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KOSMOS 2021 Gran Canaria mesocosm study on ocean alkalinity enhancement: Bi-d...
The data presented herein originates from a mesocosm study conducted as part of the EU H2020 OceanNETs project, aimed at investigating the ecological ramifications of ocean... -
Geochemistry of sediment core YL16-5A from the Yellowstone Lake, USA
This dataset has no description
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Geochemistry of sediment core YL16-2C from the Yellowstone Lake, USA
This dataset has no description
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Carbonate isotopes of early Eocene strata in the Xining Basin, China
Carbonate (pedogenic and vadose-grown) δ13C and δ18O values as well as clumped isotopes (∆47 values). The latter also includes temperature reconstructions derived from the ∆47... -
Compiled reservoir ages from sediment cores from the Northeast Atlantic
This dataset has no description
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Radiocarbon chronology of sediment core SO213/2_76-2
This dataset has no description
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Radiocarbon chronology of sediment core PS97/137-1
This dataset has no description
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Radiocarbon chronology of sediment core MD07-3088
This dataset has no description
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(Table S3c) 14C ages measured on Globigerinoides ruber of sediment core KNR15...
*Came et al.. 2003; #Sortor and Lund. 2011.14C ages, 14C plateaus, and age conversion into calendar ages in three sediment cores from the tropical and subtropical South... -
(Table S3b) 14C ages measured on Globigerinoides sacculifer of sediment core ...
Jaeschke et al.. 2007; 14C ages from GeoB 3910-2. depths are correlated based on tuned Ti/Ca ratios (see Table S2).14C ages, 14C plateaus, and age conversion into calendar ages... -
(Table S3a) 14C ages measured on Globigerina bulloides of sediment core GeoB1...
*KIA 555: conventional 14C age from Littlel et al. (1997); #KIA4109 and #KIA 4110: conventional 14C age from Vidal et al. (1999).14C ages, 14C plateaus, and age conversion into... -
(Table S1 b) Definition of planktic 14C plateaus for sediment core GeoB3910-1
Very low sedimentation rates below Plateau 3 suggest hiatus. -
(Table S1 a) Definition of planktic 14C plateaus for sediment core GeoB1711-4
Plateau No. 1 - 3: By comparison with Suigetsu Plateau 3 the short length of Plateau 3 may be explained by a ~200-yr drop in local 14C reservoir age over Plateau 3. Its actual... -
Seawater carbonate chemistry and physiological metrics and gene expression re...
We examined gene expression responses of >2-year coral transplant experiment to ambient and low pH common garden sites of three species of reef-building corals (Porites... -
Nitrous oxide production rates and stable isotopes in the Benguela Upwelling ...
Upwelling systems are significant sources of atmospheric nitrous oxide (N₂O). The Benguela Upwelling System is one of the most productive regions worldwide and a temporally... -
Atlantic inflow into the southern Nordic Seas at the onset of the LGM promote...
Tephra analysis (FMAZ II-1 tephra marker) on a network of ten marine sediment cores in the northern North Atlantic is presented as well as radiocarbon dates (14C) by Accelerator... -
Summer hydrographic conditions at proglacial fjord entrances along East Green...
Here we present results from a synoptic survey of the pan‐east Greenland coastal system from the entrance of fjords at Cape Farewell (59°N) to Kaiser Franz Josef Fjord (73°N).... -
Global marine radiocarbon data compilation for the last deglaciation
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Nitrous oxide production rates and stable isotopes in the Benguela Upwelling ...
Upwelling systems are significant sources of atmospheric nitrous oxide (N₂O). The Benguela Upwelling System is one of the most productive regions worldwide and a temporally... -
Seawater carbonate chemistry for the transgenerational experiment on synergis...
Metazoan adaptation to global change relies on selection of standing genetic variation. Determining the extent to which this variation exists in natural populations,...