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Carbon and oxygen isotope characteristics of foraminiferan from northern South China Sea sediments and their significance to late Quaternary hydrate decomposition

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Abstract

Carbon and oxygen isotope and dating analyses of foraminiferan in sediment cores collected from three different areas of the northern slope of the South China Sea were conducted, in order to examine the records of the gas hydrate decomposition events since the late Quaternary under the conditions of methane seepage. The results show that: 1) the δ 13C values of the benthic foraminiferan Uvigerina spp. (size range of 0.25–0.35 mm) are from −0.212% to −0.021% and the δ 18O values of the planktonic foraminiferan Globigerinoides ruber (size range of 0.25–0.35 mm) are from −0.311% to −0.060%; 2) three cores (ZD2, ZD3 and ZS5) from the bottom of a hole are aged for 11 814, 26 616 and 64 090 a corresponding to the early oxygen isotope stage (MIS) I, III and IV final period, respectively; 3) a negative-skewed layer of carbon isotope corresponds to that of MIS II (cold period), whose degree of negative bias is −0.2‰; and 4) the δ 13C compositions of foraminiferans are similar to those of the Blake Ridge and the Gulf of Mexico sediments of the late Quaternary. According to the analysis, the reasons for these results are that the studied area is a typical area of methane seep environment in the area during MIS II due to the global sea-level fall and sea pressure decrease. Gas hydrate is decomposed and released, and a large number of light carbon isotopes of methane are released into the ocean, dissolved to inorganic carbon (DIC) pool and recorded in the foraminiferan shells. A pyrite layer developed in the negative bias layers of the foraminiferans confirms that the δ 13C of foraminiferans is more affected by methane and less by the reduction of marine productivity and early diagenesis. The use of foraminiferan δ 13C could accurately determine late Quaternary hydrate release events and provide evidence for both reconstructing the geological history of methane release events and exploring natural gas hydrate.

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References

  1. BROOKS J M, FIELD N E, KENNICUTT M C. Observations of gas hydrates and in marine sediments, offshore northern California [J]. Marine Geology, 1991, 96(1): 103–109.

    Article  Google Scholar 

  2. BOROWSKI W S, PAULL C K, UESSLER III W. Global and local variations of interstitial sulfate gradients in deep water, continental margin sediments: Sensitivity to underling methane and gas hydrates [J]. Marine Geology, 1999, 159: 131–154.

    Article  Google Scholar 

  3. GINSBURG G D, SOLOVIEV V A, CRANSTON R E. Gas hydrate from the continental slope offshore Sakhalin Island, Okhotsk Sea [J]. Marine Geology, 1993, 13(1): 41–48.

    Google Scholar 

  4. CHAPPELLAZ J, BLUNLER T, RAYNAUD D. Synchronous changes in atmospheric CH4 and Greenland climate between 40 and 8 ka BP [J]. Nature, 1993, 366: 443–445.

    Article  Google Scholar 

  5. LEVIN L A, WHITCRAFT C R, MENDOZA G F, GONZALEZ J P, COWIE G L. Oxygen and organic matter thresholds for benthic faunal activity on the Pakistan Margin oxygen minimum zone (700–1 100 m) [J]. Deep-Sea Research II, 2009, 56: 449–471.

    Article  Google Scholar 

  6. OSCAR S, LAURA S, MIGUEL A M. Effects of sample pre-treatment on the δ13C and δ18O values of living benthic foraminifera [J]. Chemical Geology, 2008, 257: 218–220.

    Article  Google Scholar 

  7. SENGUPTA B K, PLATON E, BERNHARD J M. Foraminiferal colonization of hydrocarbon-seep bacterial mats and underlying sediment, Gulf of Mexico slope [J]. Journal of Foraminifera Research, 1997, 20: 292–300.

    Article  Google Scholar 

  8. PAULL C K, UESSLER III W, BOROWSKI W S. Methane-rich plumes on the Carolina continental rise: Associations with gas hydrate [J]. Geology, 1995, 23(1): 89–92.

    Article  Google Scholar 

  9. CORLISS B H. Microhabitats of benthic foraminifera within deep-sea sediments [J]. Nature, 1985, 314: 435–438.

    Article  Google Scholar 

  10. BERNHARD J M. Potential symbionts in bathyal foraminifera [J]. Science, 2003, 299: 861.

    Article  Google Scholar 

  11. BREUER E, LAW G, WOULDS C, COWIE G L, PEPPE O, SCHWARTZ M, SHIMMIELD G, McKINLAY S. Sedimentary oxygen consumption and micro distribution at sites across the Arabian Sea Oxygen Minimum Zone (Pakistan Margin) [J]. Deep-Sea Research II, 2009, 56: 296–304.

