{"id":7614,"date":"2016-06-14T02:40:23","date_gmt":"2016-06-14T02:40:23","guid":{"rendered":"https:\/\/www.darkenergybiosphere.org\/?post_type=publication&#038;p=7598"},"modified":"2016-10-14T19:06:37","modified_gmt":"2016-10-14T19:06:37","slug":"chemistry-of-hot-springs-along-the-eastern-lau-spreading-center","status":"publish","type":"publication","link":"https:\/\/www.darkenergybiosphere.org\/publication\/chemistry-of-hot-springs-along-the-eastern-lau-spreading-center\/","title":{"rendered":"Chemistry of hot springs along the Eastern Lau Spreading Center"},"content":{"rendered":"<p>The Eastern Lau Spreading Center (ELSC) is the southernmost part of the back-arc spreading axis in the Lau Basin, west of the Tonga trench and the active Tofua volcanic arc. Over its 397-km length it exhibits large and systematic changes in spreading rate, magmatic\/tectonic processes, and proximity to the volcanic arc. In 2005, we collected 81 samples of vent water from six hydrothermal fields along the ELSC. The chemistry of these waters varies both within and between vent fields, in response to changes in substrate composition, temperature and pressure, pH, water\/rock ratio, and input from magmatic gases and subducted sediment. Hot-spring temperatures range from 229\u00b0 to 363\u00a0\u00b0C at the five northernmost fields, with a general decrease to the south that is reversed at the Mariner field. The southernmost field, Vai Lili, emitted water at up to 334\u00a0\u00b0C in 1989 but had a maximum venting temperature of only 121\u00a0\u00b0C in 2005, due to waning activity and admixture of bottom seawater into the subseafloor plumbing system. Chloride varies both within fields and from one field to another, from a low of 528\u00a0mmol\/kg to a high of 656\u00a0mmol\/kg, and may be enriched by phase separation and\/or leaching of Cl from the rock. Concentrations of the soluble elements K, Rb, Cs, and B likewise increase southward as the volcanic substrate becomes more silica-rich, especially on the Valu Fa Ridge. Iodine and \u03b4<sup>7<\/sup>Li increase southward, and \u03b4<sup>11<\/sup>B decreases as B increases, apparently in response to increased input from subducted sediment as the arc is approached. Species that decrease southward as temperature falls are Si, H<sub>2<\/sub>S, Li, Na\/Cl, Fe, Mn, and <sup>87<\/sup>Sr\/<sup>86<\/sup>Sr, whereas pH, alkalinity, Ca, and Sr increase. Oxygen isotopes indicate a higher water\/rock ratio in the three systems on Valu Fa Ridge, consistent with higher porosity in more felsic volcanic rocks. Vent waters at the Mariner vent field on the Valu Fa Ridge are significantly hotter, more acid and metal-rich, less saline, and richer in dissolved gases and other volatiles, including H<sub>2<\/sub>S, CO<sub>2<\/sub>, and F, than the other vent fields, consistent with input of magmatic gases. The large variations in geologic and geophysical parameters produced by back-arc spreading along the ELSC, which exceed those along mid-ocean ridge spreading axes, produce similar large variations in the composition of vent waters, and thus provide new insights into the processes that control the chemistry of submarine hot springs.<\/p>\n","protected":false},"template":"","tags":[],"publication_type":[19],"_links":{"self":[{"href":"https:\/\/www.darkenergybiosphere.org\/wp-json\/wp\/v2\/publication\/7614"}],"collection":[{"href":"https:\/\/www.darkenergybiosphere.org\/wp-json\/wp\/v2\/publication"}],"about":[{"href":"https:\/\/www.darkenergybiosphere.org\/wp-json\/wp\/v2\/types\/publication"}],"wp:attachment":[{"href":"https:\/\/www.darkenergybiosphere.org\/wp-json\/wp\/v2\/media?parent=7614"}],"wp:term":[{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.darkenergybiosphere.org\/wp-json\/wp\/v2\/tags?post=7614"},{"taxonomy":"publication_type","embeddable":true,"href":"https:\/\/www.darkenergybiosphere.org\/wp-json\/wp\/v2\/publication_type?post=7614"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}