Carbon input belowground is the major C flux contributing to leaf litter mass loss: Evidences from a 13C labelled-leaf litter experiment

被引:137
作者
Rubino, M. [1 ]
Dungait, J. A. J. [2 ]
Evershed, R. P. [2 ]
Bertolini, T. [1 ]
De Angelis, P. [3 ]
D'Onofrio, A. [1 ]
Lagomarsino, A. [3 ]
Lubritto, C. [1 ]
Merola, A. [1 ]
Terrasi, F. [1 ]
Cotrufo, M. F. [1 ]
机构
[1] Univ Naples 2, Dipartimento Sci Ambientali, I-81110 Caserta, Italy
[2] Univ Bristol, Bristol Biogeochem Res Ctr, Organ Geochem Unit, Sch Chem, Bristol BS8 1TS, Avon, England
[3] Univ Tuscia, Dipartimento Sci Ambiente Forestale & Sue Risorse, I-01100 Viterbo, Italy
关键词
Stable carbon isotopes; Leaf litter decomposition; Soil organic matter; Soil microbial biomass; Carbon cycling; PLFA; SOIL MICROBIAL COMMUNITIES; FIELD DECOMPOSITION; AGRICULTURAL SOILS; PRIMARY SUCCESSION; POPLAR PLANTATION; FATTY-ACIDS; DYNAMICS; CO2; BIOMASS; QUANTIFICATION;
D O I
10.1016/j.soilbio.2010.02.018
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Partitioning of the quantities of C lost by leaf litter through decomposition into (i) CO2 efflux to the atmosphere and (ii) C input to soil organic matter (SOM) is essential in order to develop a deeper understanding of the litter-soil biogeochemical continuum. However, this is a challenging task due to the occurrence of many different processes contributing to litter biomass loss. With the aim of quantifying different fluxes of C lost by leaf litter decomposition, a field experiment was performed at a short rotation coppice poplar plantation in central Italy. Populus nigra leaf litter, enriched in C-13 (delta C-13 similar to +160 parts per thousand) was placed within collars to decompose in direct contact with the soil (delta C-13 similar to -26 parts per thousand) for 11 months. CO2 efflux from within the collars and its isotopic composition were determined at monthly intervals. After 11 months, remaining litter and soil profiles (0-20 cm) were sampled and analysed for their total C and C-13 content. Gas chromatography (GC), GC-mass spectrometry (MS) and GC-combustion-isotope ratio (GC/C/IRMS) were used to analyse phospholipid fatty acids (PLFA) extracted from soil samples to identify the groups of soil micro-organisms that had incorporated litter-derived C and to determine the quantity of C incorporated by the soil microbial biomass (SMB). By the end of the experiment, the litter had lost about 80% of its original weight. The fraction of litter c lost as an input into the soil (67 +/- 12% of the total C loss) was found to be twice as much as the fraction released as CO2 to the atmosphere (30 +/- 3%), thus demonstrating the importance of quantifying fitter-derived C input to soils, in litter decomposition studies. The mean delta C-13 values of PLFAs in soil (delta C-13 = -12.5 parts per thousand) showed sustained incorporation of litter-derived C after one year (7.8 +/- 1.6% of total PLFA-C). Thus, through the application of stable C-13 isotope analyses, we have quantified two major C fluxes contributing to litter decomposition, at macroscopic and microscopic levels. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1009 / 1016
页数:8
相关论文
共 56 条
  • [21] Quantification of dung carbon incorporation in a temperate grassland soil following spring application using bulk stable carbon isotope determinations
    Dungait, JAJ
    Bol, R
    Evershed, RP
    [J]. ISOTOPES IN ENVIRONMENTAL AND HEALTH STUDIES, 2005, 41 (01) : 3 - 11
  • [22] 13C-Labelling of lipids to investigate microbial communities in the environment
    Evershed, RP
    Crossman, ZM
    Bull, ID
    Mottram, H
    Dungait, JAJ
    Maxfield, PJ
    Brennand, EL
    [J]. CURRENT OPINION IN BIOTECHNOLOGY, 2006, 17 (01) : 72 - 82
  • [23] Carbon isotopic fractionation during decomposition of plant materials of different quality
    Fernandez, I
    Mahieu, N
    Cadisch, G
    [J]. GLOBAL BIOGEOCHEMICAL CYCLES, 2003, 17 (03)
  • [24] Reciprocal transfer of carbon and nitrogen by decomposer fungi at the soil-litter interface
    Frey, SD
    Six, J
    Elliott, ET
    [J]. SOIL BIOLOGY & BIOCHEMISTRY, 2003, 35 (07) : 1001 - 1004
  • [25] Frostegard A, 1997, APPL ENVIRON MICROB, V63, P2224
  • [26] FROSTEGARD A, 1993, APPL ENVIRON MICROB, V59, P3605
  • [27] Long-term dynamics of pine and hardwood litter in contrasting environments: toward a global model of decomposition
    Gholz, HL
    Wedin, DA
    Smitherman, SM
    Harmon, ME
    Parton, WJ
    [J]. GLOBAL CHANGE BIOLOGY, 2000, 6 (07) : 751 - 765
  • [28] Gleixner G., 2001, GLOBAL BIOGEOCHEM CY, P201, DOI DOI 10.1016/B978-012631260-7/50017-0
  • [29] Accounting for variability in soil microbial communities of temperate upland grassland ecosystems
    Grayston, SJ
    Griffith, GS
    Mawdsley, JL
    Campbell, CD
    Bardgett, RD
    [J]. SOIL BIOLOGY & BIOCHEMISTRY, 2001, 33 (4-5) : 533 - 551
  • [30] TURNOVER OF CARBON THROUGH THE MICROBIAL BIOMASS IN SOILS WITH DIFFERENT TEXTURES
    GREGORICH, EG
    VORONEY, RP
    KACHANOSKI, RG
    [J]. SOIL BIOLOGY & BIOCHEMISTRY, 1991, 23 (08) : 799 - 805