Palaeoclimate records in compound-specific δD values of a lipid biomarker in ombrotrophic peat

被引:182
作者
Xie, S
Nott, CJ
Avsejs, LA
Volders, F
Maddy, D
Chambers, FM
Gledhill, A
Carter, JF
Evershed, RP
机构
[1] Univ Bristol, Sch Chem, Organ Geochem Unit, Bristol BS8 1TS, Avon, England
[2] Univ Newcastle Upon Tyne, Dept Geog, Newcastle Upon Tyne NE1 7RU, Tyne & Wear, England
[3] Cheltenham & Gloucester Coll Higher Educ, GEMRU, Ctr Environm Change & Quaternary Res, Cheltenham GL50 4AZ, Glos, England
关键词
peat; n-alkanes; deuterium; Sphagnum; climate change; Holocene;
D O I
10.1016/S0146-6380(00)00116-9
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Compound-specific deltaD values recorded by means of gas chromatography-thermal conversion-isotope ratio mass spectrometry (GC-TC-IRMS) of the biomarker n-alkane (n-tricosane; n-C-23) representative of the dominant Sphagnum species in a 40 cm peat profile from Bolton Fell Moss, Cumbria, UK, correlate with vegetation changes in the past >200 years (age depth model based on Pb-210 dating). The bog vegetation is sensitive to climate change correlating with the global scale cooler period of the later 19th and early 20th centuries. The correlation with meteorological records suggests compound-specific deltaD values of lipid biomarkers have potential for use as a new climate proxy. (C) 2000 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:1053 / 1057
页数:5
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