Arsenic speciation in Mono Lake, California: Response to seasonal stratification and anoxia

• Published in: Geochimica et cosmochimica acta Vol. 69; no. 8; pp. 1925 - 1937
• Main Authors: Hollibaugh, James T., Carini, Steve, Gürleyük, Hakan, Jellison, Robert, Joye, Samantha B., LeCleir, Gary, Meile, Christof, Vasquez, Lydia, Wallschläger, Dirk
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 15.04.2005
• Subjects: USA, California, Mono L; USA, Great Basin; USA, California
• ISSN: 0016-7037; 1872-9533
• DOI: 10.1016/j.gca.2004.10.011

Mono Lake is a closed-basin, alkaline, hypersaline lake located at the western edge of the Great Basin in eastern California. We studied the distribution of arsenic (As) species in the water column of Mono Lake between February and November, 2002. This period captured the seasonal progression from winter mixing, through summer thermal stratification, to autumn overturn. Arsenic speciation was determined by ion chromatography-inductively coupled-plasma-mass spectrometry of samples preserved in the field by flash-freezing in liquid nitrogen. We found that arsenic speciation was dominated (>90%) by arsenate when oxygen was detectable. Once levels fell below 6 μmol/L O 2, arsenic speciation shifted to dominance by reduced species. Arsenate and arsenite co-occurred in a transition zone immediately below the base of the oxycline and low but significant concentrations of arsenate were occasionally detected in sulfidic hypolimnion samples. Thio-arsenic species were the dominant form of As found in sulfidic waters. Maxima of thio-arsenic species with stoichiometries consistent with mono-, di- and trithio-arsenic occurred in succession as sulfide concentration increased. A compound with a stoichiometry consistent with trithio-arsenic was the dominant As species (∼50% of total As) in high sulfide (2 mmol/L) bottom water. Lower concentrations of total As in bottom water relative to surface water suggest precipitation of As/S mineral phases in response to sulfide accumulation during prolonged anoxia.