<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Yang, Ningfang</style></author><author><style face="normal" font="default" size="100%">Kathleen A. Welch</style></author><author><style face="normal" font="default" size="100%">Mohajerin, T. Jade</style></author><author><style face="normal" font="default" size="100%">Telfeyan, Katherine</style></author><author><style face="normal" font="default" size="100%">Chevis, Darren A.</style></author><author><style face="normal" font="default" size="100%">Grimm, Deborah A.</style></author><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author><author><style face="normal" font="default" size="100%">White, Christopher D.</style></author><author><style face="normal" font="default" size="100%">Johannesson, Karen H.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Comparison of arsenic and molybdenum geochemistry in meromictic lakes of the McMurdo Dry Valleys, Antarctica: Implications for oxyanion-forming trace element behavior in permanently stratified lakes</style></title><secondary-title><style face="normal" font="default" size="100%">Chemical Geology</style></secondary-title><short-title><style face="normal" font="default" size="100%">Chemical Geology</style></short-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year><pub-dates><date><style  face="normal" font="default" size="100%">05/2015</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://linkinghub.elsevier.com/retrieve/pii/S0009254115001874http://api.elsevier.com/content/article/PII:S0009254115001874?httpAccept=text/xmlhttp://api.elsevier.com/content/article/PII:S0009254115001874?httpAccept=text/plain</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">404</style></volume><pages><style face="normal" font="default" size="100%">110 - 125</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;&lt;span style=&quot;color: rgb(46, 46, 46); font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; font-size: 16px; line-height: 23.6800003051758px; word-spacing: -1.24453127384186px;&quot;&gt;Water samples were collected for arsenic (As) and molybdenum (Mo) analysis from different depths in Lakes Hoare and Fryxell, both of which are located in the Taylor Valley within the McMurdo Dry Valleys of Antarctica. Sampling depths within each lake were chosen to capture variations in As and Mo concentrations and As speciation in the oxic mixolimnia and anoxic monimolimnia of these meromictic lakes. Arsenic concentrations ranged from 0.67&amp;nbsp;nmol&amp;nbsp;kg&lt;/span&gt;&lt;sup style=&quot;font-size: 0.75em; font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; line-height: 0; color: rgb(46, 46, 46); word-spacing: -1.24453127384186px;&quot;&gt;&amp;minus;&amp;nbsp;1&lt;/sup&gt;&lt;span style=&quot;color: rgb(46, 46, 46); font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; font-size: 16px; line-height: 23.6800003051758px; word-spacing: -1.24453127384186px;&quot;&gt;&amp;nbsp;to 3.54&amp;nbsp;nmol&amp;nbsp;kg&lt;/span&gt;&lt;sup style=&quot;font-size: 0.75em; font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; line-height: 0; color: rgb(46, 46, 46); word-spacing: -1.24453127384186px;&quot;&gt;&amp;minus;&amp;nbsp;1&lt;/sup&gt;&lt;span style=&quot;color: rgb(46, 46, 46); font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; font-size: 16px; line-height: 23.6800003051758px; word-spacing: -1.24453127384186px;&quot;&gt;&amp;nbsp;in Lake Hoare and from 1.69&amp;nbsp;nmol&amp;nbsp;kg&lt;/span&gt;&lt;sup style=&quot;font-size: 0.75em; font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; line-height: 0; color: rgb(46, 46, 46); word-spacing: -1.24453127384186px;&quot;&gt;&amp;minus;&amp;nbsp;1&lt;/sup&gt;&lt;span style=&quot;color: rgb(46, 46, 46); font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; font-size: 16px; line-height: 23.6800003051758px; word-spacing: -1.24453127384186px;&quot;&gt;&amp;nbsp;to 17.5&amp;nbsp;nmol&amp;nbsp;kg&lt;/span&gt;&lt;sup style=&quot;font-size: 0.75em; font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; line-height: 0; color: rgb(46, 46, 46); word-spacing: -1.24453127384186px;&quot;&gt;&amp;minus;&amp;nbsp;1&lt;/sup&gt;&lt;span