n-alkanol ratios as proxies of paleovegetation and paleoclimate in a peat-lacustrine core in southern China since the last deglaciation

Yongnian Zheng1,2,3, Shucheng Xie2, Xiaomin Liu3, Wei Zhou1, Philip A. Meyers4
1State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, China
2Key Laboratory of Biogeology and Environmental Geology of Ministry of Education (China University of Geosciences), Wuhan, China
3State Key Laboratory of Continental Dynamics/Department of Geology, Northwest University, Xi’an, China
4The University of Michigan

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Bull I D, van Bergen P F, Nott C J, Poulton P R, 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

Cranwell P A (1984). Lipid geochemistry of sediments from Upton Broad, a small productive lake. Organic Geochemistry, 7: 25–37

Dalton C, Birks H J B, Brooks S J, Cameron N G, Evershed R P, Peglar S M, Scott J A, Thompson R (2005). A multi-proxy study of lakedevelopment in response to catchment changes during the Holocene at Lochnagar, North-East Scotland. Palaeogeography, Palaeoclimatology, Palaeoecology, 221: 175–201

Ficken K J, Barber K E, Eglinton G (1998a). Lipid biomarker, δ13C and plant macrofossil stratigraphy of a Scottish montane peat bog over the last two millennia. Organic Geochemistry, 28: 217–237

Ficken K J, Li B, Swain D L, Eglinton G (2000). An n-alkane proxy for the sedimentary inputs of submerged/floating freshwater aquatic macrophytes. Organic Geochemistry, 31: 745–749

Ficken K J, Street-Perrott F A, Perrott R A, Swain D L, Olago D O, Eglinton G (1998b). Glacial/interglacial variations in carbon cycling revealed by molecular and isotope stratigraphy of Lake Nkunga, Mt. Kenya, East Africa. Organic Geochemistry, 29: 1701–1719

Huang Y, Street-Perrott F A, Perrott R A, Metzger P, Eglinton G (1999). Glacial-interglacial environmental changes inferred from molecular and compound-specific δ13C analyses of sediments from Sacred Lake, Mt. Kenya. Geochimica et Cosmochimica Acta, 63: 1383–1404

Hughen K A, Eglinton T I, Xu L, Makou M (2004). Abrupt tropical vegetation response to rapid climate changes. Science, 304: 1955–1959

Jansen B, Haussmann N S, Tonneijck F H, Verstraten J M, de Voogt T (2008). Characteristic straight-chain lipid ratios as a quick method to assess past forest-paramo transitions in the Ecuadorian Andes. Palaeogeography, Palaeoclimatology, Palaeoecology, 262: 129–139

Jansen B, Nierop K G J, Hageman J A, Cleef A, Verstraten J M (2006). The straightchain lipid biomarker composition of plant species responsible for the dominant biomass production along two altitudinal transects in the Ecuadorian Andes. Organic Geochemistry, 37: 1514–1536

Meyer P A, Ishiwatari R (1993). Lacustine organic geochemistry: an overview of indicators of organic sources and diagenesis in lake sediments. Organic Geochemistry, 20: 867–900

Moucawi J, Fustec E, Jambu P A A, Jacquesy R (1981a). Biooxidation of added and natural hydrocarbons in soils: effect of iron. Soil Biology & Biochemistry, 13: 335–342

Moucawi J, Fustec E, Jambu P, Jacquesy R (1981b). Decomposition of lipids in soils: free and esterified fatty acids, alcohols and ketones. Soil Biology & Biochemistry, 13: 461–468

Naafs D F W, van Bergen P F, Boogert S J, de Leeuw J W (2004). Solvent-extractable lipids in an acid andic forest soil: variations with depth and season. Soil Biology & Biochemistry, 36: 297–308

Nierop K G J, Jansen B, Hageman J A, Verstrate J M (2006). The complementarity of extractable and ester-bound lipids in a soil profile under pine. Plant Soil, 286: 269–285

Nierop K G J, Tonneijck F H, Jansen B, Verstraten J M (2007). Oranic matter in volcanic ash soils under forest and páramo along an Ecuadorian altitudinal transect. Soil Science Society of America Journal, 71: 1119–1127

Nott C J, Xie S, Avsejs L A, Maddy D, Chambers F M, Evershed R P (2000). n-alkane distributions in ombrotrophic mires as indicators of vegetation change related to climatic variation. Organic Geochemistry, 31: 231–235

Rieley G, Collier R J, Jones D M, Eglinton G (1991). The biogeochemistry of Ellesme Lake, UK.I: source correlation of leaf wax inputs to the sedimentary lipid record. Organic Geochemistry, 17: 901–912

