PrefaceSpecial issue on “shallow-water hydrothermal venting”
Section snippets
Acknowledgements
[LW]
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Subaqueous hot springs in Köyceğiz Lake, Dalyan Channel and Fethiye-Göcek Bay (SW Turkey): Locations, chemistry and origins
2017, Journal of Volcanology and Geothermal ResearchCitation Excerpt :This amount of energy was roughly equal to the world's total energy consumption at that time (1976). Similarly, Prol-Ledesma et al. (2005) described “shallow hydrothermal activity” as an interesting but not-as-yet well-studied phenomenon, where shallow means a water depth < 200 m, and they stated “Shallow-water vents provide accessible geological and chemical settings for studying the interaction of hydrothermal fluids with unconsolidated sediments, seawater, and basement rocks”. More recently, Suarez-Arriaga et al. (2014) declared that submarine geothermal resources have not been sufficiently used and studied yet, but they could cover the world's considerable energy demand of in an environmentally friendly way by integrating on-land geothermal prospecting experience and offshore hydrocarbon exploitation technology.
The response of benthic meiofauna to hydrothermal emissions in the Pontine Archipelago, Tyrrhenian Sea (central Mediterranean Basin)
2016, Journal of Marine SystemsCitation Excerpt :These submarine sites have been found in different tectonic settings at different depths, from shallow to deep water, and in substrates with various composition (Tivey, 2007). In particular, shallow-water hydrothermal vents have been reported especially in close relation to recent subaerial and submarine volcanic activity (e.g. Dando et al., 1999, 2000; de Ronde et al., 2001; Geptner et al., 2002; Italiano and Nuccio, 1991; Prol-Ledesma et al., 2005; Stoffers et al., 1999; Zhirmunsky and Tarasov, 1990), although some of them were discovered on mid-ocean ridges (Cardigos et al., 2005; Fricke et al., 1989; German et al., 1994) and in continental margin settings undergoing tectonic extension (e.g. Melwani and Kim, 2008; Prol-Ledesma et al., 2004; Vidal et al., 1978). Since their first discovery in the marine realm, hydrothermal vents attracted an increasing attention of scientific community mainly due to: 1) their importance in commercial resource exploration (e.g. hydrothermal related deposits; Hannington et al., 2011; Hein et al., 2013; Rona, 2008); 2) highly sensitive marine ecosystems they host; 3) possible implications for ocean chemistry, i.e. ocean acidification (e.g. Davis et al., 2003; Hall-Spencer et al., 2008; Jupp and Schultz, 2004; Vance et al., 2009).
Arsenic in hot springs of Bahía Concepción, Baja California Peninsula, México
2013, Chemical GeologyShallow submarine hydrothermal activity with significant contribution of magmatic water producing talc chimneys in the Wakamiko Crater of Kagoshima Bay, southern Kyushu, Japan
2013, Journal of Volcanology and Geothermal ResearchCitation Excerpt :This venting site was named the Wakamikenu hot venting (WHV) site (Fig. 2), within which we found three vents that were emitting hot fluid from the top or foot of the chimneys (Fig. 3). Such shallow-water (≤ 200 m) hydrothermal systems have been studied actively and accumulated knowledge recently (e.g., Sedwick and Stüben, 1996; Pichler et al., 1999, and see the special issue on “shallow-water hydrothermal venting” edited by Prol-Ledesma et al., 2005). Actively venting chimneys in a shallow-water hydrothermal system are very rare, although hydrothermal mineral mounds of similar shape have been reported at the Calypso vent site (167-m depth) off White Island, New Zealand (Sarano et al., 1989).
Estimation of sediment accumulation rates using naturally occuring <sup>210</sup>Pb models in Gülbahçe Bay, Aegean Sea, Turkey
2012, Journal of Environmental RadioactivityCitation Excerpt :The maximum recorded temperatures at the fluid outlets of submarine vents in the Aegean Sea are reported to vary between 33 °C at Yali and more than 119 °C at South of Milos (Dando et al., 1999) between 35 °C and 37 °C at the hydrothermal karst springs of Gülbahçe Bay (Tarcan, 2001). The chemical composition of vented gases in shallow area is similar to some deep vents, where carbon dioxide predominates (Dando et al., 2000; Pitchler et al., 1999), although in some cases, hydrogen sulfide (de Ronde et al., 2001), or even methane (Prol-Ledesma et al., 2002, 2005) may predominate. Chemical elements (Karageorgis et al., 2005) and compounds (Bayhan et al., 2001; Pehlivanoglou et al., 2000) can move up and down in water coulomn via adsorption onto suspendent particulate matter (SPM) (Karageorgis and Anagnostou, 2001).
Seawater dynamics and environmental settings after November 2002 gas eruption off Bottaro (Panarea, Aeolian Islands, Mediterranean Sea)
2010, Continental Shelf ResearchCitation Excerpt :Fluid discharges in the marine environment take place in many geological settings with large volumes of gas released, mostly in relation to volcanic and hydrothermal activity, and active faults (Prol-Ledesma et al., 2005; Dando et al., 2000; Géli et al., 2008).