Carbon and oxygen stable isotopes measured on benthic foraminifera from IODP Site 323-U1343
High latitude deep water upwelling has the potential to control global climate over glacial timescales through the biological pump and ocean-atmosphere CO2 exchange. However, there is currently a lack of continuous long nutrient upwelling records with which to assess this mechanism. In this study we...
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Format: | Dataset |
Language: | English |
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PANGAEA
2019
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.906181 https://doi.org/10.1594/PANGAEA.906181 |