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δ¹¹B, Mg/Ca, and input variables for calculated pH and CO₂ during the late Pl...
This dataset has no description
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Mg/Ca and different methods to calculate SST at ODP Sites 165-999 and 144-871
This dataset has no description
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Isotopes measured on Uvigerina peregrina, Globigerinoides ruber sensu stricto...
This dataset has no description
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Isotopes measured on Cibicidoides wuellerstorfi from ODP Site 165-999
This dataset has no description
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δ¹¹B-derived pCO₂ calculated with different treatments of Mg/Ca-derived SST a...
pCO₂ (in parts per million) calculated from δ¹¹B as the maximum probability of 10,000 realisations of the Monte Carlo simulation, and calculated with different Mg/Ca-temperature... -
Fragmentation index and percentage sand from ODP Site 144-871
This dataset has no description
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Orbital CO₂ reconstruction using boron isotopes during the late Pleistocene a...
This data set reports two highly resolved δ¹¹B-derived CO₂ records during the late Pleistocene (0-400 ky) from ODP Sites 999 (Caribbean) and 871 (West Pacific) based on the... -
Isotope ratios and B/Ca across Eocene Thermal Maximum 2 of ODP Hole 208-1265A
This dataset has no description
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Isotope ratios, Mg/Ca and B/Ca across Eocene Thermal Maximum 2 of ODP Hole 19...
This dataset has no description
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Isotope ratios across Paleocene-Eocene Thermal Maximum of ODP Site 198-1209
This dataset has no description
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B/Ca ratios across Eocene Thermal Maximum 2 of ODP Hole 198-1209A
This dataset has no description
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Stable isotope ratios, and trace elements from Pacific and S. Atlantic mid-la...
Eocene Thermal Maximum 2 (ETM‐2; 54.1 Ma) was the second largest Eocene hyperthermal. Like the Paleocene‐Eocene Thermal Maximum (PETM), ETM‐2 was characterized by massive carbon... -
Foraminifera boron isotope, sea surface temperature, salinity, pH and pCO2 da...
Data presented here are trace-elements and boron isotope composition of planktic foraminifera G. ruber (250-355 μm) along with reconstructed surface ocean temperature, salinity,... -
Benthic boron isotope data and associated pH determinations, from paper on Ce...
Boron isotope data on benthic foraminifera, spanning 1 to 59 Ma, and used to reconstruct deep ocean pH change over the Cenozoic. Data are from ODP sites spanning water depths... -
Boron isotope, trace elements and pH data (1990-2013) of the Porites lutea co...
Atmospheric CO2 rise in post-industrial era has resulted in decline in surface ocean pH, commonly known as “ocean acidification (OA)”, which has become a threat to marine... -
Boron and carbon isotope, and B/Ca data for a Siderastrea siderea coral core ...
Massive scleractinian corals provide unique opportunities to reconstruct past climatic and chemical changes in the ocean, where there is no additional information. Regular pH...