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Raman and FTIR spectroscopy of natural oxalates: Implications for the evidence of life on Mars
作者姓名:R.L.Frost  YANGJing  ZheDing
作者单位:[1]InorganicMaterialsResearchProgram,QueenslandUniversityofTechnology,2GeorgeStreet,Brisbane,GPOBox2434,Queensland4001,Australia; [2]SchoolofMaterials,ChinaUniversityofGeosciences,Beijing100083,China
摘    要:Evidence for the existence of primitive life forms such as lichens and fungi can be based upon the formarion of oxalates. Oxalates are most readily detected using Raman spectroscopy. A comparative study of a suite of natural oxalates including weddellite, whewellite, moolooite,humboldtine, glushinskite, natroxalate and oxammite has been undertaken using Raman spectroscopy. The minerals are characterised by the Raman position of the CO stretching vibration which is cation sensitive. The band is observed at 1468 cm^-1 for weddellite, 1489 cm^-1 for moolooite, 1471cm^-1 for glushinskite and 1456 cm^-1 for natroxalate. Except for oxammite, the infrared and Raman spectra are mutually exclusive indicating the minerals are bidentate. Differences are also observed in the water OH stretching bands of the minerals. The significance of this work rests with the ability of Raman spectroscopy to identify oxalates which often occur as a film on a host rock. As such Raman spectroscopy has the potential to identify the existence or pre-existence of life forms on planets such as Mars.

关 键 词:火星  地外生命  草酸盐  草酸铵石  草酸镁石  拉曼光谱学  傅里叶变换红外光谱学
收稿时间:2003-03-28
修稿时间:2003-05-02

Raman and FTIR spectroscopy of natural oxalates: Implications for the evidence of life on Mars
R.L.Frost YANGJing ZheDing.Raman and FTIR spectroscopy of natural oxalates: Implications for the evidence of life on Mars[J].Chinese Science Bulletin,2003,48(17):1844-1852.
Authors:Frost  R L  Yang  Jing  Ding  Zhe
Institution:R. L. Frost1, YANG Jing2 & Zhe Ding1 1. Inorganic Materials Research Program, Queensland University of Technology, 2 George Street, Brisbane, GPO Box 2434, Queensland 4001, Australia; 2. School of Materials, China University of Geosciences, Beijing 100083, China
Abstract:Evidence for the existence of primitive life forms such as lichens and fungi can be based upon the for-mation of oxalates. Oxalates are most readily detected using Raman spectroscopy. A comparative study of a suite of natural oxalates including weddellite, whewellite, moolooite, humboldtine, glushinskite, natroxalate and oxammite has been undertaken using Raman spectroscopy. The minerals are characterised by the Raman position of the CO stretch-ing vibration which is cation sensitive. The band is observed at 1468 cm-1 for weddellite, 1489 cm-1 for moolooite, 1471 cm-1 for glushinskite and 1456 cm-1 for natroxalate. Except for oxammite, the infrared and Raman spectra are mutually exclusive indicating the minerals are bidentate. Differences are also observed in the water OH stretching bands of the minerals. The significance of this work rests with the ability of Raman spectroscopy to identify oxalates which often occur as a film on a host rock. As such Raman spectroscopy has the potential to identify the existence or pre-existence of life forms on planets such as Mars.
Keywords:oxalate  weddellite  moolooite  humboldtine  natroxalate  oxammite  glushinskite  
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