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The Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK. Now at Lamont-Doherty Earth Observatory of Columbia University, NY 10964-8000, USA
Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK
The Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK.
Department of Earth Sciences, University of Leeds, Leeds LS2 9JT Great Britain
Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK
Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Cambridge, UK
Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK
Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, United Kingdom
Department of Earth Sciences, University of Cambridge, Cambridge, UK
Department of Earth Sciences, University of Cambridge, Cambridge, CB3 3EQ, UK
Department of Earth Sciences, The University of Leeds, Leeds LS2 9JT Great Britain
Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, USA
Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, UK
Department of Earth Sciences, Cambridge University, Downing Street, Cambridge CB2 3EQ, UK
Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, UK
Department of Earth Sciences, University of Cambridge, Cambridge CB3 0EZ Engla
87 Sr / 86 Sr and 18 O / 16 O ratios, interstitial water chemistry and diagenesis in deep-sea carbonate sediments of the Ontong Java Plateau
87Sr/86Sr, 143Nd/144Nd and REEs in Silurian phosphatic fossils
A biomineralization model for the incorporation of trace elements into foraminiferal calcium carbonate
A Cenozoic seawater Sr/Ca record from benthic foraminiferal calcite and its application in determining global weathering fluxes
A chemical model of the buoyant and neutrally buoyant plume above the TAG vent field, 26 degrees N, Mid-Atlantic Ridge
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