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Relationship between biomarkers and iron speciation and their environmental significance in plateau subsidence lacus: an example of Luguhu Lake, southeastern Tibetan Plateau

Published online by Cambridge University Press:  15 February 2021

Zixiang WANG Open the ORCID record for Zixiang WANG [Opens in a new window]  and
Lina SUN
Zixiang WANG
Affiliation:
College of Resources and Environment, Yangtze University, Wuhan430100, China Key Laboratory of Oil and Gas Resources and Exploration Technology, Yangtze University, Wuhan430100, China
Lina SUN*
Affiliation:
Hubei Cooperative Innovation Center of Unconventional Oil and Gas (Yangtze University), Wuhan, Hubei430100, China
*
*Corresponding author. Email: [email protected]
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Abstract

Herein, we present a synthetic study combining iron (Fe) speciation and biomarkers in sediment samples from Luguhu Lake to investigate their relationship and the environmental significance thereof. Mössbauer spectroscopy and gas chromatography–mass spectrometry were used for these measurements. The results suggest that (a) there is a strong negative correlation between Fe2+/Fe3+ and the ratio of pristane to phytane (Pr/Ph), indicating that both Fe2+/Fe3+ and Pr/Ph effectively present the inorganic and organic aspects, respectively, of the oxidation–deoxidation environment in Luguhu Lake; (b) palaeotemperature may be a factor, in addition to the redox conditions, that affects the Fe2+/Fe3+ ratio, and it might play a favourable role in studies of palaeotemperature; and (c) the relative abundance of Fe in Luguhu Lake is affected by the palaeoclimate and the environment in which the palaeosediment was deposited. The mechanism of change in the total area (the total absorption area of Mössbauer spectrum) with the palaeoenvironment seems to be explained by the loss of Fe, which occurs as the water drains out of the lake, and the increase in Fe loss from the sediment as rainfall levels increase.

Keywords

Mössbauer spectroscopypaleo-climateoxidation–deoxidation environmentpaleotemperature
Type
Articles
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 111 , Issue 4 , December 2020 , pp. 259 - 266
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Copyright
Copyright © The Author(s) 2021. Published by Cambridge University Press on behalf of The Royal Society of Edinburgh

