相关数据集
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 ocean feedbacks that am
PANGAEA50
Planktonic foraminifera of sediment trap samples
Biweekly sediment trap samples and concurrent hydrographic measurements collected between March 2005 and October 2008 from the Cariaco Basin, Venezuela, are used to assess the relationship between [CO
PANGAEA20
Records of Neogene ocean carbonate chemistry using the boron isotope pH proxy
Over the course of the Neogene, the Earth underwent profound climatic shifts from the sustained warmth of the middle Miocene to the development of Plio-Pleistocene...
B2FIND10
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...
B2FIND30
(Tables 2, 3) Element ratios of planktonic foraminifera from western Pacific surface sediments
Accurately quantifying deep-sea calcite dissolution is crucial for understanding the role of the marine carbonate system in regulating atmospheric pCO2 over millennia. We compare a foraminifer-fragmen
PANGAEA10
