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Interstitial water analysis from IODP Hole 323-U1342A
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1341B
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1341A
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1340B
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 323-U1339B
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 320-U1331B
Geocode = Top depth CSF-A (m) -
Interstitial water analysis from IODP Hole 320-U1331A
Geocode = Top depth CSF-A (m) -
(Table 1) Sulphur content and stable isotope ratios of ODP Leg 129 holes
The mineralogy of S-bearing phases, S-contents, and S-isotopic compositions of sediments and interstitial waters were determined for three cores drilled during Leg 129 in the... -
(Table 1) Chemical and isotopic composition of pore fluids in cores TGC-1 and...
The role of sediment diagenesis in the marine cycles of Li and B is poorly understood. Because Li and B are easily mobilized during burial and are consumed in authigenic clay... -
Biogeochemistry in sediment core HE180_1904
This dataset has no description
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Biogeochemistry in sediment core HE180_1866
This dataset has no description
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Biogeochemistry in sediment core HE180_1860
This dataset has no description
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Chemical composition in sediment core KOT97-3MUC
This dataset has no description
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Chemical composition and stable sulfur isotopes in sediment core KOT97-3GC
This dataset has no description
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Ex situ microsensor profiles of sulfide concentration and pH in/outside mat 1...
Biogeochemical measurements in sediment cores collected with the submersible JAGO (pusch cores) and a TV-MUC in the Black Sea during MSM15/1, Northwest Crimea (HYPOX Project),... -
Bottom water chemistry measured on surface sediments during Mare Nigrum cruis...
Due to the nature of the sediment, frequent air bubling through the sediment occurred during the multicorer recovery. As a result some results for the oxygen concentration and... -
Microbial diversity and physicochemistry of an estuarine phototrophic bloom i...
Organic-rich, brackish water bodies are common along coastlines and important for the biogeochemical cycling of carbon, nitrogen, sulfur, and phosphorus. These ecosystems are... -
Increased temperature reduces the positive effect of sulfide-detoxification m...
Seagrass meadows form essential ecological components in coastal zones but are rapidly declining worldwide due to anthropogenic impacts, including eutrophication and climate...