A chronological framework for the British Quaternary based on Bithynia opercula

Penkman, K.E.H.; Preece, R.C.; Bridgland, D.R.; Keen, D.H.; Meijer, T.; Parfitt, S.A.; White, T.S.; Collins, M.J.

doi:10.1038/nature10305

All Outputs (3)

Geoconservation for science and society: challenges and opportunities. (2011)
Journal Article
Prosser, C., Bridgland, D., Brown, E., & Larwood, J. (2011). Geoconservation for science and society: challenges and opportunities. Proceedings of the Geologists' Association, 122(3), 337-342. https://doi.org/10.1016/j.pgeola.2011.01.007

Dynamic Devensian ice flow in NE England: a sedimentological reconstruction. (2011)
Journal Article
Davies, B., Roberts, D., Bridgland, D., & Ó Cofaigh, C. (2011). Dynamic Devensian ice flow in NE England: a sedimentological reconstruction. Boreas: An International Journal of Quaternary Research, 41, https://doi.org/10.1111/j.1502-3885.2011.00237.x

A chronological framework for the British Quaternary based on Bithynia opercula (2011)
Journal Article
Penkman, K., Preece, R., Bridgland, D., Keen, D., Meijer, T., Parfitt, S., …Collins, M. (2011). A chronological framework for the British Quaternary based on Bithynia opercula. Nature, 476(7361), 446-449. https://doi.org/10.1038/nature10305

Marine and ice-core records show that the Earth has experienced a succession of glacials and interglacials during the Quaternary (last ~2.6 million years), although it is often difficult to correlate fragmentary terrestrial records with specific cycl... Read More about A chronological framework for the British Quaternary based on Bithynia opercula.