Potential for analysis of carbonaceous matter on Mars using Raman spectroscopy

被引:14
作者
Hutchinson, Ian B. [1 ]
Parnell, John [2 ]
Edwards, Howell G. M. [1 ,3 ]
Jehlicka, Jan [4 ]
Marshall, Craig P. [5 ]
Harris, Liam V. [1 ]
Ingley, Richard [1 ]
机构
[1] Univ Leicester, Space Res Ctr, Dept Phys & Astron, Leicester LE1 7RH, Leics, England
[2] Univ Aberdeen, Kings Coll, Dept Geol & Petr Geol, Aberdeen AB24 3UE, Scotland
[3] Univ Bradford, Sch Life Sci, Ctr Astrobiol & Extremophiles Res, Bradford BD7 1DP, W Yorkshire, England
[4] Charles Univ Prague, Fac Sci, Inst Geochem Mineral & Mineral Resources, Prague 12843 2, Czech Republic
[5] Univ Kansas, Dept Geol, Lawrence, KS 66045 USA
关键词
Raman spectroscopy; Carbonaceous matter; Mars; Planetary exploration; ORGANIC-WALLED MICROFOSSILS; BARBERTON GREENSTONE-BELT; EARTHS EARLIEST FOSSILS; STRUCTURAL-CHARACTERIZATION; EXOMARS MISSION; BETA-CAROTENE; SOUTH-AFRICA; MICRO-RAMAN; APEX CHERT; LIFE;
D O I
10.1016/j.pss.2014.07.006
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The ESA/Roscosmos ExoMars rover will be launched in 2018. The primary aim of the mission will be to find evidence of extinct or extant life by extracting samples from the subsurface of Mars. The rover will incorporate a drill that is capable of extracting cores from depths of up to 2 m, a Sample Preparation and Distribution System (SPDS) that will crush the core into small grains and a suite of analytical instruments. A key component of the analytical suite will be the Raman Laser Spectrometer (RLS) that will be used to probe the molecular and mineralogical composition of the samples. In this work we consider the capability of the proposed Raman spectrometer to detect reduced carbon (possibly associated with evidence for extinct life) and to identify the level of thermal alteration/maturity. The Raman analysis of 21 natural samples of shale (originating from regions exhibiting different levels of thermal maturity) is described and it is shown that reduced carbon levels as low as 0.08% can be readily detected. It is also demonstrated that the Raman spectra obtained with the instrument can be used to distinguish between samples exhibiting high and low levels of thermal maturity and that reduced carbon can be detected in samples exposed to significant levels of oxidation (as expected on the surface of Mars). (C) 2014 Published by Elsevier Ltd.
引用
收藏
页码:184 / 190
页数:7
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