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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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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... -
B/Ca, δ¹¹B and calcifying fluid carbonate chemistry reconstruction of Porites...
Samples were collected from two Porites sp. coral cores in the Southwestern Pacific, specifically at Nomuka Iki Island (Tonga). Parameters measured in this study include boron... -
B/Ca, δ¹¹B and calcifying fluid carbonate chemistry reconstruction of Porites...
Samples were collected from two Porites sp. coral cores in the Southwestern Pacific, specifically at Rotuma Island (Fiji). Parameters measured in this study include boron stable... -
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,... -
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... -
Diatom boron isotope data from ODP Site 882 over the intensification of North...
Diatom boron and boron isotope data from ODP Site 882 in the subarctic Pacific Ocean over the intensification of Northern Hemisphere glaciation (iNHG) at 2.73 Ma. -
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... -
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... -
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... -
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... -
δ¹¹B, Mg/Ca, and input variables for calculated pH and CO₂ during the late Pl...
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Isotopes measured on Uvigerina peregrina, Globigerinoides ruber sensu stricto...
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Isotopes measured on Cibicidoides wuellerstorfi from ODP Site 165-999
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Fragmentation index and percentage sand from ODP Site 144-871
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Isotope ratios and B/Ca across Eocene Thermal Maximum 2 of ODP Hole 208-1265A
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Isotope ratios, Mg/Ca and B/Ca across Eocene Thermal Maximum 2 of ODP Hole 19...
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Isotope ratios across Paleocene-Eocene Thermal Maximum of ODP Site 198-1209
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B/Ca ratios across Eocene Thermal Maximum 2 of ODP Hole 198-1209A
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