Oxygen 18–salinity relationship simulated by an oceanic general circulation model

Author:

Delaygue Gilles,Jouzel Jean,Dutay Jean-Claude

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference20 articles.

1. R.G. Fairbanks, C.D. Charles and J.D. Wright, Origin of global meltwater pulses, in: R.E. Taylor, A. Long and R.S. Kra (Eds.), Radiocarbon after four Decades: An Interdisciplinary Perspective, Springer-Verlag, New York, 1992, pp. 473–500.

2. H. Craig and L.I. Gordon, Deuterium and Oxygen 18 variations in the Ocean and the Marine Atmosphere, in: E. Tongiorgi (Ed.), Stable Isotopes in Oceanographic Studies and Paleotemperatures, Consiglio Nazionale delle Ricerche, Laboratorio di Geologia Nucleare, Pisa, Spoleto, 1965, pp. 9–130.

3. H. Östlund, H. Craig, W.S. Broecker and D. Spenser, GEOSECS Atlantic, Pacific and Indian ocean expeditions, vol. 7, IDOE NSF, Washington, DC, 1987.

4. Oxygen isotope constraints on surface ocean temperatures;Broecker;Quat. Res.,1986

5. Paleosalinity and δ18O: a critical assessment;Rohling;J. Geophys. Res.,1998

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