Dataset - B2FIND

Absolute concentrations of BDGTs and PDGTs in sediments from expeditions M84/...

Butanetriol and pentanetriol dialkyl glycerol tetraethers (BDGTs and PDGTs) are membrane lipids recently discovered in sedimentary environments and in the methanogenic archaeon...

Pore water chemistry of gravity core GeoB15101-7

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Water chemistry of CTD cast GeoB15101-6

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Water chemistry of CTD cast GeoB15101-1

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Archaeal lipid concentration and isotopic data in Black Sea and underlying se...

Archaeal lipids in marine sediments are important biomarkers widely used as indicators of paleoclimate and benthic archaeal ecology. However, the relative contributions of...

Published pore water and solid phase data from cores GeoB15105-1, GeoB15105-2...

An understanding of how the coupled cycles of carbon, iron and sulfur in sediments respond to environmental change throughout Earth history requires the reconstruction of...

Archaeal lipid concentration and isotopic data in sediments from expeditions ...

Archaea occupy an important niche in the global carbon cycle and their lipids are widely used as indicators of environmental conditions in both paleoenvironmental and modern...

Geochemical and quinone biomarker concentrations in the Black Sea water colum...

The stratified water column of the Black Sea serves as a model ecosystem for studying the interactions of microorganisms with major biogeochemical cycles. Here, we provide...

Late Lutetian Thermal Maximum - crossing a thermal threshold in Earth's clima...

Microbial production of methane is an important terminal metabolic process during organic matter degradation in marine sediments. It is generally acknowledged that...

Temperature proxies of sediment cores from the Sea of Marmara

Reconstructing ocean temperature values is a major target in paleoceanography and climate research. However, most temperature proxies are organism-based and thus suffer from an...

Pore water chemistry of sediment core GeoB15101-7 and water chemistry of CTD ...

Submarine brine lakes feature sharp and persistent concentration gradients between seawater and brine, though these should be smoothed out by free diffusion in open ocean...