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Evidence for bias in C/N, δ13C, δ15N values of bulk organic matter, and on environmental interpretation, from a lake sedimentary sequence by pre-analysis acid treatment methods. (2011)
Journal Article
Brodie, C., Casford, J., Lloyd, J., Leng, M., Heaton, T., Kendrick, C., & Zong, Y. (2011). Evidence for bias in C/N, δ13C, δ15N values of bulk organic matter, and on environmental interpretation, from a lake sedimentary sequence by pre-analysis acid treatment methods. Quaternary Science Reviews, 30(21-22), 3076-3087. https://doi.org/10.1016/j.quascirev.2011.07.003

Seismic stratigraphy records the deglacial history of Jakobshavn Isbrae, West Greenland (2011)
Journal Article
Hogan, K., Dix, J., Lloyd, J., Long, A., & Cotterill, C. (2011). Seismic stratigraphy records the deglacial history of Jakobshavn Isbrae, West Greenland. Journal of Quaternary Science, 26(7), 757-766. https://doi.org/10.1002/jqs.1500

Jakobshavn Isbræ is one of the largest ice streams in the Greenland Ice Sheet, presently draining c. 6.5% of the Inland Ice. Here we present high-resolution Chirp and Sparker sub-bottom profiles from a seismic survey conducted just outside of the Jak... Read More about Seismic stratigraphy records the deglacial history of Jakobshavn Isbrae, West Greenland.

A 100 year record of ocean temperature control on the stability of Jakobshavn Isbrae, West Greenland (2011)
Journal Article
Lloyd, J., Moros, M., Perner, K., Telford, R., Kuijpers, A., Jansen, E., & McCarthy, D. (2011). A 100 year record of ocean temperature control on the stability of Jakobshavn Isbrae, West Greenland. Geology, 39(9), 867-870. https://doi.org/10.1130/g32076.1

An understanding of the interaction between ice sheet dynamics and forcing mechanisms, such as oceanic and atmospheric circulation, is important because of the potential contribution of these processes to constraining models that seek to predict futu... Read More about A 100 year record of ocean temperature control on the stability of Jakobshavn Isbrae, West Greenland.

Centennial scale benthic foraminiferal record of late Holocene oceanographic variability in Disko Bugt, West Greenland (2011)
Journal Article
Perner, K., Moros, M., Lloyd, J., Kuijpers, A., Telford, R., & Harff, J. (2011). Centennial scale benthic foraminiferal record of late Holocene oceanographic variability in Disko Bugt, West Greenland. Quaternary Science Reviews, 30(19-20), 2815-2826. https://doi.org/10.1016/j.quascirev.2011.06.018

A new centennial scale benthic foraminiferal record of late Holocene climate variability and oceanographic changes off West Greenland (Disko Bugt) highlights substantial subsurface water mass changes (e.g. temperature and salinity) of the West Greenl... Read More about Centennial scale benthic foraminiferal record of late Holocene oceanographic variability in Disko Bugt, West Greenland.

Evidence for bias in C and N concentrations and δ13C composition of terrestrial and aquatic organic materials due to pre-analysis acid preparation methods (2011)
Journal Article
Brodie, C., Leng, M., Casford, J., Kendrick, C., Lloyd, J., Zong, Y., & Bird, M. (2011). Evidence for bias in C and N concentrations and δ13C composition of terrestrial and aquatic organic materials due to pre-analysis acid preparation methods. Chemical Geology, 282(3-4), 67-83. https://doi.org/10.1016/j.chemgeo.2011.01.007

Interaction between subsurface ocean waters and calving of Jakobshavn Isbræ during the Late Holocene (2011)
Journal Article
Andresen, C., McCarthy, D., Dylmer, C., Seidenkrantz, M., Kuijpers, A., & Lloyd, J. (2011). Interaction between subsurface ocean waters and calving of Jakobshavn Isbræ during the Late Holocene. Holocene, 21(2), 211-224. https://doi.org/10.1177/0959683610378877

A marine sediment core from Vaigat in Disko Bugt, West Greenland, has been analysed in terms of lithology, dinoflagellate cysts and foraminifera in order to evaluate the influence of oceanographic variability on West Greenland glacier stability. The... Read More about Interaction between subsurface ocean waters and calving of Jakobshavn Isbræ during the Late Holocene.