地球微生物过程与潜在烃源岩的形成: 钙质微生物岩

杨浩; 王永标; 陈林; 董曼

Volume 32 Issue 6

Jun. 2007

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Article Navigation > Earth Science > 2007 > 32(6): 797-802

YANG Hao, WANG Yong-biao, CHEN Lin, DONG Man, 2007. Calci-Microbialite as a Kind of Potential Hydrocarbon Source Rock and Its Geomicrobiological Processes. Earth Science, 32(6): 797-802.

Citation:

YANG Hao, WANG Yong-biao, CHEN Lin, DONG Man, 2007. Calci-Microbialite as a Kind of Potential Hydrocarbon Source Rock and Its Geomicrobiological Processes. Earth Science, 32(6): 797-802.

YANG Hao, WANG Yong-biao, CHEN Lin, DONG Man, 2007. Calci-Microbialite as a Kind of Potential Hydrocarbon Source Rock and Its Geomicrobiological Processes. Earth Science, 32(6): 797-802.

Citation:

YANG Hao, WANG Yong-biao, CHEN Lin, DONG Man, 2007. Calci-Microbialite as a Kind of Potential Hydrocarbon Source Rock and Its Geomicrobiological Processes. Earth Science, 32(6): 797-802.

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Calci-Microbialite as a Kind of Potential Hydrocarbon Source Rock and Its Geomicrobiological Processes

1.
Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
The Center of Paleontology and Stratigraphy, Jilin University, Changchun 130026, China

Received Date: 2007-08-23
Publish Date: 2007-11-25

Abstract

Abstract

Calci-microbialite is a special carbonate buildup, formed due to the activities of different kinds of microbes. Most of microbialites were developed in Precambrian or at the great transitional stages in Phanerozoic. Widespread microbialites have been found both in North and South China. Abundant microfossils preserved in the microbialites show high-level productivity during deposition. The obviously lower value of Mo isotope shows that the seafloor is of anoxic condition during the long time of Precambrian. The sharp reduction of Th/U value as well as the wide spread pyrite in shallow carbonate platforms indicate that the ocean environment is anoxic after end-Permian mass extinction. High-level productivity and anoxic sedimentary environment favor the efficient preservation of organic matter and thus the formation of source rocks. Bitumen observed in many outcrops of Precambrian and Late Devonian microbialites further raises the possibility of calci-microbialite as a potential hydrocarbon source rock.
- calci-microbialite,
- potential hydrocarbon source rock,
- geomicrobes

