Zinc, Isotopes and Ocean Sediment: What’s the Link to Earth’s Future Climate?

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issue 19: oceans
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Published: Dec 3, 2018

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Matthew Druce
Chemistry Department, University of Otago.
Ruth Napper

Abstract

During the Earth’s history, similar periods of rapid climate change have taken place and are recorded in ocean sediments that archive these analogous time periods. In a circular way, the oceans can provide a means for us to resolve the uncertainties surrounding the Earth’s future.

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No. 19 (2018): oceans
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Articles

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Author Biographies

Matthew Druce, Chemistry Department, University of Otago.

Matt Druce is a PhD candidate in the Chemistry Department, University of Otago.

Ruth Napper

Ruth Napper is an artist and maker of contemporary jewellery.