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Microbial and molecular fossils from the Permian Zoophycos in South China 被引量:6

Microbial and molecular fossils from the Permian Zoophycos in South China
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摘要 The trace fossil Zoophycos was enriched in the lower part of the Guadalupian Maokou Formation of Permian in Laibin, Guangxi of South China, and characterized by observable lamellae within its spreiten. Associated with these lamellae are the prolific coccus- and spirillum-shaped microbe fossils. These microbes morphologically identified are 0.4―3.0 μm in diameter or length. Molecular fossils, including normal alkanes (dominated by C18, without an odd-over-even predominance), acyclic isoprenoids (such as pristane (Pr) and phytane (Ph)), extended tricyclic terpanes, pentacyclic triterpanes, steranes, al-kylcyclohexanes, dibenzothiophenes, benzonaphthothiophenes, benzobisbenzothiophenes, were in-strumentally identified in the wackestone characterized by the occurrence of abundant Zoophycos (composite ichnofabric indices are 4) and crowded microbial fossils. The value of the Pr/Ph ratio is less than 1, indicative of a dysoxic condition. The identification of abundant sulfur compounds (the thio-phene series) related to the contribution of reductive sulfur favors the occurrence of sulphate-reducing bacteria. The association of abundant microbial colonies with microbial molecular fossils within the spreiten suggests that trace fossils Zoophycos would be a multifunctional garden carefully constructed by the Zoophycos-producer, where different microbial colonies were orderly and carefully planted and cultured in different minor lamellae within spreiten. Hence, it is proposed that the Zoophycos-producer symbiosed with microbial colonies on the mutual basis of food supply and the redox conditions. The trace fossil Zoophycos was enriched in the lower part of the Guadalupian Maokou Formation of Permian in Laibin, Guangxi of South China, and characterized by observable lamellae within its spreiten. Associated with these lamellae are the prolific coccus- and spirillum-shaped microbe fossils. These microbes morphologically identified are 0.4–3.0 μm in diameter or length. Molecular fossils, including normal alkanes (dominated by C18, without an odd-over-even predominance), acyclic isoprenoids (such as pristane (Pr) and phytane (Ph)), extended tricyclic terpanes, pentacyclic triterpanes, steranes, alkylcyclohexanes, dibenzothiophenes, benzonaphthothiophenes, benzobisbenzothiophenes, were instrumentally identified in the wackestone characterized by the occurrence of abundant Zoophycos (composite ichnofabric indices are 4) and crowded microbial fossils. The value of the Pr/Ph ratio is less than 1, indicative of a dysoxic condition. The identification of abundant sulfur compounds (the thiophene series) related to the contribution of reductive sulfur favors the occurrence of sulphate-reducing bacteria. The association of abundant microbial colonies with microbial molecular fossils within the spreiten suggests that trace fossils Zoophycos would be a multifunctional garden carefully constructed by the Zoophycos-producer, where different microbial colonies were orderly and carefully planted and cultured in different minor lamellae within spreiten. Hence, it is proposed that the Zoophycos-producer symbiosed with microbial colonies on the mutual basis of food supply and the redox conditions.
出处 《Science China Earth Sciences》 SCIE EI CAS 2007年第8期1121-1127,共7页 中国科学(地球科学英文版)
基金 the Special Project of Basic Research of China (Grant No. 2005CCA05000) the National Natural Science Foundation of China (Grant Nos. 40472020, 40621002 and 40525008) the Research Fund for the Doctoral Program of Higher Education of China (Grant No. 2004000127) other projects (Grant Nos. IRT0546 and G0800-06-ZS-319)
关键词 TRACE FOSSILS ZOOPHYCOS microbes molecular FOSSILS PERMIAN South China trace fossils Zoophycos microbes molecular fossils Permian South China
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  • 1GONG Yiming, XU Ran, TANG Zhongdao & LI Baohua Faculty of Earth Science, China University of Geosciences, Wuhan 430074, China,Laboratory of Marine Geology, Tongji University, Shanghai 200092, China.The Upper Devonian orbital cyclostratigraphy and numerical dating conodont zones from Guangxi,South China[J].Science China Earth Sciences,2005,48(1):32-41. 被引量:15
  • 2GONG Yiming,LI Baohua,SI Yuanlan,WU Yi.Late Devonian red tide and mass extinction[J].Chinese Science Bulletin,2002,47(13):1138-1144. 被引量:14
  • 3Hinrichs K U. A molecular recorder of methane hydrate destabilization[J]. Geochemistry Geophysics Geosystems,2001, 2(1):2000GC0001 118.
  • 4Rohmer M, Bouvier-Nave P, Ourisson G. Distribution of hopanoid triterpenes in prokaryotes [J].Journal of General Microbiology, 1984, 130:1 137-1 150.
  • 5Hinrichs K U, Hmelo L, Sylva S P. Molecular fossils record of elevated methane levels in late Pleistocene coastal waters[J].Science, 2003, 229:1 214-1 217.
  • 6Summons R E, Powell T G. Chlorobiaceae in Palaeozoic seas revealed by biological markers, isotopes and geology [J].Nature, 1986, 319:763-765.
  • 7Summons R E, Powell T G. Identification of aryl isoprenoids in source rocks and crude oils: Biological markers for the green sulphur bacteria[J]. Geochimica et Cosmochimica Acta,1987, 51:557-566.
  • 8Yu K, Fan P, Philp R P. Novel biomarkers found in South Florida basin [J].Organic Geochemistry, 1990, 15:433-438.
  • 9Grice K, Schaeffer P, Schwark L, et al. Changes in palaeoenvironmental conditions during deposition of Permian Kupferschiefer (Lower Rhine Basin, northwest Germany) inferred from molecular and isotopic compositions of biomarker components[J].Organic Geochemistry, 1997, 26: 677-690.
  • 10Sinninghe D J S, Kock-van D A C, de Leeuw J W. Identification of long-chain isoprenoid alkylbenzenes in sediments and crude oils [J].Geochimica et Cosmochimica Acta, 1988, 52:2 671-2 677.

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