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Organic fraction of the total carbon burial flux deduced from carbon isotopes across the Permo-Triassic boundary at Meishan, Zhejiang Province, China

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Abstract

By combining the carbon cycle model with the records of carbonate and organic (kerogen) carbon isotope, this paper presents the calculation of the fraction of organic carbon burial (f org) of beds 23–40 at the global boundary stratotype section and point (GSSP) of the Permian-Triassic boundary at Meishan, Zhejiang Province. The resulting calculation produces two episodes of f org maxima observed to occur at beds 23–24 and 27–29, which respectively corresponds to the two episodic anoxic events indicated by the flourish of green sulfur bacteria. Two episodic f org minima occurred at beds 25–26 and 32–34, generally coincident with the flourish of cyanobacteria (bed 26 and upper part of beds 29 to 34) as shown by the high value of 2-melthyhopnoanes. It appears that the f org is related to the redox conditions, with greater f org values observed under the reductive condition. The relationship between f org and the total organic carbon (TOC) content was complex. The f org value was low at some beds with a high TOC content (such as bed 26), while high observed at some beds with a low TOC content (e.g. bed 27). This association infers the important contribution of primary productivity to the TOC content. The original organic burial could be thus calculated through the configuration of the function of the primary productivity and f org, which can be used to correct the residual TOC measured today. This investigation indicates that compiling the organic-inorganic carbon isotopes with the carbon cycle model favors to understand the fraction of organic carbon burial, providing information for the reconstruction of the coupling among biota, environments and organic burial.

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References

  • Bowering S A, Erwin D H, Jin Y G, et al (1988). U/Pb zircon geochronalogy and tempo of the end Permian mass extinction. Science, 280: 1,039–1,045

    Google Scholar 

  • Cao C Q, Wang W, Jin Y G (2002). Carbon isotope excursions across the Permian-Triassic boundary in the Meishan Section, Zhejiang Province, China. Chinese Science Bulletin, 47: 1,125–1,129

    Google Scholar 

  • Dai J X, Li J, Luo X, et al (2005). Alkane carbon isotope composition and gas source in giant gas field of Ordos basin. Acta Petrolei Sinica, 26: 18–26 (in Chinese with English abstract)

    Google Scholar 

  • Gao B, Fan M, Liu W H, et al (2005). Carbon isotope features and genetic type of natural gas in Tahe oil field. Oil & Gas Geology, 26: 618–622 (in Chinese with English abstract)

    Google Scholar 

  • Grice K, Cao C, Love G D, et al (2005). Photic zone euxinia during the Permian-Triassic superanoxic event. Science, 307: 706–709

    Article  Google Scholar 

  • Guo Q J, Liu C Q, Strauss H, et al (2004). Isotopic investigation of Late Neoproterozoic and Early Cambrian carbon cycle on the northern Yangtze platform, South China. Acta Geoscientica Sinica, 25: 151–156 (in Chinese with English abstract)

    Google Scholar 

  • Haas J, Demény A, Hips K, et al (2007). Environmental changes in the Permian-Triassic boundary interval recorded on a western Tethyan ramp in the Bükk Mts, Hungary. Global and Planetary Change, 55: 136–154

    Article  Google Scholar 

  • Hayes J M, Strauss H, Kaufman A J (1999). The abundance of 13C in marine organic matter and isotopic fractionation in the global biogeochemical cycle of carbon during the past 800 Ma. Chemical Geology, 161: 103–125

    Article  Google Scholar 

  • Huang X Y, Jaio D, Lu L Q. et al (2007). The fluctuating environment associated with the episodic biotic crisis during the Permian-Triassic transition: Evidence from microbial biomarkers in Changing, Zhejiang Province. Science in China (Series D), 50: 1,052–1,059

    Google Scholar 

  • Krull E S, Lehrmann D J, Druke D, et al (2004). Stable carbon isotope stratigraphy across the Permian-Triassic boundary in shallow marine carbonate platforms, Nanpanjiang basin, South China. Palaeogeography, Palaeoclimatology, Palaeoecology, 204: 297–315

    Article  Google Scholar 

  • Kump L R (1991). Interpreting carbon-isotope excursions:strangelove oceans. Geology, 19: 299–302

    Article  Google Scholar 

  • Kump L R, Arthur M A (1999). Interpreting carbon-isotope excursions: Carbonates and organic matter. Chemical Geology, 161: 181–198

    Article  Google Scholar 

  • Kump L R, Garrels R M (1986). Modeling atmospheric O2 in the global sedimentary redox cycle. Am J Sci, 286: 337–360

    Article  Google Scholar 

  • Li Y C, Zhou Z Z (2002). Massive dissociation of gas hydrate during oceanic anoxia as a cause of mass extinction at the end Permian. Geology-Geochemistry, 30: 57–63 (in Chinese with English abstract)

    Google Scholar 

  • Magaritz M, Bart R, Baud A, et al (1988). The carbon-isotope shift at the Permian/Triassic boundary in the southern Alps is gradual. Nature, 331: 337–339

