FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2810403804> ?p ?o ?g. }

• W2810403804 endingPage "2030" @default.
• W2810403804 startingPage "2015" @default.
• W2810403804 abstract "Research Article| June 28, 2018 Rapid biotic rebound during the late Griesbachian indicates heterogeneous recovery patterns after the Permian-Triassic mass extinction Xu Dai; Xu Dai 1State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China Search for other works by this author on: GSW Google Scholar Haijun Song; Haijun Song † 1State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China †Corresponding author: haijun.song@aliyun.com. Search for other works by this author on: GSW Google Scholar Paul B. Wignall; Paul B. Wignall 2School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK Search for other works by this author on: GSW Google Scholar Enhao Jia; Enhao Jia 1State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China Search for other works by this author on: GSW Google Scholar Ruoyu Bai; Ruoyu Bai 1State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China Search for other works by this author on: GSW Google Scholar Fengyu Wang; Fengyu Wang 1State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China Search for other works by this author on: GSW Google Scholar Jing Chen; Jing Chen 3Yifu Museum of China University of Geosciences, Wuhan 430074, China Search for other works by this author on: GSW Google Scholar Li Tian Li Tian 1State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China Search for other works by this author on: GSW Google Scholar GSA Bulletin (2018) 130 (11-12): 2015–2030. https://doi.org/10.1130/B31969.1 Article history received: 12 Nov 2017 rev-recd: 04 Mar 2018 accepted: 20 May 2018 first online: 28 Jun 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Xu Dai, Haijun Song, Paul B. Wignall, Enhao Jia, Ruoyu Bai, Fengyu Wang, Jing Chen, Li Tian; Rapid biotic rebound during the late Griesbachian indicates heterogeneous recovery patterns after the Permian-Triassic mass extinction. GSA Bulletin 2018;; 130 (11-12): 2015–2030. doi: https://doi.org/10.1130/B31969.1 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 SocietyGSA Bulletin Search Advanced Search Abstract New fossil data from two Early Triassic (Griesbachian to Dienerian) sections from South China show unusually high levels of both benthic and nektonic taxonomic richness occurring in the late Griesbachian. In total, 68 species (including 26 newly originated species) representing mollusks, brachiopods, foraminifers, conodonts, ostracods, and echinoderms occur in the late Griesbachian, indicating well-established and relatively complex marine communities. Furthermore, the nekton shows higher origination rates than the benthos. Analyses of the sedimentary facies and size distribution of pyrite framboids show that this high-diversity interval is associated with well-oxygenated environments. In contrast to the previously suggested scenario, which inferred that persistently harsh environmental conditions impeded the biotic recovery during the Early Triassic, our new findings, combined with recent work, indicate a fitful regional recovery pattern after the Permian-Triassic crisis, resulting in three main diversity highs: late Griesbachian–early Dienerian, early–middle Smithian, and Spathian. The transient rebound episodes were therefore influenced by both extrinsic local (e.g., redox condition, temperature) and intrinsic (e.g., biological tolerances, origination rates) parameters. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2810403804 created "2018-07-10" @default.
• W2810403804 creator A5003484610 @default.
• W2810403804 creator A5010329374 @default.
• W2810403804 creator A5013519684 @default.
• W2810403804 creator A5014347484 @default.
• W2810403804 creator A5021580247 @default.
• W2810403804 creator A5043138062 @default.
• W2810403804 creator A5048379858 @default.
• W2810403804 creator A5081056955 @default.
• W2810403804 date "2018-06-28" @default.
• W2810403804 modified "2023-09-24" @default.
• W2810403804 title "Rapid biotic rebound during the late Griesbachian indicates heterogeneous recovery patterns after the Permian-Triassic mass extinction" @default.
• W2810403804 cites W1143759192 @default.
• W2810403804 cites W1538161997 @default.
• W2810403804 cites W1571253122 @default.
• W2810403804 cites W1594670463 @default.
