Pleistocene Ice Sheets

Large and rapid climatic changes have taken place during the Quaternary associated with glacial and interglacial cycles. The extent and thickness of the major high latitude ice sheets acts as a primary control on estimates of sea level changes and positions of shorelines during the Quaternary and are also used as a palaeodataset against which current global climate models are tested.The evidence for these climatic changes primarily comes from Antarctic and Arctic ice cores, ocean sediments and the glacial record on land. To-date there has been relatively little investigation of the signature of these rapid climate change events within offshore sedimentary sequences utilising the now extensive oil industry seismic reflection and bore hole datasets that exist for many sedimentary basins.

A wealth of commercial 3D seismic reflection data covers the North Sea basin with almost 'wall-to-wall' carpet coverage from north to the south along the basin axis covering 53°-63°N. Using these data, in combination with BGS well data and legacy high resolution 2D seismic data, our work has shown how industrial 3D seismic data can be used in the field of marine Quaternary Geology leading to important discoveries about the glaciations in the North Sea area, and a significant revision of the Quaternary glacial history of central North Sea area.

Mega-scale glacial lineations

Fig.1a. Mega-scale glacial lineations, imaged at 80m beneath seabed, central North Sea, image width~10km. Figure 1b.  Morphology of buried tunnel valleys (central North Sea); blue-red contours =180m. Figure 1c. Cross cutting tunnel valleys in plan view at ~280m beneath sea bed. Image width ~18km.

We have made several significant discoveries. For example on  3D seismic reflection data we have observed several features, including mega-scale-scale glacial lineations (Figure 1 above), that document the presence of grounded Quaternary ice sheets on the seabed/landsurface over a 160 km wide area between 56°-60° N (Fig1). Through this work we have shown that the British-Irish and Scandinavian icesheets were confluent in the North Sea during the last major glaciation between 29–22 14C ka BP (Graham et al 2007). Were were very lucky to be able to use from material recovered from the first BGS borehole drilled in Quaternary sediments in the UK sector of the North Sea in over 10 years  to provide a new chronology (with radiocarbon dating) and interpretation of depositional environment for the most recent glacial events in the central North Sea (Graham et al. 2010).  This work was done as part of a collaborative British Geological Survey-Imperial College project.

Our analysis of buried tunnel valleys, features carved beneath the ice by sub-glacial meltwaters (Fig 2), has allowed us for the first time to directly document  with geomorphic evidence the expansion of NW European ice sheets covering NW Europe at least seven times since the middle Pleistocene, inline with that observed from oceanic and Greenland/Antarctic palaeoclimate proxies. These results constrain reconstructions of the extent and limits of NW European ice-sheets in the last 460 Kyr which will inform future models of ice-sheet extents prior to the Last Glacial Maximum, in response to climate forcing. The paper summarising these results published on North Sea tunnel valleys by Stewart & Lonergan in Geology (March 2011) is available for download here.

Figure 2. Cross-cutting tunnel valleys in the Central North Sea as imaged on 3D seismic data; From Stewart et al (2013).

We have also looked in detail at the Moray Firth area to investigate how an icestream within the British-Irish ice sheet decayed after the Last Glacial Maximum (since c.21,000 yrs). In the last 10-13 years there has been  significant research effort on understanding the dynamics of ice sheets  and particularly how they decay, with the of  aim of predicting how the Greenland and Antarctic ice sheets may behave in response to global warming. Numerical models  predict rapid and dynamic oscillations of the British Isles ice sheet margins; in this work we demonstrate such behavior for the Moray Firth ice stream and document the landsystem assemblage that formed during icestream advance and retreat (Graham et al. 2009).

image of seafloor bathymetryFigure 3. 3D image of seafloor bathymetry from 3D sesimic data illustrating crescentic push ridges on a moraine formed by the Moray Firth ice stream. From Graham et al. (2009).


For further information contact Lidia Lonergan
 Collaborators: Martyn Stoker (BGS); Jenny Collier and Gary Hampson

Completed Research Projects

  • Reconstructing Pleistocene ice limits in the Central North Sea: implications for climate change . Ali Graham PhD
  • Morphology and evolution of pleistocene subglacial tunnel valleys in the north sea. Margaret Stewart PhD


Stewart, M.A, Lonergan, L., Hampson, GJ. (2013) Pleistocene Tunnel Valleys in the UK Central North Sea: Regional Extents and Generations. Quaternary Science Reviews, 72; 1-17

Stewart, MA, Lonergan, L, Hampson, GJ. (2012) 3D Seismic Analysis of Buried Tunnel Valleys in the Central North Sea: Tunnel Valley Sedimentary Architecture. From: Huuse, M., Redfern, J., Le Heron, D. P., Dixon, R. J., Moscariello, A. & Craig, J. (eds) Glaciogenic Reservoirs and Hydrocarbon Systems. Geological Society, London, Special Publications, 368,

Graham AGC, Stoker MS, Lonergan L, Bradwell T, Stewart MA. (2011) Pleistocene Glaciations of the North Sea basin. In: Ehlers J, Gibbard P (Eds). Quaternary Glaciations: Extent and Chronology - "A closer look" (2nd edition). Elsevier, 261-278.

Stewart, M.A., Lonergan, L. (2011) Direct evidence for seven glacial cycles in the Middle-Late Pleistocene of NW Europe. Geology 39, 283-286.

 Graham, A., Lonergan L., Stoker M.S. (2010). Depositional environments and chronology of Late Weichselian glaciation and deglaciation in the central North Sea Boreas 39, 471-491.

Graham, A., Lonergan L., Stoker M.S. (2009). Seafloor glacial features reveal the extent, and decay of the last British Ice Sheet, east of Scotland; Journal of Quaternary Science 24,117-138.

Graham, A., Lonergan L., Stoker M.S., (2007). Evidence for Late Pleistocene ice stream activity in the Witch Ground Basin, central North Sea, from 3D seismic reflection data. Quaternary Science Reviews, 26, 627-643 doi:10.1016/j.quascirev.2006.11.004

Lonergan, L., Maidment, S. & Collier, J.S. (2006). Pleistocene tunnel valleys in the North Sea: 3D Morphology and Evolution. J of Quaternary Sci. 21, 891-903.  DOI: 10.1002/jqs.1015.

Stoker, M.S. Bradwell, T., Lonergan L. & Graham A. (2005) Scratching the Surface, Planet Earth Spring 2005, p.23 NERC publication.