Rapid transfer of photosynthetic carbon through the plant-soil system in differently managed species-rich grasslands

被引:91
作者
De Deyn, G. B. [1 ,2 ]
Quirk, H. [1 ]
Oakley, S. [3 ]
Ostle, N. [3 ]
Bardgett, R. D. [1 ]
机构
[1] Univ Lancaster, Lancaster Environm Ctr, Soil & Ecosyst Ecol Lab, Lancaster LA1 4YQ, England
[2] Netherlands Inst Ecol, Dept Terr Ecol, NL-6700AB Wageningen, Netherlands
[3] Lancaster Environm Ctr, Ctr Ecol & Hydrol, Lancaster LA1 4AP, England
基金
英国生物技术与生命科学研究理事会;
关键词
ACTIVE RHIZOSPHERE MICROORGANISMS; MICROBIAL COMMUNITY COMPOSITION; BOTANICALLY DIVERSE HAYMEADOWS; FATTY-ACID PROFILES; BIOMASS RATIOS; CLIMATE-CHANGE; ELEVATED CO2; SEQUESTRATION; RESTORATION; VEGETATION;
D O I
10.5194/bg-8-1131-2011
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Plant-soil interactions are central to short-term carbon (C) cycling through the rapid transfer of recently assimilated C from plant roots to soil biota. In grassland ecosystems, changes in C cycling are likely to be influenced by land use and management that changes vegetation and the associated soil microbial communities. Here we tested whether changes in grassland vegetation composition resulting from management for plant diversity influences short-term rates of C assimilation and transfer from plants to soil microbes. To do this, we used an in situ C-13-CO2 pulse-labelling approach to measure differential C uptake among different plant species and the transfer of the plant-derived C-13 to key groups of soil microbiota across selected treatments of a long-term plant diversity grassland restoration experiment. Results showed that plant taxa differed markedly in the rate of C-13 assimilation and concentration: uptake was greatest and C-13 concentration declined fastest in Ranunculus repens, and assimilation was least and C-13 signature remained longest in mosses. Incorporation of recent plant-derived C-13 was maximal in all microbial phosopholipid fatty acid (PLFA) markers at 24 h after labelling. The greatest incorporation of C-13 was in the PLFA 16:1 omega 5, a marker for arbuscular mycorrhizal fungi (AMF), while after 1 week most C-13 was retained in the PLFA18:2 omega 6,9 which is indicative of assimilation of plant-derived C-13 by saprophytic fungi. Our results of C-13 assimilation and transfer within plant species and soil microbes were consistent across management treatments. Overall, our findings suggest that plant diversity restoration management may not directly affect the C assimilation or retention of C by individual plant taxa or groups of soil microbes, it can impact on the fate of recent C by changing their relative abundances in the plant-soil system. Moreover, across all treatments we found that plant-derived C is rapidly transferred specifically to AMF and decomposer fungi, indicating their consistent key role in the cycling of recent plant derived C.
引用
收藏
页码:1131 / 1139
页数:9
相关论文
共 47 条
[1]  
Bardgett RD, 1996, BIOL FERT SOILS, V22, P261, DOI 10.1007/BF00382522
[2]   The measurement of soil fungal:bacterial biomass ratios as an indicator of ecosystem self-regulation in temperate meadow grasslands [J].
Bardgett, RD ;
McAlister, E .
BIOLOGY AND FERTILITY OF SOILS, 1999, 29 (03) :282-290
[3]   Plant-soil interactions and the carbon cycle [J].
Bardgett, Richard D. ;
De Deyn, Gerlinde B. ;
Ostle, Nicholas J. .
JOURNAL OF ECOLOGY, 2009, 97 (05) :838-839
[4]   Increased N availability in grassland soils modifies their microbial communities and decreases the abundance of arbuscular mycorrhizal fungi [J].
Bradley, Kate ;
Drijber, Rhae A. ;
Knops, Jean .
SOIL BIOLOGY & BIOCHEMISTRY, 2006, 38 (07) :1583-1595
[5]   Plant species richness, elevated CO2, and atmospheric nitrogen deposition alter soil microbial community composition and function [J].
Chung, Haegeun ;
Zak, Donald R. ;
Reich, Peter B. ;
Ellsworth, David S. .
GLOBAL CHANGE BIOLOGY, 2007, 13 (05) :980-989
[6]   Temperature sensitivity of soil carbon decomposition and feedbacks to climate change [J].
Davidson, EA ;
Janssens, IA .
NATURE, 2006, 440 (7081) :165-173
[7]   Plant functional traits and soil carbon sequestration in contrasting biomes [J].
De Deyn, Gerlinde B. ;
Cornelissen, Johannes H. C. ;
Bardgett, Richard D. .
ECOLOGY LETTERS, 2008, 11 (05) :516-531
[8]  
DEDEYN GB, 2011, J APPL ECOL IN PRESS, DOI DOI 10.1111/J.1365-2664.2010.01925
[9]   Community shifts and carbon translocation within metabolically-active rhizosphere microorganisms in grasslands under elevated CO2 [J].
Denef, K. ;
Bubenheim, H. ;
Lenhart, K. ;
Vermeulen, J. ;
Van Cleemput, O. ;
Boeckx, P. ;
Mueller, C. .
BIOGEOSCIENCES, 2007, 4 (05) :769-779
[10]   Microbial community composition and rhizodeposit-carbon assimilation in differently managed temperate grassland soils [J].
Denef, Karolien ;
Roobroeck, Dries ;
Manimel Wadu, Mihiri C. W. ;
Lootens, Peter ;
Boeckx, Pascal .
SOIL BIOLOGY & BIOCHEMISTRY, 2009, 41 (01) :144-153