Articles | Volume 14, issue 7
https://doi.org/10.5194/cp-14-991-2018
© 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-14-991-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
10 Jul 2018
Research article |
| 10 Jul 2018
| 10 Jul 2018
Paleoceanography and ice sheet variability offshore Wilkes Land, Antarctica – Part 1: Insights from late Oligocene astronomically paced contourite sedimentation
Ariadna Salabarnada
CORRESPONDING AUTHOR
Instituto Andaluz de Ciencias de la Tierra, CSIC-Univ. de Granada, Armilla, 18100, Spain
Invited contribution by Ariadna Salabarnada, recipient of the EGU Climate: Past, Present & Future Outstanding Student Poster and PICO Award 2016.
Carlota Escutia
Instituto Andaluz de Ciencias de la Tierra, CSIC-Univ. de Granada, Armilla, 18100, Spain
Ursula Röhl
MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, 28359 Bremen, Germany
C. Hans Nelson
Instituto Andaluz de Ciencias de la Tierra, CSIC-Univ. de Granada, Armilla, 18100, Spain
Robert McKay
Antarctic Research Centre, Victoria University of Wellington, Wellington, 6140, New Zealand
Francisco J. Jiménez-Espejo
Department of Biogeochemistry, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Kanagawa, 237-0061, Japan
Peter K. Bijl
Department of Earth Sciences, Marine Palynology and Palaeoceanography, Faculty of Geosciences, Laboratory of Palaeobotany and Palynology, Utrecht University, Princetonlaan 8a, 3584 CB Utrecht, the Netherlands
Julian D. Hartman
Department of Earth Sciences, Marine Palynology and Palaeoceanography, Faculty of Geosciences, Laboratory of Palaeobotany and Palynology, Utrecht University, Princetonlaan 8a, 3584 CB Utrecht, the Netherlands
Stephanie L. Strother
Department of Geography and Environmental Sciences, Faculty of Engineering and Environment, Northumbria University, Newcastle upon Tyne, NE1 8ST, UK
Ulrich Salzmann
Department of Geography and Environmental Sciences, Faculty of Engineering and Environment, Northumbria University, Newcastle upon Tyne, NE1 8ST, UK
Dimitris Evangelinos
Instituto Andaluz de Ciencias de la Tierra, CSIC-Univ. de Granada, Armilla, 18100, Spain
Adrián López-Quirós
Instituto Andaluz de Ciencias de la Tierra, CSIC-Univ. de Granada, Armilla, 18100, Spain
José Abel Flores
Department of Geology, University of Salamanca, Salamanca, 37008, Spain
Francesca Sangiorgi
Department of Earth Sciences, Marine Palynology and Palaeoceanography, Faculty of Geosciences, Laboratory of Palaeobotany and Palynology, Utrecht University, Princetonlaan 8a, 3584 CB Utrecht, the Netherlands
Minoru Ikehara
Center for Advanced Marine Core research, Kochi University, Nankoku, Kochi, 783-8502, Japan
Henk Brinkhuis
Department of Earth Sciences, Marine Palynology and Palaeoceanography, Faculty of Geosciences, Laboratory of Palaeobotany and Palynology, Utrecht University, Princetonlaan 8a, 3584 CB Utrecht, the Netherlands
NIOZ, Royal Netherlands Institute for Sea Research, and Utrecht University, Landsdiep 4, 1797SZ 't Horntje, Texel, the Netherlands
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Cited
32 citations as recorded by crossref.
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32 citations as recorded by crossref.
