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Bulk chemistry measurements and XRF spectra of sediments from the high latitu...
This dataset has no description
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Multibeam bathymetry raw data (Kongsberg EM 122 entire dataset) of RV SONNE d...
Multibeam data were collected with RV Sonne along the route of cruise SO264 and data acquisition was continuously monitored during the survey. Multibeam sonar system was... -
Documentation of sediment core SO264_63-2
This dataset has no description
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Documentation of sediment core SO264_55-1
This dataset has no description
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XRF-retrieved productivity and carbonate data of sediment core SO264_66-2
The XRF-scanning measurements were carried out with an Avaatech XRF core scanner. The X-ray excitation scanning settings were 10 kV at 150 mA with no filter for a count time of... -
XRF-retrieved productivity and carbonate data of sediment core SO264_55-1, ln...
The XRF-scanning measurements were carried out with an Avaatech XRF core scanner. The X-ray excitation scanning settings were 10 kV at 150 mA with no filter for a count time of... -
XRF-retrieved productivity and carbonate data of sediment core SO264_55-1
The XRF-scanning measurements were carried out with an Avaatech XRF core scanner. The X-ray excitation scanning settings were 10 kV at 150 mA with no filter for a count time of... -
XRF-retrieved productivity and carbonate data of sediment core SO264_15-2
The XRF-scanning measurements were carried out with an Avaatech XRF core scanner. The X-ray excitation scanning settings were 10 kV at 150 mA with no filter for a count time of... -
Alkenone content of sediment core SO264_51-2
Alkenones were analyzed by GC (HP-6891) fitted with a flame ionization detector (GC-FID) using Helium as carrier gas (1.5 ml min 1 constant flow). -
Alkenone content of sediment core SO264_15-2
Alkenones were analyzed by GC (HP-6891) fitted with a flame ionization detector (GC-FID) using Helium as carrier gas (1.5 ml min 1 constant flow). -
Sand content of sediment core SO264_55-1
Sediment samples were freeze-dried and washed through a 63-µm sieve. -
CaCO3 content and carbonate accumulation rates of sediment core SO264_66-2
The CaCO3 content was calculated from TC and TOC which were measured by a CNS-analyzer (Elementar vario EL III) and a carbon/sulfur analyzer (Eltra CS-800). -
CaCO3 content and carbonate accumulation rates of sediment core SO264_55-1
The CaCO3 content was calculated from TC and TOC which were measured by a CNS-analyzer (Elementar vario EL III) and a carbon/sulfur analyzer (Eltra CS-800). -
CaCO3 content and carbonate accumulation rates of sediment core SO264_15-2
The CaCO3 content was calculated from TC and TOC which were measured by a CNS-analyzer (Elementar vario EL III) and a carbon/sulfur analyzer (Eltra CS-800). -
Sedimentation and accumulation rate of sediment core SO264_55-1
This dataset has no description
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Stable oxagen isotope ratios of benthic foraminifera of sediment core SO264_55-1
Benthic oxygen isotopes were measured on a Thermo Finnigan MAT 253 isotope ratio mass-spectrometer coupled to an automated KIEL IV CARBO preparation device. -
Geochemistry of the Pauzhetka tephra intervals in sediment core SO264_66-2
he XRF-scanning measurements were carried out with an Avaatech XRF core scanner at the AWI in Bremerhaven. The X-ray excitation scanning settings were 10 kV at 150 mA with no... -
Geochemistry of the Pauzhetka tephra intervals in sediment core SO264_62-2
he XRF-scanning measurements were carried out with an Avaatech XRF core scanner at the AWI in Bremerhaven. The X-ray excitation scanning settings were 10 kV at 150 mA with no... -
Geochemistry of the Pauzhetka tephra intervals in sediment core SO264_56-2
he XRF-scanning measurements were carried out with an Avaatech XRF core scanner at the AWI in Bremerhaven. The X-ray excitation scanning settings were 10 kV at 150 mA with no... -
Geochemistry of the Pauzhetka tephra intervals in sediment core SO264_55-1
he XRF-scanning measurements were carried out with an Avaatech XRF core scanner at the AWI in Bremerhaven. The X-ray excitation scanning settings were 10 kV at 150 mA with no...
