-
Southern Ocean Sea Surface Temperature Anomaly Stacks
This dataset has no description
-
Recalibrated age model and sea surface temperatures of sediment core SO136_11...
This dataset has no description
-
(Table A.1) Locations, satellite-derived spring sea ice concentrations (SpSIC...
This dataset has no description
-
Sediment grain size, organic matter, and pigments for the surface layers of t...
This dataset has no description
-
Mineralogy of surface sediment samples from the Arctic Ocean
This dataset has no description
-
OHGDGT global surface sediment data
Here, we compile an extensive global surface sediment dataset of OH-isoGDGTs as well as regular isoprenoid GDGTs (isoGDGTs), with both data generated at NIOZ and previously... -
Chloride concentrations and calculated gas hydrate saturations in sediments c...
During cruise SO266/1 deep sediment cores were collected using MARUM-MeBo200 from Formosa Ridge and Four-Way Closure Ridge, South China Sea. Near-surface sediments were... -
Chloride concentrations and calculated gas hydrate saturations in sediments c...
During cruise SO266/1 deep sediment cores were collected using MARUM-MeBo200 from Formosa Ridge and Four-Way Closure Ridge, South China Sea. Near-surface sediments were... -
Carbonate contents in sediments collected at Four-Way Closure Ridge, RV Sonne...
During cruise SO266/1 deep sediment cores were collected using MARUM-MeBo200 from Formosa Ridge and Four-Way Closure Ridge, South China Sea. Near-surface sediments were... -
Carbonate contents in sediments collected at Formosa Ridge, RV Sonne cruise S...
During cruise SO266/1 deep sediment cores were collected using MARUM-MeBo200 from Formosa Ridge and Four-Way Closure Ridge, South China Sea. Near-surface sediments were... -
Biomarker concentrations in gravity core MSM45_19-2
Sea ice and paleoenvironmental conditions were reconstructed based on gravity core MSM45_19-2 from the northern Labrador Shelf. Gravity core MSM45_19-2 was obtained during R/V... -
Dry bulk density and major element contents in bottom sediments of Core AMK21...
This dataset has no description
-
Analysis of minerals from Arctic Ocean sediments
The Arctic Ocean System is a key player regarding the climatic changes of Earth. Its highly sensitive ice Cover, the exchange of surface and deep water masses with the global... -
Diatom assemblage of gravity core DG12-GC04 obtained on the Drygalski Basin i...
The samples for diatom assemblage were selected at nine horizons from GC01 and GC04, respectively. The sediment treatment, slide preparation, and diatom counting were carried... -
Diatom assemblage of gravity core DG12-GC01 obtained on the Drygalski Basin i...
The samples for diatom assemblage were selected at nine horizons from GC01 and GC04, respectively. The sediment treatment, slide preparation, and diatom counting were carried... -
Sediment properties of gravity core DG12-GC05 obtained on the Drygalski Basin...
The MS was measured at 1 cm interval using Bartington MS-2B susceptibility meter. The WC was also measured at 1 cm interval using 1 cm thick subsamples by calculating the... -
Sediment properties of gravity core DG12-GC04 obtained on the Drygalski Basin...
The MS was measured at 1 cm interval using Bartington MS-2B susceptibility meter. The WC was also measured at 1 cm interval using 1 cm thick subsamples by calculating the... -
Sediment properties of gravity core DG12-GC02 obtained on the Drygalski Basin...
The MS was measured at 1 cm interval using Bartington MS-2B susceptibility meter. The WC was also measured at 1 cm interval using 1 cm thick subsamples by calculating the... -
Sediment properties of gravity core DG12-GC01 obtained on the Drygalski Basin...
The MS was measured at 1 cm interval using Bartington MS-2B susceptibility meter. The WC was also measured at 1 cm interval using 1 cm thick subsamples by calculating the... -
Clay mineral composition of gravity core DG12-GC04 obtained on the Drygalski ...
The samples for clay mineral compositions were collected from GC01 and GC04 at 10 or 20 cm intervals. The organic matter was removed using 10% H2O2, and the fine fraction...