Near-surface Heating of Young Rift Sediment Causes Mass Production and Discharge of Reactive Dissolved Organic Matter. (scientific article published on 22 March 2017)

The Guaymas Basin Hiking Guide to Hydrothermal Mounds, Chimneys, and Microbial Mats: Complex Seafloor Expressions of Subsurface Hydrothermal Circulation

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Oil biodegradation. Water droplets in oil are microhabitats for microbial life

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Thermal and geochemical influences on microbial biogeography in the hydrothermal sediments of Guaymas Basin, Gulf of California

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The impact of microbial metabolism on marine dissolved organic matter

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Recalcitrant dissolved organic carbon fractions

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Methane hydrate-bearing seeps as a source of aged dissolved organic carbon to the oceans

Q57411344

Spatial heterogeneity and underlying geochemistry of phylogenetically diverse orange and white Beggiatoa mats in Guaymas Basin hydrothermal sediments

Q57816582

Carbon release by off-axis magmatism in a young sedimented spreading centre

Q57851936

Assessing the apparent imbalance between geochemical and biochemical indicators of meso- and bathypelagic biological activity: What the @$♯! is wrong with present calculations of carbon budgets?

Q58068903

Prokaryotic respiration and production in the meso- and bathypelagic realm of the eastern and western North Atlantic basin

Q58068926

Ocean margins as a significant source of organic matter to the deep open ocean

Q59058607

Mats of giant sulphur bacteria on deep-sea sediments due to fluctuating hydrothermal flow

Q59066194

Deep marine biosphere fuelled by increasing organic matter availability during burial and heating

Q59086031

Hydrothermal oil of Guaymas Basin and implications for petroleum formation mechanisms

Q59086045

Hydrothermal petroleum in mineralized mounds at the seabed of Guaymas Basin