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Radiocarbon dates and benthic foraminifer (Uvigerina spp.) tie points for sit...
Sediment cores at sites J1002 and J1007 were collected from the Chilean Margin during D/V JOIDES Resolution Expedition 379T (JR100) in 2019. We generated age models for sites... -
Uranium and thorium concentrations for sites J1007, Chilean Margin
Sediment cores at sites J1007 awere collected from the Chilean Margin during D/V JOIDES Resolution Expedition 379T (JR100) in 2019. Sedimentary U/Th derived from natural gamma... -
Uranium and thorium concentrations for sites J1002, Chilean Margin
Sediment cores at sites J1002 awere collected from the Chilean Margin during D/V JOIDES Resolution Expedition 379T (JR100) in 2019. Sedimentary U/Th derived from natural gamma... -
Reconstructed biogenic opal percentage and accumulation for site J1007, Chile...
Sediment cores at sites J1007 were collected from the Chilean Margin during D/V JOIDES Resolution Expedition 379T (JR100) in 2019. Sedimentary Green/Blue (G/B) ratio data were... -
Reconstructed biogenic opal percentage for site J1002, Chilean Margin
Sediment cores at sites J1002 were collected from the Chilean Margin during D/V JOIDES Resolution Expedition 379T (JR100) in 2019. Sedimentary Green/Blue (G/B) ratio data were... -
Measured biogenic opal percentage for sites J1002 and J1007, Chilean Margin
Sediment cores at sites J1002 and J1007 were collected from the Chilean Margin during D/V JOIDES Resolution Expedition 379T (JR100) in 2019. Sedimentary Green/Blue (G/B) ratio... -
Organic carbon percentage for site J1007, Chilean Margin
Sediment core J1007 was collected from the Chilean Margin during D/V JOIDES Resolution Expedition 379T (JR100) in 2019. Measured organic carbon contents were compared to the G/B... -
Age model, biogenic opal contents and sedimentary U/Th for sites J1002 and J1...
Sediment cores at sites J1002 and J1007 were collected from the Chilean Margin during D/V JOIDES Resolution Expedition 379T (JR100) in 2019. Sedimentary Green/Blue (G/B) ratio... -
Mean sub-millennial AMOC strength in the North Atlantic during the Holocene
This dataset includes estimates of mean sub-millennial AMOC strength in the North Atlantic, derived from combined sedimentary 231Pa/230Th data. Using AMOC–231Pa/230Th... -
Holocene 231Pa/230Th ratios, Uranium isotopes and biogenic Opal concentration...
To investigate the variability of the Atlantic Meridional Overturning Circulation (AMOC) during the Holocene in the North Atlantic, we analyzed radioisotopes (230Th, 231Pa,... -
Holocene 231Pa/230Th ratios, Uranium isotopes and biogenic Opal concentration...
To investigate the variability of the Atlantic Meridional Overturning Circulation (AMOC) during the Holocene in the North Atlantic, we analyzed radioisotopes (230Th, 231Pa,... -
Opal differences between IODP Hole 385-U1545A and 385-U1549A
This dataset has no description
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Opal determination for IODP Hole 385-U1545A
This dataset has no description
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Opal determination for IODP Hole 385-U1549A
This dataset has no description
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X-Ray Fluoresence data of Barium and Titanium for IODP Hole 385-U1549A
The X-ray fluorescence (XRF) core scanning data presented here was obtained from sediment cores collected during IODP Expedition 385 in the Guaymas Basin, Gulf of California.... -
X-Ray Fluoresence data of Barium and Titanium for IODP Hole 385-U1545A
The X-ray fluorescence (XRF) core scanning data presented here was obtained from sediment cores collected during IODP Expedition 385 in the Guaymas Basin, Gulf of California.... -
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...
