Global microbial carbonate proliferation after the end-Devonian mass extinction: Mainly controlled by demise of skeletal bioconstructors
Microbial carbonates commonly flourished following mass extinction events. The end-Devonian (Hangenberg) mass extinction event is a first-order mass extinction on the scale of the ‘Big Five’ extinctions. However, to date, it is still unclear whether global microbial carbonate proliferation occurred...
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| Veröffentlicht in: | Scientific reports 2016-12, Vol.6 (1), p.39694-39694, Article 39694 |
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| description | Microbial carbonates commonly flourished following mass extinction events. The end-Devonian (Hangenberg) mass extinction event is a first-order mass extinction on the scale of the ‘Big Five’ extinctions. However, to date, it is still unclear whether global microbial carbonate proliferation occurred after the Hangenberg event. The earliest known Carboniferous stromatolites on tidal flats are described from intertidal environments of the lowermost Tournaisian (Qianheishan Formation) in northwestern China. With other early Tournaisian microbe-dominated bioconstructions extensively distributed on shelves, the Qianheishan stromatolites support microbial carbonate proliferation after the Hangenberg extinction. Additional support comes from quantitative analysis of the abundance of microbe-dominated bioconstructions through the Famennian and early Tournaisian, which shows that they were globally distributed (between 40° latitude on both sides of the palaeoequator) and that their abundance increased distinctly in the early Tournaisian compared to the latest Devonian (Strunian). Comparison of variations in the relative abundance of skeleton- versus microbe-dominated bioconstructions across the Hangenberg and ‘Big Five’ extinctions suggests that changes in abundance of skeletal bioconstructors may play a first-order control on microbial carbonate proliferation during extinction transitions but that microbial proliferation is not a general necessary feature after mass extinctions. |
| doi_str_mv | 10.1038/srep39694 |
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The end-Devonian (Hangenberg) mass extinction event is a first-order mass extinction on the scale of the ‘Big Five’ extinctions. However, to date, it is still unclear whether global microbial carbonate proliferation occurred after the Hangenberg event. The earliest known Carboniferous stromatolites on tidal flats are described from intertidal environments of the lowermost Tournaisian (Qianheishan Formation) in northwestern China. With other early Tournaisian microbe-dominated bioconstructions extensively distributed on shelves, the Qianheishan stromatolites support microbial carbonate proliferation after the Hangenberg extinction. Additional support comes from quantitative analysis of the abundance of microbe-dominated bioconstructions through the Famennian and early Tournaisian, which shows that they were globally distributed (between 40° latitude on both sides of the palaeoequator) and that their abundance increased distinctly in the early Tournaisian compared to the latest Devonian (Strunian). Comparison of variations in the relative abundance of skeleton- versus microbe-dominated bioconstructions across the Hangenberg and ‘Big Five’ extinctions suggests that changes in abundance of skeletal bioconstructors may play a first-order control on microbial carbonate proliferation during extinction transitions but that microbial proliferation is not a general necessary feature after mass extinctions.</description><identifier>ISSN: 2045-2322</identifier><identifier>EISSN: 2045-2322</identifier><identifier>DOI: 10.1038/srep39694</identifier><identifier>PMID: 28009013</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>704/106/413 ; 704/158/2462 ; 704/2151/213/4116 ; 704/2151/3930 ; 704/2151/414 ; Abundance ; Carbonates ; Carboniferous ; Devonian ; Extinction ; Fossils ; Humanities and Social Sciences ; Intertidal environment ; Mass extinctions ; multidisciplinary ; Relative abundance ; Science ; Skeleton ; Stromatolites ; Tidal flats</subject><ispartof>Scientific reports, 2016-12, Vol.6 (1), p.39694-39694, Article 39694</ispartof><rights>The Author(s) 2016</rights><rights>Copyright Nature Publishing Group Dec 2016</rights><rights>Copyright © 2016, The Author(s) 2016 The Author(s)</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a461t-547475d7df3cca9c41c12e9031496264bdf01b67f96b37185378233f40ced3953</citedby><cites>FETCH-LOGICAL-a461t-547475d7df3cca9c41c12e9031496264bdf01b67f96b37185378233f40ced3953</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC5180103/pdf/$$EPDF$$P50$$Gpubmedcentral$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC5180103/$$EHTML$$P50$$Gpubmedcentral$$Hfree_for_read</linktohtml><link.rule.ids>230,314,727,780,784,864,885,27924,27925,41120,42189,51576,53791,53793</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/28009013$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Yao, Le</creatorcontrib><creatorcontrib>Aretz, Markus</creatorcontrib><creatorcontrib>Chen, Jitao</creatorcontrib><creatorcontrib>Webb, Gregory E.