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Global marine radiocarbon data compilation for the last deglaciation, spline ...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Global marine radiocarbon data compilation for the last deglaciation, global ...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Global marine radiocarbon data compilation for the last deglaciation, zonal a...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
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... -
Coral Li/Mg records of deep sea temperature during the last deglaciation
Fossil scleractinian corals were collected from the Galápagos platform in the East Equatorial Pacific (0°N, 90°E) on cruises MV1007 and NA064 from water depths between 419 and... -
Boron isotope composition of fossil Desmophyllum dianthus coral samples from ...
Uncertainty on mean coral d11B values is based on the pooled standard deviation of all the replicates in this study divided by square root of n, to give a measure of the... -
Boron isotope composition of fossil Desmophyllum dianthus coral samples from ...
This dataset has no description
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Master track of Nathaniel B. Palmer cruise NBP11-03 in 1 min resolution
This dataset has no description
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EM-120 multibeam swath bathymetry collected during Nathaniel B. Palmer cruise...
Data acquisition was performed using a multibeam sonar system Simrad EM-120 from Kongsberg. Raw data are delivered within Simrad current multibeam vendor format.Raw multibeam... -
Drake passage cold-water coral ages during NBP cruises NBP11-03 and NBP08-05
The Antarctic Cold Reversal (ACR; 14.7 to 13 ka) phase of the last deglaciation saw a pause in the rise of atmospheric pCO2 and Antarctic temperature, contrasted with warming in... -
Drake passage cold-water coral Ba/Ca and boron isotopes during NBP cruises NB...
The Antarctic Cold Reversal (ACR; 14.7 to 13 ka) phase of the last deglaciation saw a pause in the rise of atmospheric pCO2 and Antarctic temperature, contrasted with warming in...
