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Swath sonar multibeam EM120 bathymetry during METEOR cruise M72/3 with links ...
Multibeam data were collected during R/V Meteor cruise M72/3 leading to easterly Black Sea. Multibeam sonar system was Kongsberg Simrad EM-120. Data are unprocessed and may... -
(Table EA2) Geochemical proxy data along river-mouth to deep-basin transects
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(Table 6) Radiocarbon concentrations and conventional radiocarbon ages of n-C...
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(Table 5) Average terrestrial residence times of vascular plant biomarkers fo...
n-C29+31 alkanes terrestrial residence time: Calculated subtracting the respective sediment core top ages (Table 3) from the calibrated ages (Table 4).GeoB7621-1: n-C29-alkane... -
(Table 4) Radiocarbon and stable carbon isotopic data along river-mouth to de...
Errors are given as 1 Sigma analytical uncertainty. -
(Table 3) Expected core top ages based on published sedimentation rates witho...
Sedimentarion rate: Based on data from Calvert et al. (1987, 1991), Jones and Gagnon (1994), Arthur and Dean (1998), Gulin (2000), Gulin et al. (2002), Aycik et al. (2004),... -
14C specific radiocarbon ages and bulk ages accompanied by geochemical proxys...
Transfer of organic carbon (OC) from the terrestrial to the oceanic carbon pool is largely driven by riverine and aeolian transport. Before transport, however, terrigenous... -
Long-chain diols in rivers
Long-chain diols (LCDs) occur widespread in marine environments and also in lakes and rivers. Transport of LCDs from rivers may impact the distribution of LCDs in coastal... -
Hydrate abundances at the high-flux Batumi seep area in the southeastern Blac...
Submarine gas hydrates are a major global reservoir of the potent greenhouse gas methane. Since current assessments of worldwide hydrate-bound carbon vary by one order of... -
Mineralogical and stable isotope analyses of carbonates from the eastern Blac...
Authigenic carbonates associated with cold seeps provide valuable archives of changes in the long-term seepage activity. To investigate the role of shallow-buried hydrates on... -
Gas analysis of sediment cores from the Batumi seep area
Detailed knowledge of the extent of post-genetic modifications affecting shallow submarine hydrocarbons fueled from the deep subsurface is fundamental for evaluating source and... -
Pore-water concentration of chloride in sediment cores and equilibrium temper...
Vodyanitskii mud volcano is located at a depth of about 2070 m in the Sorokin Trough, Black sea. It is a 500-m wide and 20-m high cone surrounded by a depression, which is... -
Long-chain diols in rivers measured in SPM and sediments
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(Table S2) Additional samples from the Black Sea used for core-top SST assess...
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(Table 4) GDGT relative distributions and ratios from surface sediments from ...
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(Table 3) Sea surface temperature (SST) proxy data and in situ SSTs calculate...
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(Table 2) Results of radiocarbon and stable carbon isotope measurements of su...
Errors denote 1sigma analytical uncertainties. NOSAMS ID unless specified by prefix ETH referring to samples <25 µg C measured using the MICADAS gas ion source system at ETH... -
(Table 1) Sampling locations and previously published geochemical data (TOC a...
Sample ages for the oxic and suboxic stations include a mass balance correction for bioturbation assuming a mixed layer depth of 15 cm. -
Profile of sediment echo sounding during METEOR cruise M72/3a and M72/3b with...
File format description see: Data Acquisition of ATLAS PARASTORE, Atlas Hydrographic (2007), Operator Manual ATLAS PARASTORE, Doc. Id.: ED 6006 G 212:/Version: 4.0/Edition:... -
(Table 5) Unit-specific lengths (LsUx), pore fluid volumes (VpfUx), pore flui...
a assuming average sediment porosities Ø of 0.85 (Unit 1), 0.72 (Unit 2), and 0.61 (Unit 3), respectively, according to data provided by Haeckel et al. (2008) and Reitz et al....
