FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3039345230> ?p ?o ?g. }

• W3039345230 endingPage "116417" @default.
• W3039345230 startingPage "116417" @default.
• W3039345230 abstract "Organic geochemistry and palynology reveal major organofacies changes in the marginal marine Polish Basin during the early Toarcian linked to changes in environmental conditions. Increasing water salinity and enhanced biomass contributions from phytoplankton, adopted to brackish conditions, attest to periodic marine ingressions into the paralic, hyposaline Polish Basin. Marine ingressions occurred upon reoccurring sea level rises concomitant with i) the Pliensbachian-Toarcian boundary carbon isotope excursion (Pl-Toa-CIE) and ii) the stepped Toarcian carbon isotope excursion (Toa-CIE), the latter marking the Toarcian Oceanic Anoxic Event (Toa-OAE). Strata with marine influences indicate an intermittent connection of the Polish Basin with the Tethys and attest to a close correlation between regional shoreline progradation and evolution of global climate and sea-level. Organic geochemistry indicated the link between sea level fluctuations and the Toa-CIEs, although in some areas of the Polish Basin the sea level rise was balanced by massively increased sediment delivery, caused by enhanced hydrological cycling that lead to intensified weathering and erosion in the hinterland. Enhanced hydrological cycling further led to the remobilization of organic matter of pre-Toarcian age. This points to erosion of older organic-rich rocks containing significant abundances of marine and terrestrial organic matter that was partly oxidized and re-deposited along with autochthonous Toarcian organic matter. Provenance areas identified point to two main sources, most likely Carboniferous terrestrial/paralic and Ordovician/Silurian marine sediments. Fossil organic matter should be considered as additional source in Toarcian carbon cycling, particularly in times of enhanced hydrological cycling, erosion and weathering. Remobilization of sedimentary fossil carbon has not been hitherto considered as a carbon source during the Toa-OAE." @default.
• W3039345230 created "2020-07-10" @default.
• W3039345230 creator A5005996014 @default.
• W3039345230 creator A5038818609 @default.
• W3039345230 creator A5050324042 @default.
• W3039345230 date "2020-09-01" @default.
• W3039345230 modified "2023-10-16" @default.
• W3039345230 title "Toarcian climate and carbon cycle perturbations – its impact on sea-level changes, enhanced mobilization and oxidation of fossil organic matter" @default.
• W3039345230 cites W1741840930 @default.
• W3039345230 cites W1973714196 @default.
• W3039345230 cites W1980332399 @default.
• W3039345230 cites W1984588636 @default.
• W3039345230 cites W1985780433 @default.
• W3039345230 cites W1987274073 @default.
• W3039345230 cites W1989120963 @default.
• W3039345230 cites W1991994411 @default.
• W3039345230 cites W1999601775 @default.
• W3039345230 cites W2012792340 @default.
• W3039345230 cites W2015414354 @default.
• W3039345230 cites W2037282588 @default.
• W3039345230 cites W2039311538 @default.
• W3039345230 cites W2041889108 @default.
• W3039345230 cites W2045386399 @default.
• W3039345230 cites W2045577686 @default.
• W3039345230 cites W2049198600 @default.
• W3039345230 cites W2057907380 @default.
• W3039345230 cites W2067601188 @default.
• W3039345230 cites W2069355839 @default.
• W3039345230 cites W2073811376 @default.
• W3039345230 cites W2075532353 @default.
• W3039345230 cites W2075833095 @default.
• W3039345230 cites W2077671227 @default.
• W3039345230 cites W2078494597 @default.
• W3039345230 cites W2083349226 @default.
• W3039345230 cites W2087917706 @default.
• W3039345230 cites W2093290405 @default.
• W3039345230 cites W2094389216 @default.
• W3039345230 cites W2100451784 @default.
• W3039345230 cites W2130529687 @default.
• W3039345230 cites W2135475224 @default.
• W3039345230 cites W2144805683 @default.
• W3039345230 cites W2150802815 @default.
• W3039345230 cites W2326669813 @default.
• W3039345230 cites W2336329814 @default.
• W3039345230 cites W2466337770 @default.
• W3039345230 cites W2516408479 @default.
• W3039345230 cites W2558715874 @default.
• W3039345230 cites W2566115017 @default.
• W3039345230 cites W2748920119 @default.
• W3039345230 cites W2783067866 @default.
• W3039345230 cites W2794563711 @default.
• W3039345230 cites W2797913866 @default.
• W3039345230 cites W2901427535 @default.
• W3039345230 cites W2903939507 @default.
• W3039345230 cites W2918806787 @default.
• W3039345230 cites W2943547454 @default.
• W3039345230 cites W2970099468 @default.
• W3039345230 cites W2986613334 @default.
• W3039345230 cites W2999762139 @default.
• W3039345230 cites W3017276564 @default.
• W3039345230 cites W4253646848 @default.
• W3039345230 cites W618381329 @default.
• W3039345230 doi "https://doi.org/10.1016/j.epsl.2020.116417" @default.
• W3039345230 hasPublicationYear "2020" @default.
• W3039345230 type Work @default.
• W3039345230 sameAs 3039345230 @default.
• W3039345230 citedByCount "14" @default.
• W3039345230 countsByYear W30393452302021 @default.
• W3039345230 countsByYear W30393452302022 @default.
• W3039345230 countsByYear W30393452302023 @default.
• W3039345230 crossrefType "journal-article" @default.
• W3039345230 hasAuthorship W3039345230A5005996014 @default.
• W3039345230 hasAuthorship W3039345230A5038818609 @default.
• W3039345230 hasAuthorship W3039345230A5050324042 @default.
• W3039345230 hasConcept C109007969 @default.
• W3039345230 hasConcept C110872660 @default.
• W3039345230 hasConcept C111368507 @default.
• W3039345230 hasConcept C126559015 @default.
• W3039345230 hasConcept C127313418 @default.
• W3039345230 hasConcept C151730666 @default.
• W3039345230 hasConcept C158787203 @default.
• W3039345230 hasConcept C17409809 @default.
• W3039345230 hasConcept C18903297 @default.
• W3039345230 hasConcept C2780049196 @default.
• W3039345230 hasConcept C2816523 @default.
• W3039345230 hasConcept C40724407 @default.
• W3039345230 hasConcept C48743137 @default.
• W3039345230 hasConcept C6494504 @default.
• W3039345230 hasConcept C6939412 @default.
• W3039345230 hasConcept C86803240 @default.
• W3039345230 hasConcept C94336100 @default.
• W3039345230 hasConceptScore W3039345230C109007969 @default.
• W3039345230 hasConceptScore W3039345230C110872660 @default.
• W3039345230 hasConceptScore W3039345230C111368507 @default.
• W3039345230 hasConceptScore W3039345230C126559015 @default.
• W3039345230 hasConceptScore W3039345230C127313418 @default.
• W3039345230 hasConceptScore W3039345230C151730666 @default.
• W3039345230 hasConceptScore W3039345230C158787203 @default.

• next