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The Paleocene-Eocene Thermal Maximum (PETM; ~ 56 million years ago (Ma) is the most severe carbon cycle perturbation event of the Cenozoic. Although the PETM is associated with warming in both the surface (~up to 8°C) and deep ocean (~up to 5°C), there are relatively fe... View more
Aze, T., Pearson, P.N., Dickson, A.J., Badger, M.P.S., Bown, P.R., Pancost, R.D., Gibbs, S.J., Huber, B.T., Leng, M.J., Coe, A.L., Cohen, A.S. and Foster, G.L. (2014) Extreme warming of tropical waters during the Paleocene-Eocene Thermal Maximum. Geology.42. 739-742
Bornemann, A., Norris, R.D., Lyman, J.A., D'Haenens, S., Groeneveld, J., Röhl, U., Farley, K.A. and Speijer, R.P. (2014) Persistent environmental change after the Paleocene-Eocene Thermal Maximum in the eastern North Atlantic. Earth and Planetary Science Letters 394, 70-81.
Carmichael, M.J., Inglis, G.N., Badger, M.P., Naafs, B.D.A., Behrooz, L., Remmelzwaal, S., Monteiro, F.M., Rohrssen, M., Farnsworth, A., Buss, H.L. Dickson, A.J, Valdes, P.J., Lunt, D.J and Pancost, R.D. (2017) Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum. Global and Planetary Change, 157,114-138.
Carmichael, M.J., Pancost, R.D., Lunt, D. (2018) Changes in the occurrence of extreme precipitation events at the Paleocene-Eocene thermal maximum. Global and Planetary Change. 501, 24-36.
Colcord, D.E., Cadieux, S.B., Brassell, S.C., Castañeda, I.S., Pratt, L.M. and White, J. (2015) Assessment of branched GDGTs as temperature proxies in sedimentary records from several small lakes in southwestern Greenland. Organic Geochemistry. 82, 33-41.
Collinson, M., Hooker, J. and Grocke, D. (2003) Cobham lignite bed and penecontemporaneous macrofloras of southern England: A record of vegetation and fire across the Paleocene-Eocene Thermal Maximum. Special Papers - Geological Society of American, 333-350.
Collinson, M.E., Smith, S.Y., van Konijnenburg-van Cittert, J.H., Batten, D.J., van der Burgh, J., Barke, J. and Marone, F. (2013) New observations and synthesis of Paleogene heterosporous water ferns. International Journal of Plant Sciences.174, 350-363.
Collinson, M.E., Steart, D.C., Harrington, G.J., Hooker, J.J., Scott, A.C., Allen, L.O., Glasspool, I.J. and Gibbons, S.J. (2009) Palynological evidence of vegetation dynamics in response to palaeoenvironmental change across the onset of the Paleocene‐Eocene Thermal Maximum at Cobham, Southern England. Grana 48, 38-66.
Currano, E.D., Wilf, P., Wing, S.L., Labandeira, C.C., Lovelock, E.C. and Royer, D.L.. (2008) Sharply increased insect herbivory during the Paleocene-Eocene Thermal Maximum. PNAS 105, 1960-1964.
Damsté, J.S.S., Rijpstra, W.I.C., Foesel, B.U., Huber, K.J., Overmann, J., Nakagawa, S., Kim, J.J., Dunfield, P.F., Dedysh, S.N. and Villanueva, (2018) An overview of the occurrence of ether-and ester-linked iso-diabolic acid membrane lipids in microbial cultures of the Acidobacteria: Implications for brGDGT paleoproxies for temperature and pH. Organic Geochemistry. 124, 63-76.