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• W4308491286 endingPage "115342" @default.
• W4308491286 startingPage "115342" @default.
• W4308491286 abstract "The Meridiani Planum region on Mars has extensive sulfate-rich sedimentary deposits (∼20 wt% SO42−) that are hypothesized to have formed from regional groundwater upwelling that led to the precipitation of secondary Fe-, Mg-, Ca-sulfate minerals and cementation of basaltic sediments. However, the primary source of sulfur (S) for these abundant secondary sulfate minerals is unclear. Therefore, in this study the contributions of volcanic S via surface water and groundwater were investigated in the terrestrial basaltic analogs of Hawaii and Iceland to determine the importance of active volcanism and climate on S cycling as well as the resulting timescale of aqueous activity in the Meridiani Planum region. SO42− fluxes (contributions) were calculated in metric tons/yr using historical data from online repositories and normalized to the catchment area to determine the SO42− load in metric tons/yr/km2. Our results show that the SO42− load is greatly affected by climate, typically ranging from ∼7.3 to 170 metric tons/yr/km2 under wetter conditions and ∼ 2.6 to 43 metric tons/yr/km2 under dry conditions. Active S degassing and accompanying S-rich mineralization from current hydrothermal activity greatly increased the SO42− loads (∼2.8 to 170 metric tons/yr/km2) compared to non-active catchments (2.6 to 13 metric tons/yr/km2). Younger basaltic bedrock with greater permeability and groundwater-rock interactions was also found to be important, resulting in higher SO42− loads (∼26 to 170 metric tons/yr/km2) compared to older, less permeable catchments (∼2.6 to 12 metric tons/yr/km2). Based on these terrestrial SO42− loads in Hawaii and Iceland, we calculated a range of possible loads and timescales of SO42− transport in Meridiani Planum under variable environmental conditions. Results show that the smallest SO42− loads and longest timescales would occur in Meridiani under dry, non-volcanically active conditions, typically requiring ∼16 to 65 Ma of an active aqueous system, as in the older catchments of Hawaii and Iceland. Conversely, the largest SO42− fluxes and shortest timescales would occur under wet, volcanically active conditions, requiring ∼1.0 to 6.9 Ma, as in the younger catchments of Hawaii and Iceland. Our results suggest that moderately wet conditions with some active hydrothermal S input would be needed to transport and deposit the equivalent mass of SO42− currently present in the sulfate-rich deposits of Meridiani Planum." @default.
• W4308491286 created "2022-11-12" @default.
• W4308491286 creator A5023512946 @default.
• W4308491286 creator A5025388105 @default.
• W4308491286 date "2023-02-01" @default.
• W4308491286 modified "2023-09-26" @default.
• W4308491286 title "Aqueous sulfate contributions in terrestrial basaltic catchments: Implications for understanding sulfate sources and transport in Meridiani Planum, Mars" @default.
• W4308491286 cites W1967942093 @default.
• W4308491286 cites W1968326025 @default.
• W4308491286 cites W1976011994 @default.
• W4308491286 cites W1978452162 @default.
• W4308491286 cites W1978518981 @default.
• W4308491286 cites W1979138369 @default.
• W4308491286 cites W1981061458 @default.
• W4308491286 cites W1981098344 @default.
• W4308491286 cites W1986859129 @default.
• W4308491286 cites W1995098015 @default.
• W4308491286 cites W1995122722 @default.
• W4308491286 cites W1996098826 @default.
• W4308491286 cites W1996830410 @default.
• W4308491286 cites W1997369152 @default.
• W4308491286 cites W2000179986 @default.
• W4308491286 cites W2002100043 @default.
• W4308491286 cites W2003153757 @default.
• W4308491286 cites W2003548976 @default.
• W4308491286 cites W2004013850 @default.
• W4308491286 cites W2005609972 @default.
• W4308491286 cites W2006657345 @default.
• W4308491286 cites W2008913098 @default.
• W4308491286 cites W2008926625 @default.
• W4308491286 cites W2011753735 @default.
• W4308491286 cites W2017348906 @default.
• W4308491286 cites W2018287068 @default.
• W4308491286 cites W2020107146 @default.
• W4308491286 cites W2022074935 @default.
• W4308491286 cites W2028016258 @default.
• W4308491286 cites W2028052484 @default.
• W4308491286 cites W2031445615 @default.
• W4308491286 cites W2032975370 @default.
• W4308491286 cites W2036026278 @default.
• W4308491286 cites W2037676155 @default.
• W4308491286 cites W2042830459 @default.
• W4308491286 cites W2044160398 @default.
• W4308491286 cites W2046944925 @default.
• W4308491286 cites W2051830721 @default.
• W4308491286 cites W2053412041 @default.
• W4308491286 cites W2053544177 @default.
• W4308491286 cites W2053653952 @default.
• W4308491286 cites W2055545854 @default.
• W4308491286 cites W2056139793 @default.
• W4308491286 cites W2057324854 @default.
• W4308491286 cites W2060123769 @default.
• W4308491286 cites W2060393110 @default.
• W4308491286 cites W2064811573 @default.
• W4308491286 cites W2066308693 @default.
• W4308491286 cites W2067703344 @default.
• W4308491286 cites W2071304901 @default.
• W4308491286 cites W2074004502 @default.
• W4308491286 cites W2074333960 @default.
• W4308491286 cites W2075652315 @default.
• W4308491286 cites W2078066621 @default.
• W4308491286 cites W2078938542 @default.
• W4308491286 cites W2081130960 @default.
• W4308491286 cites W2082203753 @default.
• W4308491286 cites W2082544810 @default.
• W4308491286 cites W2090865634 @default.
• W4308491286 cites W2099507384 @default.
• W4308491286 cites W2101433261 @default.
• W4308491286 cites W2102090896 @default.
• W4308491286 cites W2102920959 @default.
• W4308491286 cites W2103526828 @default.
• W4308491286 cites W2117104744 @default.
• W4308491286 cites W2117325609 @default.
• W4308491286 cites W2121006557 @default.
• W4308491286 cites W2125599253 @default.
• W4308491286 cites W2129281798 @default.
• W4308491286 cites W2133286479 @default.
• W4308491286 cites W2133623351 @default.
• W4308491286 cites W2143047176 @default.
• W4308491286 cites W2156470002 @default.
• W4308491286 cites W2169233615 @default.
• W4308491286 cites W2171242011 @default.
• W4308491286 cites W2322387302 @default.
• W4308491286 cites W2365143092 @default.
• W4308491286 cites W2416641870 @default.
• W4308491286 cites W2472883030 @default.
• W4308491286 cites W2517154379 @default.
• W4308491286 cites W2526353906 @default.
• W4308491286 cites W2553459211 @default.
• W4308491286 cites W2569498280 @default.
• W4308491286 cites W2586433278 @default.
• W4308491286 cites W2606268793 @default.
• W4308491286 cites W2726834852 @default.
• W4308491286 cites W2794174579 @default.
• W4308491286 cites W2800067198 @default.
• W4308491286 cites W2900656041 @default.
• W4308491286 cites W2908459647 @default.
• W4308491286 cites W2982200312 @default.

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