Episodic fresh surface waters in the Eocene Arctic Ocean

Autor: Brinkhuis, H, Schouten, S, Collinson, M. E., Sluijs, A, SINNINGHE DAMST, J. S., Dickens, G. R., Huber, M, Cronin, T. M., Onodera, J, Takahashi, K, Bujak, J. P., Stein, R, VAN DER BURGH, J, Eldrett, J. S., Harding, I. C., Lotter, A. F., Sangiorgi, F, VAN KONIJNENBURG VAN CITTERT, H, DE LEEUW, J. W., Matthiessen, J, Backman, J, Moran, K, Clemens, S, Eynaud, F, Gattacceca, J, Jakobsson, M, Jordan, R, Kaminski, M, King, J, Koc, N, Martinez, N. C., Mcinroy, D, Moore, T. C., O'Regan, M, Plike, H, Rea, B, Rio, Domenico, Sakamoto, T, Smith, D. C., ST JOHN, K. E. K., Suto, I, Suzuki, N, Watanabe, M, Yamamoto, M.

Publikováno v: Nature
Nature, Nature Publishing Group, 2006, 441 (7093), pp.606-609. ⟨10.1038/nature04692⟩
Nature, 2006, 441 (7093), pp.606-609. ⟨10.1038/nature04692⟩

It has been suggested, on the basis of modern hydrology and fully coupled palaeoclimate simulations, that the warm greenhouse conditions that characterized the early Palaeogene period (55-45 Myr ago) probably induced an intensified hydrological cycle

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::25b47769315fd555a10e948e4bd0d7b9
http://hdl.handle.net/11577/1564701