Mineral crusts and mold holes in Martian rocks: Evidence of microbes on ancient Mars
Hong-Xia Jiang1, Ya-Sheng Wu2,3*, Li-Jing Liu4, Gong-Liang Yu5, Xiao-Qun Yang6
1Hebei Key Laboratory of Strategic Critical Mineral Resources, Hebei GEO University, Shijiazhuang 050031, China. jianghx@hgu.edu.cn
2University of Chinese Academy of Sciences, Beijing 100049, China.
3Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China. wys@mail.igcas.ac.cn
4State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, 710069, Xi’an, China. liulijing@nwu.edu.cn
5Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan 430072, Hubei Province, China. yugl@ihb.ac.cn
6Sinopec Petroleum Exploration and Production Research Institute, Beijing 100083, China. yangxq873.syky@sinopec.com
*corresponding author: wys@mail.igcas.ac.cn.
Abstract
Experimental studies and observations of modern microbialites in natural environments indicate that the metabolic action of some microbes can cause minerals to precipitate on their surface and form crusts enclosing the microbes. The holes left by degradation of died microbes are called mold holes. Mineral crusts and mold holes are widespread in present and ancient microbial rocks on Earth and are evidence of once presence of microbes. Structures similar to Earth’s fossils and stromatolites and organic compounds have been found in previous studies on the photographs of Martian rocks taken by the Perseverance rover, suggesting that the Mars may have supported life. Based on an analysis of the photos by NASA's Perseverance rover in July 2022, of two drilling cores and a circular abraded surface at the Jezero crater area of Mars, this paper reports that the Martian rocks have dense mineral crusts and mold holes, suggesting that they were formed by microbial-induced precipitation, confirming the once presence of microbial communities on ancient Mars. Based on the size of the mold holes, the microbes that formed the rocks are probably cyanobacteria.
Key words: Mars, life, mineral crust, mold hole, microbialites, biolith, microbiolith
Cite it as: Jiang, H.X., Wu, Y.S., Liu, L.J., Yu, G.L., Yang, X.Q. 2024. Mineral crusts and mold holes in Martian rocks: Evidence of microbes on ancient Mars. Biopetrology, 4(1): 1-9. https://biopetrology.com/upload/mcamhi.pdf