Articles | Volume 16, issue 21
https://doi.org/10.5194/bg-16-4201-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-16-4201-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Phytoplankton community disruption caused by latest Cretaceous global warming
Johan Vellekoop
CORRESPONDING AUTHOR
Department of Earth and Environmental Sciences, Division of Geology,
KU Leuven, 3001 Heverlee, Belgium
Lineke Woelders
Department of Earth and Environmental Sciences, Division of Geology,
KU Leuven, 3001 Heverlee, Belgium
Appy Sluijs
Department of Earth Sciences, Marine Palynology and Paleoceanography,
Laboratory of Palaeobotany and Palynology, Utrecht University, 3584CB,
Utrecht, the Netherlands
Kenneth G. Miller
Department of Earth and Planetary Sciences, Rutgers University,
Piscataway, New Jersey 08854, USA
Robert P. Speijer
Department of Earth and Environmental Sciences, Division of Geology,
KU Leuven, 3001 Heverlee, Belgium
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17 citations as recorded by crossref.
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- Comparative Analysis of the conditions for the red tidies development at the Cretaceous–Paleogene boundary of the Stevens Klint and Zumaia sections P. Egorov et al. 10.1088/1755-1315/1229/1/012034
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- Clumped-isotope-derived climate trends leading up to the end-Cretaceous mass extinction in northwestern Europe H. O'Hora et al. 10.5194/cp-18-1963-2022
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- Palynostratigraphical analysis of the late Maastrichtian – early Danian in the Gaviotín Formation, Punta del Este Basin, Uruguay G. Daners et al. 10.1016/j.marpetgeo.2022.105728
- Paleoenvironmental and paleoclimatic changes during the Late Cretaceous and Cretaceous–Paleogene (K/Pg) boundary transition in Tattofte, External Rif, northwestern Morocco: implications from dinoflagellate cysts and palynofacies H. Jbari & H. Slimani 10.1016/j.palwor.2021.08.002
- Influence of the Latest Maastrichtian Warming Event on planktic foraminiferal assemblages and ocean carbonate saturation at Caravaca, Spain V. Gilabert et al. 10.1016/j.cretres.2021.104844
- Calcareous dinoflagellate cyst distribution across the K/Pg boundary at DSDP site 577, Shatsky Rise, western North Pacific Ocean S. McLachlan & V. Pospelova 10.1016/j.marmicro.2021.102057
- Cretaceous large igneous provinces: from volcanic formation to environmental catastrophes and biological crises L. Percival et al. 10.1144/SP544-2023-88
- A high-resolution record of environmental changes from a Cretaceous-Paleogene section of Seymour Island, Antarctica R. Scasso et al. 10.1016/j.palaeo.2020.109844
- Global Mean and Relative Sea-Level Changes Over the Past 66 Myr: Implications for Early Eocene Ice Sheets K. Miller et al. 10.3389/esss.2023.10091
- Dinoflagellate cyst-based paleoenvironmental reconstructions and phytoplankton paleoecology across the Cretaceous–Paleogene (K/Pg) boundary interval, Vancouver Island, British Columbia, Canada S. McLachlan & V. Pospelova 10.1016/j.cretres.2021.104878
- Distribution of Dinoflagellate cyst assemblages and palynofacies in the Upper Cretaceous deposits from the neritic Bou Lila section, External Rif (northwestern Morocco): Implications for the age, biostratigraphic correlations and paleoenviromental reconstructions H. Slimani et al. 10.1016/j.marmicro.2020.101951
Latest update: 12 Oct 2024
Short summary
Our micropaleontological analyses on three cores from New Jersey (USA) show that the late Maastrichtian warming event (66.4–66.1 Ma), characterized by a ~ 4.0 °C warming of sea waters on the New Jersey paleoshelf, resulted in a disruption of phytoplankton communities and a stressed benthic ecosystem. This increased ecosystem stress during the latest Maastrichtian potentially primed global ecosystems for the subsequent mass extinction following the Cretaceous–Paleogene boundary impact.
Our micropaleontological analyses on three cores from New Jersey (USA) show that the late...
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