</creatorcontrib><creatorcontrib>Wang, Xiangdong</creatorcontrib><title>Global microbial carbonate proliferation after the end-Devonian mass extinction: Mainly controlled by demise of skeletal bioconstructors</title><title>Scientific reports</title><addtitle>Sci Rep</addtitle><addtitle>Sci Rep</addtitle><description>Microbial carbonates commonly flourished following mass extinction events. The end-Devonian (Hangenberg) mass extinction event is a first-order mass extinction on the scale of the ‘Big Five’ extinctions. However, to date, it is still unclear whether global microbial carbonate proliferation occurred after the Hangenberg event. The earliest known Carboniferous stromatolites on tidal flats are described from intertidal environments of the lowermost Tournaisian (Qianheishan Formation) in northwestern China. With other early Tournaisian microbe-dominated bioconstructions extensively distributed on shelves, the Qianheishan stromatolites support microbial carbonate proliferation after the Hangenberg extinction. Additional support comes from quantitative analysis of the abundance of microbe-dominated bioconstructions through the Famennian and early Tournaisian, which shows that they were globally distributed (between 40° latitude on both sides of the palaeoequator) and that their abundance increased distinctly in the early Tournaisian compared to the latest Devonian (Strunian). Comparison of variations in the relative abundance of skeleton- versus microbe-dominated bioconstructions across the Hangenberg and ‘Big Five’ extinctions suggests that changes in abundance of skeletal bioconstructors may play a first-order control on microbial carbonate proliferation during extinction transitions but that microbial proliferation is not a general necessary feature after mass extinctions.</description><subject>704/106/413</subject><subject>704/158/2462</subject><subject>704/2151/213/4116</subject><subject>704/2151/3930</subject><subject>704/2151/414</subject><subject>Abundance</subject><subject>Carbonates</subject><subject>Carboniferous</subject><subject>Devonian</subject><subject>Extinction</subject><subject>Fossils</subject><subject>Humanities and Social Sciences</subject><subject>Intertidal environment</subject><subject>Mass extinctions</subject><subject>multidisciplinary</subject><subject>Relative abundance</subject><subject>Science</subject><subject>Skeleton</subject><subject>Stromatolites</subject><subject>Tidal flats</subject><issn>2045-2322</issn><issn>2045-2322</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNplkctuFDEQRVuIiEQhC34AWWIDSE386odZIKFAQqQgNrBuud3lxMFtD7Y7Yv6Az6ZGk4wG4o1LquNbt3yr6gWj7xgV_WlOsBKqVfJJdcSpbGouOH-6Vx9WJznfUjwNV5KpZ9Uh7ylVlImj6s-Fj6P2ZHYmxdFhZXQaY9AFyCpF7ywkXVwMRNsCiZQbIBCm-hPcxeB0ILPOmcDv4oLZYO_JV-2CXxMTQ8H3HiYyrskEs8tAoiX5J3goOGd0EZlc0mJKTPl5dWC1z3Byfx9XP84_fz_7Ul99u7g8-3hVa9myUjeyk10zdZMVxmhlJDOMg6KCSdXyVo6TpWxsO6vaUXSsb0TXcyGspAYmoRpxXH3Y6q6WcYbJANrUflglN-u0HqJ2w7-d4G6G63g3NKyn-OEo8PpeIMVfC-Qy4GoGvNcB4pIHnMm7Hv1wRF_9h97GJQVcDymlpGyV2gi-2VKYQMY07c4Mo8Mm4mEXMbIv993vyIdAEXi7BTK2wjWkvZGP1P4CRDSy0Q</recordid><startdate>20161223</startdate><enddate>20161223</enddate><creator>Yao, Le</creator><creator>Aretz, Markus</creator><creator>Chen, Jitao</creator><creator>Webb, Gregory E.</creator><creator>Wang, Xiangdong</creator><general>Nature Publishing Group UK</general><general>Nature Publishing Group</general><scope>C6C</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7X7</scope><scope>7XB</scope><scope>88A</scope><scope>88E</scope><scope>88I</scope><scope>8FE</scope><scope>8FH</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FYUFA</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>K9.</scope><scope>LK8</scope><scope>M0S</scope><scope>M1P</scope><scope>M2P</scope><scope>M7P</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>7X8</scope><scope>5PM</scope></search><sort><creationdate>20161223</creationdate><title>Global microbial carbonate proliferation after the end-Devonian mass extinction: Mainly controlled by demise of skeletal bioconstructors</title><author>Yao, Le ; 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The end-Devonian (Hangenberg) mass extinction event is a first-order mass extinction on the scale of the ‘Big Five’ extinctions. However, to date, it is still unclear whether global microbial carbonate proliferation occurred after the Hangenberg event. The earliest known Carboniferous stromatolites on tidal flats are described from intertidal environments of the lowermost Tournaisian (Qianheishan Formation) in northwestern China. With other early Tournaisian microbe-dominated bioconstructions extensively distributed on shelves, the Qianheishan stromatolites support microbial carbonate proliferation after the Hangenberg extinction. Additional support comes from quantitative analysis of the abundance of microbe-dominated bioconstructions through the Famennian and early Tournaisian, which shows that they were globally distributed (between 40° latitude on both sides of the palaeoequator) and that their abundance increased distinctly in the early Tournaisian compared to the latest Devonian (Strunian). Comparison of variations in the relative abundance of skeleton- versus microbe-dominated bioconstructions across the Hangenberg and ‘Big Five’ extinctions suggests that changes in abundance of skeletal bioconstructors may play a first-order control on microbial carbonate proliferation during extinction transitions but that microbial proliferation is not a general necessary feature after mass extinctions.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><pmid>28009013</pmid><doi>10.1038/srep39694</doi><tpages>1</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | 704/106/413 704/158/2462 704/2151/213/4116 704/2151/3930 704/2151/414 Abundance Carbonates Carboniferous Devonian Extinction Fossils Humanities and Social Sciences Intertidal environment Mass extinctions multidisciplinary Relative abundance Science Skeleton Stromatolites Tidal flats |
| title | Global microbial carbonate proliferation after the end-Devonian mass extinction: Mainly controlled by demise of skeletal bioconstructors |
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