FTIR microspectroscopy of Ediacaran phosphatized microfossils from the Doushantuo Formation, Weng'an, South China

被引:21
|
作者
Igisu, Motoko [1 ,2 ]
Komiya, Tsuyoshi [1 ]
Kawashima, Mika [3 ]
Nakashima, Satoru [3 ]
Ueno, Yuichiro [4 ,5 ]
Han, Jian [6 ,7 ]
Shu, Degan [6 ,7 ]
Li, Yong [8 ]
Guo, Junfeng [8 ]
Maruyama, Shigenori [4 ,5 ]
Takai, Ken [2 ,5 ,9 ]
机构
[1] Univ Tokyo, Dept Earth Sci & Astron, Meguro Ku, Tokyo 1538902, Japan
[2] Japan Agcy Marine Earth Sci & Technol JAMSTEC, Precambrian Ecosyst Lab, Yokosuka, Kanagawa 2370061, Japan
[3] Osaka Univ, Dept Earth & Space Sci, Toyonaka, Osaka 5600043, Japan
[4] Tokyo Inst Technol, Dept Earth & Planetary Sci, Meguro Ku, Tokyo 1528551, Japan
[5] Tokyo Inst Technol, Earth Life Sci Inst, Tokyo 1528551, Japan
[6] Northwest Univ, Dept Geol, Xian 710069, Peoples R China
[7] Northwest Univ, Key Lab Continental Dynam, Xian 710069, Peoples R China
[8] Changan Univ, Sch Earth Sci & Resources Management, Xran 710054, Peoples R China
[9] Japan Agcy Marine Earth Sci & Technol JAMSTEC, Subsurface Geobiol Adv Res SUGAR Project, Yokosuka, Kanagawa 2370061, Japan
基金
日本学术振兴会;
关键词
Embryo-like fossil; Algal fossils; Doushantuo Formation; Micro-MR; Aliphatic hydrocarbon; MICRO-RAMAN SPECTROSCOPY; GIANT SULFUR BACTERIA; ANIMAL EMBRYOS; LASER-RAMAN; CARBONACEOUS MATERIAL; FOSSILIZED NUCLEI; INFRARED MICROSPECTROSCOPY; EXPERIMENTAL TAPHONOMY; WATER DISTRIBUTION; METAMORPHIC ROCKS;
D O I
10.1016/j.gr.2013.05.002
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Phosphatized microfossils from ca. 580 Ma from the Doushantuo Formation in the Weng'an region of South China were analyzed by Fourier transform infrared (FOR) microspectroscopy for their chemical characterization. Two morpho-types of phosphatized embryo-like fossils (Megasphaera and Megaclonophycus) were analyzed, together with algal fossils. Transmission IR spectra of the microfossils have absorption bands of around 2960 cm(-1) and 2925 cm(-1), indicating the presence of aliphatic hydrocarbon (anti-symmetric aliphatic CH3 and aliphatic CH2), and have an additional band of around 1595 cm(-1), probably derived from aromatic moieties (aromatic C=C). In addition, IR microscopic mapping shows that aliphatic hydrocarbon and aromatics are distributed inside the embryo-like fossils. The embryo-like fossils appear to show three types of CH3/CH2 peak height ratios (R-3/2) and aromatic C=C/CH2 peak height ratios (R-C=C/2 values): (1) high-R-3/2/low-R-C=C/2 type (R-3/2 = similar to 02-1.0 and R-C=C/2 similar to 0-2), (2) low-R-3/2/medium-R-C=C/2 type (R-3/2 = similar to 0.2-0.6 and R-C=C/2 = similar to 1-4); and (3) low-R-3/2/high-R-C=C/2 type (R-3/2 = similar to 02-0.6 and R-C=C/2 similar to 1-8). All three types are contained in both Megasphaera and Megaclonophycus. Raman spectra for the carbonaceous matter within the rock sample show a similar degree of thermal alteration, indicating that the organics were embedded in situ prior to thermal maturation. The IR spectroscopic differences might reflect differences in original organic compositions of microorganisms, and/or immediate post-mortem alteration. This suggests that the origins of phosphatized embryo-like fossils are more diverse than was previously recognized on the basis of their morphology. A comparison of R-3/2 and R-C=C/2 values in the embryo-like fossils with those of the algal fossils and the extant microorganisms indicates the possible interpretation that some of the embryo-like fossils belong to animal embryo, others are algae, but none of them originate from bacteria. (C) 2013 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:1120 / 1138
页数:19
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