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Foraminifera density analyses of sediment core ML1208-16BB from central equat...
Constraints on deep ocean carbonate chemistry are critical for understanding the processes responsible for glacial-interglacial changes in atmospheric pCO2 and the ocean... -
Trace Elements of sediment core ML1208-16BB from central equatorial Pacific
Quantitative constraints on deep ocean carbonate chemistry are critical for understanding the processes responsible for glacial-interglacial changes in atmospheric pCO2 and the... -
Calcium carbonate, sedimentary organic carbon, and shell weight of selected p...
To understand the variations in carbonate burial for the last 30 kiloannum (ka), we have utilized a core from the Ocean DrillingProgram (ODP), Site716A (04.56°N and 73.17°E)...