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References

Arnold, G. L., Anbar, A. D., Barling, J., et al., 2004. Molyb-denum isotope evidence for widespread anoxia in mid-Proterozoic oceans. Science, 304 (5667): 87-90. doi: 10.1126/science.1091785
Baud, A., Cirilli, S., Marcoux, J., 1997. Biotic response to mass extinction: The lowermost Triassic microbialites. Facies, 36: 238-242.
Baud, A., Richoz, S., Marcoux, J., 2005. Calci microbial caprocks from the basal Triassic units of the Taurus (SW Turkey), an anachronistic facies before the biotic recov-ery. Comptes Rendus. Palevol. , 4 (6-7): 569-582. doi: 10.1016/j.crpv.2005.03.001
Baud, A., Richoz, S., Pruss, S. B., 2007. The lower Triassic anachronistic carbonate facies in space and time. Globaland Planetary Change, 55 (1-3): 81-89. doi: 10.1016/j.gloplacha.2006.06.008
Burne, R. V., Moore, I. S., 1987. Microbialites: Organosedi-mentary deposits of benthic microbial communities. Palaios, 2 (3): 241-254. doi: 10.2307/3514674
Cao, R. J., Yuan, X. L., 2003. Brief history and current status of stromatolite study in China. Acta Micropalaeontologica Sinica, 20 (1): 5-14 (in Chinese with English abstract).
Chen, J. B., 1993. Progress and problems in research on stro-matolites. In: Zhu, S. X., et al., eds., The stromatolites of China. Tianjin Univ. Press, Tianjin, 205-214 (in Chinese with English abstract).
Dai, Y. D., Chen, M. E., Wang, Y., 1996. Development and per-spective of research for microbialites. Advances in Earth Sci-ence, 11 (2): 209-215 (in Chinese with English abstract).
Dupraz, C., Visscher, P. T., Baumgartner, L. K., et al., 2004. Microbe-mineral interactions: Early carbonate precipitation in a hypersaline lake (Eleuthera Island, Ba-hamas). Sedimentology, 51: 745-765. doi: 10.1111/j.1365-3091.2004.00649.x
Heydari, E., Hassanzadeh, J., Wade, W. J., et al., 2003. Per-mian-Triassic boundary interval in the Abadeh section of Iran with implications for mass extinction: Part 1. Sedimentology. Palaeogeography, Palaeoclimatology, Palaeoecology, 193 (3-4): 405-423. doi: 10.1016/S0031-0182(03)00258-X
Hips, K., Haas, J., 2006. Calcimicrobial stromatolites at the Permian-Triassic boundary in a western Tethyan sec-tion, Bükk Mountains, Hungary. Sedimentary Geology, 185: 239-253. doi: 10.1016/j.sedgeo.2005.12.016
Kershaw, S., Zhang, J., Lan, G., 1999. A microbialite carbonate crust at the Permian-Triassic boundary in South China, and its palaeoenvironmental significance. Palaeogeography, Palaeoclimatology, Palaeoecology, 146: 1-18. doi: 10.1016/S0031-0182(98)00139-4
Konishi, Y., Prince, J., Knott, B., 2001. The fauna of throm-bolitic microbialites, Lake Clifton, Western Australia. Hydrobiologia, 457 (1-3): 39-47.
Lehrmann, D. J., 1999. Early Triassic calcimicrobial mounds and biostromes of the Nanpanjiang basin, South China. Geology, 27 (4): 359-362. doi: 10.1130/0091-7613(1999)027<0359:ETCMAB>2.3.CO;2
Li, Y. C., Zhou, Z. Z., 2002. Massive dissociation of gas hydrateduring oceanic anoxia as a cause of mass extinction at the end of Permian. Geology Geochemistry, 30 (1): 57-63 (inChinese with English abstract).
Liang, Y. Z., Cao, R. J., Zhang, L. Y., et al., 1984. Pseud-ogymnosolenaceae of Late Precambrian in China. Geo-logical Publishing House, Beijing, 1-200 (in Chinese).
Liang, Y. Z., Wang, Y., Du, R. L., 1993. Structural deformation of microstromatolite in the Bayan Obo Group of Inner Mongolia and its geological significance. Geological Bulletin of China, 3: 229-238 (in Chinese with English abstract).
Liang, Y. Z., Zhu, S. X., Gao, Z. J., et al., 1995. New progress in the study of stratomalites—microbialite. Regional Geology of China, 1: 57-65 (in Chinese with English abstract).
Marcoux, J., Baud, A., 1986. The Permo-Triassic boundary in the Antalya nappes (western Taurides, Turkey). Me-moria della Societa Geologica Italiana, 34: 243-252.
