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Study of the varve record from Erlongwan maar lake, NE China, over the last 13 ka BP

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  • Geology
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Chinese Science Bulletin

Abstract

In a sediment sequence from Erlongwan maar lake that spans the last 13 ka BP, two main varve types can be recognized: biogenic varves (from the present to ∼11.2 ka BP, 0–632 cm) and clastic varves (from ∼11.2 to ∼12.7 ka BP, 632–700 cm). Based on the dominant types of algae contained in the sediment, the biogenic varves can be classified into dinocyst-biogenic varves (0–63 cm) and mixed (dinocyst and diatom)-biogenic varves (214–632 cm). In this paper, the formation process and components of the varve are described, the possible reason for the types of varve changing throughout the record is discussed and a high-resolution varve chronology is established spanning the last 13 ka BP. Although further varve counting and error assessment are needed, the results presented here represent a solid foundation for studying the palaeoclimate record of Erlongwan maar lake.

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References

  1. Liu J Q, Liu T S, Chu G Q et al. Maar lake and varve chronology. Quat Sci (in Chinese), 1996, (4): 353–358

  2. Shen J, Liu X Q, Wang S M, et al. Palaeoclimatic changes in the Qinghai Lake area during the last 18000 years. Quatern Int, 2005, 136: 131–140

    Google Scholar 

  3. Brauer A, Negendank J F W. The value of annually laminated lake sediments in Palaeoenvironment reconstruction. Quatern Int, 2002, 88: 1–3

    Google Scholar 

  4. Liu J Q, Lu H Y, Negendank J F W, Mingram J, et al. Periodicity of Holocene climate variations in the Huguangyan maar lake. Chin Sci Bull, 2000, 45(18): 1712–1717

    Article  Google Scholar 

  5. Li W C, Li S J, Pu P M. Review on the high resolution varved lake sediments as a proxy of paleoenvironment. Adv Earth Scis (in Chinese), 1999, 14(2): 172–176

    Google Scholar 

  6. Saarnisto M. Annually laminated lake sediments. In: Berglund B E, ed. Handbook of Holocene Palaeoecology and Palaeohydrology. New York: John Wiley & Sons Ltd, 1986. 343–370

    Google Scholar 

  7. Zolitschka B, Brauer A, Negendank J F W, et al. Annually dated late Weichselian continental paleoclimate record from the Eifel, Germany. Geology, 2000, 28(9): 783–786

    Article  CAS  Google Scholar 

  8. Liu Q, You H T, Liu J Q. Methodology of studying on varved lake sediments and its significance. Quat Sci (in Chinese), 2004, 24(6): 683–694

    Google Scholar 

  9. Michel J M. An overview of climatic variability and its casual mechanisms. Quatern Res, 1976, 6: 481–493

    Article  Google Scholar 

  10. Kemp A E S, Baldauf J G, Pearce R B. Origins and palaeoceanographic significance of laminated diatom ooze from the Eastern Equatorial Pacific Ocean. In: Kemp A E S, ed. Palaeoclimatology and Palaeoceanography from Laminated Sediments. London: Geological Society Special Publication. No 116, 1996. 243–252

    Google Scholar 

  11. O’sullivan P E. Annually-laminated lake sediments and the study of Quaternary environmental changes—A review. Quat Sci R, 1983, 1: 245–313

    Article  CAS  Google Scholar 

  12. Anderson R Y, Dean W E. Lacustrine varve formation through time. Palaeogeo P, 1988, 62: 215–235

    Article  Google Scholar 

  13. Mingram J, Allen J, Brüchmann C,et al. Maar and crater lakes of the Long Gang Volcanic Field (N.E.China)-Overview, laminated sediments, and vegetation history of the last 900 years. Quatern Int, 2004, 123–125: 135–147

    Google Scholar 

  14. Mingram J, Negendank J F W, Brauer A, et al. Long cores from small lakes—recovering up to 100 m-long lake sediment sequences with a high-precision rod-operated piston corer (Usinger-corer). J Paleolimnol, 2007, 32: 517–528

    Article  Google Scholar 

  15. You H T, Liu Q, Liu J Q, et al. Research methodology prelimimary results for varved lacustrine sediments of the Sihailongwan maar lake. Earth Environ (in Chinese), 2006, 34(2): 71–76

    Google Scholar 

  16. Frank U. Rock magnetic studies on sediments from Erlongwan maar lake, Long Gang Volcanic Field, Jilin Province, NE China. Geophy J Int, 2007, 168(1): 13–26

    Article  Google Scholar 

  17. Reimer P, Baillie M G L, Bard E, et al. Intcal04 terrestrial radiocarbon age calibration, 0–26 cal kyr BP. Radiocarbon, 2004, 46(3): 1029–1058

    CAS  Google Scholar 

  18. Chu G Q, Gu Z Y, Xu B, et al. Varve chronology and radiometric dating (137Cs, 210Pb) from the Sihailongwan maar, Northeastern China. Quat Sci (in Chinese), 2005, 25(2): 202–207

    Google Scholar 

  19. Chu G Q, Sun Q, Rioual P, et al. Dinocyst microlaminations and freshwater “red tides” recorded in Lake Xiaolongwan, northeastern China. J Paleolimnol, 2007(in press), doi: 10.1007/s10933-007-9106-1

  20. You H T, Liu Q, Liu J Q. A comparative study on model sedimentation rates with varve dating, 137Cs and 210Pb dating in Erlongwan maar lake, NE China. J Jilin Univ (Earth Sci Edition) (in Chinese), 2007, 37(1): 59–64

    Google Scholar 

Download references

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Correspondence to You HaiTao.

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Supported by CAS Key Project (Grant No. KZCX3-SW-145) and the National Natural Science Foundation of China (Grant No. 4032014043)

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You, H., Liu, J., Liu, Q. et al. Study of the varve record from Erlongwan maar lake, NE China, over the last 13 ka BP. Chin. Sci. Bull. 53, 262–266 (2008). https://doi.org/10.1007/s11434-007-0448-x

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  • DOI: https://doi.org/10.1007/s11434-007-0448-x

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