Matches in SemOpenAlex for { <https://semopenalex.org/work/W3003886674> ?p ?o ?g. }
- W3003886674 endingPage "1611" @default.
- W3003886674 startingPage "1593" @default.
- W3003886674 abstract "Abstract The Toarcian Oceanic Anoxic Event (T-OAE, c . 182 Ma) represents a major perturbation of the carbon cycle marked by widespread black shale deposition. Consequently, the onset of the T-OAE has been linked to the combined effects of global warming, high productivity, basin restriction and salinity stratification. However, the processes that led to termination of the event remain elusive. Here, we present palynological data from Arctic Siberia (Russia), the Viking Corridor (offshore Norway) and the Yorkshire Coast (UK), all spanning the upper Pliensbachian – upper Toarcian stages. Rather than a ‘dinoflagellate cyst black-out’, as recorded in T-OAE strata of NW Europe, both the Arctic and Viking Corridor records show high abundance and dinoflagellate diversity throughout the T-OAE interval as calibrated by C-isotope records. Significantly, in the Arctic Sea and Viking Corridor, numerous species of the Parvocysta and Phallocysta suites make their first appearance in the lower Toarcian Falciferum Zone much earlier than in Europe, where these key dinoflagellate species appeared suddenly during the Bifrons Zone. Our results indicate migrations of Arctic dinoflagellate species, driven by relative sea-level rise in the Viking Corridor and the establishment of a S-directed circulation from the Arctic Sea into the Tethys Ocean. The results support oceanographic models, but are at odds with some interpretations based on geochemical proxies. The migration of Arctic dinoflagellate species coincides with the end of the T-OAE and marks the arrival of oxygenated, low-salinity Arctic waters, triggering a regime change from persistent euxinia to more dynamic oxygen conditions." @default.
- W3003886674 created "2020-02-07" @default.
- W3003886674 creator A5021196149 @default.
- W3003886674 creator A5023682302 @default.
- W3003886674 creator A5030556340 @default.
- W3003886674 creator A5034890416 @default.
- W3003886674 creator A5037213164 @default.
- W3003886674 creator A5055756953 @default.
- W3003886674 creator A5081706474 @default.
- W3003886674 creator A5089643314 @default.
- W3003886674 date "2019-12-13" @default.
- W3003886674 modified "2023-10-13" @default.
- W3003886674 title "Enhanced Arctic-Tethys connectivity ended the Toarcian Oceanic Anoxic Event in NW Europe" @default.
- W3003886674 cites W1505358646 @default.
- W3003886674 cites W1566907460 @default.
- W3003886674 cites W1594593947 @default.
- W3003886674 cites W1686116366 @default.
- W3003886674 cites W1853384289 @default.
- W3003886674 cites W1932213836 @default.
- W3003886674 cites W1939766437 @default.
- W3003886674 cites W1967446424 @default.
- W3003886674 cites W196769100 @default.
- W3003886674 cites W1970262611 @default.
- W3003886674 cites W1974514800 @default.
- W3003886674 cites W1977171142 @default.
- W3003886674 cites W1978064530 @default.
- W3003886674 cites W1984441670 @default.
- W3003886674 cites W1985780433 @default.
- W3003886674 cites W1986117620 @default.
- W3003886674 cites W1990868760 @default.
- W3003886674 cites W1991994411 @default.
- W3003886674 cites W1993289627 @default.
- W3003886674 cites W1994056142 @default.
- W3003886674 cites W1994116172 @default.
- W3003886674 cites W1999506323 @default.
- W3003886674 cites W2003186674 @default.
- W3003886674 cites W2007180063 @default.
- W3003886674 cites W2007535331 @default.
- W3003886674 cites W2014503814 @default.
- W3003886674 cites W2037610129 @default.
- W3003886674 cites W2039311538 @default.
- W3003886674 cites W2049198600 @default.
- W3003886674 cites W2054618954 @default.
- W3003886674 cites W2054704638 @default.
- W3003886674 cites W2060155491 @default.
- W3003886674 cites W2061345314 @default.
- W3003886674 cites W2062752588 @default.
- W3003886674 cites W2067417937 @default.
- W3003886674 cites W2068117559 @default.
- W3003886674 cites W2070661327 @default.
- W3003886674 cites W2074629798 @default.
- W3003886674 cites W2075532353 @default.
- W3003886674 cites W2078769491 @default.
- W3003886674 cites W2079945897 @default.
- W3003886674 cites W2084201797 @default.
- W3003886674 cites W2086443259 @default.
- W3003886674 cites W2089222523 @default.
- W3003886674 cites W2093257301 @default.
- W3003886674 cites W2095734921 @default.
- W3003886674 cites W2100916381 @default.
- W3003886674 cites W2111607661 @default.
- W3003886674 cites W2114587608 @default.
- W3003886674 cites W2115254336 @default.
- W3003886674 cites W2122059247 @default.
- W3003886674 cites W2149733981 @default.
- W3003886674 cites W2152510189 @default.
- W3003886674 cites W2192197685 @default.
- W3003886674 cites W2210284146 @default.
- W3003886674 cites W2305613090 @default.
- W3003886674 cites W2313056624 @default.
- W3003886674 cites W2326669813 @default.
- W3003886674 cites W2332261214 @default.
- W3003886674 cites W2333096464 @default.
- W3003886674 cites W2340052022 @default.
- W3003886674 cites W2512839081 @default.
- W3003886674 cites W2568091621 @default.
- W3003886674 cites W2622444222 @default.
- W3003886674 cites W2736333740 @default.
- W3003886674 cites W2765608430 @default.
- W3003886674 cites W2775628958 @default.
- W3003886674 cites W2783067866 @default.
- W3003886674 cites W2792382008 @default.
- W3003886674 cites W2797913866 @default.
- W3003886674 cites W2888277423 @default.
- W3003886674 cites W2897201028 @default.
- W3003886674 cites W2901427535 @default.
- W3003886674 cites W2902495802 @default.
- W3003886674 cites W3007298644 @default.
- W3003886674 cites W3048394244 @default.
- W3003886674 doi "https://doi.org/10.1017/s0016756819001262" @default.
- W3003886674 hasPublicationYear "2019" @default.
- W3003886674 type Work @default.
- W3003886674 sameAs 3003886674 @default.
- W3003886674 citedByCount "24" @default.
- W3003886674 countsByYear W30038866742020 @default.
- W3003886674 countsByYear W30038866742021 @default.
- W3003886674 countsByYear W30038866742022 @default.
- W3003886674 countsByYear W30038866742023 @default.