FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2999707118> ?p ?o ?g. }

• W2999707118 endingPage "119457" @default.
• W2999707118 startingPage "119457" @default.
• W2999707118 abstract "This study presents new stable carbon and oxygen isotope data from Lower Cretaceous lacustrine carbonate rock samples recovered from a well drilled in the Santos Basin, offshore southeast Brazil. These samples represent a record of a continental environment just prior to the opening of the South Atlantic Ocean and the ultimate break-up of Gondwanaland. The geochemical data, along with carbonate mineralogy, indicate repeated cycles of lake level variation that could be attributed to climatic oscillations. Despite the absence of correlations between δ13C and δ18O values, facies analysis and the isotopic and mineralogical data suggest that lake hydrology was essentially closed for most of the depositional interval studied here. The existence of persisting trends of nearly constant δ13C values with a spread in δ18O values though, suggests long water residence times in the palaeolake, equilibrium between atmosphere and lake water CO2, as well as significant evaporation of water. The overall geological model that emerges unveils a more comprehensive picture of the depositional conditions that favoured the continuity of a significant carbonate factory in the middle of the Gondwanan continent, corroborating previous studies that suggested the lasting existence of a large and somewhat shallow endorheic lake in the area during the Early Cretaceous. As a result of this recorded trend strongly suggesting equilibrium between lake waters DIC (dissolved inorganic carbon) reservoir and atmospheric CO2, the data are most consistent with lacustrine deposition rather than precipitation of travertine, contrasting with some suggestions for the genesis of the carbonates of the Barra Velha Formation. Finally, this apparent equilibrium with the atmosphere likely left a preserved record in the continental carbonates of the final stages that preceded a major global environmental disturbance associated with an increase in atmospheric CO2, known for this time as the Oceanic Anoxic Event (OAE) 1a. If this is correct, it also helps to put further time constraints on this studied interval, which should not be younger than Barremian age, and to provide a regional continental perspective on a global event." @default.
• W2999707118 created "2020-01-23" @default.
• W2999707118 creator A5005235814 @default.
• W2999707118 creator A5024527509 @default.
• W2999707118 creator A5061409205 @default.
• W2999707118 creator A5061782747 @default.
• W2999707118 creator A5070285311 @default.
• W2999707118 creator A5085465618 @default.
• W2999707118 date "2020-03-01" @default.
• W2999707118 modified "2023-10-09" @default.
• W2999707118 title "Environmental conditions of deposition of the Lower Cretaceous lacustrine carbonates of the Barra Velha Formation, Santos Basin (Brazil), based on stable carbon and oxygen isotopes: A continental record of pCO2 during the onset of the Oceanic Anoxic Event 1a (OAE 1a) interval?" @default.
• W2999707118 cites W1552509298 @default.
• W2999707118 cites W1753926244 @default.
• W2999707118 cites W1894009859 @default.
• W2999707118 cites W1976172506 @default.
• W2999707118 cites W1981554422 @default.
• W2999707118 cites W1982501612 @default.
• W2999707118 cites W1984491575 @default.
• W2999707118 cites W1985005684 @default.
• W2999707118 cites W1985260036 @default.
• W2999707118 cites W1989094481 @default.
• W2999707118 cites W1994625158 @default.
• W2999707118 cites W2002477667 @default.
• W2999707118 cites W2007460213 @default.
• W2999707118 cites W2014796857 @default.
• W2999707118 cites W2030202003 @default.
• W2999707118 cites W2040610203 @default.
• W2999707118 cites W2041414242 @default.
• W2999707118 cites W2047821851 @default.
• W2999707118 cites W2056212443 @default.
• W2999707118 cites W2058695708 @default.
• W2999707118 cites W2069217550 @default.
• W2999707118 cites W2069299766 @default.
• W2999707118 cites W2081582907 @default.
• W2999707118 cites W2087829981 @default.
• W2999707118 cites W2090584708 @default.
• W2999707118 cites W2090887314 @default.
• W2999707118 cites W2091065315 @default.
• W2999707118 cites W2093175720 @default.
• W2999707118 cites W2094300388 @default.
• W2999707118 cites W2100384649 @default.
• W2999707118 cites W2114261226 @default.
• W2999707118 cites W2116562977 @default.
• W2999707118 cites W2122192644 @default.
• W2999707118 cites W2123643570 @default.
• W2999707118 cites W2141458985 @default.
• W2999707118 cites W2194494583 @default.
• W2999707118 cites W2229288588 @default.
• W2999707118 cites W2327897834 @default.
• W2999707118 cites W2489702557 @default.
• W2999707118 cites W2522822380 @default.
• W2999707118 cites W2603234425 @default.
• W2999707118 cites W2734605197 @default.
• W2999707118 cites W2775262878 @default.
• W2999707118 cites W2782645152 @default.
• W2999707118 cites W2793843209 @default.
• W2999707118 cites W2863449753 @default.
• W2999707118 cites W2913387978 @default.
• W2999707118 cites W2941195061 @default.
• W2999707118 cites W995534035 @default.
• W2999707118 doi "https://doi.org/10.1016/j.chemgeo.2019.119457" @default.
• W2999707118 hasPublicationYear "2020" @default.
• W2999707118 type Work @default.
• W2999707118 sameAs 2999707118 @default.
• W2999707118 citedByCount "24" @default.
• W2999707118 countsByYear W29997071182020 @default.
• W2999707118 countsByYear W29997071182021 @default.
• W2999707118 countsByYear W29997071182022 @default.
• W2999707118 countsByYear W29997071182023 @default.
• W2999707118 crossrefType "journal-article" @default.
• W2999707118 hasAuthorship W2999707118A5005235814 @default.
• W2999707118 hasAuthorship W2999707118A5024527509 @default.
• W2999707118 hasAuthorship W2999707118A5061409205 @default.
• W2999707118 hasAuthorship W2999707118A5061782747 @default.
• W2999707118 hasAuthorship W2999707118A5070285311 @default.
• W2999707118 hasAuthorship W2999707118A5085465618 @default.
• W2999707118 hasConcept C109007969 @default.
• W2999707118 hasConcept C121332964 @default.
• W2999707118 hasConcept C12294951 @default.
• W2999707118 hasConcept C126753816 @default.
• W2999707118 hasConcept C127313418 @default.
• W2999707118 hasConcept C146588470 @default.
• W2999707118 hasConcept C151730666 @default.
• W2999707118 hasConcept C158787203 @default.
• W2999707118 hasConcept C17409809 @default.
• W2999707118 hasConcept C182348080 @default.
• W2999707118 hasConcept C185059815 @default.
• W2999707118 hasConcept C18903297 @default.
• W2999707118 hasConcept C191897082 @default.
• W2999707118 hasConcept C192562407 @default.
• W2999707118 hasConcept C19320362 @default.
• W2999707118 hasConcept C22117777 @default.
• W2999707118 hasConcept C2780659211 @default.
• W2999707118 hasConcept C62520636 @default.
• W2999707118 hasConcept C64297162 @default.
• W2999707118 hasConcept C6494504 @default.
• W2999707118 hasConcept C69384203 @default.
• W2999707118 hasConcept C71468253 @default.

• next