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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... -
Clay mineral composition of gravity core DG12-GC02 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... -
Clay mineral composition of gravity core DG12-GC01 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... -
Sediment properties of sediment core RS14_GC3
This dataset has no description
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Sediment properties of sediment core RS14_GC2
This dataset has no description
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Sediment properties of sediment core RS14_GC1
This dataset has no description
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Geochemical proxies of sediment core RS14_GC3
This dataset has no description
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Geochemical proxies of sediment core RS14_GC2
This dataset has no description
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Geochemical proxies of sediment core RS14_GC1
This dataset has no description
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Sediment properties, geochemical proxies, clay mineral composition and diatom...
For the reconstruction of paleoenvironment and retreat of grounding line and calving line, 14C ages, X-radiograph, magnetic susceptibility, granulometry, biogenic opal, total... -
Sediment properties and geochemical proxies of gravity cores obtained on the ...
For the reconstruction of paleoenvironment, 14C ages, magnetic susceptibility, number of gravel, granulometry, biogenic opal, total organic carbon, d13C, total nitrogen, d15N,... -
Physico-chemical conditions during a summer-autumn transition in the Ross Sea...
Here we present physico-chemical data collected during two research cruises conducted to and across the Ross Sea, Antarctica in the summer of 2018 (February-March) and 2019... -
Derived geomorphic features (shapefiles) from multibeam bathymetry processed ...
Bathymetry from multibeam echo sounding data in Pennell Trough, Ross Sea, Antarctica was collected onboard the RVIB Nathaniel B. Palmer (NBP) 15-02 cruise using a Kongsberg... -
Multibeam bathymetry processed data (Kongsberg EM 122 working area dataset) o...
Bathymetry from multibeam echo sounding data in Pennell Trough, Ross Sea, Antarctica was collected onboard the RVIB Nathaniel B. Palmer (NBP) 15-02 cruise using a Kongsberg...