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References

6. References

Baas, M., Pancost, R., Geel, B. V. & Sinninghe Damsté, J. S. 2000. A comparative study of lipids in sphagnum species. Organic Geochemistry 31, 535–41.CrossRefGoogle Scholar
Brassell, S. C., Wardroper, A. M. K., Thomson, I. D., Maxwell, J. R. & Eglinton, G. 1981. Specific acyclic isoprenoids as biological markers of methanogenic bacteria in marine sediments. Nature 290, 693–96.CrossRefGoogle ScholarPubMed
Chen, F., Huang, X. & Yang, M. 2006. Westerly dominated Holocene climate model in arid Central Asia: case study on Bosten Lake, Xinjiang, China. Quaternary Sciences 26, 881–87.Google Scholar
Chen, J., Wan, G. Chen, Z. & Huang, R. 1999. Chemical elements in sediments of lake Erhai and palaeoclimate evolution. Geochemica 28, 562–70.Google Scholar
Didyk, B. M., Simoneit, B. R. T., Brassell, S. C. & Eglinton, G. 1978. Organic geochemical indicators of palaeoenvironmental conditions of sedimentation. Nature 272, 216–22.CrossRefGoogle Scholar
Dyar, M. D., Agresti, D. G., Schaefer, M. W., Grant, C. A. & Sklute, E. C. 2006. Mössbauer Spectroscopy of earth and planetary materials. Annual Review of Earth & Planetary Sciences 34, 83–125.CrossRefGoogle Scholar
Eglinton, G. & Hamilton, R. J. 1967. Leaf epicuticular waxes. Science (New York, N.Y.) 156, 1322–35.CrossRefGoogle ScholarPubMed
Ficken, K. J., Li, B., Swain, D. L. & Eglinton, G. 2000. An n-alkane proxy for the sedimentary input of submerged/floating freshwater aquatic macrophytes. Organic Geochemistry 31, 745–49.CrossRefGoogle Scholar
Fu, J. & Sheng, G. 1992. Molecular organic geochemistry and its application to the study of paleoclimate and paleoenvironments. Quaternary Sciences 4, 306–20.Google Scholar
Grice, K., Schaeffer, P., Schwark, L. & Maxwell, J. R. 1997. Changes in palaeoenvironmental conditions during deposition of the Permian Kupferschiefer (lower Rhine Basin, Northwest Germany) inferred from molecular and isotopic compositions of biomarker components. Organic Geochemistry 26, 677–90.CrossRefGoogle Scholar
Han, J. & Calvin, M. 1969. Hydrocarbon distribution of algae and bacteria, and microbiological activity in sediments. Proceedings of the National Academy of Sciences of the United States of America 64, 436.CrossRefGoogle ScholarPubMed
He, P. Y. 1989. Paleotemperature of the Lushan Mountain in relation to the ratio of ferric oxide to ferrous oxide from quaternary deposits. Bulletin of the Institute of Geomechanics CAGS 13, 61–70.Google Scholar
Heiri, O. & Millet, L. 2005. Reconstruction of late glacial summer temperatures from chironomid assemblages in Lac Lautrey (Jura, France). Journal of Quaternary Science 20, 33–44.CrossRefGoogle Scholar
Hilton, J., Long, G. J. Chapman, J. S. & Lishman, J. P. 1986. Iron mineralogy in sediments. a Mössbauer study. Geochimica et Cosmochimica Acta 50, 2147–51.CrossRefGoogle Scholar
Jiang, X., Wang, S. & Yang, X. 1998. Paleoclimatic and environmental changes over the last 30000 years in Heqing basin, Yunnan province. Journal of Lake Sciences 10, 10–16.Google Scholar
Kuno, A., Zheng, G. D., Matsuo, M., Takano, B., Shi, J. A. & Wang, Q. 2002. Mössbauer Spectroscopic study on vertical distribution of iron species in sediments from Qinghai Lake, China. Hyperfine Interactions 141–42, 321–26.CrossRefGoogle Scholar
Lacombe, J. L. & Schurer, P. J. 1990. Mössbauer effect study of the glacial to post-glacial transition in the sediment of Georgie Lake. Hyperfine Interactions 57, 2251–56.CrossRefGoogle Scholar
Li, C. & Zhu, Z. 2002. Geochemical records and their paleoclimate significance in Owens Lake, western USA. Quaternary Sciences 22, 578–88.Google Scholar
Li, H. & Xu, T. 1979. The geobotanical expedition on Lake Lugu. Acta Botanica Yunnanica 1, 125–37.Google Scholar
Li, S., Wang, X. Xia, W., et al. 2004. The little ice age climate fluctuations derived from lake sediments of Guolucuo, Qinghai-Xizang Plateau. Quaternary Sciences 24, 578–84.Google Scholar
Manning, P. G. & Ash, L. A. 1979. Mössbauer spectral studies of pyrite, ferric and high-spin ferrous distributions in sulfiderich sediments from Moira Lake, Ontario. Canadian Mineralogist 17, 111–15.Google Scholar
Meters, P. A. 2003. Applications of organic geochemistry to paleolimnological reconstructions: a summary of examples from the Laurentian Great Lakes. Organic Geochemistry 34, 261–89.Google Scholar
Meters, P. A. & Ishiwatari, R. 1993. Lacustrine organic geochemistry – an overview of indicators of organic matter sources and diagenesis in lake sediments. Organic Geochemistry 20, 867–900.Google Scholar
Ou, J., Wang, Y. Yang, H., Wang, H., Gao, W. & Xu, M. 2012. Distribution characteristics of n-alkanes and δ13C in the lake sediments and their environmental significance. Journal of Nanjing Normal University (Natural Science Edition) 35, 98–105.Google Scholar
Poynter, J. & Eglinton, G. 1990. Molecular composition of three sediments from Hole 717C: the Bengal Fan. Proceedings of the Ocean Drilling Program, 116 Scientific Results.CrossRefGoogle Scholar
Qi, Y., Ensling, J. & Guetlich, P. 2004a. A Mössbauer spectroscopic study of sediments from Qinghai Lake. Journal of Salt Lake Research 12, 11–15.Google Scholar
Qi, Y., Ensling, J. & Guetlich, P. 2004b. A Mössbauer spectroscopic study of salt lake sediments. Journal of Salt Lake Research 12, 1–7.Google Scholar
