CPI values of terrestrial higher plant-derived long-chain n-alkanes: a potential paleoclimatic proxy
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- 作者：Zhiguo Rao (1) (2)
Zhaoyu Zhu (1)
Suping Wang (2)
Guodong Jia (1)
Mingrui Qiang (2)
Yi Wu (1) - 关键词：long ; chain n ; alkanes ; CPI values ; paleoclimatic proxy
- 刊名：Frontiers of Earth Science
- 出版年：2009
- 出版时间：September 2009
- 年：2009
- 卷：3
- 期：3
- 页码：266-272
- 全文大小：252KB
- 参考文献：1. Bi X H, Sheng G Y, Liu X H, Li C, Fu JM (2005). Molecular and carbon and hydrogen isotopic composition / n-alkanes in plant leaf waxes. Organic Geochemistry, 36: 1405鈥?417 CrossRef
2. Brincat D, Yamada K, Ishiwatayi R, Uemura H, Naraoka H (2000). Molecular-isotopic stratigraphy of long-chain / n-alkanes in Lake Baikal Holocene and glacial age sediments. Organic Geochemistry, 31: 287鈥?94 CrossRef
3. Cranwell P A (1981). Diagenesis of free and bound lipids in terrestrial detritus deposited in a lacustrine sediment. Organic Geochemistry, 3: 79鈥?9 CrossRef
4. Cranwell P A (1984). Lipid geochemistry of sediments from Upton Broad, a small productive lake. Organic Geochemistry, 7: 25鈥?7 CrossRef
5. Cranwell P A, Eglinton G, Robinson N (1987). Lipids of aquatic organisms as potential contributiors to lacustrine sediments. Organic Geochemistry, 11(6): 513鈥?27 CrossRef
6. Eglinton G, Hamilton R J (1967). Leaf epicuticular waxes. Science, 156: 1322鈥?335 CrossRef
7. Ficken K J, Street-Perrott F A, Perrott R A, Swainb D L, Olagoc D O, Eglinton G (1998). Glacial/interglacial variations in carbon cycling revealed by molecular and isotope stratigraphy of Lake Nkunga, Mt. Kenya, East Africa. Organic Geochemistry, 29: 1701鈥?719 CrossRef
8. Freeman K H, Hayes J M, Trendel J M, Albrecht P (1990). Evidence from carbon isotope measurements for diverse origins of sedimentary hydrocarbons. Nature, 343: 254鈥?56 CrossRef
9. Huang Y S, Street-Perrott F A, Metcalfe S E, Brenner M, Moreland M, Freeman K H (2001). Climate change as the dominant control on glacial-interglacial variation in C3 and C4 plant abundance. Science, 293: 1647鈥?651 CrossRef
10. Huang Y S, Street-Perrott F A, Perrott R A, Metzger P, Eglinton G (1999). Glacial-interglacial environmental changes inferred from molecular and compound-specific 未13C analyses of sediments from Sacred Lake, Mt. Kenya. Geochimica et Cosmochimica Acta, 63: 1383鈥?404 CrossRef
11. Ishiwatari R, Hirakawa Y, Uzaki M, Yamada K, Yada T (1994). Organic geochemistry of the Japan Sea sediments. 1. Bulk organic matter and hydrocarbon analyses of core KH-79-3, C-3 from the Oki Ridge fro paleoenvironment assessments. Journal of Oceanogrphy, 50: 179鈥?95 CrossRef
12. Jia G D, Wei K, Chen F J, Peng PA (2008). Soil / n-alkane 未D vs. altitude gradients along Mount Gongga, China. Geochimica et Cosmochimica Acta, 72: 5165鈥?174 CrossRef
13. Kawamura K, Ishimura Y, Yamazaki K (2003). Four years’ observation of terrestrial lipid class compounds on marine aerosols from the western North Pacific. Global Biogeochemical Cycles, 17(1): 1003, doi:10.1029/2001GB001810 CrossRef
14. Krull E, Sachse D, M眉gler I, Thiele A, Gleixner G (2006). Compound-specific 未13C and 未2H analyses of plant and soil organic matter: a preliminary assessment of the effects of vegetation change on ecosystem hydrology. Soil Biology & Biochemistry, 38: 3211鈥?221 CrossRef
