Matches in SemOpenAlex for { <https://semopenalex.org/work/W2097673402> ?p ?o ?g. }
- W2097673402 endingPage "974" @default.
- W2097673402 startingPage "955" @default.
- W2097673402 abstract "Abstract Nodular carbonates (“calcretes”) in continental foreland-basin strata of the Early Cretaceous Cedar Mountain Formation (CMF) in eastern Utah yield δ13C and δ18O records of changes in the exogenic carbon cycle related to oceanic anoxic events (OAEs), and terrestrial paleoclimate. Chemostratigraphic profiles of both forebulge and foredeep sections show two prominent positive δ13C excursions, each with a peak value of −3%0 VPDB, and having background δ13C values of about −6%0 VPDB. These excursions correlate with the global early Aptian (Ap7) and late Aptian–early Albian (Ap12-Al1) carbon isotope excursions. Aptian–Albian positive δ13C excursions in the CMF also correspond to 3–4 per mil increases in carbonate δ18O. These phenomena record local aridification events. The chemostratigraphic profile on the thinner forebulge section of the CMF is calibrated, for the first time, by a radiogenic U-Pb date of 119.4 ± 2.6 Ma on a carbonate bed, and by detrital zircon U-Pb dates on two bounding sandstone units (maximum depositional ages of 146 Ma and 112 Ma). Petrographic observations and diagenetic analyses of micritic to microsparitic carbonates from nodules indicate palustrine origins and demonstrate that they crystallized in shallow early meteoric phreatic environments. Meteoric calcite lines derived from CMF carbonates have δ18O values ranging between −8.1 to −7.5%0 VPDB, supporting an estimate of zonal mean groundwater δ18O of −6%0 VSMOW for an Aptian–Albian paleolatitude of 34° N. Furthermore, our two chemostratigraphic profiles exhibit a generally proportionate thinning of correlative strata from the foredeep on to the forebulge, suggesting that there were consistently lower rates of accumulation on the forebulge during the Aptian–Albian. Identification of the global Aptian–Albian δ13C excursions in purely continental strata, as demonstrated in this paper, opens a new avenue of research by identifying specific stratigraphic intervals that record the terrestrial paleoclimatic impacts of perturbations of the global carbon cycle." @default.
- W2097673402 created "2016-06-24" @default.
- W2097673402 creator A5014581226 @default.
- W2097673402 creator A5028101783 @default.
- W2097673402 creator A5034448431 @default.
- W2097673402 creator A5047905444 @default.
- W2097673402 creator A5050627671 @default.
- W2097673402 creator A5053991815 @default.
- W2097673402 creator A5061919419 @default.
- W2097673402 creator A5062759957 @default.
- W2097673402 date "2010-11-01" @default.
- W2097673402 modified "2023-10-18" @default.
- W2097673402 title "Correlation of Aptian-Albian Carbon Isotope Excursions in Continental Strata of the Cretaceous Foreland Basin, Eastern Utah, U.S.A." @default.
- W2097673402 cites W127908135 @default.
- W2097673402 cites W1489110358 @default.
- W2097673402 cites W1499713561 @default.
- W2097673402 cites W1562742035 @default.
- W2097673402 cites W1565225215 @default.
- W2097673402 cites W1575720263 @default.
- W2097673402 cites W1620286502 @default.
- W2097673402 cites W1871959888 @default.
- W2097673402 cites W1901354518 @default.
- W2097673402 cites W1971346015 @default.
- W2097673402 cites W1984491575 @default.
- W2097673402 cites W1986697352 @default.
- W2097673402 cites W1989094481 @default.
- W2097673402 cites W1989917856 @default.
- W2097673402 cites W1991487937 @default.
- W2097673402 cites W1998995868 @default.
- W2097673402 cites W2000179313 @default.
- W2097673402 cites W2008831534 @default.
- W2097673402 cites W2022000360 @default.
- W2097673402 cites W2022393502 @default.
- W2097673402 cites W2028095175 @default.
- W2097673402 cites W2035366718 @default.
- W2097673402 cites W2037287448 @default.
- W2097673402 cites W2050045661 @default.
- W2097673402 cites W2053259135 @default.
- W2097673402 cites W2058540279 @default.
- W2097673402 cites W2060323442 @default.
- W2097673402 cites W2067774309 @default.
- W2097673402 cites W2068257128 @default.
- W2097673402 cites W2074719200 @default.
- W2097673402 cites W2080526091 @default.
- W2097673402 cites W2081034583 @default.
- W2097673402 cites W2085401592 @default.
- W2097673402 cites W2088077327 @default.
- W2097673402 cites W2088970901 @default.
- W2097673402 cites W2090788098 @default.
- W2097673402 cites W2094290315 @default.
- W2097673402 cites W2096453514 @default.
- W2097673402 cites W2101772626 @default.
- W2097673402 cites W2101837538 @default.
- W2097673402 cites W2110608195 @default.
- W2097673402 cites W2121269192 @default.
- W2097673402 cites W2123085228 @default.
- W2097673402 cites W2132166311 @default.
- W2097673402 cites W2143741390 @default.
- W2097673402 cites W2155104238 @default.
- W2097673402 cites W2158556978 @default.
- W2097673402 cites W2167065746 @default.
- W2097673402 cites W2169444223 @default.
- W2097673402 cites W2178590323 @default.
- W2097673402 cites W2320388366 @default.
- W2097673402 cites W2329332868 @default.
- W2097673402 cites W2331841192 @default.
- W2097673402 cites W2477858909 @default.
- W2097673402 cites W2481669548 @default.
- W2097673402 cites W2495643041 @default.
- W2097673402 cites W2797914455 @default.
- W2097673402 cites W2912219260 @default.
- W2097673402 cites W2993037320 @default.
- W2097673402 cites W3165816126 @default.
- W2097673402 cites W655934160 @default.
- W2097673402 doi "https://doi.org/10.2110/jsr.2010.086" @default.
- W2097673402 hasPublicationYear "2010" @default.
- W2097673402 type Work @default.
- W2097673402 sameAs 2097673402 @default.
- W2097673402 citedByCount "60" @default.
- W2097673402 countsByYear W20976734022012 @default.
- W2097673402 countsByYear W20976734022013 @default.
- W2097673402 countsByYear W20976734022014 @default.
- W2097673402 countsByYear W20976734022015 @default.
- W2097673402 countsByYear W20976734022016 @default.
- W2097673402 countsByYear W20976734022017 @default.
- W2097673402 countsByYear W20976734022018 @default.
- W2097673402 countsByYear W20976734022019 @default.
- W2097673402 countsByYear W20976734022020 @default.
- W2097673402 countsByYear W20976734022021 @default.
- W2097673402 countsByYear W20976734022022 @default.
- W2097673402 countsByYear W20976734022023 @default.
- W2097673402 crossrefType "journal-article" @default.
- W2097673402 hasAuthorship W2097673402A5014581226 @default.
- W2097673402 hasAuthorship W2097673402A5028101783 @default.
- W2097673402 hasAuthorship W2097673402A5034448431 @default.
- W2097673402 hasAuthorship W2097673402A5047905444 @default.
- W2097673402 hasAuthorship W2097673402A5050627671 @default.
- W2097673402 hasAuthorship W2097673402A5053991815 @default.