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Particulate concentrations and vertical fluxes of sedimentary material and ch...
CTD and nephelometric sounding data are considered along with parameters of the near-bottom currents and particulate fluxes measured by a subsurface mooring station in the... -
Chemical and mineral compositions of hydrothermal sulfide deposits from the L...
Several hydrothermal sulfide structures were sampled using the Mir manned submersibles in the relatively shallow Lucky Strike vent field, Mid-Atlantic Ridge. Bathymetric... -
Chemical composition of particulate matter and element fluxes in the eastern ...
This paper reports results of a geochemical study of suspended particulate matter and particle fluxes in the Norwegian Sea above the Bear Island slope. Concentrations of... -
Geochemical analysis of surface sediments from the ocean floor and from sea i...
Barium in marine terrigenous surface sediments of the European Nordic Seas is analysed to evaluate its potential as palaeoproductivity proxy. Biogenic Ba is calculated from Ba... -
(Table 4) Integrated biomass, chlorophyll a and phaeopigments contents, and p...
This dataset has no description
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(Table 2b) Primary production, chlorophyll a concentration, assimilation rate...
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Dry bulk density and major element contents in bottom sediments of Core AMK21...
This dataset has no description
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Stable dissolved silicon isotopes measured on CTD and underway samples during...
Dissolved stable silicon isotopes were determined in seawater samples collected during the 73rd expedition onboard RV Akademik Mstislav Keldysh (AMK73) in the Laptev Sea in... -
Primary data sets of the hydrographic atlas of the Southern Ocean
The general knowledge of the hydrographic structure of the Southern Ocean is still rather incomplete since observations particularly in the ice covered regions are cumbersome to... -
Deep-Ocean dissolved organic matter in hydrothermal vents
Oceanic dissolved organic carbon (DOC) is an important carbon pool, similar in magnitude to atmospheric CO2, but the fate of its oldest forms is not well understood (Dittmar and...