12549-017-0284-1
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DOI: https://doi.org/10.1007/s12549-017-0284-1