{"id":11654,"date":"2017-09-05T10:49:22","date_gmt":"2017-09-05T17:49:22","guid":{"rendered":"https:\/\/www.darkenergybiosphere.org\/?post_type=publication&#038;p=11654"},"modified":"2017-10-02T12:25:38","modified_gmt":"2017-10-02T19:25:38","slug":"cool-seafloor-hydrothermal-springs-reveal-global-geochemical-fluxes","status":"publish","type":"publication","link":"https:\/\/www.darkenergybiosphere.org\/publication\/cool-seafloor-hydrothermal-springs-reveal-global-geochemical-fluxes\/","title":{"rendered":"Cool seafloor hydrothermal springs reveal global geochemical fluxes"},"content":{"rendered":"<p>We present geochemical data from the first samples of spring fluids from Dorado Outcrop, a basaltic edifice on 23 M.y. old seafloor of the Cocos Plate, eastern Pacific Ocean. These samples were collected from the discharge of a cool hydrothermal system (CHS) on a ridge flank, where typical reaction temperatures in the volcanic crust are low (2\u201320\u2009\u00b0C) and fluid residence times are short. Ridge-flank hydrothermal systems extract 25% of Earth&#8217;s lithospheric heat, with a global discharge rate equivalent to that of Earth&#8217;s river discharge to the ocean; CHSs comprise a significant fraction of this global flow. Upper crustal temperatures around Dorado Outcrop are \u223c15\u2009\u00b0C, the calculated residence time is &lt;3 y, and the composition of discharging fluids is only slightly altered from bottom seawater. Many of the major ions concentrations in spring fluids are indistinguishable from those of bottom seawater; however, concentrations of Rb, Mo, V, U, Mg, phosphate, Si and Li are different. Applying these observed differences to calculated global CHS fluxes results in chemical fluxes for these ions that are \u226515% of riverine fluxes. Fluxes of K and B also may be significant, but better analytical resolution is required to confirm this result. Spring fluids also have \u223c50% less dissolved oxygen (DO) than bottom seawater. Calculations of an analytical model suggest that the loss of DO occurs primarily (&gt;80%) within the upper basaltic crust by biotic and\/or abiotic consumption. This calculation demonstrates that permeable pathways within the upper crust can support oxic water\u2013rock interactions for millions of years.<\/p>\n","protected":false},"template":"","tags":[],"publication_type":[19],"_links":{"self":[{"href":"https:\/\/www.darkenergybiosphere.org\/wp-json\/wp\/v2\/publication\/11654"}],"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=11654"}],"wp:term":[{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.darkenergybiosphere.org\/wp-json\/wp\/v2\/tags?post=11654"},{"taxonomy":"publication_type","embeddable":true,"href":"https:\/\/www.darkenergybiosphere.org\/wp-json\/wp\/v2\/publication_type?post=11654"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}