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Diatom fragment composition in the back-scattered electron images obtained fr...
The dataset of diatom fragment composition in the back-scattered electron images (BSEI) of cross thin section of laminated sediments and lamina thickness for Sections... -
Diatom analysis in subsample smear slides from IODP Hole 323-U1340A
The dataset of diatom analysis in the subsample smear slides obtained from Sections IODP323-U1340A-10H-1W, 134-149cm, 10H-2W, 001-116cm, and 14H-1W, 60-88cm. -
(Table 2) Key diatom species of IODP Hole 323-U1340A
DEPTH, sediment/rock [m] is given in mcd. -
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... -
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)
