4.7 Article

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

Journal

GONDWANA RESEARCH
Volume 25, Issue 3, Pages 1120-1138

Publisher

ELSEVIER
DOI: 10.1016/j.gr.2013.05.002

Keywords

Embryo-like fossil; Algal fossils; Doushantuo Formation; Micro-MR; Aliphatic hydrocarbon

Funding

  1. Tokyo Institute of Technology
  2. Ministry of Education, Culture, Sports, Technology and Science, Japan
  3. MEXT KAKENHI [22740351]
  4. Research Fellowship of Japan Society for the Promotion of Science for Young Scientists
  5. Multistep evolution of the Metazoa [23340152]
  6. Mitsubishi Foundation
  7. 21st Century COE program 'How to build habitable planets'
  8. Grants-in-Aid for Scientific Research [12J07955, 26106002, 22740351] Funding Source: KAKEN

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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.

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