    Article  Google Scholar 

  12. TORRES M E, MIX C, KINPORTS K. Is methane venting at the seafloor recorded by δ13C of benthic foraminiferan shells [J]. Paleoceanography, 2003, 18(3): 13.

    Article  Google Scholar 

  13. LEVIN L A, MENDOZA G F. Community structure and nutrition of deep methane seep macro benthos from the North Pacific (Aleutian) margin and the Gulf of Mexico (Florida Escarpment) [J]. Marine Ecology-An Evolutionary Perspective, 2007, 28: 131–151.

    Google Scholar 

  14. DICKENS G R, O’NEIL J R, REA D K. Dissociation of oceanic methane hydrate as a cause of the carbon excursion at the end of the Paleoceane [J]. Paleoceanography, 1995, 10: 965–971.

    Article  Google Scholar 

  15. LAMOLDA M A, PERYT D, ION J. Planktonic foraminiferal bioevents in the Coniacian/Santonian boundary interval at Olazagutia, Navarra province, Spain [J]. Cretaceous Research, 2007, 28(1): 18–29.

    Article  Google Scholar 

  16. GALLEMI J, LOPEZ G, MARTINEZ R. Macrofauna of the Cantera de Margas section, Olazagutia: Coniacian/Santonian boundary, Navarro-Cantabrian Basin, northern Spain [J]. Cretaceous Research, 2007, 28(1): 5–17.

    Article  Google Scholar 

  17. LAMOLDA M A, PAUL R C. Carbon and oxygen stable isotopes across the Coniacian/Santonian boundary at Olazagutia, northern Spain [J]. Cretaceous Research, 2007, 28(1): 37–45.

    Article  Google Scholar 

  18. WU Neng-you, ZHANG Guang-xue, YANG Sheng-xiong. Preliminary discussion on natural gas hydrate reservoir system of Shenhu area, north slope of South China Sea [J]. Natural Gas Industry, 2007, 9: 1–7.

    MATH  Google Scholar 

  19. CHEN Zhong, YANG Hua-ping. Diagenetic environment and implication of seep carbonate precipitations from the southwestern Dongsha Area, South China Sea [J]. Geo-science, 2008, 22(3): 382–389.

    Google Scholar 

  20. ZHU You-hai, ZHANG Guang-xue, LU Zhen-quan. Accumulation and potential exploration of gas hydrate in South China Sea [J]. Petroleum, 2001, 22: 6–10.

    Google Scholar 

  21. ZHANG Guang-xue, HUANG Yong-yang, ZHU You-hai. Prospect of gas hydrate resources in the South China Sea [J]. Marine Geology and Quaternary Geology, 2002, 22(1): 75–81.

    Google Scholar 

  22. RATHBURN A E, PEREZ M E, MARTIN J B. Relationships between the distribution and stable isotopic composition of living benthic foraminifera and cold methane seep biogeochemistry in Monterey Bay, California [J]. Geochemistry Geophysics Geosystems, 2003, 4(12): 1106.

    Article  Google Scholar 

  23. BERNHARD J M, HABURA A, BOWAER S S. An endobiont-bearing allogromiid from the Santa Barbara Basin: Implications for early diversification of foraminifera [J]. Journal of Geophysical Research, 2006, 111: 1–10.

    Google Scholar 

  24. LARKIN K E, GOODAY A J. Foraminiferal faunal responses to monsoon-driven changes in organic matter and oxygen availability at 140 m and 300 m water depth in the NE Arabian Sea [J]. Deep-Sea Research II, 2009, 56: 403–421.

    Article  Google Scholar 

  25. MARTIN R A, NESBITT E A, CAMPBELL K A. The effects of anaerobic methane oxidation on benthic foraminiferal assemblages and stable isotopes on the Hikurangi Margin of eastern New Zealand [J]. Marine Geology, 2010, 272: 270–284.

    Article  Google Scholar 

  26. SCHUMACHER S, JORISSEN F J, DISSARD D, LARKIN K E, GOODAY A J. Live (Rose Bengal stained) and dead benthic foraminifera from the oxygen minimum zone of the Pakistan continental margin (Arabian Sea) [J]. Marine Micropaleontology, 2007, 62: 45–73.

    Article  Google Scholar 

  27. FAIRBANKS R G, MORTLOCK R A, CHIU T C, CAO L, KAPLAN A, GUILDERSON T P, FAIRBANKS T W, BLOOM A L. Marine radiocarbon calibration curve spanning 100 000 to 50 000 years B.P. based on paired 230Th/234U/238U and 14C dates on pristine corals [J]. Quaternary Science Review, 2005, 24: 1781–1796.