15. Laboratory of Organic Geochemistry and Sedimentation, Institute of Geochemistry, Chinese Academy of Sciences (1982). Organic Geochemistry. Beijing: Science Press, 64鈥?6 (in Chinese)
16. Liang B, Xie S C, Gu Y S, Guo J Q, Ruan X Y, Yi Y, Huang J H (2005). Distribution of / n-alkanes as indicative of paleovegetationa changes in Pleistocene red earth in Xuancheng, Anhui. Earth Science-Journal of China University of Geosciences, 30(2): 129鈥?32 (in Chinese with English abstract)
17. Liu W G, Huang Y S, An Z S, Clemens S C., Li L, Prell W L, Ning Y F (2005). Summer monsoon intensity controls C4/C3 plants abundance during the last 35 ka in the Chinese Loess Plateau: carbon isotope evidence from bulk organic matter and individual leaf waxes. Palaeogeography Palaeoclimatology Palaeoecology, 220: 243鈥?54 CrossRef
18. Liu W G, Zhang P, Sun Y B, Huang Y S, Guo Z T, An Z S (2008). Molecule fossil evidence for paleovegetation changes in the central of Chinese Loess Plateau during 7-2Ma - Zhaojiachuan profile as an example. Quaternary Science, 28(5): 806鈥?11 (in Chinese with English abstract)
19. Meyers 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鈥?00 CrossRef
20. Pagani M, Pedentchouk N, Huber M, Sluijs A, Shouten S, Brinkhuis H, Sinninghe D J S, Dickens G R (2006). Arctic hydrology during global warming at the Palaeocene-Eocene thermal maximum. Nature, 442: 671鈥?75 CrossRef
21. Rao Z G, Jia G D, Zhu Z Y, Wu Y, Zhang JW (2008). Comparison of the carbon isotope composition of total organic carbon and long-chain nalkanes from surface soils in eastern China and their significance. Chinese Science Bulletin, 53(24): 3921鈥?927 CrossRef
22. Ratnayake N P, Suzuki N, Okada M, Takagi M (2006). The variations of stable carbon isotope ratio of land plant-derived / n-alkanes in deep-sea sediments from the Bearing Sea and the North Pacific Ocean during the last 250000 years. Chemical Geology, 228: 197鈥?08 CrossRef
23. Rieley G, Collier R J, Jones D M, Eglinton G (1991a). The biogeochemistry of Ellesmere Lake, UK- I: source correlation of leaf wax inputs to the sedimentary lipid record. Organic Geochemistry, 17: 901鈥?12 CrossRef
24. Rieley G, Collier R J, Jones D M, Eglinton G, Eakin P A, Fallick A E (1991b). Sources of sedimentary lipids deduced from carbon isotope analyses of individual compounds. Nature, 352: 425鈥?27 CrossRef
25. Schefu脽 E, Schouten S, Schneider R R (2005). Climatic controls on central African hydrology during the past 20, 000 years. Nature, 437: 1003鈥?006 CrossRef
26. Smith FA, Freeman K H (2006). Influence of physiology and climate on 毛D of leaf wax / n-alkanes from C3 and C4 grasses. Geochimica et Cosmochimica Acta, 70: 1172鈥?187 CrossRef
27. Street-Perrott F A, Huang Y S, Perrott R A, Eglinton G, Barker P, Ben Khelifa L, Harkness D D, Olago D O (1997). Impact of lower atmospheric carbon dioxide on tropical mountain ecosystems. Science, 278: 1422鈥?426 CrossRef
28. Sun D H, An Z S, Shaw J, Bloemendal J, Sun Y B (1998). Magnetostratigraphy and palaeoclimatic significance of Late Tertiary aeolian sequences in the Chinese Loess Plateau. Geophysical Journal International, 134 (1): 207鈥?12 CrossRef
