Compound-specific δD-δ13C analyses of n-alkanes extracted from terrestrial and aquatic plants

被引:384
作者
Chikaraishi, Y [1 ]
Naraoka, H [1 ]
机构
[1] Tokyo Metropolitan Univ, Dept Chem, Hachioji, Tokyo 1920397, Japan
基金
日本学术振兴会;
关键词
terrestrial plant; aquatic plant; n-alkane; delta D; delta C-13;
D O I
10.1016/S0031-9422(02)00749-5
中图分类号
Q5 [生物化学]; Q7 [分子生物学];
学科分类号
071010 ; 081704 ;
摘要
Stable hydrogen and carbon isotopic compositions of individual n-alkanes were determined for various terrestrial plants (33 samples including 27 species) and aquatic plants (six species) in natural environments from Japan and Thailand. In C3 plants, n-alkanes extracted from angiosperms have a deltaD value of -152+/-26parts per thousand (relative to Standard Mean Ocean Water [SMOW]) and delta(13)C value of -36.1+/-2.7parts per thousand (relative to Peedde Belemnite [PDB]), and those from gymnosperms have a deltaD value of -149+/-16parts per thousand and delta(13)C value of -31.6+/-1.7parts per thousand. Angiosperms have n-alkanes depleted in C-13 relative to gymnosperms. n-Alkanes from C4 plants have a deltaD value of - 171+/-12parts per thousand and delta(13)C value of -20.5+/-2.1parts per thousand, being a little depleted in D and much enriched in C-13 compared to C3 plants. n-Alkanes of CAM plants are a little depleted in D and vary widely in 813 C relative to those of C3 and C4 plants. In aquatic plants, n-alkanes from freshwater plants have a deltaD value of -187+/-16parts per thousand and delta(13)C value of -25.3+/-1.9parts per thousand, and those from seaweeds have a deltaD value of - 155+/-34parts per thousand and delta(13)C value of -22.8+/-1.0parts per thousand. All n-alkanes from various plant classes are more depleted in D and C-13 relative to environmental water and bulk tissue, respectively. In addition, the hydrogen and carbon isotopic fractionations during n-alkane synthesis are distinctive for these various plant classes. While C3 plants have smaller isotopic fractionations in both D and C-13 seaweed has larger isotopic fractionations. (C) 2003 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:361 / 371
页数:11
相关论文
共 36 条
[1]   A comparative study of lipids in Sphagnum species [J].
Baas, M ;
Pancost, R ;
van Geel, B ;
Damsté, JSS .
ORGANIC GEOCHEMISTRY, 2000, 31 (06) :535-541
[2]  
Ball DJ, 1998, SPORTS EXERC INJURY, V4, P3
[3]   Quantitative production of H2 by pyrolysis of gas chromatographic effluents [J].
Burgoyne, TW ;
Hayes, JM .
ANALYTICAL CHEMISTRY, 1998, 70 (24) :5136-5141
[4]  
CASTILLO JBD, 1967, PHYTOCHEMISTRY, V6, P391
[5]   COMPOUND-SPECIFIC DELTA-C-13 ANALYSES OF LEAF LIPIDS FROM PLANTS WITH DIFFERING CARBON-DIOXIDE METABOLISMS [J].
COLLISTER, JW ;
RIELEY, G ;
STERN, B ;
EGLINTON, G ;
FRY, B .
ORGANIC GEOCHEMISTRY, 1994, 21 (6-7) :619-627
[6]   LIPIDS OF AQUATIC ORGANISMS AS POTENTIAL CONTRIBUTORS TO LACUSTRINE SEDIMENTS .2. [J].
CRANWELL, PA ;
EGLINTON, G ;
ROBINSON, N .
ORGANIC GEOCHEMISTRY, 1987, 11 (06) :513-527
[7]  
Deines P., 1980, Handbook of environmental isotope geochemistry, P329, DOI DOI 10.1016/B978-0-444-41780-0.50015-8
[8]   MECHANISM OF CARBON ISOTOPE FRACTIONATION ASSOCIATED WITH LIPID-SYNTHESIS [J].
DENIRO, MJ ;
EPSTEIN, S .
SCIENCE, 1977, 197 (4300) :261-263
[9]   An n-alkane proxy for the sedimentary input of submerged/floating freshwater aquatic macrophytes [J].
Ficken, KJ ;
Li, B ;
Swain, DL ;
Eglinton, G .
ORGANIC GEOCHEMISTRY, 2000, 31 (7-8) :745-749
[10]   LIPIDS OF GEOCHEMICAL SIGNIFICANCE IN MICROSCOPIC ALGAE .1. HYDROCARBONS OF GEOCHEMICAL SIGNIFICANCE IN MICROSCOPIC ALGAE [J].
GELPI, E ;
SCHNEIDER, H ;
MANN, J ;
ORO, J .
PHYTOCHEMISTRY, 1970, 9 (03) :603-+