    Article  Google Scholar 

  28. YEAL B S, JEAN C P. Carbon and oxygen isotopic composition of planktonic foraminifera from laboratory culture, plankton tows and recent sediment: implications for the reconstruction of paleoclimatic conditions and of the global carbon cycle [J]. Journal of Foraminiferan Research, 1985, 15(4): 302–320.

    Article  Google Scholar 

  29. QIAN Jian-xing. A study of Paleoceanography in the South China Sea during the Late Quaternary [M]. Beijing: Science Press, 1999: 20–21. (in Chinese)

    Google Scholar 

  30. MARTINSON D G, IMBRIE T C, SHACHLETON N J. Age dating and the orbital theory of the ice ages: Development of a high-resolution 0 to 300000 year chronostratigraghy [J]. Quaternary Research, 1987, 27: 1–29.

    Article  Google Scholar 

  31. WU Shi-guo, QIN Yun-shan. The research of deepwater depositional system in the northern South China Sea [J]. Sedimentology, 2009, 27(5): 922–930.

    Google Scholar 

  32. CHEN Fang. Benthic foraminifera and stable isotopic composition of gas hydrate-bearing sediments from Shenhu in the northern South China Sea [J]. Marine Geology and Quaternary Geology, 2010, 30(2): 1–8.

    Article  Google Scholar 

  33. LI Xue-jie. Preliminary study of gas hydrate in the northern slope of the South China Sea: Evidences from ODP [J]. South China Sea Geology Research, 2004, 16–28.

  34. MACAVOY S E, MORGAN E, CARNEY R S, MACKO S A. Chemoautotrophic production incorporated by heterotrophs in Gulf of Mexico hydrocarbon seeps: An examination of mobile benthic predators and seep residents [J]. Journal of Shellfish Research, 2008, 27: 153–161.

    Article  Google Scholar 

  35. MEYER K M, YUB M, JOST A B, KELLEY B M, PAYNE J L. δ13C evidence that high primary productivity delayed recovery from end-Permian mass extinction [J]. Earth and Planetary Science Letters, 2011, 302: 378–384.

    Article  Google Scholar 

  36. CHEN Fang, SU Xin, LU Hong-feng. Carbon stable isotopic composition of benthic foraminifera from the north of South China Sea: Indicator of methane-rich environment [J]. Marine Geology and Quaternary Geology, 2007, 27(4): 1–7.

    Google Scholar 

  37. GOODAY A J, NOMAKI H, KITAZATO H. Modern deep-sea benthic foraminifera: A brief review of their biodiversity and trophic diversity [C]// AUSTIN W E N, JAMES R H. Biogeochemical Controls on Palaeoceanographic Environmental Proxies. London: Special Publications, 2009, 303: 97–119.

    Google Scholar 

  38. COWIE G L, LEVIN L A. Benthic biological and biogeochemical patterns and processes across an oxygen minimum zone (Pakistan Margin, NE Arabian Sea) [J]. Deep-Sea Research II, 2009, 56: 261–270.

    Article  Google Scholar 

  39. SHACKLETON N J, OPDYKE N D. Oxygen isotope and palaeomagnetic stratigraphy of equatorial Pacific core V28-238: Oxygen isotope temperature and ice volumes on a 100000 year and 1000000 year scale [J]. Quaternary Research, 1973, 3: 39–55.

    Article  Google Scholar 

  40. WANG Pin-xian. Western Pacific in glacial cycles: Seasonality in marginal seas and variabilities of warn pool [J]. Science China Series D, 1998, 28(1): 1–6.

    Google Scholar 

  41. CHEN Mu-hong, TU Xin, ZHENG Feng. Relations between sedimentary sequence and paleoclimatic change during last 200 ka in South China Sea [J]. Chinese Science Bulletin, 2000, 45(5): 542–548.

    Article  Google Scholar 

  42. THURBER A R, KROGOR K, NEIRA C, WIKLUND H, LEVIN L A. Stable isotope signatures and methane use by New Zealand cold seep benthos [J]. Marine Geology, 2010, 272: 260–269.

    Article  Google Scholar 

  43. CHAPPELL W S, SHACKLETON N J. Oxygen isotopes and sea level [J]. Nature, 1986, 324: 137–140.

    Article  Google Scholar 

  44. ROLLION C, EREZ J, ZILLBERMAN T. Intra-shell oxygen isotope ratios in the benthic foraminifera genus Amphistegina and the influence of seawater carbonate chemistry and temperature on this ratio [J]. Geochimica et Cosmochimica Acta, 2008, 72: 6006–6014.

    Article  Google Scholar 

  45. LEVIN L A. Ecology of cold seep sediments: Interactions of fauna with flow, chemistry, and microbes [J]. Oceanography Marine Biology, 2005, 43: 1–46.

