Boron isotopes as a proxy for pH in siliceous and calcareous marine algae
Rising CO2 in the atmosphere has directly led to a reduction in surface ocean pH - a process known as ocean acidification. There is a need to understand past climates in terms of ocean pH change in order to be able to relate these to the current effects of climate change on marine organisms. One way...
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University of Southampton
2017
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.729769 |