Articles | Volume 17, issue 5
https://doi.org/10.5194/cp-17-2091-2021
© Author(s) 2021. 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-17-2091-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
15 Oct 2021
Research article |
| 15 Oct 2021
| 15 Oct 2021
Climate, cryosphere and carbon cycle controls on Southeast Atlantic orbital-scale carbonate deposition since the Oligocene (30–0 Ma)
Anna Joy Drury
CORRESPONDING AUTHOR
MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, 28359 Bremen, Germany
Department of Earth Sciences, University College London, Gower Street, London, WC1E 6BT, UK
Diederik Liebrand
MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, 28359 Bremen, Germany
Thomas Westerhold
MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, 28359 Bremen, Germany
Helen M. Beddow
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Utrecht, the Netherlands
David A. Hodell
Department of Earth Science, University of Cambridge, Cambridge, EH9 3FE, UK
Nina Rohlfs
MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, 28359 Bremen, Germany
Roy H. Wilkens
School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, Hawaii 96822, USA
Mitchell Lyle
College of Earth, Ocean, and Atmospheric Science, Oregon State
University, Corvallis, Oregon 97331, USA
David B. Bell
School of GeoSciences, University of Edinburgh, Edinburgh, CB2 3EQ, UK
Dick Kroon
School of GeoSciences, University of Edinburgh, Edinburgh, CB2 3EQ, UK
Heiko Pälike
MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, 28359 Bremen, Germany
Lucas J. Lourens
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Utrecht, the Netherlands
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- A Global Reassessment of the Spatial and Temporal Expression of the Late Miocene Biogenic Bloom Q. Pillot et al. 10.1029/2022PA004564
- 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
- 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
- Abrupt conclusion of the late Miocene-early Pliocene biogenic bloom at 4.6-4.4 Ma B. Karatsolis et al. 10.1038/s41467-021-27784-6
17 citations as recorded by crossref.
- Late Miocene Onset of Tasman Leakage and Southern Hemisphere Supergyre Ushers in Near‐Modern Circulation B. Christensen et al. 10.1029/2021GL095036
- Drivers of Late Miocene Tropical Sea Surface Cooling: A New Perspective From the Equatorial Indian Ocean C. Martinot et al. 10.1029/2021PA004407
- Recognizing the Role of Tropical Seaways in Modulating the Pacific Circulation N. Tan et al. 10.1029/2022GL099674
- Secular and orbital-scale variability of equatorial Indian Ocean summer monsoon winds during the late Miocene C. Bolton et al. 10.5194/cp-18-713-2022
- Early Miocene Intensification of the North African Hydrological Cycle: Multi‐Proxy Evidence From the Shelf Carbonates of Malta R. Zammit et al. 10.1029/2022PA004414
- Atmospheric CO2 Estimates for the Late Oligocene and Early Miocene Using Multi‐Species Cross‐Calibrations of Boron Isotopes L. Anderson et al. 10.1029/2022PA004569
- Hydroclimate dynamics during the Plio-Pleistocene transition in the northwest Pacific realm R. Vaucher et al. 10.1016/j.gloplacha.2023.104088
- Accelerated marine carbon cycling forced by tectonic degassing over the Miocene Climate Optimum F. Liu et al. 10.1016/j.scib.2023.12.052
- Facies character and skeletal composition of heterozoan carbonates in a high-energy confined embayment (Miocene, Finale Ligure Limestone, NW Italy) G. Della Porta et al. 10.1016/j.sedgeo.2022.106209
- Late Miocene to Early Pliocene benthic foraminifera from the Tasman Sea (International Ocean Discovery Program Site U1506) M. Gastaldello et al. 10.5194/jm-43-1-2024
- Orbitally‐driven Palaeogene to Neogene deposition in the western South Atlantic (Espírito Santo Basin) and its correlation with global sea level T. Santos et al. 10.1111/sed.13104
- A benthic foraminifera perspective of the Late Miocene-Early Pliocene Biogenic Bloom at ODP Site 1085 (Southeast Atlantic Ocean) M. Gastaldello et al. 10.1016/j.palaeo.2024.112040
- Abrupt climate changes and the astronomical theory: are they related? D. Rousseau et al. 10.5194/cp-18-249-2022
- Nature and origin of variations in pelagic carbonate production in the tropical ocean since the mid-Miocene (ODP Site 927) P. Cornuault et al. 10.5194/bg-20-597-2023
- High-precision U-Pb geochronology for the Miocene Climate Optimum and a novel approach for calibrating age models in deep-sea sediment cores J. Kasbohm et al. 10.1130/G52255.1
- The Late Miocene‐Early Pliocene Biogenic Bloom: An Integrated Study in the Tasman Sea M. Gastaldello et al. 10.1029/2022PA004565
- A Global Reassessment of the Spatial and Temporal Expression of the Late Miocene Biogenic Bloom Q. Pillot et al. 10.1029/2022PA004564
3 citations as recorded by crossref.
- 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
- 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
- Abrupt conclusion of the late Miocene-early Pliocene biogenic bloom at 4.6-4.4 Ma B. Karatsolis et al. 10.1038/s41467-021-27784-6
Latest update: 13 Dec 2024
Short summary
We use the first high-resolution southeast Atlantic carbonate record to see how climate dynamics evolved since 30 million years ago (Ma). During ~ 30–13 Ma, eccentricity (orbital circularity) paced carbonate deposition. After the mid-Miocene Climate Transition (~ 14 Ma), precession (Earth's tilt direction) increasingly drove carbonate variability. In the latest Miocene (~ 8 Ma), obliquity (Earth's tilt) pacing appeared, signalling increasing high-latitude influence.
We use the first high-resolution southeast Atlantic carbonate record to see how climate dynamics...
