Articles | Volume 13, issue 7
https://doi.org/10.5194/cp-13-855-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-13-855-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Water-mass evolution in the Cretaceous Western Interior Seaway of North America and equatorial Atlantic
James S. Eldrett
CORRESPONDING AUTHOR
Shell International Exploration & Production B.V, Kesslerpark 1,
2288 GS Rijswijk, the Netherlands
Paul Dodsworth
StrataSolve Ltd, 42 Gaskell Street, Stockton Heath, Warrington, WA4
2UN, UK
Steven C. Bergman
Shell International Exploration and Production Inc, 200 N. Dairy Ashford, Houston, TX 77079, USA
Milly Wright
Chemostrat Inc., 3760 Westchase Drive, Houston, Texas, TX 77042, USA
Daniel Minisini
Shell International Exploration and Production Inc, 200 N. Dairy Ashford, Houston, TX 77079, USA
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- Revisiting paleoenvironmental analyses and interpretations of organic-rich deposits: The importance of TOC corrections B. Hart & M. Hofmann 10.1016/j.orggeochem.2022.104434
- Quantifying the pattern of organic carbon burial through Cretaceous Oceanic Anoxic Event 2 H. Guo et al. 10.1016/j.earscirev.2024.104903
- Distribution of Albian dinoflagellate cyst associations along a proximal–distal transect across the Iberian margin R. Sánchez-Pellicer et al. 10.1016/j.cretres.2018.08.004
- New Constraints on Global Geochemical Cycling During Oceanic Anoxic Event 2 (Late Cretaceous) From a 6‐Million‐year Long Molybdenum‐Isotope Record A. Dickson et al. 10.1029/2020GC009246
Latest update: 17 Nov 2024
Short summary
This contribution integrates new data on the main components of organic matter, geochemistry, and stable isotopes for the Cenomanian to Coniacian stages of the Late Cretaceous, along a north–south transect from the Cretaceous Western Interior Seaway to the equatorial western Atlantic and Southern Ocean. Distinct palynological assemblages and geochemical signatures allow insights into palaeoenvironmental conditions and water-mass evolution during this greenhouse climate period.
This contribution integrates new data on the main components of organic matter, geochemistry,...