Schwark L, Zink K, Lechterbeck J (2002). Reconstruction of postglacial to early Holocene vegetation history in terrestrial Central Europe via cuticular lipid biomarkers and pollen records from lake sediments. Geology, 30: 463–466

Stuiver M, Reimer P J (1993). Extended 14C data-base and revised Calib 3.1 14C age calibration program. Radiocarbon, 35: 215–230

Stuiver M, Reimer P J, Bard E, Beck J W, Burr G S, Hughen K A, Kromer B, McCormac G, van der Plicht J, Spurk M (1998). INTCAL98 Radiocarbon age calibration. Radiocarbon, 40: 1041–1083

Sun X J, Luo Y L (2004). From pollen record to paleovegetation: Reply to “A discussion on the vegetation types during LAST DEGLACIATION time in South China”. Quaternary Sciences, 24(2): 217–221 (in Chinese with English abstract)

Tulloch A (1976). Chemistry of waxes of higher plants. In: Kolattukudy P, ed. Chemistry and Biochemistry of Natural Waxes. Amsterdam: Elsevier, 201–235

van Bergen P F, Bull I D, Poulton P R, Evershed R P (1997). Organic geochemical studies of soils from the Rothamsted Classical Experiments. I. Total lipid extracts, solvent insoluble residues and humic acids from Broadbalk Wilderness. Organic Geochemistry, 26: 117–135

van Bergen P F, Nott C J, Bull I D, Poulton P R, Evershed R P (1998). Organic geochemical studies of soils from the Rothamsted Classical Experiments - IV. Preliminaryresults from a study of the effect of soil pH on organic matter decay. Organic Geochemistry, 29: 1779–1795

Wang R J, Li J (2003). Quaternary high-resolution opal records and its paleo productivity implication at ODP site 1143. Chinese Science Bulletin, 48(4): 363–367

Wang Y J, Cheng H, Lawrence Edwards R, He Y, Kong X G, An Z S, Wu J Y, Kelly M J, Dykoski C A, Li X D (2005). The Holocene Asian Monsoon: Links to solar changes and North Atlantic climate. Science, 308(6): 854–857

Wu G X, Sun X J (2000). Late Quaternary organic-wall Phytoplankton record in northern slope of South China Sea and its paleoenvironmental significance. Marine Geology and Quaternary Geology, 20(2): 57–63 (in Chinese with English abstract)

Xie S, Evershed R P (2002). The climatic and biological change information from the peat molecular fossil records. Chinese Science Bulletin, 46: 1–5

Xie S, Nott C J, Avsejs L A, Maddy D, Chambers F, Evershed R P (2004). Molecular and isotopic stratigraphy in an ombrotrophic mire for palaeoclimate reconstruction. Geochimica et Cosmochimica Acta, 68: 2849–2862

Xie S, Nott C J, Avsejs L A, Volders F, Maddy D, Chambers F M, Gledhill A, Carter J F, Evershed R P (2000). Palaeoclimate records in compound-specific δD values of a lipid biomarker in ombrotrophic peat. Organic Geochemistry, 31: 1053–1057

Zhang Z H, Zhao M X, Eglinton G, Lu H Y, Huang C Y (2006). Leaf wax lipids as paleovegetational and paleoenvironmental proxies for the Chinese Loess Plateau over the last 170 ka. Quaternary Science Reviews, 25: 575–594

Zheng Y H, Zhou W J, Meyers P A, Xie S (2007). Lipid biomarkers in the Zoige-Hongyuan peat deposit: indicators of Holocene climate change in west China. Organic Geochemistry 38: 1927–1940

Zheng Y H, Zhou W J, Xie S C, Yu X F (2009). A comparative study of n-alkane biomarker and pollen records: an example from southern China. Chinese Science Bulletin, 54: 1065–1072

Zheng Z (2004). Holocene environmental changes in the tropical and subtropical areas of the south China and the relation to human activities. Quaternary Science, 24(4): 390–391 (in Chinese with English abstract)

Zhou W J, Xie S, Meyers P A, Zheng Y (2005). Reconstruction of late glacial and Holocene climate evolution in southern China from geolipids and pollen in the Dingnan peat sequence. Organic Geochemistry, 36: 1272–1284

Zhou W J, Yu X F, Jull A J, Burr G, Xiao J Y, Lu X F, Xian F (2004). High-resolution evidence from southern China of an early Holocene optimum and a mid-Holocene dry event during the past 18000 years. Quaternary Research, 62: 39–48