    Article  Google Scholar 

  46. WOULDS C, COWIE G L. Sedimentary pigments on the Pakistan margin: Controlling factors and organic matter dynamics [J]. Deep-Sea Research II, 2009, 56: 347–357.

    Article  Google Scholar 

  47. ROBINSON C A, BERNHARD J M, LEVIN L A. Surficial hydrocarbon seep infauna from the Blake Ridge (Atlantic Ocean, 2150 m) and the Gulf of Mexico (690-2 240 m) [J]. Marine Geology, 2004, 25(4): 313–336.

    Google Scholar 

  48. GOODAY A J, LEVIN L A, SILVA A. Faunal responses to oxygen gradients on the Pakistan margin: A comparison of foraminiferans, macrofauna and megafauna [J]. Deep-Sea Research II, 2009, 56: 488–502.

    Article  Google Scholar 

  49. SILVA A, GOODAY A J. Large organic-walled Protista (Gromia) in the Arabian Sea: Density, diversity, distribution and ecology [J]. Deep-Sea Research II, 2009, 56: 422–433.

    Article  Google Scholar 

  50. BOROWSKI W S, HOEHLER T M, ALPERIN M J. Significance of anaerobic methane oxidation in methane rich sediments overlying the Blake Ridge gas hydrate [C]// Proceedings of the Ocean Drilling Program, Scientific Results. College Station, Texas: Ocean Drilling Program, 2000: 179–191.

    Google Scholar 

  51. JORGENSEN B B, WEBER A, ZOPFI J. Sulfate reduction and anaerobic oxidation in Black Sea sediments [J]. Deep-sea Research Part I, 2001, 48: 2097–2120.

    Article  Google Scholar 

  52. ROLLION C, MANGIN D, CHAMPENOIS M. Development and applications of oxygen and carbon isotopic measurements of biogenic carbonates by ion microprobe [J]. Geostandards and Geoanalytical Research, 2007, 31: 39–50.

    Article  Google Scholar 

  53. DATTAGUPTA S, ARTHUR M A, FISHER C R. Modification of sediment geochemistry by the hydrocarbon seep tubeworm Lamellibrachia luymesi: A combined empirical and modeling approach [J]. Geochimica et Cosmochimica Acta, 2008, 72: 2298–2315.

    Article  Google Scholar 

  54. LU Miao-an, MA Zhi-jie, CHEN Mu-hong. Rapid carbon isotope negative excursion events during the penultimate deglaciation in western Pacific marginal sea areas and their origins [J]. Quaternary Science, 2002, 22(4): 349–358.

    Google Scholar 

  55. HUANG Yong-yang, SUESS E, WU Neng-you. Methane and natural gas hydrate geology in the northern of South China Sea [M]. Beijing: Geology Press, 2008, 67–71. (in Chinese)

    Google Scholar 

  56. HAYWARD B W, GRENFELL H R, SABAA A T, KAY J. Using foraminiferal faunas as proxies for low tide level in the estimation of Holocene tectonic subsidence, New Zealand [J]. Marine Micropaleontology, 2010, 76: 23–36.

    Article  Google Scholar 

  57. MILLO C, SARNTHEIN M, ERLENKHEUSER H. Methane-induced early diagenesis of foraminiferal testsin the southwestern Greenland Sea [J]. Marine Micropaleontology, 2005, 58: 1–12.

    Article  Google Scholar 

  58. OLIVER F, GERHARD S, HELMUT E. Stable isotope composition of Late Cretaceous benthic foraminifera from the southern South Atlantic: Biological and environmental effects [J]. Marine Micropaleontology, 2006, 58: 135–157.

    Article  Google Scholar 

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Authors and Affiliations

  1. State Key Laboratory of Marine Environment Science (Xiamen University), Xiamen, 361005, China

    Huai-yan Lei  (雷怀彦), Chao Cao  (曹超), Wen-jia Ou  (欧文佳), Chu-jun Gong  (龚楚君) & Chun-xiao Shi  (史春潇)

  2. Third Institute of Oceanography, State Oceanic Administration, Xiamen, 361005, China

    Chao Cao  (曹超)

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  1. Huai-yan Lei  (雷怀彦)
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Correspondence to Chao Cao  (曹超).

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Foundation item: Project(40976035) supported by the National Natural Science Foundation of China; Project(2009CB219501) supported by the National Basic Research Program of China; Project(908-ZC-I-07) supported by the Special Program of Comprehensive Survey and Assessment Offshore China Sea

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Lei, Hy., Cao, C., Ou, Wj. et al. Carbon and oxygen isotope characteristics of foraminiferan from northern South China Sea sediments and their significance to late Quaternary hydrate decomposition. J. Cent. South Univ. Technol. 19, 1728–1740 (2012). https://doi.org/10.1007/s11771-012-1200-5

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