Modelling the impact of Siboglinids on the biogeochemistry of the Captain Arutyunov mud volcano (Gulf of Cadiz)

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Interactive comment on “Modelling the impact of Siboglinids on the biogeochemistry of the Captain Arutyunov mud volcano (Gulf of Cadiz)” by K. Soetaert et al

reply: It is true that certain bacteria are able to bridge the gap between concentration fronts of oxygen/nitrate and sulfide. This is particularly true for the Thioploca rather than for Beggiatoa, and is mostly found in environments characterized with sharp gradients of oxygen and sulfide close to the sediment surface. During investigations at the Captain Arutyunov mud volcano a comprehensive ...

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Interactive comment on “Modelling the impact of Siboglinids on the biogeochemistry of the Captain Arutyunov mud volcano (Gulf of Cadiz)” by K. Soetaert et al

This is a very interesting study of the influence of frenulate siboglinids on the biogeochemistry of an active mud volcano. The authors demonstrate the alteration of oxygen, sulfide, sulfate, and methane profiles and flux rates by the activity of the frenulate worms. It also makes some strong predictions about the controls on the worm’s growth by the geochemical conditions it inhabits. This is ...

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Impact of Siboglinids on mud volcano biogeochemistry

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Seabed methane emissions and the habitat of frenulate tubeworms on the Captain Arutyunov mud volcano (Gulf of Cadiz)

Submarine mud volcanism represents an important pathway for methane from deeper reservoirs to the surface, where it enters the benthic carbon cycle. To quantify overall methane release from the Captain Arutyunov mud volcano (CAMV) and to assess the contribution of macrobenthic seep organisms to the regulation of the benthic methane flux, we linked water column methane concentrations, seabed met...

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ژورنال

عنوان ژورنال: Biogeosciences

سال: 2012

ISSN: 1726-4189

DOI: 10.5194/bg-9-5341-2012