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

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• 作者：Motoko Igisu ; Tsuyoshi Komiya ; Mika Kawashima ; Satoru Nakashima ; Yuichiro Ueno ; Jian Han ; Degan Shu ; Yong Li ; Junfeng Guo ; Shigenori Maruyama ; Ken Takai
• 关键词：Embryo-like fossil ; Algal fossils ; Doushantuo Formation ; Micro-FTIR ; Aliphatic hydrocarbon
• 刊名：Gondwana Research
• 出版年：April, 2014
• 年：2014
• 卷：25
• 期：3
• 页码：1120-1138
• 全文大小：4569 K

文摘

Phosphatized microfossils from ca. 580 Ma from the Doushantuo Formation in the Weng'an region of South China were analyzed by Fourier transform infrared (FTIR) 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^鈭?#xA0;1 and 2925 cm^鈭?#xA0;1, indicating the presence of aliphatic hydrocarbon (anti-symmetric aliphatic CH₃ and aliphatic CH₂), and have an additional band of around 1595 cm^鈭?#xA0;1, probably derived from aromatic moieties (aromatic CC). 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 CC/CH₂ peak height ratios (R_CC/2 values): (1) high-R_3/2/low-R_CC/2 type (R_3/2 = ~ 0.2-1.0 and R_CC/2 ~ 0-2), (2) low-R_3/2/medium-R_CC/2 type (R_3/2 = ~ 0.2-0.6 and R_CC/2 = ~ 1-4); and (3) low-R_3/2/high-R_CC/2 type (R_3/2 = ~ 0.2-0.6 and R_CC/2 ~ 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_CC/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.