CPI values of terrestrial higher plant-derived long-chain
Zhiguo RAO, Zhaoyu ZHU, Suping WANG, Guodong JIA, Mingrui QIANG, Yi WU
CPI values of terrestrial higher plant-derived long-chain
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.
long-chain n-alkanes / CPI values / paleoclimatic proxy
[1] |
Bi X H, Sheng G Y, Liu X H, Li C, Fu J M (2005). Molecular and carbon and hydrogen isotopic composition n-alkanes in plant leaf waxes. Organic Geochemistry, 36: 1405-1417
CrossRef
Google scholar
|
[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: 287-294
CrossRef
Google scholar
|
[3] |
Cranwell P A (1981). Diagenesis of free and bound lipids in terrestrial detritus deposited in a lacustrine sediment. Organic Geochemistry, 3: 79-89
CrossRef
Google scholar
|
[4] |
Cranwell P A (1984). Lipid geochemistry of sediments from Upton Broad, a small productive lake. Organic Geochemistry, 7: 25-37
CrossRef
Google scholar
|
[5] |
Cranwell P A, Eglinton G, Robinson N (1987). Lipids of aquatic organisms as potential contributiors to lacustrine sediments. Organic Geochemistry, 11(6): 513-527
CrossRef
Google scholar
|
[6] |
Eglinton G, Hamilton R J (1967). Leaf epicuticular waxes. Science, 156: 1322-1335
CrossRef
Google scholar
|
[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: 1701-1719
|
[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: 254-256
CrossRef
Google scholar
|
[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: 1647-1651
CrossRef
Google scholar
|
[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 δ13C analyses of sediments from Sacred Lake, Mt. Kenya. Geochimica et Cosmochimica Acta, 63: 1383-1404
CrossRef
Google scholar
|
[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: 179-195
CrossRef
Google scholar
|
[12] |
Jia G D, Wei K, Chen F J, Peng P A (2008). Soil n-alkane δD vs. altitude gradients along Mount Gongga, China. Geochimica et Cosmochimica Acta, 72: 5165-5174
CrossRef
Google scholar
|
[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
Google scholar
|
[14] |
Krull E, Sachse D, Mügler I, Thiele A, Gleixner G (2006). Compound-specific δ13C and δ2H analyses of plant and soil organic matter: a preliminary assessment of the effects of vegetation change on ecosystem hydrology. Soil Biology & Biochemistry, 38: 3211-3221
CrossRef
Google scholar
|
[15] |
Laboratory of Organic Geochemistry and Sedimentation, Institute of Geochemistry, Chinese Academy of Sciences (1982). Organic Geochemistry. Beijing: Science Press, 64-76 (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): 129-132 (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: 243-254
CrossRef
Google scholar
|
[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 7–2 Ma – Zhaojiachuan profile as an example. Quaternary Science, 28(5): 806-811 (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: 867-900
CrossRef
Google scholar
|
[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: 671-675
CrossRef
Google scholar
|
[21] |
Rao Z G, Jia G D, Zhu Z Y, Wu Y, Zhang J W (2008). Comparison of the carbon isotope composition of total organic carbon and long-chain n-alkanes from surface soils in eastern China and their significance. Chinese Science Bulletin, 53(24): 3921-3927
CrossRef
Google scholar
|
[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: 197-208
CrossRef
Google scholar
|
[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: 901-912
CrossRef
Google scholar
|
[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: 425-427
CrossRef
Google scholar
|
[25] |
Schefuß E, Schouten S, Schneider R R (2005). Climatic controls on central African hydrology during the past 20, 000 years. Nature, 437: 1003-1006
CrossRef
Google scholar
|
[26] |
Smith F A, Freeman K H (2006). Influence of physiology and climate on δD of leaf wax n-alkanes from C3and C4grasses. Geochimica et Cosmochimica Acta, 70: 1172-1187
CrossRef
Google scholar
|
[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: 1422-1426
CrossRef
Google scholar
|
[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): 207-212
CrossRef
Google scholar
|
[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): 77-81
|
[30] |
Wang Z Y, Xie S C, Chen F H (2004). n-alkane distribution as indicator for paleo-vegetation: an example from Yuanbao S1paleosol in Linxia, Gansu Province. Quaternary Sciences, 24 (2): 231-235 (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 δ13C of bulk organic matter as a record of paleovegetation in some loess-paleosol sequences in the Chinese Loess Plateau. Quaternary Research, 62(1): 86-93
CrossRef
Google scholar
|
[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: 367-377
CrossRef
Google scholar
|
[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): 170-177
CrossRef
Google scholar
|
[34] |
Yang M S, Zhang H C, Lei G L, Zhang W X, 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): 976-984 (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: 575-594
CrossRef
Google scholar
|
[36] |
Zhang Z H, Zhao M X, Lu H Y, Faiia A M (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: 467-481
CrossRef
Google scholar
|
[37] |
Zhong Y X, Chen F H, AN C B, Xie S C, Huang X Y (2007). Holocene vegetation cover in Qin’an area of western Chinese Loess Plateau revealed by n-alkane. Chinese Science Bulletin, , 52(12): 1692-1698
CrossRef
Google scholar
|
/
〈 | 〉 |