• W2810403804 cites W1927557167 @default.
• W2810403804 cites W1945199925 @default.
• W2810403804 cites W1966572506 @default.
• W2810403804 cites W1976104635 @default.
• W2810403804 cites W1976370168 @default.
• W2810403804 cites W1985237884 @default.
• W2810403804 cites W1986680391 @default.
• W2810403804 cites W1987104322 @default.
• W2810403804 cites W1993372534 @default.
• W2810403804 cites W1994510458 @default.
• W2810403804 cites W1994992326 @default.
• W2810403804 cites W1995629764 @default.
• W2810403804 cites W1995922654 @default.
• W2810403804 cites W1996341408 @default.
• W2810403804 cites W1997437344 @default.
• W2810403804 cites W1997935222 @default.
• W2810403804 cites W1998090451 @default.
• W2810403804 cites W2000383815 @default.
• W2810403804 cites W2003064666 @default.
• W2810403804 cites W2003414014 @default.
• W2810403804 cites W2007158528 @default.
• W2810403804 cites W2007813456 @default.
• W2810403804 cites W2011947668 @default.
• W2810403804 cites W2015146979 @default.
• W2810403804 cites W2016009288 @default.
• W2810403804 cites W2020407003 @default.
• W2810403804 cites W2025900801 @default.
• W2810403804 cites W2029537332 @default.
• W2810403804 cites W2038292898 @default.
• W2810403804 cites W2040508060 @default.
• W2810403804 cites W2041211732 @default.
• W2810403804 cites W2042189603 @default.
• W2810403804 cites W2043109300 @default.
• W2810403804 cites W2055608377 @default.
• W2810403804 cites W2060117327 @default.
• W2810403804 cites W2063112221 @default.
• W2810403804 cites W2064606556 @default.
• W2810403804 cites W2067417188 @default.
• W2810403804 cites W2067885793 @default.
• W2810403804 cites W2072406000 @default.
• W2810403804 cites W2075177728 @default.
• W2810403804 cites W2078542443 @default.
• W2810403804 cites W2084836756 @default.
• W2810403804 cites W2087136138 @default.
• W2810403804 cites W2092617449 @default.
• W2810403804 cites W2092703246 @default.
• W2810403804 cites W2101625633 @default.
• W2810403804 cites W2103760463 @default.
• W2810403804 cites W2112164433 @default.
• W2810403804 cites W2124219564 @default.
• W2810403804 cites W2134357070 @default.
• W2810403804 cites W2136158978 @default.
• W2810403804 cites W2157354465 @default.
• W2810403804 cites W2160118267 @default.
• W2810403804 cites W2161347331 @default.
• W2810403804 cites W2163486924 @default.
• W2810403804 cites W2179370565 @default.
• W2810403804 cites W2213096039 @default.
• W2810403804 cites W2281239912 @default.
• W2810403804 cites W2324965518 @default.
• W2810403804 cites W2335304256 @default.
• W2810403804 cites W2497090368 @default.
• W2810403804 cites W2505144080 @default.
• W2810403804 cites W2509800553 @default.
• W2810403804 cites W2529501031 @default.
• W2810403804 cites W2549562970 @default.
• W2810403804 cites W2555975945 @default.
• W2810403804 cites W2562756274 @default.
• W2810403804 cites W2588343230 @default.
• W2810403804 cites W2592021744 @default.
• W2810403804 cites W2621037399 @default.
• W2810403804 cites W2623432683 @default.
• W2810403804 cites W2724769795 @default.
• W2810403804 cites W2729265959 @default.
• W2810403804 cites W2747840661 @default.
• W2810403804 cites W2750391460 @default.
• W2810403804 cites W354745309 @default.
• W2810403804 cites W4239656501 @default.
• W2810403804 doi "https://doi.org/10.1130/b31969.1" @default.
• W2810403804 hasPublicationYear "2018" @default.
• W2810403804 type Work @default.

• next