FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W873443637> ?p ?o ?g. }

• W873443637 endingPage "14" @default.
• W873443637 startingPage "1" @default.
• W873443637 abstract "The early diagenetic formation of dolomite in modern aquatic environments is limited mostly to evaporitic and marine-anoxic, organic-rich sediments dominated by bacterial sulfate reduction (BSR). In such environments, bacterial activity lowers the energy barriers for the nucleation and growth of dolomite and thus promotes the formation of non-stoichiometric, highly disordered and metastable (proto)dolomite. Although the boundary conditions for the formation of modern (proto)dolomites are considered to be generally understood, the role of BSR during limestone dolomitization in ancient marine environments remains questionable. Herein, we present a study about the physicochemical conditions and processes, which led to the formation of partly dolomitized limestone and dolostone in the presence of BSR on a stable carbonate platform during the Upper Jurassic at Oker (Northern German Basin). The dolomite textures, the spatial trace elemental patterns of the dolomite and of the surrounding limestone and the results of δ18O and δ13C isotope analyses reveal that the Oker dolomite has been formed by the early diagenetic replacement of magnesian calcite precursors at temperatures between 26 °C and 37 °C. We interpret the mineralizing fluids responsible for dolomitization as pristine-marine to slightly evaporitic and reducing seawater being modified during shallow seepage reflux and/or evaporitic tidal pumping. The elevated δ34SCAS values (+ 17.9 to + 19.7‰, V-CDT) of the Oker dolomite, compared to ambient Upper Jurassic seawater, indicate that BSR facilitated dolomite formation. For the first time, we show that a linear anti-correlation exists between decreasing carbonate-associated sulfate (CAS) contents in dolomite and increasing ordering ratio of the dolomite lattice structure, with the degree of cation order in dolomite to be given by: degree of cation order(Dol): = − 0.018·CAS(Dol) + 68.3 (R2 = 0.98). This correlation implies that the CAS content of sedimentary dolomite can be used as a measure for dolomite maturity. The relationships between the ambient (paleo)environmental controls, the resultant dolomitization pathways and subsequently the structure and the composition of the precipitating dolomite are presented and discussed in relation to the stability of modern and ancient (proto)dolomites throughout burial diagenesis." @default.
• W873443637 created "2016-06-24" @default.
• W873443637 creator A5009488476 @default.
• W873443637 creator A5013157752 @default.
• W873443637 creator A5021360659 @default.
• W873443637 creator A5023085486 @default.
• W873443637 creator A5034850692 @default.
• W873443637 creator A5042828801 @default.
• W873443637 creator A5049501022 @default.
• W873443637 creator A5058741948 @default.
• W873443637 creator A5067749897 @default.
• W873443637 creator A5073021685 @default.
• W873443637 creator A5077040204 @default.
• W873443637 date "2015-09-01" @default.
• W873443637 modified "2023-10-16" @default.
• W873443637 title "The role of bacterial sulfate reduction during dolomite precipitation: Implications from Upper Jurassic platform carbonates" @default.
• W873443637 cites W1536058474 @default.
• W873443637 cites W1943121318 @default.
• W873443637 cites W1967628674 @default.
• W873443637 cites W1971957115 @default.
• W873443637 cites W1976131977 @default.
• W873443637 cites W1984007724 @default.
• W873443637 cites W1984849392 @default.
• W873443637 cites W1993898064 @default.
• W873443637 cites W1996137722 @default.
• W873443637 cites W2002145143 @default.
• W873443637 cites W2003315307 @default.
• W873443637 cites W2005391004 @default.
• W873443637 cites W2009063669 @default.
• W873443637 cites W2017918382 @default.
• W873443637 cites W2019795776 @default.
• W873443637 cites W2020370474 @default.
• W873443637 cites W2020434687 @default.
• W873443637 cites W2021862772 @default.
• W873443637 cites W2024405815 @default.
• W873443637 cites W2032435490 @default.
• W873443637 cites W2033432841 @default.
• W873443637 cites W2035154510 @default.
• W873443637 cites W2041710079 @default.
• W873443637 cites W2046020514 @default.
• W873443637 cites W2060971146 @default.
• W873443637 cites W2062219322 @default.
• W873443637 cites W2066450007 @default.
• W873443637 cites W2066774031 @default.
• W873443637 cites W2068250761 @default.
• W873443637 cites W2068324827 @default.
• W873443637 cites W2071091649 @default.
• W873443637 cites W2071402402 @default.
• W873443637 cites W2075417561 @default.
• W873443637 cites W2077568485 @default.
• W873443637 cites W2078575433 @default.
• W873443637 cites W2080602377 @default.
• W873443637 cites W2081009732 @default.
• W873443637 cites W2087280943 @default.
• W873443637 cites W2088498028 @default.
• W873443637 cites W2090774054 @default.
• W873443637 cites W2097627207 @default.
• W873443637 cites W2103242979 @default.
• W873443637 cites W2124804210 @default.
• W873443637 cites W2133038839 @default.
• W873443637 cites W2136991385 @default.
• W873443637 cites W2155328428 @default.
• W873443637 cites W2156215403 @default.
• W873443637 cites W2315477082 @default.
• W873443637 cites W300313049 @default.
• W873443637 cites W4245377069 @default.
• W873443637 doi "https://doi.org/10.1016/j.chemgeo.2015.07.020" @default.
• W873443637 hasPublicationYear "2015" @default.
• W873443637 type Work @default.
• W873443637 sameAs 873443637 @default.
• W873443637 citedByCount "72" @default.
• W873443637 countsByYear W8734436372016 @default.
• W873443637 countsByYear W8734436372017 @default.
• W873443637 countsByYear W8734436372018 @default.
• W873443637 countsByYear W8734436372019 @default.
• W873443637 countsByYear W8734436372020 @default.
• W873443637 countsByYear W8734436372021 @default.
• W873443637 countsByYear W8734436372022 @default.
• W873443637 countsByYear W8734436372023 @default.
• W873443637 crossrefType "journal-article" @default.
• W873443637 hasAuthorship W873443637A5009488476 @default.
• W873443637 hasAuthorship W873443637A5013157752 @default.
• W873443637 hasAuthorship W873443637A5021360659 @default.
• W873443637 hasAuthorship W873443637A5023085486 @default.
• W873443637 hasAuthorship W873443637A5034850692 @default.
• W873443637 hasAuthorship W873443637A5042828801 @default.
• W873443637 hasAuthorship W873443637A5049501022 @default.
• W873443637 hasAuthorship W873443637A5058741948 @default.
• W873443637 hasAuthorship W873443637A5067749897 @default.
• W873443637 hasAuthorship W873443637A5073021685 @default.
• W873443637 hasAuthorship W873443637A5077040204 @default.
• W873443637 hasConcept C108970007 @default.
• W873443637 hasConcept C109007969 @default.
• W873443637 hasConcept C111368507 @default.
• W873443637 hasConcept C127313418 @default.
• W873443637 hasConcept C130452526 @default.
• W873443637 hasConcept C146588470 @default.
• W873443637 hasConcept C151730666 @default.

• next