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Interstitial water analysis from IODP Hole 323-U1345B
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1345A
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1344C
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1344A
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1343E
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1343B
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1343A
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1342B
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1342A
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1341B
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1340B
Geocode = Top depth CSF-A (m) -
Sea-ice biomarkers, benthic and planktonic foraminiferal geochemistry, and be...
The dataset compiles sea-ice biomarkers (IP25, HBI II, HBI III, Triene E, Brassicasterol, Campesterol, Cholesterol, β- sitosterol) together with benthic and planktonic... -
Sea-ice biomarkers, benthic and planktonic foraminiferal geochemistry, and be...
The dataset compiles sea-ice biomarkers (IP25, HBI II, HBI III, Triene E, Brassicasterol, Campesterol, Cholesterol, β- sitosterol) together with benthic and planktonic... -
Uranium-Thorium analysis from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Silica weight percent from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Silicon isotopes from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Radiocarbon ages from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Nitrogen weight percent from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Diatom abundance from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Age model data from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we...
