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

Zacke A, Voigt S, Joachimski M, Gale AS, Ward DJ, Tuetken T (2009)


Publication Type: Journal article

Publication year: 2009

Journal

Publisher: Geological Society

Book Volume: 166

Pages Range: 969-980

DOI: 10.1144/0016-76492008-068

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. © 2009 Geological Society of London.

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APA:

Zacke, A., Voigt, S., Joachimski, M., Gale, A.S., Ward, D.J., & Tuetken, T. (2009). Surface water freshening and high-latitude river discharge in the Eocene North Sea. Journal of the Geological Society, 166, 969-980. https://doi.org/10.1144/0016-76492008-068

MLA:

Zacke, Anne, et al. "Surface water freshening and high-latitude river discharge in the Eocene North Sea." Journal of the Geological Society 166 (2009): 969-980.

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