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Quantifying potassium (K), uranium (U) and thorium (Th) of IODP Site 323-U1343C
This dataset has no description
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Quantifying potassium (K), uranium (U) and thorium (Th) of IODP Site 323-U1343A
This dataset has no description
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Quantifying potassium (K), uranium (U) and thorium (Th) of IODP Site 323-U1343E
This dataset has no description
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Smear slide grain counts from IODP Site 323-U1342
Here we present new grain count data from from Integrated Ocean Drilling Program (IODP) Expedition 323 Site U1342 Holes A, C, and D. New records of sediment composition from... -
Interstitial water analysis from IODP Hole 323-U1342A
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1340B
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-U1342B
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-U1343B
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-U1344A
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-U1345A
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1345B
Geocode = Top depth CSF-A (m) -
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... -
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... -
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... -
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...