- Paleoceanography and ice sheet variability offshore Wilkes Land, Antarctica – Part 2: Insights from Oligocene–Miocene dinoflagellate cyst assemblages P. Bijl et al. 10.5194/cp-14-1015-2018
- Geomorphology of Ona Basin, southwestern Scotia Sea (Antarctica): Decoding the spatial variability of bottom-current pathways A. López-Quirós et al. 10.1016/j.margeo.2020.106113
- Millimetre-scale biomarker heterogeneity in lacustrine shale identifies the nature of signal-averaging and demonstrates anaerobic respiration control on organic matter preservation and dolomitization H. Xu et al. 10.1016/j.gca.2023.03.008
- Large obliquity-paced Antarctic ice-volume fluctuations suggest melting by atmospheric and ocean warming during late Oligocene S. Brzelinski et al. 10.1038/s43247-023-00864-9
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- Methane hydrate dissociation across the Oligocene–Miocene boundary B. Kim & Y. Zhang 10.1038/s41561-022-00895-5
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- Subduction initiation in the Scotia Sea region and opening of the Drake Passage: When and why? S. van de Lagemaat et al. 10.1016/j.earscirev.2021.103551
- A review of Antarctic ice sheet fluctuations records during Cenozoic and its cause and effect relation with the climatic conditions M. Pandey et al. 10.1016/j.polar.2021.100720
- Absence of a strong, deep-reaching Antarctic Circumpolar Current zonal flow across the Tasmanian gateway during the Oligocene to early Miocene D. Evangelinos et al. 10.1016/j.gloplacha.2021.103718
- Oligocene paleoceanographic changes based on an interbasinal comparison of Cibicidoides spp. δ18O records and a new compilation of data H. Lee & K. Jo 10.1016/j.palaeo.2018.09.016
- Integrated stratigraphy and paleontology of the lower Miocene Monte León Formation, southeastern Patagonia, Argentina: Unraveling paleoenvironmental changes and factors controlling sedimentation A. Parras et al. 10.1016/j.palaeo.2020.109701
- Late Pliocene to recent depositional processes on the Sabrina Coast (East Antarctica): the diatom contribution R. Tolotti et al. 10.5194/jm-43-349-2024
- Late Oligocene-Miocene proto-Antarctic Circumpolar Current dynamics off the Wilkes Land margin, East Antarctica D. Evangelinos et al. 10.1016/j.gloplacha.2020.103221
- Opposite response modes of NADW dynamics to obliquity forcing during the late Paleogene H. Lee et al. 10.1038/s41598-020-70020-2
- Strength and variability of the Oligocene Southern Ocean surface temperature gradient F. Hoem et al. 10.1038/s43247-022-00666-5
- Deep water inflow slowed offshore expansion of the West Antarctic Ice Sheet at the Eocene-Oligocene transition G. Uenzelmann-Neben et al. 10.1038/s43247-022-00369-x
- Palynofacies as sea-level-sensitive proxy in Early Cretaceous marine mudstones – A critical evaluation H. Thöle et al. 10.1016/j.coal.2024.104645
- The influence of Totten Glacier on the Late Cenozoic sedimentary record F. Donda et al. 10.1017/S0954102020000188
- Late Quaternary high-resolution seismic stratigraphy and core-based paleoenvironmental reconstructions in Ona Basin, southwestern Scotia Sea (Antarctica) A. López-Quirós et al. 10.1016/j.margeo.2021.106565
- Late Eocene–early Miocene evolution of the southern Australian subtropical front: a marine palynological approach F. Hoem et al. 10.5194/jm-40-175-2021
- Late Miocene‐Pliocene Vigorous Deep‐Sea Circulation in the Southeast Indian Ocean: Paleoceanographic and Tectonic Implications G. Tagliaro et al. 10.1029/2021PA004303
- Late Miocene onset of the modern Antarctic Circumpolar Current D. Evangelinos et al. 10.1038/s41561-023-01356-3
- Retreat patterns and dynamics of the former Norske Trough ice stream (NE Greenland): An integrated geomorphological and sedimentological approach A. López-Quirós et al. 10.1016/j.quascirev.2023.108477
- Climatic and tectonic drivers of late Oligocene Antarctic ice volume B. Duncan et al. 10.1038/s41561-022-01025-x
- Evolution of Sea Surface Temperature in the Southern Mid‐latitudes From Late Oligocene Through Early Miocene J. Guitián & H. Stoll 10.1029/2020PA004199
- Paleoceanography and ice sheet variability offshore Wilkes Land, Antarctica – Part 3: Insights from Oligocene–Miocene TEX<sub>86</sub>-based sea surface temperature reconstructions J. Hartman et al. 10.5194/cp-14-1275-2018
- Sedimentary model for mixed depositional systems along the Pacific margin of the Antarctic Peninsula: Decoding the interplay of deep-water processes S. Rodrigues et al. 10.1016/j.margeo.2022.106754
- Using high‐resolution XRF analyses as a sequence stratigraphic tool in a mudstone‐dominated succession (Early Cretaceous, Lower Saxony Basin, Northern Germany) H. Thöle et al. 10.1002/dep2.83
- Late Cenozoic sea-surface-temperature evolution of the South Atlantic Ocean F. Hoem et al. 10.5194/cp-19-1931-2023
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Short summary
Here we reconstruct ice sheet and paleoceanographic configurations in the East Antarctic Wilkes Land margin based on a multi-proxy study conducted in late Oligocene (26–25 Ma) sediments from IODP Site U1356. The new obliquity-forced glacial–interglacial sedimentary model shows that, under the high CO2 values of the late Oligocene, ice sheets had mostly retreated to their terrestrial margins and the ocean was very dynamic with shifting positions of the polar fronts and associated water masses.
Here we reconstruct ice sheet and paleoceanographic configurations in the East Antarctic Wilkes...