style=&quot;color: rgb(46, 46, 46); font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; font-size: 16px; line-height: 23.6800003051758px; word-spacing: -1.24453127384186px;&quot;&gt;&amp;nbsp;in Lake Fryxell. Molybdenum concentrations varied between 5.05&amp;nbsp;nmol&amp;nbsp;kg&lt;/span&gt;&lt;sup style=&quot;font-size: 0.75em; font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; line-height: 0; color: rgb(46, 46, 46); word-spacing: -1.24453127384186px;&quot;&gt;&amp;minus;&amp;nbsp;1&lt;/sup&gt;&lt;span style=&quot;color: rgb(46, 46, 46); font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; font-size: 16px; line-height: 23.6800003051758px; word-spacing: -1.24453127384186px;&quot;&gt;&amp;nbsp;and 43&amp;nbsp;nmol&amp;nbsp;kg&lt;/span&gt;&lt;sup style=&quot;font-size: 0.75em; font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; line-height: 0; color: rgb(46, 46, 46); word-spacing: -1.24453127384186px;&quot;&gt;&amp;minus;&amp;nbsp;1&lt;/sup&gt;&lt;span style=&quot;color: rgb(46, 46, 46); font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; font-size: 16px; line-height: 23.6800003051758px; word-spacing: -1.24453127384186px;&quot;&gt;&amp;nbsp;in Lake Hoare, and between 3.52&amp;nbsp;nmol&amp;nbsp;kg&lt;/span&gt;&lt;sup style=&quot;font-size: 0.75em; font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; line-height: 0; color: rgb(46, 46, 46); word-spacing: -1.24453127384186px;&quot;&gt;&amp;minus;&amp;nbsp;1&lt;/sup&gt;&lt;span style=&quot;color: rgb(46, 46, 46); font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; font-size: 16px; line-height: 23.6800003051758px; word-spacing: -1.24453127384186px;&quot;&gt;&amp;nbsp;and 25.5&amp;nbsp;nmol&amp;nbsp;kg&lt;/span&gt;&lt;sup style=&quot;font-size: 0.75em; font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; line-height: 0; color: rgb(46, 46, 46); word-spacing: -1.24453127384186px;&quot;&gt;&amp;minus;&amp;nbsp;1&lt;/sup&gt;&lt;span style=&quot;color: rgb(46, 46, 46); font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; font-size: 16px; line-height: 23.6800003051758px; word-spacing: -1.24453127384186px;&quot;&gt;&amp;nbsp;in Lake Fryxell. Concentrations of As and Mo generally increased with depth in the mixolimnion of each lake, consistent with uptake near the ice&amp;ndash;water interface by organic particles and/or Fe/Mn oxides/oxyhydroxides, followed by gravitational settling and regeneration/remineralization at depth in the vicinity of the redoxcline. Arsenic concentrations either remained constant (Hoare) or increased with depth (Fryxell) in the anoxic monimolimnia, whereas Mo exhibited dramatic decreases in concentrations across the redoxcline in both lakes. Geochemical modeling predicts that As and Mo occur as thioanions in the anoxic bottom waters of Lakes Hoare and Fryxell, and further that the contrasting behavior of both trace elements reflects the respective reactivity of their thioanions towards Fe-sulfide minerals such as mackinawite (FeS) and/or pyrite (FeS&lt;/span&gt;&lt;sub style=&quot;font-size: 0.75em; font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; line-height: 0; color: rgb(46, 46, 46); word-spacing: -1.24453127384186px;&quot;&gt;2&lt;/sub&gt;&lt;span style=&quot;color: rgb(46, 46, 46); font-family: Arial, Helvetica, 'Lucida Sans Unicode', 'Microsoft Sans Serif', 'Segoe UI Symbol', STIXGeneral, 'Cambria Math', 'Arial Unicode MS', sans-serif; font-size: 16px; line-height: 23.6800003051758px; word-spacing: -1.24453127384186px;&quot;&gt;). More specifically, the geochemical model suggests that Fe-sulfide mineral precipitation in the anoxic monimolimnia of both lakes regulates dissolved sulfide concentrations at levels that are too low for As-sulfide minerals (e.g., orpiment, realgar) to precipitate, whereas mackinawite and/or pyrite react(s) with particle reactive thiomolybdate anions, possibly forming an Fe&amp;ndash;Mo&amp;ndash;S mineral that precipitates and, hence, leads to Mo removal from solution.&lt;/span&gt;&lt;/p&gt;</style></abstract><section><style face="normal" font="default" size="100%">110</style></section></record></records></xml>