Qiu, S. Y., Liang, Y. Z., Cao, R. J., et al., 1992. Late Pre-cambrian stromatolites and related mineral product. Northwest University Press, Xi′an (in Chinese).
Riding, R., Liang, L. Y., 2005. Geobiology of microbial carbon-ates: Metazoan and seawater saturation state influences onsecular trends during the Phanerozoic. Palaeogeography, Palaeoclimatology, Palaeoecology, 219: 101-115. doi: 10.1016/j.palaeo.2004.11.018
Sano, H., Nakashima, K., 1997. Lowermost Triassic (Gries-bachian) microbial bindstone-cementstone, Southwest Japan. Facies, 36: 1-24. doi: 10.1007/BF02536874
Sheehan, P. M., Harris, M. T., 2004. Microbialite resurgence af-ter the Late Ordovician extinction. Nature, 430: 75-78. doi: 10.1038/nature02654
Shen, J. W., Webb, G. E., 2004a. Famennian (Upper Devoni-an) calcimicrobial (Renalcis) reef at Miaomen, Guilin, Guangxi, South China. Palaeogeography, Palaeoclima-tology, Palaeoecology, 204: 373-394. doi: 10.1016/S0031-0182(03)00737-5
Shen, J. W., Webb, G. E., 2004b. Famennian (Upper Devonian) stromatolite reefs at Shatang, Guilin, Guangxi, South Chi-na. Sedimentary Geology, 170 (1-2): 63-84. doi: 10.1016/j.sedgeo.2004.06.004
[84]	Walter, M. R., 1994. Stromatolites: The main geological source of information on the evolution of early benthos. In: Bengtson, S., ed., Early life on earth. Columbia U. P., New York, 270-286.
Wang, Y. B., Tong, J. N., Wang, J. S., et al., 2005. Calcimicrobialite after end-Permian mass extinctionin South China and its palaeoenvir-onmental significance. Chinese Science Bulletin, 50: 665-671. doi: 10.1360/982004-323
Wignall, P. B., Twitchett, R. J., 1996. Oceanic anoxia and the end Permian mass extinction. Science, 272: 1155-1158. doi: 10.1126/science.272.5265.1155
Wignall, P. B., Twitchett, R. J., 1999. Unusual intraclastic limestones in Lower Triassic carbonates and their bear-ing on the aftermath of the end-Permian mass extinc-tion. Sedimentology, 46 (2): 303-316. doi: 10.1046/j.1365-3091.1999.00214.x
Wignall, P. B., Twitchett, R. J., 2002. Permian-Triassic sedi-mentology of Jameson Land, East Greenland: Incised submarine channels in an anoxic basin. Journal of the Geological Society, 159: 691-703. doi: 10.1144/0016-764900-120
Xie, S. C., Gong, Y. M., Tong, J. N., et al., 2006. Advance-ment from paleontology to geobiology. Chinese Science Bulletin, 51 (19): 2327-2336 (in Chinese). doi: 10.1007/s11434-006-2111-3
Xie, S. C., Pancost R. D., Yin H. F., et al., 2005. Two epi-sodes of microbial change coupled with Permo/Triassic faunal mass extinction. Nature, 434: 494-497. doi: 10.1038/nature03396
Yan, X. Q., Meng, F. W., Yuan, X. L., 2006. Geochemical characteristics of the cherts of the Neoproterozoic Jiud-ingshan Formation in northern Jiangsu and Anhui prov-inces. Acta Micropalaeontologica Sinica, 23 (3): 295-302 (in Chinese with English abstract).
Zhu, S. X., et al., 1993. The stromatolites of China. Tianjin Univ. Press, Tianjin, 1-263 (in Chinese).
曹瑞骥, 袁训来, 2003. 中国叠层石研究的历史和现状. 微体古生物学报, 20 (1): 5-14. doi: 10.3969/j.issn.1000-0674.2003.01.002
[104]	陈晋镳, 1993. 叠层石研究的进展和问题. 见: 朱士兴, 等, 中国叠层石. 天津: 天津大学出版社, 205-214.
戴永定, 陈孟莪, 王尧, 1996. 微生物岩研究的发展与展望. 地球科学进展, 11 (2): 209-215. doi: 10.3321/j.issn:1001-8166.1996.02.016
李玉成, 周忠泽, 2002. 华南二叠纪末缺氧海水中的有毒气体与生物集群绝灭. 地质地球化学, 30 (1): 57-63. doi: 10.3969/j.issn.1672-9250.2002.01.010
梁玉左, 曹瑞骥, 张录易, 等, 1984. 晚前寒武纪假裸枝叠层石. 北京: 地质出版社.
梁玉左, 王楫, 杜汝霖, 1993. 内蒙古白云鄂博群中微小型叠层石(Ministrmatilites) 的构造变形及其地质意义. 地质通报, 3: 229-238. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD199303005.htm
梁玉左, 朱士兴, 高振家, 等, 1995. 叠层石研究的新进展——微生物岩. 中国区域地质, 1: 57-65. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD501.008.htm
邱树玉, 梁玉左, 曹瑞骥, 等, 1992. 晚前寒武纪叠层石及相关矿产. 西安: 西北大学出版社.
谢树成, 龚一鸣, 童金南, 等, 2006. 从古生物学到地球生物学的跨越. 科学通报, 51 (19): 2327-2336. doi: 10.3321/j.issn:0023-074X.2006.19.018
严贤勤, 孟凡巍, 袁训来, 2006. 徐淮地区新元古代九顶山组燧石结核的地球化学特征. 微体古生物学报, 23 (3): 295-302. doi: 10.3969/j.issn.1000-0674.2006.03.005
朱士兴, 等, 1993. 中国叠层石. 天津: 天津大学出版社, 1-263.