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Lipid distribution in a subtropical southern China stalagmite as a record of soil ecosystem response to paleoclimate change

Published online by Cambridge University Press:  20 January 2017

Shucheng Xie ,
Yi Yi ,
Junhua Huang ,
Chaoyong Hu ,
Yanjun Cai ,
Matthew Collins  and
Andy Baker
Shucheng Xie*
Affiliation:
China University of Geosciences, Wuhan 430074, People’s Republic of China Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, People’s Republic of China
Yi Yi
Affiliation:
China University of Geosciences, Wuhan 430074, People’s Republic of China
Junhua Huang
Affiliation:
China University of Geosciences, Wuhan 430074, People’s Republic of China
Chaoyong Hu
Affiliation:
China University of Geosciences, Wuhan 430074, People’s Republic of China
Yanjun Cai
Affiliation:
Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, People’s Republic of China
Matthew Collins
Affiliation:
NRG, Drummond Building, Devonshire Terrace, University of Newcastle-upon-Tyne, NE1 7RU, UK
Andy Baker
Affiliation:
Centre for Land Use and Water Resources Research (CLUWRR), University of Newcastle-upon-Tyne, NE1 7RU, UK
*
*Corresponding author. E-mail address:[email protected] (S. Xie).
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Abstract

Lipid extracts from a 61.7-cm-long subtropical stalagmite in southern China, spanning the period of ca. 10,000–21,000 yr ago as constrained by U–Th dating, were analyzed using gas chromatography–mass spectrometry. The higher plants and microorganisms in the overlying soils contribute a proportion of n-alkanes identified in the stalagmite. The occurrence of LMW (lower molecular weight) n-alkanols and n-alkan-2-ones in the stalagmite was mainly related to the soil microorganisms. We suggest that HMW (higher molecular weight) n-alkanols and n-alkan-2-ones identified in the stalagmite originate from soil organics and reflect input from contemporary vegetation. Shifts in the ratio of LMW to HMW n-alkanols or n-alkan-2-ones indicative of the variation of soil ecosystems (e.g., microbial degradation of organic matter and/or the relative abundance of soil microorganisms to higher plants) are comparable with the subtropical alkenone-SST (sea surface temperature) record of the same period. The similar trends seen in the δ13C data and the lipid parameters in this stalagmite imply that the overlying soil ecosystem response to climate might be responsible for the variation of δ13C values.

Keywords

BiomarkersMonsoon climateQuaternarySouthern ChinaSpeleothem
Type
Research Article
Information
Quaternary Research , Volume 60 , Issue 3 , November 2003 , pp. 340 - 347
Copyright
University of Washington

