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Number of items: 8.


Dickson, Alexander J.; Cohen, Anthony S. and Coe, Angela L. (2012). Seawater oxygenation during the Paleocene-Eocene Thermal Maximum. Geology, 40(7) pp. 639–642.

Dickson, Alexander J. and Cohen, Anthony S. (2012). A molybdenum isotope record of Eocene Thermal Maximum 2: implications for global ocean redox during the early Eocene. Paleoceanography, 27(3), article no. PA3230. file


Dickson, Alexander J.; Leng, Melanie J.; Maslin, Mark A. and Röhl, Ursula (2010). Oceanic, atmospheric and ice-sheet forcing of South East Atlantic Ocean productivity and South African monsoon intensity during MIS-12 to 10. Quaternary Science Reviews, 29(27-28) pp. 3936–3947. file

Dickson, Alexander J.; Leng, Melanie J.; Maslin, Mark A.; Sloane, Hilary J.; Green, Joanne; Bendle, James A.; McClymont, Erin L. and Pancost, Richard D. (2010). Atlantic overturning circulation and Agulhas leakage influences on southeast Atlantic upper ocean hydrography during marine isotope stage 11. Paleoceanography, 25 PA3208. file


Dickson, Alexander J.; Beer, Christopher J.; Dempsey, Ciara; Maslin, Mark A.; Bendle, James A.; McClymont, Erin L. and Pancost, Richard D. (2009). Oceanic forcing of the Marine Isotope Stage 11 interglacial. Nature Geoscience, 2(6) pp. 428–433. file


Dickson, Alexander J.; Austin, William E. N.; Hall, Ian R.; Maslin, Mark A. and Kucera, Michal (2008). Centennial-scale evolution of Dansgaard-Oeschger events in the northeast Atlantic Ocean between 39.5 and 56.5 ka B.P. Paleoceanography, 23(3) PA3206. file

Dickson, A. J.; Leng, M. J. and Maslin, M. A. (2008). Mid-depth South Atlantic Ocean circulation and chemical stratification during MIS-10 to 12: implications for atmospheric CO2. Climate of the Past, 4(4) pp. 333–344. file


Maslin, Mark; Austin, Patrick; Dickson, Alexander; Murlis, John; Owen, Matthew and Panizzo, Virginia (2007). Are we on target? Audit of UK Greenhouse Gas emissions to 2020: will current Government policies achieve significant reductions? UCL Environment Institute, London, U.K.. file

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