Surface water freshening and high-latitude river discharge in the Eocene North Sea.

Zacke, A., Voigt, Silke, Gale, A. S. and Joachimski, M. M. (2009) Surface water freshening and high-latitude river discharge in the Eocene North Sea. Journal of the Geological Society, 166 . pp. 969-980. DOI 10.1144/0016-76492008-068.

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Abstract

A shark-tooth apatite δ18O record of the early Palaeogene North Sea reflects changes in regional hydrography by showing variable temperatures and salinities. A 2–4 Ma period in the early Eocene was particularly influenced by substantial surface-water freshening, indicated by a 3–4‰ reduction of δ18O values. The magnitude of the δ18O decrease indicates a depletion in 18O of surface waters by 2–3‰ relative to Eocene mean ocean water. This value is lower than that of coeval lakes reconstructed from freshwater gastropod δ18O values from the Paris Basin, suggesting that large rivers with high-latitude catchment areas drained into the North Sea. The period of surface-water freshening began close to the Palaeocene – Eocene thermal maximum, when relative sea-level fall, tectonic uplift and basaltic volcanism caused a temporary isolation of the North Sea. North Atlantic and North Sea surface waters became reconnected during a series of early Eocene transgressions.

Document Type: Article
Keywords: Surface-water freshening, river discharge, North Sea, Eocene
Research affiliation: OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-P-OZ Paleo-Oceanography
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1144/0016-76492008-068
ISSN: 0016-7649
Date Deposited: 15 Sep 2009 12:04
Last Modified: 17 Oct 2019 07:21
URI: http://oceanrep.geomar.de/id/eprint/1965

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