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References

Albro, P.W., (1976). Bacterial waxes. Kolattukudy, P.E. Chemistry and Biochemistry of Natural Waxes. Elsevier, Amsterdam. 419–445.Google Scholar
Baker, A., Genty, D., and Smart, P., (1998). High-resolution records of soil humification and paleoclimate change from variations in speleothem luminescence excitation and emission wavelengths. Geology 26, 903–906.Google Scholar
Baker, A., Caseldine, C.J., Gilmour, M.A., Charman, D., Proctor, C.J., Hawkesworth, C.J., and Phillips, N., (1999). Stalagmite luminescence and peat humification records of palaeomoisture for the last 2500 years. Earth and Planetary Science Letters 165, 157–162.Google Scholar
Bard, E., Rostek, F., Turon, J.-L., and Gendreau, S., (2000). Hydrological impact of Heinrich events in the subtropical Northeast Atlantic. Science 289, 1321–1324.Google Scholar
Beynen, P., van Bourbonniere, R., Ford, D., and Schwarcz, H., (2002). Organic substances in cave drip waters. studies from Marengo Cave, Indiana. Canadian Journal of Earth Sciences 39, 279–284.Google Scholar
Boutton, T. W., Nordt, L. C., Archer, S. R., Midwood, A. J., Casar, I., (1993). Stable carbon isotope ratios of soil organic matter and their potential use as indicators of paleoclimate. in: Isotope Techniques in the Study of Past and Current Environmental Changes in the Hydrosphere and the Atmosphere. International Atomic Energy Agency, Vienna, Austria. pp. 445–452.Google Scholar
Brincat, D., Yamada, K., Ishiwatari, R., Uemura, H., and Naraoka, H., (2000). Molecular-isotopic stratigraphy of long-chain n-alkanes in Lake Baikal Holocene and glacial age sediments. Organic Geochemistry 31, 287–294.Google Scholar
Broecker, W.S., (1994). Massive iceberg discharges as triggers for global climate change. Nature 372, 421–424.CrossRefGoogle Scholar
Bull, I.D., van Bergen, P.F., Nott, C.J., Poulton, P.R., and Evershed, R.P., (2000). Organic geochemical studies of soils from the Rothamsted classical experiments. V. The fate of lipids in different long-term experiments. Organic Geochemistry 31, 389–408.Google Scholar
Coplen, T.B., Winograd, I.J., Landwehr, J.M., and Riggs, A.C., (1994). 500,000-year stable carbon isotopic record from Devils Hole, Nevada. Science 263, 361–365.Google Scholar
Cranwell, P.A., (1973). Branched-chain and cyclopropanoid acids in a recent sediments. Chemical Geology 11, 307–313.Google Scholar
Cranwell, P.A., Eglinton, G., and Robinson, N., (1987). Lipids of aquatic organisms as potential contributors to lacustrine sediments, II. Organic Geochemistry 6, 513–527.Google Scholar
Dorale, J.A., Gonzalez, L.A., Reagan, M.K., Pickett, D.A., Murrell, M.T., and Baker, R.G., (1992). A high-resolution record of Holocene climate change in speleothem calcite from cold water cave, Northeast Iowa. Science 258, 1628–1630.Google Scholar
Dorale, J.A., Edwards, R.L., Ito, E., and Gonzalez, L.A., (1998). Climate and vegetation history of the mid-continent from 75 to 25 ka. a speleothem record from Crevice Cave, Missouri, USA. Science 282, 1871–1874.Google Scholar
Edwards, R.L., Chen, J.H., and Wasserburg, G.J., (1987). 238U–234U–230Th–232Th systematics and the precise measurement of time over the past 500,000 years. Earth and Planetary Science Letters 81, 175–192.Google Scholar
Frappier, A., Sahagian, D., Gonzalez, L.A., and Carpenter, S.J., (2002). El Niño events recorded by stalagmite carbon isotope. Science 298, 565 Google Scholar
Freeman, K.H., and Colarusso, L.A., (2001). Molecular and isotopic records of C4 grassland expansion in the late Miocene. Geochimica et Cosmochimica Acta 65, 1439–1454.Google Scholar
Frumkin, A., Ford, D., and Schwarcz, H., (2000). Paleoclimate and vegetation of the last glacial cycles in Jerusalem from a speleothem record. Global Biogeochemical Cycles 14, 863–870.Google Scholar
Gelpi, E., Schneider, H., Mann, J., and Oro, T., (1990). Hydrocarbons of geochemical significance in microscopic algae. Phytochemistry 9, 603–612.CrossRefGoogle Scholar
Genty, D., Baker, A., Massault, M., Proctor, C., Gilmour, M., Pons, E., and Hamelin, B., (2001). Stalagmite dead carbon proportion variation. paleodissolution process and soil organic matter dynamics recorder — implications for 13C variations in stalagmites. Geochimica et Cosmochimica Acta 65, 3443–3457.CrossRefGoogle Scholar
Genty, D., Blamart, D., Ouhadi, R., Gilmour, M. A., Baker, A., Jouzel, A., Van-Exter, S., (2003). Greenland ice core chronologies constrained by Dansgaard–Oeschger events preserved in a SW-France stalagmite (31–83 ka). Nature Google Scholar
