A 3600 years paleoclimatic change inferred from organic δ13C and TOC/TN of the Gucheng Lake sediments, southeast China

Shen Ji; Ryo Matsumoto; Wang Su-min

doi:10.1007/BF02850885

Your Location：

Home >

Browse articles >

A 3600 years paleoclimatic change inferred from organic δ13C and TOC/TN of the Gucheng Lake sediments, southeast China

Updated：2023-05-16

- A 3600 years paleoclimatic change inferred from organic δ13C and TOC/TN of the Gucheng Lake sediments, southeast China
- Journal of Oceanology and Limnology Vol. 15, Issue 3, Pages: 279-284(1997)
- Affiliations：
  
  1. Geological Institute University of Tokyo
  2. Nanjing Institute of Geography and Limnology
- Author bio：
- Funds：
- DOI：10.1007/BF02850885
  CLC：
- Online First：31 January 2013，
  
  Published：1997
- Accepted：
Scan QR Code
Ji, S., Matsumoto, R. & Su-min, W. A 3600 years paleoclimatic change inferred from organic δ13C and TOC/TN of the Gucheng Lake sediments, southeast China., Chin. J. Ocean. Limnol. 15, 279–284 (1997). https://doi.org/10.1007/BF02850885
DOI：

Ji, S., Matsumoto, R. & Su-min, W. A 3600 years paleoclimatic change inferred from organic δ13C and TOC/TN of the Gucheng Lake sediments, southeast China., Chin. J. Ocean. Limnol. 15, 279–284 (1997). https://doi.org/10.1007/BF02850885 DOI：

摘要

Abstract

A 6.2 m thick core of Gucheng Lake sediment provided a 3600 years record of climate change. The contents of the TOC in the core changed from 2.63% to 8.48%

and the δ13C values of organic matter were from −21.54% to −27.3%. The TOC/TN ratios indicated that the organic materials in sediments were from lake plankton and land-derived plants. The 2.9–22 m core interval with high TOC/TN ratios

low δ13C values and low contents of TOC indicated a cold climate stage. The 6.2–5.5 m and 0.4–0.1 m intervals were characterized by low TOC/TN ratios

high δ13C values and high contents of TOC

and reflected temperate climate stages.

关键词

Keywords

references

Bender, M. M., 1971. Variations in the13C/12C ratios of plants in relation to the pathway of photosynthetic carbon dioxide fractionation.Phytochemistry. 10: 1234–1244.

Cormie, A. B., Schwarez, H. P., 1994. Stable isotopes of nitrogen and carbon of North American White-tailed deer and implications for paleodictary and other food web studies. Palacogeogr.,Palaeoclimatol., Palaeoecol. 107: 227–241.

Degens, E. T., 1969. Biogeochemistry of stable carbon isotocpe.In: Organic Geochemistry (eds, G. Eglinton and M. T. J. Murphy) pp. 304–329.

Hudson, J. D., Anderson, T. F., 1989. Ocean temperatures and isotoic compositions through time.Tran. R. Soc. Edinburg Earth Sci. 80: 183–192.

Krantz, D. E., Williams, D. F., Jones, D. S., 1987. Ecological and palaeoenvironmental information using stable isotope profiles from living and fossi molluses.Palaeogeogr., Palacoclimatol., Palaeoecol. 58: 249–266.

Ma, Y., Wang, S. M., Hongxi, P., 1996. Singnificance of diatom and pigment in the study on palaeoenvironmental evolution.Journal of Lake Sciences 8(1): 16–26. (in Chinese)

Marshall, J. D., 1992. Climatie and oceanographic isotopic signals from the carbonate rock record and their preservation.Geol. Mag. 129: 143–160.

Nakai, N., 1986. Paleoenvironmental features of Lake Biwa deduced from carbon isotope compositions and organic C/N ratios of the upper 800 m samples of 1400 m cored column.Proc. Jap. Acad. 62B: 279–282.

Nakai, N., Koyama, M., 1987. Reconstruction of paleoenvironment from the view-points of the inorganic constituents, C/N ratio and carbon isotopic ratio in the 1400 m core taken from Lake Biwa,In: S. Horie (Editor), History of Lake Biwa. Kyoto Univ. Contrib. pp. 137–156.

Ran, G. H., Froelich, P. N., Takahashi, T. et al., 1991. Does sedimentary organic δ13C record variations in Quaternary ocean CO2 (aq)?Paleoceanography 6: 335–347.

Sackett, W. M., Eckelman, W. R., Bender, M. L. et al., 1965. Temperature dependence of carbon isotope composition in marine plankton and sediments.Science 148: 235–237.

Smith, B. N., Epstein, S., 1971. Two categories of13C/12C ratios for higher plants.Plant Physiol. 47: 380–384.

Teeri, J. A., Stowe, L. G., 1976. Climate patterns and the distribution of C4 grasses in North America.Oecologia. 23: 1–12.

Tiezen, L. L., 1978. Carbon isotope fractionation in biological materials.Nature 276: 97–98.

Van der Merwe, N. J., 1982. Carbon isotopes, photosynthesis and archacology.Am. Sci. 70: 596–606.

Wang, S. M., 1995. Paleolimnology of Hulun Lake. Publishing House of Chinese Science and Technology University, Hefei.

Xiang, L., Wang, S. M., 1994. Determination of recent varying, sedimentation rates in Gucheng Lake using210Pb and137Cs.Mem. of Nanjing Inst. of Geog. and Limnol. Acad. Sinica. 11: 70–82. (in Chinese)

Yang, X. D., Wang, S. M., Ji, L. et al., 1994. Spore-pollen assemblage and environmental change of Gucheng Lake since Late Holocene.Journal of Lake Sciences. 6(3): 233–239. (in Chinese)

Views

Downloads

CSCD

Alert me when the article has been cited

Submit

Tools

Publicity Resources

Paleoclimatic change inferred from carbon isotope composition of organic matter in sediments of Dabusu Lake, Jilin Province, China

Paleosalinity reconstruction in offshore lacustrine basins based on elemental geochemistry: a case study of Middle-Upper Eocene Shahejie Formation, Zhanhua Sag, Bohai Bay Basin

Quantifying the non-conservative production of potential temperature over the past 22 000 years

Origin of carbonate materials in the northern Basin of Lake Baikal and its relationship to holocene paleoclimate

Experimental Study of TBCC Engine Performance inLow Speed Wind Tunnel

Related Author

Zhang Enlou

Yang Xiangdong

Shen Ji

Wenfu CUI

Dali YUE

Shenghe WU

Long SUN

Cunjie ZHANG

Related Institution

Nanjing Institute of Geography & Limnology Chinese Academy of Sciences

Shengli Oil Production Plant, Shengli Oilfield Company, SINOPEC

College of Geosciences, China University of Petroleum

National Key Laboratory of Petroleum Resources and Engineering, China University of Petroleum

Physical Oceanography Laboratory/CIMST, Ocean University of China and Qingdao National Laboratory for Marine Science and Technology

Address：Editorial Office of JOL, 88 Haijun Rd. Qingdao, 266000, China
Tel：+86-532-82898754 Email：jol@qdio.ac.cn
Technical support is provided by Beijing Founder electronics co., LTD 京ICP备09064830号-19 京公网安备11010802024621
It is recommended to read the content of this site in Chrome&IE9+. Please switch to extreme mode in browser 360.
Cookies We use cookies to help provide and enhance our service and tailor content. By continuing, you agree to the use of cookies.

⁰