HONG Y T,HONG B,LIN Q H,et al.Inverse phase oscillations between the east Asian and Indian Ocean summer monsoons during the last12000years and paleo-El Nin?[J].Earth and Planetary Science Letters,2003,231;337-346.
[2]
TILLMAN P K,HOLZKAMPER S,KUHRY P,et al.Long-term climate variability in continental subarctic Canada;A6200-year record derived from stable isotopes in peat[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2010,298;235-246.
[3]
SKRZYPEK G,ENGEL Z,CHUMAN T,et al.Distichia peat-A new stable isotope paleoclimate proxy for the Andes[J].Earth and Planetary Science Letters,2011,307;298-308.
[4]
BENNER R,FOGEL M L,SPRAGUE E K.Depletion of in lignin and its implications for stable isotope studies[J].Nature,1987,329;708-710.
[5]
DENNES P.The isotopic composition of reduced organic carbon[M]//FRIZ P,FONTES J C,Eds,Handbook of environmental isotope geoehemistry Vol.l,The terrestrial Enviormnent.Amsterdam;Elsevie,1980,329-406.
[6]
ANCHUKAITIS K J,EVANS M N,LANGE T,et al.Consequences of a rapid cellulose extraction technique for oxygen isotope and radiocarbon analyses[J].Analytical Chemistry,2008,80;2035-2041.
[7]
GREEN J W.Methods of carbonhydate chemistry[M].New York,NY;Academic Press,1963,9-21.
[8]
洪冰.单种属泥炭纤维素碳稳定同位素组成与全新世西南季风变化[D].贵阳;中国科学院研究生院,2005.[HONG Bing.Correlation between Indian ocean summer monsoon and stable carbon isotopic composition from mono-species plant cellulose in the holocene[D].Guiyang;Graduate School of Chinese Academy of Sciences,2005.]
[9]
SAUER P E,MILLER G H,OVERPEVK J H.Oxygen isotope ratios of organic matter in arctic lakes as a paleoclimate proxy;field and laboratory investigations[J].Journal of Paleolimnology,2001,25;43-64.
[10]
WOLFE B B,EDWARDS T W D.Hydrologic control on the oxygen isotope relation between sediment cellulose and lake water,western Taimyr Peninsula,Russia:implications for the use of surfacesediment calibrations in paleolimnology[J].Journal of Paleolimnology,1997,18;183-191.
[11]
WOLFE B B,FALCONE M D,CLOGG-WRIGHT K P,et al.Progress in isotope paleohydrology using lake sediment cellulose[J].Journal of Paleolimnology,2007,37;221-231.
[12]
ZANAZZI A,MORA G.Paleoclimatic implications of the relationship between oxygen isotope ratios of moss cellulose and source water in wetlands of lake superior[J].Chemical Geology,2005,222;281-291.
[13]
DALEY T J,BARBER K E,PERROTT F A,et al.Holocene climate variability revealed by oxygen isotope analysis of sphagnum cellulose from Walton moss,northern England[J].Quaternary Science Reviews,2010,29;1590-1601.
[14]
MENOT-COMBES G,BURNS S T,Leuenberger M.Variations of18O/16O in plants from temperate peat bogs(Switzerland);implications for paleoclimatic studies[J].Earth and Planetary Science Letters,2002,202;419-434.
[15]
RINNE K T,BOETTGER T,LOADER N J,et al.On the purification of cellulose from resinous wood for stable isotope(H,C and O)analysis[J].Chemical Geology,2005,222(1-2);75-82.
[16]
BOETTGER T,HAUPT M,KNOLLER K,et al.Wood cellulose preparation methods and mass spectrometric analyses of δ13C,δ18O,and nonexchangeable δ2H values in cellulose,sugar,and starch;an interlaboratory comparison[J].Anal Chem,2007,79(12);4603-4612.
[17]
MOSCHEN R,KüHL N,REHBERGER I,et al.Stable carbon and oxygen isotopes in sub-fossil sphagnum;assessment of their applicability for palaeoclimatology[J].Chemical Geology,2009,259;262-272.