George, S.C., and Jardine, D.R., (1994). Ketones in a Proterozoic dolerite sill. Organic Geochemistry 21, 829–839.Google Scholar
Gong, C., and Hollander, D.J., (1999). Evidence for differential degradation of alkenones under contrasting bottom water oxygen conditions. implication for paleotemperature reconstruction. Geochimica et Cosmochimica Acta 63, 405–411.CrossRefGoogle Scholar
Harmon, R.S., Thompson, P., Schwarcz, H.P., and Ford, D.C., (1978). Late Pleistocene palaeoclimates of North America as inferred from stable isotope studies of cave speleothems. Quaternary Research 9, 54–70.Google Scholar
Hernandez, M.E., Mead, R., Peralba, M.C., and Jaffe, R., (2001). Origin and transport of n-alkan-2-ones in a subtropical estuary. potential biomarkers for seagrass-derived organic matter. Organic Geochemistry 32, 21–32.Google Scholar
Hill, C.A., and Forti, P., (1986). Cave Minerals of the World. National Speleological Society, Huntsville, AL.Google Scholar
Holmgren, K., and Karlen, W., (1995). Paleoclimatic significance of the stable isotopic composition and petrology of a Late Pleistocene stalagmite from Botswana. Quaternary Research 43, 320–328.Google Scholar
Huang, J., Hu, C., and Yuan, D., (2001). Stable isotope and trace element record of a stalagmite in Heshang Cave, Hubei and its palaeoclimatic significance. Science in China (Series E) 44, 123–128.Google Scholar
Huang, Y., Lockheart, M.J., Collister, J.W., and Eglinton, G., (1995). Molecular and isotopic biogeochemistry of the Miocene Clarkia formation: Hydrocarbons anrd alcohols. Organic Geochemistry 23, 785–801.Google Scholar
Huang, Y., Bol, R., Harkness, D.D., Ineson, P., and Eglinton, G., (1996). Post-glacial variations in distributions, 13C and 14C contents of aliphatic hydrocarbons and bulk organic matter in three types of Br. Acid upland soils. Organic Geochemistry 24, 273–287.CrossRefGoogle Scholar
Huang, Y., Street-Perrott, F.A., Perrott, F.A., Metzger, P., and Eglinton, G., (1999). Glacial-interglacial environment changes inferred from the molecular and compound-specific δ13C analyses of sediments from Sacred Lake, Mt Kenya. Geochimica et Cosmochimica Acta 63, 1383–1404.Google Scholar
Jaffe, R., Cabrera, A., Hausmann, K., and Carvajal-Chitty, H., (1993). On the origin and fate of n-alkan-2-ones in freshwater environments. Manning, D. Organic Geochemistry: Applications in Energy and the Natural Environment. Manchester University Press, Manchester. 356–359.Google Scholar
Jaffe, R., Mead, R., Hernandez, M.E., Peralba, M.C., and DiGuida, O.A., (2001). Origin and transport of sedimentary organic matter in two subtropical estuaries. a comparative, biomarker-based study. Organic Geochemistry 32, 507–526.Google Scholar
Jambu, P., Ambles, A., Jaquesy, J.C., Secouet, B., and Parlanti, E., (1993). Incorporation of natural alcohols from plant residues into a hydromorphic forest-podzol. Journal of Soil Science 44, 135–146.CrossRefGoogle Scholar
Jones, J.E., (1969). Studies on lipids of soil micro-organisms with particular reference to hydrocarbons. Journal of General Microbiology 59, 145–152.Google Scholar
Kawamura, K., and Ishiwatari, R., (1985). Distribution of lipid-class compounds in bottom sediments of freshwater lakes with different tropic status in Japan. Chem. Geol. 51, 123–133.Google Scholar
Kienast, M., Steinke, S., Stattegger, K., and Calvert, S.E., (2001). Synchronous tropical South China Sea SST change and Greenland warming during deglaciation. Science 291, 2132–2134.Google Scholar
Kukla, G., and An, Z., (1989). Loess stratigraphy in central China. Palaeogeography, Palaeoclimatology, Palaeoecology 72, 203–225.CrossRefGoogle Scholar
Lehtonen, K., and Ketola, M., (1990). Occurrence of long-chain acyclic methyl ketones in Sphagnum and Carex peats of various degrees of humification. Organic Geochemistry 15, 275–280.Google Scholar
Li, W.-X., Lundberg, J., Dickin, A.P., Ford, D.C., Schwarcz, H.P., McNutt, R., and Williams, D., (1989). High-precision mass-spectrometric uranium-series dating of cave deposits and implications for palaeoclimate studies. Nature 339, 534–536.Google Scholar
Lockheart, M.J., van Bergen, P.F., and Evershed, R.P., (2000). Chemotaxonomic classification of fossil leaves from the Miocene Clarkia lake deposit, Idaho, USA based on n-alkyl lipid distributions and principal component analyses. Organic Geochemistry 31, 1223–1246.CrossRefGoogle Scholar
Logan, G.A., Smiley, C.J., and Eglinton, G., (1995). Preservation of fossil leaf waxes in association with their source tissues, Clarkia, N. Idaho, U.S.A.. Geochimica et Cosmochimica Acta 59, 751–763.Google Scholar
