A novel pathway of soil organic matter formation by selective preservation of resistant straight-chain biopolymers: chemical and isotope evidence

被引:144
作者
Lichtfouse, E
Chenu, C
Baudin, F
Leblond, C
Da Silva, M
Behar, F
Derenne, S
Largeau, C
Wehrung, P
Albrecht, P
机构
[1] INPL, ENSAIA, INRA, Lab Sols & Environm, F-54505 Vandoeuvre Les Nancy, France
[2] INRA, Unite Sci Sol, F-78026 Versailles, France
[3] Univ Paris 06, CNRS, URA 1761, Lab Stratig, F-75252 Paris 05, France
[4] IFP Energies Nouvelles, F-92506 Rueil Malmaison, France
[5] Ecole Natl Super Chim, CNRS, UMR 7573, Lab Chim Bioorgan & Organ Phys, F-75231 Paris 05, France
[6] Univ Strasbourg, Lab Geochim Organ, F-67008 Strasbourg, France
关键词
C-13 of soil alkanes; NMR; resistant aliphatic biopolymer; pyrolysis of humin;
D O I
10.1016/S0146-6380(98)00005-9
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
A resistant soil organic residue, "humin", has been analyzed by solid-state C-13-NMR and pyrolysis followed by molecular and C-13 determination of the pyrolysate alkane-alkene fraction. The results show the occurrence of highly aliphatic, straight-chain biopolymer material as a substantial part of soil organic matter. They confirm the hypothesis by which a part of soil organic matter can be formed by selective preservation of resistant highly aliphatic microbial polymers. This pathway is additional to the longstanding neogenesis hypothesis involving recondensation of small polar molecules such as amino acids, carbohydrates and phenols. (C) 1998 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:411 / 415
页数:5
相关论文
共 24 条
[1]   Structure and origin of insoluble and non-hydrolyzable, aliphatic organic matter in a forest soil [J].
Augris, N ;
Balesdent, J ;
Mariotti, A ;
Derenne, S ;
Largeau, C .
ORGANIC GEOCHEMISTRY, 1998, 28 (1-2) :119-124
[2]  
Behar F., 1984, ORG GEOCHEM, V6, P587, DOI 10.1016/0146-6380(84)90081-0
[3]   The chemical composition of soil organic matter in classical humic compound fractions and in bulk samples - A review [J].
Beyer, L .
ZEITSCHRIFT FUR PFLANZENERNAHRUNG UND BODENKUNDE, 1996, 159 (06) :527-539
[4]   INCORPORATION OF XENOBIOTICS INTO SOIL HUMUS [J].
BOLLAG, JM ;
LOLL, MJ .
EXPERIENTIA, 1983, 39 (11) :1221-1231
[5]  
de Leeuw J.W., 1993, ORG GEOCHEM, P23, DOI [DOI 10.1007/978-1-4615-2890-6, 10.1007/978-1-4615-2890-6_2]
[6]  
DELEEUW JW, 1992, NATURWISSENSCHAFTEN, V79, P331
[7]   SIMILAR MORPHOLOGICAL AND CHEMICAL VARIATIONS OF GLOEOCAPSOMORPHA-PRISCA IN ORDOVICIAN SEDIMENTS AND CULTURED BOTRYOCOCCUS-BRAUNII AS A RESPONSE TO CHANGES IN SALINITY [J].
DERENNE, S ;
METZGER, P ;
LARGEAU, C ;
VANBERGEN, PF ;
GATELLIER, JP ;
DAMSTE, JSS ;
DELEEUW, JW ;
BERKALOFF, C .
ORGANIC GEOCHEMISTRY, 1992, 19 (4-6) :299-313
[8]   CHEMICAL EVIDENCE OF KEROGEN FORMATION IN SOURCE ROCKS AND OIL SHALES VIA SELECTIVE PRESERVATION OF THIN RESISTANT OUTER WALLS OF MICROALGAE - ORIGIN OF ULTRALAMINAE [J].
DERENNE, S ;
LARGEAU, C ;
CASADEVALL, E ;
BERKALOFF, C ;
ROUSSEAU, B .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1991, 55 (04) :1041-1050
[9]   COMPARISON OF TORBANITES OF VARIOUS ORIGINS AND EVOLUTIONARY STAGES - BACTERIAL CONTRIBUTION TO THEIR FORMATION - CAUSE OF THE LACK OF BOTRYOCOCCANE IN BITUMENS [J].
DERENNE, S ;
LARGEAU, C ;
CASADEVALL, E ;
CONNAN, J .
ORGANIC GEOCHEMISTRY, 1988, 12 (01) :43-59
[10]   Volatile compounds in archaeological plant remains and the Maillard reaction during decay of organic matter [J].
Evershed, RP ;
Bland, HA ;
vanBergen, PF ;
Carter, JF ;
Horton, MC ;
RowleyConwy, PA .
SCIENCE, 1997, 278 (5337) :432-433