29. Sun Y B, Zhou J, An Z S (2001). The Late Cenozoic eolian deposits in the Loess Plateau and the aridity of eolian dust source region. Earth Science Frontiers, 8 (1): 77鈥?1
30. Wang Z Y, Xie S C, Chen F H (2004). / n-alkane distribution as indicator for paleo-vegetation: an example from Yuanbao S1 paleosol in Linxia, Gansu Province. Quaternary Sciences, 24 (2): 231鈥?35 (in Chinese with English abstract)
31. Xie S C, Guo J Q, Huang J H, Chen F H, Wang H B, Farrimond P (2004). Restricted utility of 未13C of bulk organic matter as a record of paleovegetation in some loess-paleosol sequences in the Chinese Loess Plateau. Quaternary Research, 62(1): 86鈥?3 CrossRef
32. Yamada K, Ishiwatari R (1999). Carbon isotopic composition of long-chain / n-alkanes in the Japan Sea sediments: implication for paleoenvironmental changes over the past 85 kyr. Organic Geochemistry, 30: 367鈥?77 CrossRef
33. Yang G F, Xie S C, Huang J H, Chen Z Y (2008). Microbial Characteristics and Vegetation Changes as Recorded in Lipid Biomarker of Tianmushan Peat Bog. Earth Science Frontiers, 15 (4): 170鈥?77 CrossRef
34. Yang MS, Zhang H C, Lei G L, Zhang WX, Fan H F, Chang F Q, Niu J, Chen Y (2006). Biomarkers in weakly developed paleosol (L1SS1) in the Luochuan loess section and reconstructed paleovegetation-environment during the interstade of the Last Glaciation. Quaternary Sciences, 26(6): 976鈥?84 (in Chinese with English abstract)
35. Zhang Z H, Zhao M X, Geoffrey E, Lu H Y, Huang C Y (2006). Leaf wax lipids as paleovegetational and paleoenvironmental proxies for the Chinese Loess Plateau over the last 170 kyr. Quaternary Science Reviews, 25: 575鈥?94 CrossRef
36. Zhang Z H, Zhao MX, Lu H Y, Faiia AM (2003). Lower temperature as the main cause of C4 plant declines during the glacial periods on the Chinese Loess Plateau. Earth and Planetary Science Letters, 214: 467鈥?81 CrossRef
37. Zhong Y X, Chen F H, AN C B, Xie S C, Huang X Y (2007). Holocene vegetation cover in Qin鈥檃n area of western Chinese Loess Plateau revealed by / n-alkane. Chinese Science Bulletin, 52(12): 1692鈥?698 CrossRef - 作者单位：Zhiguo Rao (1) (2)
Zhaoyu Zhu (1)
Suping Wang (2)
Guodong Jia (1)
Mingrui Qiang (2)
Yi Wu (1)
1. Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, 510640, China
2. Key Laboratory of Western China鈥檚 Environment Systems (Ministry of Education), College of Resources and Environment, Lanzhou University, Lanzhou, 730000, China - ISSN：2095-0209
文摘
Carbon Preference Index (CPI values) of higher plant-derived long-chain n-alkanes extracted from 62 surface soil samples in eastern China exhibited a specific pattern of variations, namely gradual increase with the increasing latitudes. Such regular variations existed in both forest soil and grassland soil. Our data implied that CPI values of higher plant-derived long-chain n-alkanes had a certain connection with climatic conditions, and such a connection was not influenced by vegetation types. Together with previous data from marine sediments, loess/paleosol sequences, tertiary red clay and modern plants, our observation made us conclude that CPI values of higher plant-derived long-chain n-alkanes may be used as an excellent proxy for paleoclimatic studies.