Articles | Volume 14, issue 3
https://doi.org/10.5194/cp-14-397-2018
© 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-14-397-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Land–sea coupling of early Pleistocene glacial cycles in the southern North Sea exhibit dominant Northern Hemisphere forcing
Timme H. Donders
CORRESPONDING AUTHOR
Department of Physical Geography, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CD, Utrecht, the Netherlands
TNO – Applied Geosciences, Netherlands Organisation of Applied
Scientific Research Princetonlaan 6, 3584 CB, Utrecht, the Netherlands
Niels A. G. M. van Helmond
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CS, Utrecht, the Netherlands
Roel Verreussel
TNO – Applied Geosciences, Netherlands Organisation of Applied
Scientific Research Princetonlaan 6, 3584 CB, Utrecht, the Netherlands
Dirk Munsterman
TNO – Geological Survey of the Netherlands, Netherlands Organisation
of Applied Scientific Research, Princetonlaan 6, 3584 CB, Utrecht, the
Netherlands
Johan ten Veen
TNO – Geological Survey of the Netherlands, Netherlands Organisation
of Applied Scientific Research, Princetonlaan 6, 3584 CB, Utrecht, the
Netherlands
Robert P. Speijer
Department of Earth and Environmental Sciences, KU Leuven, 3001
Heverlee, Belgium
Johan W. H. Weijers
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CS, Utrecht, the Netherlands
now at: Shell Global Solutions International B.V., Grasweg 31, 1031
HW, Amsterdam, the Netherlands
Francesca Sangiorgi
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CS, Utrecht, the Netherlands
Francien Peterse
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CS, Utrecht, the Netherlands
Gert-Jan Reichart
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CS, Utrecht, the Netherlands
NIOZ Royal Netherlands Institute for Sea Research, 1790
AB, Den Burg, Texel, the Netherlands
Jaap S. Sinninghe Damsté
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CS, Utrecht, the Netherlands
NIOZ Royal Netherlands Institute for Sea Research, 1790
AB, Den Burg, Texel, the Netherlands
Lucas Lourens
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CS, Utrecht, the Netherlands
Gesa Kuhlmann
BGR – Federal Institute for Geosciences and Natural Resources,
Geozentrum Hannover, Stilleweg 2, 30655 Hanover, Germany
Henk Brinkhuis
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Heidelberglaan 2, 3584 CS, Utrecht, the Netherlands
NIOZ Royal Netherlands Institute for Sea Research, 1790
AB, Den Burg, Texel, the Netherlands
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- Late Pliocene to early Pleistocene climate dynamics in western North America based on a new pollen record from paleo-Lake Idaho F. Allstädt et al. 10.1007/s12549-020-00460-1
16 citations as recorded by crossref.
- New insights on subsurface energy resources in the Southern North Sea Basin area J. Doornenbal et al. 10.1144/SP494-2018-178
- First high-resolution multi-proxy palaeoenvironmental record of the Late Glacial to Early Holocene transition in the Ría de Arousa (Atlantic margin of NW Iberia) I. García-Moreiras et al. 10.1016/j.quascirev.2019.05.016
- Sediment recycling during the Holocene marine transgression in Ría de Vigo (NW Iberia): multiproxy evidence and environmental implications C. Muñoz Sobrino et al. 10.1016/j.quascirev.2024.109006
- Dinoflagellate fossils: Geological and biological applications A. Penaud et al. 10.1016/j.revmic.2018.09.003
- Early Pleistocene Tiglian sites in the Netherlands: A revised view on the significance for quaternary stratigraphy W. Westerhoff et al. 10.1016/j.quascirev.2020.106417
- Extensive marine-terminating ice sheets in Europe from 2.5 million years ago B. Rea et al. 10.1126/sciadv.aar8327
- Vegetation succession and climate change across the Plio-Pleistocene transition in eastern Azerbaijan, central Eurasia (2.77–2.45 Ma) T. Hoyle et al. 10.1016/j.palaeo.2019.109386
- Generation, migration, entrapment and leakage of microbial gas in the Dutch part of the Southern North Sea Delta J. Verweij et al. 10.1016/j.marpetgeo.2018.07.034
- The dispersal of fluvially discharged and marine, shelf-produced particulate organic matter in the northern Gulf of Mexico Y. Yedema et al. 10.5194/bg-20-663-2023
- Climate and vegetation changes in coastal ecosystems during the Middle Pleniglacial and the early Holocene: Two multi-proxy, high-resolution records from Ría de Vigo (NW Iberia) I. García-Moreiras et al. 10.1016/j.gloplacha.2019.02.015
- A new age model for the Pliocene of the southern North Sea basin: a multi-proxy climate reconstruction E. Dearing Crampton-Flood et al. 10.5194/cp-16-523-2020
- New Jersey's paleoflora and eastern North American climate through Paleogene–Neogene warm phases S. Prader et al. 10.1016/j.revpalbo.2020.104224
- The palaeontology and dating of the ‘Weybourne Crag’, an important marker horizon in the Early Pleistocene of the southern North Sea basin R. Preece et al. 10.1016/j.quascirev.2020.106177
- Dinoflagellate cyst and pollen assemblages as tracers for marine productivity and river input in the northern Gulf of Mexico Y. Yedema et al. 10.5194/jm-42-257-2023
- Small population of the largest water strider after the late Pleistocene and the implications for its conservation X. Sun et al. 10.1016/j.gene.2023.147219
- Late Pliocene to early Pleistocene climate dynamics in western North America based on a new pollen record from paleo-Lake Idaho F. Allstädt et al. 10.1007/s12549-020-00460-1
Latest update: 20 Nov 2024
Short summary
The buildup and melting of ice during the early glaciations in the Northern Hemisphere, around 2.5 million years ago, were far shorter in duration than during the last million years. Based on molecular compounds and microfossils from sediments dating back to the early glaciations we show that the temperature on land and in the sea changed simultaneously and was a major factor in the ice buildup in the Northern Hemisphere. These data provide key insights into the dynamics of early glaciations.
The buildup and melting of ice during the early glaciations in the Northern Hemisphere, around...