Articles | Volume 34, issue 1/2
https://doi.org/10.5194/sd-34-29-2025
https://doi.org/10.5194/sd-34-29-2025
Science report
 | 
03 Nov 2025
Science report |  | 03 Nov 2025

The RISeR cores: unexpected and extensive Middle Pleistocene terrestrial stratigraphy in the southern North Sea

Amy M. McGuire, Víctor Cartelle, Graham Rush, Freek S. Busschers, Kim M. Cohen, David M. Hodgson, and Natasha L. M. Barlow

Related authors

Constraining the timing and processes of pediment formation and dissection: implications for long-term evolution in the Western Cape, South Africa
Janet C. Richardson, Veerle Vanacker, David M. Hodgson, Marcus Christl, and Andreas Lang
Earth Surf. Dynam., 13, 315–339, https://doi.org/10.5194/esurf-13-315-2025,https://doi.org/10.5194/esurf-13-315-2025, 2025
Short summary
HOLSEA-NL: a Holocene water level and sea level indicator dataset for the Netherlands
Kim de Wit, Kim M. Cohen, and Roderik S. W. van de Wal
Earth Syst. Sci. Data, 17, 545–577, https://doi.org/10.5194/essd-17-545-2025,https://doi.org/10.5194/essd-17-545-2025, 2025
Short summary
Quantifying the uncertainty in the Eurasian ice-sheet geometry at the Penultimate Glacial Maximum (Marine Isotope Stage 6)
Oliver G. Pollard, Natasha L. M. Barlow, Lauren J. Gregoire, Natalya Gomez, Víctor Cartelle, Jeremy C. Ely, and Lachlan C. Astfalck
The Cryosphere, 17, 4751–4777, https://doi.org/10.5194/tc-17-4751-2023,https://doi.org/10.5194/tc-17-4751-2023, 2023
Short summary
Missing sea level rise in southeastern Greenland during and since the Little Ice Age
Sarah A. Woodroffe, Leanne M. Wake, Kristian K. Kjeldsen, Natasha L. M. Barlow, Antony J. Long, and Kurt H. Kjær
Clim. Past, 19, 1585–1606, https://doi.org/10.5194/cp-19-1585-2023,https://doi.org/10.5194/cp-19-1585-2023, 2023
Short summary
Last Interglacial sea-level data points from Northwest Europe
Kim M. Cohen, Víctor Cartelle, Robert Barnett, Freek S. Busschers, and Natasha L. M. Barlow
Earth Syst. Sci. Data, 14, 2895–2937, https://doi.org/10.5194/essd-14-2895-2022,https://doi.org/10.5194/essd-14-2895-2022, 2022
Short summary

Cited articles

Beets, D. J., Meijer, T., Beets, C. J., Cleveringa, P., Laban, C., and van der Spek, A. J.: Evidence for a Middle Pleistocene Glaciation of MIS 8 Age in the Southern North Sea, Quaternary International, 133–134, 7–19, https://doi.org/10.1016/j.quaint.2004.10.002, 2005. a
Bradley, S. L., Ely, J. C., Clark, C. D., Edwards, R. J., and Shennan, I.: Reconstruction of the Palaeo-Sea Level of Britain and Ireland Arising from Empirical Constraints of Ice Extent: Implications for Regional Sea Level Forecasts and North American Ice Sheet Volume, Journal of Quaternary Science, 38, 791–805, https://doi.org/10.1002/jqs.3523, 2023. a
Busschers, F., Kasse, C., Van Balen, R., Vandenberghe, J., Cohen, K., Weerts, H., Wallinga, J., Johns, C., Cleveringa, P., and Bunnik, F.: Late Pleistocene Evolution of the Rhine-Meuse System in the Southern North Sea Basin: Imprints of Climate Change, Sea-Level Oscillation and Glacio-Isostacy, Quaternary Science Reviews, 26, 3216–3248, https://doi.org/10.1016/j.quascirev.2007.07.013, 2007. a, b, c
Busschers, F. S., Van Balen, R. T., Cohen, K. M., Kasse, C., Weerts, H. J. T., Wallinga, J., and Bunnik, F. P. M.: Response of the Rhine–Meuse Fluvial System to Saalian Ice-sheet Dynamics, Boreas, 37, 377–398, https://doi.org/10.1111/j.1502-3885.2008.00025.x, 2008. a, b
Busschers, F. S., Cohen, K. M., Wesselingh, F., Schokker, J., Bakker, M. A. J., Van Balen, R., and Van Heteren, S.: Quaternary, in: Geology of the Netherlands, edited by: ten Veen, J., Vis, G.-J., and de Jager, Janand Wong, T., Amsterdam University Press, ISBN 978-94-6372-836-2, 2025. a, b
Download
Short summary
We present five new sediment cores, the Rates of Interglacial Sea-level Change and Responses (RISeR) cores, extracted from the southern North Sea. The cores will allow us to study the evolution of the basin in the Quaternary (the last 2.58 million years). The cores reveal widespread soil, wetland, and river deposits, reflecting a lost, predominantly terrestrial, landscape that now sits around 20 m below sea level. Understanding these landscapes is vital, as they form the foundations for a rapidly growing offshore wind industry.
Share