Ludwig, K.R., Simmons, K.R., Szabo, B.J., Winograd, I.J., Landwehr, J.M., Riggs, A.C., and Hoffman, R.J., (1992). Mass-spectrometric 230Th–234U–238U dating of the Devis hole calcite vein. Science 258, 284–287.CrossRefGoogle Scholar
Meyers, P.A., and 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
Northup, D.E., and Lavoie, K.H., (2001). Geomicrobiology of caves. a review. Geomicrobiology Journal 18, 199–220.Google Scholar
O'Neil, J.R., Clayton, R.N., and Mayeda, T.K., (1969). Oxygen isotope fractionation in divalent metal carbonates. J. Chem. Phys. 51, 5547–5558.Google Scholar
Otto, A., Walther, H., and Puttmann, W., (1994). Molecular composition of a leaf- and root-bearing Oligocene oxbow lake clay in Weisselster Basin, Germany. Organic Geochemistry 22, 275–286.Google Scholar
Porter, S.C., and An, Z., (1995). Correlation between climate events in the North Atlantic and China during the last glaciation. Nature 375, 305–308.Google Scholar
Qu, W., Dickman, M., Sumin, W., Ruijin, W., Pingzhong, Z., and Jianfa, C., (1999). Evidence for an aquatic origin of ketones found in Taihu Lake sediments. Hydrobiologia 397, 149–154.Google Scholar
Ramseyer, K., Miano, T.M., Wildberger, A., (1994). Fluorescence banding in speleothems: a fingerprint for humic substances. in: Transactions of the 7th International Meetings of IHSS, St. Augustine, Trinidad and Tobago., A-12 Google Scholar
Ramseyer, K., Miano, T.M., D'Orazio, V., Wildberger, A., Wagner, T., and Geister, J., (1997). Nature and origin of organic matter in carbonates from speleothems, marine cements and coral skeletons. Organic Geochemistry 26, 361–378.Google Scholar
Rieley, G., Collier, R.J., Jones, D.M., and Eglinton, G., (1991). The biogeochemistry of Ellesmere Lake, U.K.-1. source correlation of leaf wax inputs to the sedimentary lipid record. Organic Geochemistry 17, 901–912.Google Scholar
Schneider, J.K., Gagosian, R.B., Cochran, J.K., and Trull, T.W., (1983). Particle size distribution of n-alkanes and 210Pb in aerosols off the coast of Peru. Nature 304, 429–432.CrossRefGoogle Scholar
Schulz, H., von Rad, U., and Erlenkeuser, H., (1998). Correlation between Arabian Sea and Greenland climate oscillations of the past 110,000 years. Nature 393, 54–57.Google Scholar
Schwarcz, H.P., (1986). Geochronology and isotope geochemistry of speleothems. Fontes, J.C.h., Fritz, P. Handbook of Environmental Isotope Geochemistry Vol. 2, Elsevier, Amsterdam. 271–303.Google Scholar
Shopov, Y.Y., Ford, D.C., and Schwarcz, H.P., (1994). Luminescent microbanding in speleothems. high-resolution chronology and paleoclimate. Geology 22, 407–410.Google Scholar
Sicre, M.A., Marty, J.C., and Saliot, A., (1987). Aliphatic and aromatic hydrocarbons in different sized aerosols over the Mediterranean Sea. occurrence and origin. Atmospheric Environment 21, 2247–2259.Google Scholar
Simoneit, B.R.T., Sheng, G.-Y., Chen, X.-J., Fu, J.-M., Zhang, J., and Xu, Y.-P., (1991). Molecular marker study of extractable organic matter in aerosols from urban areas of China. Atmospheric Environment A 25, 2111–2129.CrossRefGoogle Scholar
Street-Perrott, F.A., Huang, Y., Perrott, R.A., Eglinton, G., Barker, P., Ben Khelifa, L., Harkness, D.D., and Olago, D., (1997). The impact of lower atmospheric CO2 on tropical mountain ecosystems. Science 278, 1422–1426.Google Scholar
Taylor, A., Allen, J., and Clark, P., (2002). Extraction of a weak climatic signal by an ecosystem. Nature 416, 629–632.Google Scholar
Villanueva, J., Grimalt, J.O., Cortuo, E., Vidal, L., and Labeyrie, L., (1997). A biomarker approach to the organic matter deposited in the North Atlantic during the last climatic cycle. Geochimica et Cosmochimica Acta 61, 4633–4646.Google Scholar
Wang, Y., Cheng, H., Edwards, R.L., An, Z., Wu, J., Shen, C., and Dorale, J.A., (2001). A high-resolution absolute-dated late Pleistocene monsoon record from Hulu cave, China. Science 294, 2345–2348.Google Scholar
Weete, J.D., (1976). Algal and fungal waxes. Kolattukudy, P.E. Chemistry and Biochemistry of Natural Waxes. Elsevier, Amsterdam. 349–418.Google Scholar
White, W. B., Brennan, E.S., (1989). Luminescence of speleothems due to fulvic acid and other activators. in: 10th International Congress of Speleology, . Budapest., pp. 212–214.Google Scholar
Xie, S., Nott, C.J., Avsejs, L.A., Volders, F., Maddy, D., Chambers, F.M., Gledhill, A., Carter, J.F., and Evershed, R.P., (2000). Palaeoclimate records in compound-specific δD values of a lipid biomarker in ombrotrophic peat. Organic Geochemistry 31, 1053–1057.Google Scholar