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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,... -
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... -
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.... -
Opal and Ba/Ti ratio for IODP Holes 385-U1545A and 385-U1549A
The dataset compiles paleoproductivity proxies from sediments recovered from the first 42.29 meters below the seafloor (mbsf) at Hole 385-U1545A, with a resolution of 30 cm for... -
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... -
Biogenic opal record of gravity core MSM45_19-2
Biogenic opal (BSi) concentrations were analysed as indicator for past primary productivity on gravity core MSM45_19-2 from the northern Labrador Shelf. Gravity core MSM45_19-2... -
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...
