FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2902296922> ?p ?o ?g. }

• W2902296922 endingPage "296" @default.
• W2902296922 startingPage "268" @default.
• W2902296922 abstract "The Cretaceous (upper Aptian) Romualdo Formation of the Araripe Basin, northeastern Brazil, is a marine-influenced, predominantly fine-grained siliciclastic unit. In the eastern part of the basin, it corresponds to a depositional sequence composed of two transgressive-regressive cycles. Low-diversity benthic macrofaunas document high-stress conditions. Their palaeoecological and taphonomic analysis allows for the detailed reconstruction of the palaeoenvironments and of the temporal changes in the palaeoecosystem. The transgressive part of the lower cycle is a black shale with calcareous concretions that contain excellently preserved fishes and other vertebrates (the famous “Santana fossils”), but apart from abundant ostracods and rare decapod crustaceans, benthic faunal elements are very rare due to anoxic to dysoxic conditions. A low-diversity parautochthonous molluscan fauna of small bivalves and gastropods records fluctuating dysoxic conditions during early regression. Towards the top of the measured sections (late regression), thin gastropod shell beds become conspicuous. At the top of the sections decimetre-thick shell concentrations show signs of reworking and a greater marine influence (transgressive part of the upper cycle). The distribution pattern of three benthic associations and two assemblages is almost equally shaped by three environmental parameters: The low overall species diversity, small size of the fauna, and the lack of stenohaline elements suggest lowered and fluctuating salinity conditions. Fluctuating redox conditions with anoxia to dysoxia, identified especially in the lower parts of the succession, and substrate were the other two factors shaping the faunal distribution. The late Aptian sedimentary and faunal history of the eastern part of the basin indicates restricted marine influence, coupled with increasing freshwater input during phases of sea-level lowstand, and low-energy conditions offshore, which led to widespread anoxia, especially in the lower part of the formation. Thus, palaeoecological analyses are an excellent tool to disentangle the various environmental parameters that shaped the palaeoenvironments of the basin, to understand more closely its Fossil-Lagerstätten, and to corroborate and fine-tune the sequence stratigraphic framework." @default.
• W2902296922 created "2018-12-11" @default.
• W2902296922 creator A5009085965 @default.
• W2902296922 creator A5015291250 @default.
• W2902296922 creator A5030221814 @default.
• W2902296922 creator A5042851364 @default.
• W2902296922 creator A5053215574 @default.
• W2902296922 creator A5070571132 @default.
• W2902296922 creator A5072723846 @default.
• W2902296922 creator A5076386510 @default.
• W2902296922 date "2019-03-01" @default.
• W2902296922 modified "2023-10-14" @default.
• W2902296922 title "Analysis of a Cretaceous (late Aptian) high-stress ecosystem: The Romualdo Formation of the Araripe Basin, northeastern Brazil" @default.
• W2902296922 cites W1753926244 @default.
• W2902296922 cites W1914971467 @default.
• W2902296922 cites W1964490831 @default.
• W2902296922 cites W1973192023 @default.
• W2902296922 cites W1980773740 @default.
• W2902296922 cites W1983221745 @default.
• W2902296922 cites W1998995868 @default.
• W2902296922 cites W2004720683 @default.
• W2902296922 cites W2006054477 @default.
• W2902296922 cites W2006950113 @default.
• W2902296922 cites W2009979315 @default.
• W2902296922 cites W2023121856 @default.
• W2902296922 cites W2032519593 @default.
• W2902296922 cites W2059794687 @default.
• W2902296922 cites W2064860762 @default.
• W2902296922 cites W2065781713 @default.
• W2902296922 cites W2067788615 @default.
• W2902296922 cites W2081988263 @default.
• W2902296922 cites W2089161835 @default.
• W2902296922 cites W2096692162 @default.
• W2902296922 cites W2099053943 @default.
• W2902296922 cites W2111834669 @default.
• W2902296922 cites W2118957528 @default.
• W2902296922 cites W2139892557 @default.
• W2902296922 cites W2167635447 @default.
• W2902296922 cites W2313706987 @default.
• W2902296922 cites W2404164930 @default.
• W2902296922 cites W2421790818 @default.
• W2902296922 cites W2741460040 @default.
• W2902296922 cites W2802333519 @default.
• W2902296922 cites W3190849289 @default.
• W2902296922 cites W3194457679 @default.
• W2902296922 cites W4232297496 @default.
• W2902296922 cites W4235887661 @default.
• W2902296922 cites W4241419786 @default.
• W2902296922 cites W4249457135 @default.
• W2902296922 cites W4255746133 @default.
• W2902296922 cites W4361758394 @default.
• W2902296922 cites W563929547 @default.
• W2902296922 cites W75654697 @default.
• W2902296922 doi "https://doi.org/10.1016/j.cretres.2018.11.021" @default.
• W2902296922 hasPublicationYear "2019" @default.
• W2902296922 type Work @default.
• W2902296922 sameAs 2902296922 @default.
• W2902296922 citedByCount "27" @default.
• W2902296922 countsByYear W29022969222019 @default.
• W2902296922 countsByYear W29022969222020 @default.
• W2902296922 countsByYear W29022969222021 @default.
• W2902296922 countsByYear W29022969222022 @default.
• W2902296922 countsByYear W29022969222023 @default.
• W2902296922 crossrefType "journal-article" @default.
• W2902296922 hasAuthorship W2902296922A5009085965 @default.
• W2902296922 hasAuthorship W2902296922A5015291250 @default.
• W2902296922 hasAuthorship W2902296922A5030221814 @default.
• W2902296922 hasAuthorship W2902296922A5042851364 @default.
• W2902296922 hasAuthorship W2902296922A5053215574 @default.
• W2902296922 hasAuthorship W2902296922A5070571132 @default.
• W2902296922 hasAuthorship W2902296922A5072723846 @default.
• W2902296922 hasAuthorship W2902296922A5076386510 @default.
• W2902296922 hasConcept C10277891 @default.
• W2902296922 hasConcept C109007969 @default.
• W2902296922 hasConcept C111368507 @default.
• W2902296922 hasConcept C12294951 @default.
• W2902296922 hasConcept C125471540 @default.
• W2902296922 hasConcept C126753816 @default.
• W2902296922 hasConcept C127313418 @default.
• W2902296922 hasConcept C150117547 @default.
• W2902296922 hasConcept C151730666 @default.
• W2902296922 hasConcept C18903297 @default.
• W2902296922 hasConcept C189473229 @default.
• W2902296922 hasConcept C2777620812 @default.
• W2902296922 hasConcept C6494504 @default.
• W2902296922 hasConcept C83042747 @default.
• W2902296922 hasConcept C86803240 @default.
• W2902296922 hasConcept C93257316 @default.
• W2902296922 hasConceptScore W2902296922C10277891 @default.
• W2902296922 hasConceptScore W2902296922C109007969 @default.
• W2902296922 hasConceptScore W2902296922C111368507 @default.
• W2902296922 hasConceptScore W2902296922C12294951 @default.
• W2902296922 hasConceptScore W2902296922C125471540 @default.
• W2902296922 hasConceptScore W2902296922C126753816 @default.
• W2902296922 hasConceptScore W2902296922C127313418 @default.
• W2902296922 hasConceptScore W2902296922C150117547 @default.
• W2902296922 hasConceptScore W2902296922C151730666 @default.
• W2902296922 hasConceptScore W2902296922C18903297 @default.

• next