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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... -
Calcareous nannofossil assemblage data (%) from ODP Site 202-1238
Coccoliths relative abundances (%) were analyzed spanning the last 30 ky at Site ODP 1238 (1°52.310′S, 82°46.934′W; 2203 m; 2203 m) in the EEP. -
Emiliania huxleyi morphological analysis from ODP Site 202-1238
We present data on the length and mass of Emiliania huxleyi, analyzed by using SYRACO (Systeme de Reconnaissance Automatique de Coccolithes), spanning the last 30 ky at Site ODP... -
Derived Particulate Inorganic Carbon (PIC) and Particulate Organic Carbon (PO...
We estimated E. huxleyi particulate inorganic to organic carbon ratio (PIC:POC) in order to detect changes in the carbonate counter-pump to carbon pump activity, which can act... -
Stable carbon and oxygen isotopes of benthic and planktic foraminifera and pl...
The internal development of the tropical West Pacific Warm Pool and its interaction with high latitude ocean regions on geological timescales is only poorly constrained. Based...
