叠层石
Bhattacharyya距离
火星探测计划
地质学
古生物学
生物
化学
天体生物学
人工智能
计算机科学
有机化学
碳酸盐
作者
Frank A. Corsetti,Michael C. Storrie‐Lombardi
出处
期刊:Astrobiology
[Mary Ann Liebert, Inc.]
日期:2003-12-01
卷期号:3 (4): 649-655
被引量:25
标识
DOI:10.1089/153110703322735980
摘要
It has been underappreciated that inorganic processes can produce stromatolites (laminated macroscopic constructions commonly attributed to microbiological activity), thus calling into question the long-standing use of stromatolites as de facto evidence for ancient life. Using lossless compression on unmagnified reflectance red-green-blue (RGB) images of matched stromatolite-sediment matrix pairs as a complexity metric, the compressibility index (δc, the log of the ratio of the compressibility of the matrix versus the target) of a putative abiotic test stromatolite is significantly less than the δc of a putative biotic test stromatolite. There is a clear separation in δc between the different stromatolites discernible at the outcrop scale. In terms of absolute compressibility, the sediment matrix between the stromatolite columns was low in both cases, the putative abiotic stromatolite was similar to the intracolumnar sediment, and the putative biotic stromatolite was much greater (again discernible at the outcrop scale). We propose that this metric would be useful for evaluating the biogenicity of images obtained by the camera systems available on every Mars surface probe launched to date including Viking, Pathfinder, Beagle, and the two Mars Exploration Rovers.
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