Reconstructing past ocean circulation and chemistry using benthic foraminifera : traditional and novel approaches

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Marine calcium carbonate (CaCO3) polymorphs, as calcite and aragonite (e.g., foraminifera and corals), have an important role in reconstructions of past climate and past ocean circulation, in particular when stable isotopes (e.g., O, C, B) and trace elements (e.g., Li, B, Mg, Sr) are analyzed.
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August 2014
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Rensselaer Polytechnic Institute, Troy, NY
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