High Carbonate Alkalinity Lakes on Mars and their Potential Role in an Origin of Life Beyond Earth

Author:

Hurowitz Joel A.1,Catling David C.2,Fischer Woodward W.3

Affiliation:

1. Department of Geosciences, Stony Brook University, Stony Brook, NY 11794, USA

2. Department of Earth and Space Sciences, University of Washington, Seattle, WA 98185, USA

3. Division of Geological & Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA

Abstract

The exploration of Mars has revealed that its ancient surface hosted lakes with a dazzling array of chemical and physical conditions and processes. The potential habitability of surface waters has driven studies aimed at understanding whether or not Mars once hosted life. High levels of atmospheric carbon dioxide are probable on early Mars, which means that lakes derived from weathering fluids could have contained substantial carbonate alkalinity. Recent studies show that lakes with high carbonate alkalinity are able to concentrate the phosphate and cyanide that are critical for molecular synthesis in the origin of life. While evidence for carbonate-rich Martian lakes remains limited, NASA’s Perseverance rover may reveal clues about the past existence of such waters in Jezero Crater.

Publisher

Mineralogical Society of America

Subject

Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology

Reference30 articles.

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