Articles | Volume 14, issue 3
https://doi.org/10.5194/cp-14-321-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-14-321-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Reinforcing the North Atlantic backbone: revision and extension of the composite splice at ODP Site 982
MARUM – Center for Marine Environmental Sciences, University of
Bremen, Bremen, Germany
Thomas Westerhold
MARUM – Center for Marine Environmental Sciences, University of
Bremen, Bremen, Germany
David Hodell
Department of Earth Sciences, University
of Cambridge, Cambridge CB2 3EQ, UK
Ursula Röhl
MARUM – Center for Marine Environmental Sciences, University of
Bremen, Bremen, Germany
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- Drivers of Late Miocene Tropical Sea Surface Cooling: A New Perspective From the Equatorial Indian Ocean C. Martinot et al. 10.1029/2021PA004407
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17 citations as recorded by crossref.
- Latest Miocene restriction of the Mediterranean Outflow Water: a perspective from the Gulf of Cádiz Z. Ng et al. 10.1007/s00367-021-00693-9
- Mediterranean water in the Atlantic Iberian margin reveals early isolation events during the Messinian Salinity Crisis F. Bulian et al. 10.1016/j.gloplacha.2023.104297
- An astronomically dated record of Earth’s climate and its predictability over the last 66 million years T. Westerhold et al. 10.1126/science.aba6853
- The Messinian of Agios Myron (Crete, Greece): A key to better understanding of diatomite formation on Gavdos (south of Crete) W. Zachariasse et al. 10.1016/j.palaeo.2021.110633
- The Miocene: The Future of the Past M. Steinthorsdottir et al. 10.1029/2020PA004037
- Coupled otolith and foraminifera oxygen and carbon stable isotopes evidence paleoceanographic changes and fish metabolic responses K. Agiadi et al. 10.5194/bg-21-3869-2024
- Impact of the Mediterranean-Atlantic connectivity and the late Miocene carbon shift on deep-sea communities in the Western Alboran Basin F. Bulian et al. 10.1016/j.palaeo.2022.110841
- Neogene Mass Accumulation Rate of Carbonate Sediment Across Northern Zealandia, Tasman Sea, Southwest Pacific R. Sutherland et al. 10.1029/2021PA004294
- Climate, cryosphere and carbon cycle controls on Southeast Atlantic orbital-scale carbonate deposition since the Oligocene (30–0 Ma) A. Drury et al. 10.5194/cp-17-2091-2021
- Downhole logging data for time series analysis and cyclostratigraphy C. Zeeden et al. 10.1016/j.earscirev.2023.104436
- Freshening of the Mediterranean Salt Giant: controversies and certainties around the terminal (Upper Gypsum and Lago-Mare) phases of the Messinian Salinity Crisis F. Andreetto et al. 10.1016/j.earscirev.2021.103577
- Drivers of Late Miocene Tropical Sea Surface Cooling: A New Perspective From the Equatorial Indian Ocean C. Martinot et al. 10.1029/2021PA004407
- The Early to Middle Eocene Transition: An Integrated Calcareous Nannofossil and Stable Isotope Record From the Northwest Atlantic Ocean (Integrated Ocean Drilling Program Site U1410) C. Cappelli et al. 10.1029/2019PA003686
- Variability of the Indian Monsoon in the Andaman Sea Across the Miocene‐Pliocene Transition J. Jöhnck et al. 10.1029/2020PA003923
- Reflooding and repopulation of the Mediterranean Sea after the Messinian Salinity Crisis: Benthic foraminifera assemblages and stable isotopes of Spanish basins F. Bulian et al. 10.1016/j.marmicro.2022.102160
- High-latitude biomes and rock weathering mediate climate–carbon cycle feedbacks on eccentricity timescales D. De Vleeschouwer et al. 10.1038/s41467-020-18733-w
- The Late Miocene‐Early Pliocene Biogenic Bloom: An Integrated Study in the Tasman Sea M. Gastaldello et al. 10.1029/2022PA004565
1 citations as recorded by crossref.
Latest update: 19 Nov 2024
Short summary
North Atlantic Site 982 is key to our understanding of climate evolution over the past 12 million years. However, the stratigraphy and age model are unverified. We verify the composite splice using XRF core scanning data and establish a revised benthic foraminiferal stable isotope astrochronology from 8.0–4.5 million years ago. Our new stratigraphy accurately correlates the Atlantic and the Mediterranean and suggests a connection between late Miocene cooling and dynamic ice sheet expansion.
North Atlantic Site 982 is key to our understanding of climate evolution over the past 12...