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• W2066461698 abstract "Research Article| October 01, 1998 Earliest known Carboniferous shallow-water reefs, Gudman Formation (Tn1b), Queensland, Australia: Implications for Late Devonian reef collapse and recovery G. E. Webb G. E. Webb 1Department of Earth Sciences, University of Queensland, Brisbane, QLD 4072, Australia Search for other works by this author on: GSW Google Scholar Author and Article Information G. E. Webb 1Department of Earth Sciences, University of Queensland, Brisbane, QLD 4072, Australia Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1998) 26 (10): 951–954. https://doi.org/10.1130/0091-7613(1998)026<0951:EKCSWR>2.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation G. E. Webb; Earliest known Carboniferous shallow-water reefs, Gudman Formation (Tn1b), Queensland, Australia: Implications for Late Devonian reef collapse and recovery. Geology 1998;; 26 (10): 951–954. doi: https://doi.org/10.1130/0091-7613(1998)026<0951:EKCSWR>2.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The Phanerozoic history of reefs extensively has been considered a direct reflection of the history of skeletal reef-building organisms. However, such a relationship does not characterize global mid-Paleozoic reef history. The extinction of most reef-building stromatoporoids and corals at the Frasnian-Famennian boundary correlates with the collapse of North American and European stromatoporoid-dominated reefs, but Western Australian, Russian, and Chinese reefs were much less severely affected until the late Famennian, when algae, calcimicrobes, and nonskeletal microbialites (i.e., stromatolites, thrombolites) declined globally. Additionally, reef recovery was more rapid than previously thought. Small, early Tournaisian (Tn1b) shallow-water reefs in the Gudman Formation of eastern-central Queensland substantially reduce the duration of the “reefless lag time” following Late Devonian reef decline, essentially confining it to the Strunian. Gudman reefs are dominated by microbialite, but contain a diverse, although volumetrically insignificant, skeletal fauna and flora, including large colonial corals, bryozoans, crinoids, brachiopods, and calcareous algae. Hence, mid-Paleozoic reef collapse and recovery reflect an amalgam of more-or-less independent histories of skeletal organisms, calcimicrobes, and nonskeletal microbialites, in response to regional and global environmental parameters. A better understanding of mid-Paleozoic reef history will require detailed local- and regional-scale studies to isolate global from nonglobal signals. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2066461698 title "Earliest known Carboniferous shallow-water reefs, Gudman Formation (Tn1b), Queensland, Australia: Implications for Late Devonian reef collapse and recovery" @default.
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