2008
DOI: 10.1016/j.epsl.2008.06.048
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Hydrothermal activity on the southern Mid-Atlantic Ridge: Tectonically- and volcanically-controlled venting at 4–5°S

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Cited by 77 publications
(53 citation statements)
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“…Theory that has proven robust in the deep ocean predicts that the turbulent rise of a buoyant hydrothermal plume should approximate to an inverted cone with a half-spreading angle of 30° (26). For example, in recent surveys of previously unexplored sections of Pacific, Atlantic, and Indian ridge crest, autonomous underwater vehicle (AUV) dives have relied on this same approximation to routinely intercept more than 10 different buoyant hydrothermal plumes (e.g., 27,28). Using the same approach here, we can predict that the buoyant plume signals we have intercepted at ∼500 m off bottom must originate at a source of venting-the Piccard vent site-that lies within a range of ∼250 m from this location (18°32.687′N, 81°43.170′W) within the red circle projected onto the seabed in Fig.…”
Section: Resultsmentioning
confidence: 99%
“…Theory that has proven robust in the deep ocean predicts that the turbulent rise of a buoyant hydrothermal plume should approximate to an inverted cone with a half-spreading angle of 30° (26). For example, in recent surveys of previously unexplored sections of Pacific, Atlantic, and Indian ridge crest, autonomous underwater vehicle (AUV) dives have relied on this same approximation to routinely intercept more than 10 different buoyant hydrothermal plumes (e.g., 27,28). Using the same approach here, we can predict that the buoyant plume signals we have intercepted at ∼500 m off bottom must originate at a source of venting-the Piccard vent site-that lies within a range of ∼250 m from this location (18°32.687′N, 81°43.170′W) within the red circle projected onto the seabed in Fig.…”
Section: Resultsmentioning
confidence: 99%
“…The vent system at 5°S comprises three active high temperature vent fields and several sites of diffuse emanations at depths of ~3000 m (German et al, 2008;Haase et al, 2007). At the Turtle Pits field and at Comfortless Cove, 800 m north-east of Turtle Pits, boiling and phase separation of the fluid emanations is evident, with several smokers venting at or above the conditions of the critical point of seawater (407°C at 298 bar, which is the pressure at the seafloor at this site).…”
Section: Sampling Areasmentioning
confidence: 99%
“…The southern Mid-Atlantic Ridge is formed by a divergent boundary between the South American Plate and the African Plate that is presently spreading at about 2.5 cm per year [21]. Our operations were conducted on a section of the SMAR to the north of the sites where active hydrothermal vents were first discovered by a combination of deep-tow and deep-submergence technologies culminating in photography by ABE [21] and subsequently sampled by the ROV Marum Quest [22].…”
Section: A Site Descriptionmentioning
confidence: 99%