FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4328105052> ?p ?o ?g. }

• W4328105052 endingPage "111518" @default.
• W4328105052 startingPage "111518" @default.
• W4328105052 abstract "A major bio-crisis in the Guadalupian−Lopingian transition (Capitanian−Wuchiapingian, middle−late Permian), possibly driven by the volatile eruption of the Emeishan large igneous province (LIP), was marked by the first-order collapse of global metazoan reefs and decline of fusulinid foraminifera, but with only minor impacts on other marine invertebrates (brachiopod, crustacea, other foraminifera). To assess the exact cause of this event, we conducted geochemical analyses of the shallow marine strata at the global stratotype section and point of the Guadalupian−Lopingian (G−L) boundary (GLB) in Laibin, South China, which corresponds to the last step of the Capitanian bio-crises during Emeishan volcanism. Here, we detect evidence for high temperature combustion of organic matter in air spanning the GLB (indicated by enriched coronene) that was terminated by a soil erosion event accompanied with terrestrial vegetation collapse at the mass extinction level (evidenced by enriched dibenzofuran) and a carbon isotope perturbation (a 2.5–3.5‰ negative shift of δ13Ccarb). Molybdenum data indicates oxic seawater during the combustion event, likely reflecting regression. These findings imply that large volatile volcanic eruptions of the Emeishan LIP may have caused these environmental extreme events and mass extinctions, and that relatively lower magnitude of volcanism related to Emeishan LIP may have led to impacts on terrestrial−nearshore ecosystems." @default.
• W4328105052 created "2023-03-22" @default.
• W4328105052 creator A5054451564 @default.
• W4328105052 creator A5062385838 @default.
• W4328105052 creator A5077335133 @default.
• W4328105052 date "2023-05-01" @default.
• W4328105052 modified "2023-10-16" @default.
• W4328105052 title "High-temperature combustion event spanning the Guadalupian−Lopingian boundary terminated by soil erosion" @default.
• W4328105052 cites W1801625845 @default.
• W4328105052 cites W1880555926 @default.
• W4328105052 cites W1963485296 @default.
• W4328105052 cites W1966990309 @default.
• W4328105052 cites W1969761181 @default.
• W4328105052 cites W1972477780 @default.
• W4328105052 cites W1973364692 @default.
• W4328105052 cites W1982684347 @default.
• W4328105052 cites W1990742077 @default.
• W4328105052 cites W1997469183 @default.
• W4328105052 cites W1997853880 @default.
• W4328105052 cites W1998963014 @default.
• W4328105052 cites W2004305320 @default.
• W4328105052 cites W2005868711 @default.
• W4328105052 cites W2007154755 @default.
• W4328105052 cites W2009661689 @default.
• W4328105052 cites W2016769341 @default.
• W4328105052 cites W2019736558 @default.
• W4328105052 cites W2025236804 @default.
• W4328105052 cites W2029085819 @default.
• W4328105052 cites W2029538041 @default.
• W4328105052 cites W2030603535 @default.
• W4328105052 cites W2030989612 @default.
• W4328105052 cites W2036501693 @default.
• W4328105052 cites W2051525555 @default.
• W4328105052 cites W2055105606 @default.
• W4328105052 cites W2057391595 @default.
• W4328105052 cites W2068658966 @default.
• W4328105052 cites W2069328873 @default.
• W4328105052 cites W2081829616 @default.
• W4328105052 cites W2085921787 @default.
• W4328105052 cites W2107407744 @default.
• W4328105052 cites W2116236975 @default.
• W4328105052 cites W2118709509 @default.
• W4328105052 cites W2133086566 @default.
• W4328105052 cites W2144797652 @default.
• W4328105052 cites W2160118267 @default.
• W4328105052 cites W2164801744 @default.
• W4328105052 cites W2186066584 @default.
• W4328105052 cites W2316952183 @default.
• W4328105052 cites W2469370542 @default.
• W4328105052 cites W2473761874 @default.
• W4328105052 cites W2478521007 @default.
• W4328105052 cites W2505144080 @default.
• W4328105052 cites W2529501031 @default.
• W4328105052 cites W2550343609 @default.
• W4328105052 cites W2798080436 @default.
• W4328105052 cites W2806770328 @default.
• W4328105052 cites W2807180892 @default.
• W4328105052 cites W2810123500 @default.
• W4328105052 cites W2893115522 @default.
• W4328105052 cites W2905112325 @default.
• W4328105052 cites W2912811174 @default.
• W4328105052 cites W2914278783 @default.
• W4328105052 cites W2914975190 @default.
• W4328105052 cites W2918775417 @default.
• W4328105052 cites W2939301922 @default.
• W4328105052 cites W2947098314 @default.
• W4328105052 cites W2951618739 @default.
• W4328105052 cites W2970746452 @default.
• W4328105052 cites W2981988123 @default.
• W4328105052 cites W2990434355 @default.
• W4328105052 cites W2999219571 @default.
• W4328105052 cites W3005103415 @default.
• W4328105052 cites W3011326703 @default.
• W4328105052 cites W3016065999 @default.
• W4328105052 cites W3026130405 @default.
• W4328105052 cites W3026447126 @default.
• W4328105052 cites W3034945503 @default.
• W4328105052 cites W3087435354 @default.
• W4328105052 cites W3088144394 @default.
• W4328105052 cites W3090855589 @default.
• W4328105052 cites W3091374867 @default.
• W4328105052 cites W3092794507 @default.
• W4328105052 cites W3095662282 @default.
• W4328105052 cites W3126036456 @default.
• W4328105052 cites W3131973622 @default.
• W4328105052 cites W3137576665 @default.
• W4328105052 cites W3187100039 @default.
• W4328105052 cites W415358198 @default.
• W4328105052 cites W4205935895 @default.
• W4328105052 cites W4210810903 @default.
• W4328105052 cites W4220675822 @default.
• W4328105052 cites W4283261121 @default.
• W4328105052 cites W4286698002 @default.
• W4328105052 cites W4315782259 @default.
• W4328105052 cites W62072001 @default.
• W4328105052 doi "https://doi.org/10.1016/j.palaeo.2023.111518" @default.
• W4328105052 hasPublicationYear "2023" @default.
• W4328105052 type Work @default.

• next