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dc.contributor.authorHåkansson, Eckart
dc.contributor.authorGordon, Dennis P
dc.contributor.authorTaylor, PD
dc.date.accessioned2025-03-13T11:55:23Z
dc.date.available2025-03-13T11:55:23Z
dc.date.issued2024-06-14
dc.identifier.citationHåkansson, E., Gordon, D. P., & Taylor, P. D. (2024). Bryozoa from the Maastrichtian Korojon Formation, Western Australia. In Fossils and strata. https://doi.org/10.18261/9788215072081-2024en_US
dc.identifier.issn0300-9491
dc.identifier.doi10.18261/9788215072081-2024
dc.identifier.urihttp://hdl.handle.net/10141/623274
dc.description.abstractThe first Australian Cretaceous bryozoan fauna is described from the Upper Campanian – Lower Maastrichtian Korojon Formation from the Giralia Anticline in north-western Western Australia. Bryozoans are the numerically dominant element in a sclerobiont community dependent on the abundant large inoceramids, utilizing both valves in life position as well as reworked shell fragments. A total of 68 species-level taxa are described (22 cyclostomes and 46 cheilostomes); 50 of these are new (12 cyclos-tomes and 38 cheilostomes) and the remaining 18 taxa are left at various levels of open nomenclature. They are referred to 47 genera (14 cyclostome and 33 cheilostome genera, 11 of which are new), with a total of 10 taxa left in open nomenclature. One new family, Cardabiellidae, is introduced. The total Late Cretaceous bryozoan fauna known from the Southern Hemisphere remnants of the Gondwana supercontinent – South America, Africa, India, Antarctica, Australia, Zealandia – is significantly less diverse than that known from the Northern Hemisphere, where the European Chalk Sea fauna constitutes the diversity hotspot. The addition of the Korojon fauna described here expands our knowledge of the Cretaceous bryozoan fauna from the Southern Hemisphere considerably, particularly with respect to the youngest bryozoan order, the Cheilostomata. And importantly, the Korojon fauna, more than doubles the proportion of Late Cretaceous cheilostome genera endemic to the Southern Hemisphere from 12.5% to more than 25% of the total number of Late Cretaceous genera presently known from this realm. We suggest that this significant expansion may well warrant a reassessment of the role of Southern Hemisphere bryozoan faunas in the recovery from the Cretaceous-Paleogene biotic turnover.en_US
dc.language.isoenen_US
dc.publisherScandinavian University Pressen_US
dc.rightsopenAccessen_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/deed.en
dc.titleBryozoa from the Maastrichtian Korojon Formation, Western Australiaen_US
dc.typeJournal Articleen_US
dc.identifier.eissn2637-6032
dc.identifier.journalFossils and Strataen_US
dc.date.updated2024-09-16T18:35:27Z
dc.identifier.volume70en_US
dc.identifier.startpage1-155en_US
elements.import.authorHåkansson, Eckart
elements.import.authorGordon, Dennis P
elements.import.authorTaylor, Paul D
dc.description.nhmCopyright © Eckart Håkansson, Dennis P. Gordon and Paul D. Taylor 2024. The material in this publication is covered by the Norwegian Copyright Act and published open access under a Creative Commons CC BY 4.0 licence. The attached file is the published version of the article.en_US
dc.description.nhmNHM Repository
refterms.dateFOA2025-03-13T11:55:25Z


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