Iron and phosphorus cycling under ferruginous conditions
Considering the entirety of Earth’s history, the ocean has dominantly been in an anoxic, non-sulphidic state, with the water column containing dissolved iron (termed ‘ferruginous’). Despite the significance of such conditions, the cycling of nutrients in ferruginous settings remains poorly understoo...
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University of Leeds
2018
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.745618 |