Rielley, G., Collier, R. J., Jones, D. M. & Eglinton, G. 1991. The biogeochemistry of Ellesmere Lake, U.K. – I: source correlation of leaf wax inputs to the sedimentary lipid record. Organic Geochemistry 17, 901–12.CrossRefGoogle Scholar
Shen, J., Zhang, E. & Xia, W. 2001. Records from lake sediments of the Qinghai Lake to mirror climatic and environmental changes of the past about 1000 years. Quaternary Sciences 21, 508–13.Google Scholar
Stumm, W. & Sulzberger, B. 1992. The cycling of iron in natural environments: considerations based on laboratory studies of heterogeneous redox processes. Geochimica et Cosmochimica Acta 56, 3233–57.CrossRefGoogle Scholar
Van der Claar, Z., Slomp, C. P. Rancourt, D. G., Lang, G. J. D. & Raaphorst, W. V. 2005. A Mössbauer spectroscopic study of the iron redox transition in eastern Mediterranean sediments. Geochimica et Cosmochimica Acta 69, 441–53.CrossRefGoogle Scholar
Venkatesan, M. I. & Kaplan, I. R. 1987. The lipid geochemistry of Antarctic marine sediments: Bransfield Strait. Marine Chemistry 21, 347–75.CrossRefGoogle Scholar
Voegelin, A., Senn, A. C., Kaegi, R., Hug, S. J. & Mangold, S. 2013. Dynamic Fe-precipitate formation induced by Fe(ii) oxidation in aerated phosphate-containing water. Geochimica et Cosmochimica Acta 117, 216–31.CrossRefGoogle Scholar
Wang, S. 1991. Lake sedimentology. Earth Science Review 6, 62–63.Google Scholar
Wang, Y., Fang, X., Bai, Y., Xi, X., Yang, S. & Wang, Y. 2006. Macrocyclic alkanes in modern soils of China. Organic Geochemistry 37, 146–51.CrossRefGoogle Scholar
Wang, Y., Fang, X., Bai, Y., Xi, X., Zhang, X. & Wang, Y. X. 2007. Distribution of lipids in modern soils from various regions with continuous climate (moisture-heat) change in China and their climate significance. Science in China Series D: Earth Sciences 50, 600–12.CrossRefGoogle Scholar
Wang, Y., Fang, X., Zhang, T., Li, Y., Wu, Y. He, D., Gao, Y., Meng, P. & Wang, Y. 2010. Predominance of even carbon-numbered-alkanes from lacustrine sediments in Linxia Basin, NE Tibetan Plateau: implications for climate Change. Applied Geochemistry 25, 1478–86.CrossRefGoogle Scholar
Wang, Y., Fang, X., Zhang, T., Li, Y., Wu, Y., He, D., Gao, Y., Meng, P. & Wang, Y. 2012. Distribution of biomarkers in lacustrine sediments of the Linxia Basin, NE Tibetan Plateau, NW China: significance for climate change. Sedimentary Geology 243, 108–16.CrossRefGoogle Scholar
Wang, Q., Yang, X. D., Anderson, N. John, Zhang, E. L. & Li, Y. L. 2014. Diatom response to climate forcing of a deep, alpine lake (Lugu Hu, Yunnan, SW China) during the Last Glacial Maximum and its implications for understanding regional monsoon variability. Quaternary Science Reviews 86, 1–12.CrossRefGoogle Scholar
Weiss, J. L., Gutzler, D. S., Coonrod, J. E. A. & Dahm, C. N. 2004. Seasonal and inter-annual relationships between vegetation and climate in central New Mexico, USA. Journal of Arid Environments 57, 507–34.CrossRefGoogle Scholar
Yu, S., Zhu, Z. Li, B., et al. 1998. Discussion on the climatic records of core iron elements in the core of the Tianshuihai Lake in the Qinghai-Tibet Plateau Since 23ka B.P. Marine Geology & Quaternary Geology 64–66, 68–70.Google Scholar
Zeng, X., Wang, B. & Yang, S. 2012. The terrestrial vegetation characteristics in Luguhu Lake Watershed. Journal of Yunnan University 34, 476–85.Google Scholar
Zhang, C., Chen, F. Shang, H. & Cao, J. 2004a. The paleoenvironmental significance of organic carbon isotope in lacustrine sediments in the arid China: an example from Sanjiaocheng paleolake in Minqin. Quaternary Sciences 24, 88–94.Google Scholar
Zhang, H. C., Yang, M. S., Zhang, W. X., Lei, G. L., Chang, F. Q. Yang, P. & Fan, P. 2008. Molecular fossil and paleovegetation records of paleosol s4 and adjacent loess layers in the Luochuan loess section, NW China. Science in China 51, 321–30.CrossRefGoogle Scholar
Zhang, Z., Zhao, M. Yang, X., Wang, S. & Eglinton, G. 2004b. A hydrocarbon biomarker record for the last 40 kyr of plant input to Lake Heqing, southwestern China. Organic Geochemistry 35, 595–613.CrossRefGoogle Scholar
Zheng, G. 2008. Iron speciation by Mössbauer spectroscopy and its implications in various studies on the earth surface processes. Bulletin of Mineralogy, Petrology and Geochemistry 27, 161–68.Google Scholar
Zheng, G., Takano, B., Kuno, A. & Matsuo, M. 2001. Iron speciation in modern sediment from Erhai Lake, southwestern China redox conditions in an ancient environment. Applied Geochemistry 16, 1201–13.Google Scholar
Zheng, G., Suzuki, K. Takahashi, Y., Shimizu, H., Kuno, A. & Matsuo, M. 2006. Identification of pyrite using 57Fe Mössbauer spectroscopy in core sediments from Erhai Lake, SW China combined with a series of acidic pre-treatments. Journal of Radioanalytical and Nuclear Chemistry 269, 43–50.CrossRefGoogle Scholar
Zheng, Q., Zhang, H. Ming, Q., Chang, F., Meng, H., Zhang, W., Liu, M. & Shen, C. 2014. Vegetational and environmental changes since 15ka B.P. Recorded by Lake Lugu in the southwest monsoon domain region. Quaternary Sciences 34, 1315–26.Google Scholar
Zhu, C. 1994. The application of Fe3+/Fe2+ in probing into the quaternary plaeotemperatures of Lushan Mountain. Geological Review 40, 216–20.Google Scholar