Articles | Volume 13, issue 9
https://doi.org/10.5194/cp-13-1153-2017
© 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-13-1153-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Highly variable Pliocene sea surface conditions in the Norwegian Sea
Uni Research Climate, Bjerknes Centre for Climate Research, Jahnebakken 5, 5007 Bergen, Norway
Bjørg Risebrobakken
Uni Research Climate, Bjerknes Centre for Climate Research, Jahnebakken 5, 5007 Bergen, Norway
Stijn De Schepper
Uni Research Climate, Bjerknes Centre for Climate Research, Jahnebakken 5, 5007 Bergen, Norway
Erin L. McClymont
Department of Geography, Durham University, Durham, DH1 3LE, UK
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- Limited exchange between the deep Pacific and Atlantic oceans during the warm mid-Pliocene and Marine Isotope Stage M2 “glaciation” A. Braaten et al. 10.5194/cp-19-2109-2023
- Did North Atlantic cooling and freshening from 3.65–3.5 Ma precondition Northern Hemisphere ice sheet growth? C. Karas et al. 10.1016/j.gloplacha.2019.103085
- Climate Evolution Through the Onset and Intensification of Northern Hemisphere Glaciation E. McClymont et al. 10.1029/2022RG000793
- Icebergs in the Nordic Seas Throughout the Late Pliocene Y. Smith et al. 10.1002/2017PA003240
- Sclerochronological evidence of pronounced seasonality from the late Pliocene of the southern North Sea basin and its implications A. Johnson et al. 10.5194/cp-18-1203-2022
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- Buoyancy forcing: a key driver of northern North Atlantic sea surface temperature variability across multiple timescales B. Risebrobakken et al. 10.5194/cp-19-1101-2023
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- Carbon export from mountain forests enhanced by earthquake-triggered landslides over millennia N. Frith et al. 10.1038/s41561-018-0216-3
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- Northern Hemisphere Glaciation: Its Tectonic Origin in the Neogene Uplift H. Ou 10.3390/glacies1010003
- Seasonal sea ice cover during the warm Pliocene: Evidence from the Iceland Sea (ODP Site 907) C. Clotten et al. 10.1016/j.epsl.2017.10.011
- The PhanSST global database of Phanerozoic sea surface temperature proxy data E. Judd et al. 10.1038/s41597-022-01826-0
- Controls of precipitation and vegetation variability on the NE Tibetan Plateau during the late Pliocene warmth (~3.5–3.0 Ma) F. Schwarz et al. 10.1016/j.gloplacha.2021.103707
- First monodontid cetacean (Odontoceti, Delphinoidea) from the early Pliocene of the north‐western Pacific Ocean H. Ichishima et al. 10.1002/spp2.1244
- Orbital, tectonic and oceanographic controls on Pliocene climate and atmospheric circulation in Arctic Norway S. Panitz et al. 10.1016/j.gloplacha.2017.12.022
- Group 2i Isochrysidales produce characteristic alkenones reflecting sea ice distribution K. Wang et al. 10.1038/s41467-020-20187-z
- Reduced Arctic sea ice extent during the mid-Pliocene Warm Period concurrent with increased Atlantic-climate regime W. Rahaman et al. 10.1016/j.epsl.2020.116535
- Tracking Holocene palaeostratification and productivity changes in the Western Irish Sea: A multi-proxy record M. Woods et al. 10.1016/j.palaeo.2019.06.004
2 citations as recorded by crossref.
Discussed (preprint)
Latest update: 08 Nov 2024
Short summary
We present a high-resolution multi-proxy study of the Norwegian Sea, covering the 5.33 to 3.14 Ma time window within the Pliocene. We show that large-scale climate transitions took place during this warmer than modern time, most likely in response to ocean gateway transformations. Strong warming at 4.0 Ma in the Norwegian Sea, when regions closer to Greenland cooled, indicate that increased northward ocean heat transport may be compatible with expanding glaciation and Arctic sea ice growth.
We present a high-resolution multi-proxy study of the Norwegian Sea, covering the 5.33 to...