    Article  Google Scholar 

  • Magaritz M, Krishnamurthy R V, Holser W T (1992). The Parallel trend of organic and inorganic carbon isotope in Alps. American Journal of Science, 292: 727–739

    Article  Google Scholar 

  • McCrea J M (1950). The isotopic chemistry of carbonates and a paleotemperature scale. The Journal of Chemical Physics, 18: 849–857

    Article  Google Scholar 

  • Payne J L, Lehrmann D J, Wei J Y, et al (2004). Large perturbations of the carbon cycle during recovery from the end-Permian extinction. Science, 305: 506–509

    Article  Google Scholar 

  • Riccardi A, Kump L R, Arthur M A, et al (2007). Carbon isotopic evidence for chemocline upward excursions during the end-Permian event. Palaeogeography, Palaeoclimatology, Palaeoecology, 248: 73–81

    Article  Google Scholar 

  • Smith R M H, MacLeod K G (1994). Sedimentology and carbon isotope stratigraphy across the Permian-Triassic boundary in the Karoo Basin, South Africa. Journal of African Earth Sciences, 27: 185–186

    Google Scholar 

  • Teng G E, Liu W H, Xu Y C, et al (2004). Organic carbon isotope record in marine sediment and its environment significance: An example from Ordos basin, NW China. Petroleum Exploration and Development, 31: 11–16 (in Chinese with English abstract)

    Google Scholar 

  • Teng G E, Liu W H, Xu Y C, et al (2006). Comprehensive geochemical identification of high evolved marine carbonate rocks as hydrocarbonsource rocks as exemplified by the Ordos basin. Science in China (Series D), 49: 384–396

    Article  Google Scholar 

  • Voigt S, Andrew S G, Voigt T (2006). Sea-level change, carbon cycling and palaeoclimate during the Late Cenomanian of northwest Europe: An integrated palaeoenvironmental analysis. Cretaceous Research, 27: 836–858

    Article  Google Scholar 

  • Wang C J, Liu Y M, Liu H X L, et al (2005). Geochemical significance of the relative enrichment of Pristane and the negative excursion of δ13CPr across the Permian-Triassic boundary at Meishan, China. Chinese Science Bulletin, 50: 2213–2225

    Article  Google Scholar 

  • Xie S C, Pancost R, Yin H F, et al (2005). Two episodes of microbial change coupled with Permo/Triassic faunal mass extinction. Nature, 434: 494–497

    Article  Google Scholar 

  • Xie S C, Pancost R D, Huang X Y, et al (2007a). Molecular and isotopic evidence for episodic environment change across the Permo/Triassic boundary at Meishan in South China. Global and Planetary Change, 55(1):56–65

    Article  Google Scholar 

  • Xie S C, Pancost R D, Huang J H, et al (2007b). Changes in the global carbon cycle occurred as two episodes during the Permo/Triassic crisis. Geology (in press)

  • Xu D Y, Yan Z (1993). Carbon isotope and iridium event markers near the Permian/Triassic boundary in the Meishan Section, Zhejiang Province, China. Paleogeography, Paleoclimatology, Paleoecology, 104: 171–175

    Article  Google Scholar 

  • Xu Y C, Shen P, Liu W H, et al (2001). Isotopic composition characteristics and identification of immature and low-mature oils. Chinese Science Bulletin, 46: 1,923–1,929

    Google Scholar 

  • Yin H F, Zhang K X, Tong J N, et al (2001). The Global Stratotype Section and Point (GSSP) of the Permian-Triassic boundary. Episodes, 24: 102–114

    Google Scholar 

  • Zhang F, Feng Q L, He W H, et al (2006a). Multidisciplinary stratigraphy across the Permian-Triassic boundary in deep-water environment of the Dongpan Section, south China. Norwegian Journal of Geology, 125–131

  • Zhang S C, Wang R L, Jin Z J, et al (2006b). The relationship between the Cambrian-Ordovician high-TOC source rock development and paleoenvironment variations in the Tarim basin, Western China: Carbon and oxygen isotope evidence. Acta Geologica Sinica, 80: 459–466 (in Chinese with English abstract)

    Google Scholar 

Download references

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Authors and Affiliations

  1. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China

    Huang Junhua, Luo Genming, Bai Xiao & Tang Xinyan

  2. Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China

    Huang Junhua & Luo Genming

Authors
  1. Huang Junhua
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  2. Luo Genming
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  3. Bai Xiao
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  4. Tang Xinyan
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Correspondence to Huang Junhua.

Additional information

Journal of China University of Geosciences, 2007, 32(6): 767–773 [译自: 地球科学—中国地质大学学报]

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Huang, J., Luo, G., Bai, X. et al. Organic fraction of the total carbon burial flux deduced from carbon isotopes across the Permo-Triassic boundary at Meishan, Zhejiang Province, China. Front. Earth Sci. China 1, 425–430 (2007). https://doi.org/10.1007/s11707-007-0052-z

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