Seasonal switchgrass ecotype contributions to soil organic carbon, deep soil microbial community composition and rhizodeposit uptake during an extreme drought

被引:31
作者
Stewart, Catherine E. [1 ,2 ]
Roosendaal, Damaris [1 ]
Denef, Karolien [3 ]
Pruessner, Elizabeth [1 ]
Comas, Louise H. [4 ]
Sarath, Gautam [5 ]
Jin, Virginia L. [6 ]
Schmer, Marty R. [6 ]
Soundararajan, Madhavan [7 ]
机构
[1] USDA ARS, Soil Management & Sugar Beet Res Unit, Suite 100,2150 Ctr Ave,Bldg D, Ft Collins, CO 80526 USA
[2] Colorado State Univ, Nat Resource Ecol Lab, Ft Collins, CO 80523 USA
[3] Colorado State Univ, Dept Chem, CIF, Ft Collins, CO 80523 USA
[4] USDA ARS, Water Management & Syst Res Unit, Suite 320,2150 Ctr Ave,Bldg D, Ft Collins, CO 80526 USA
[5] Univ Nebraska, Wheat Sorghum & Forage Res Unit, USDA ARS, 251 Filley Hall, Lincoln, NE 68683 USA
[6] Univ Nebraska, Agroecosyst Management Res Unit, USDA ARS, 251 Filley Hall, Lincoln, NE 68583 USA
[7] Univ Nebraska, Dept Biochem, Lincoln, NE 68588 USA
关键词
Switchgrass; Soil microbial biomass; PLFA; Soil C sequestration; C-13 stable isotope probing; DECOMPOSITION; MATTER; PLANT; DYNAMICS; SEQUESTRATION; CULTIVARS; PROFILES; TURNOVER; PATTERNS; TRAITS;
D O I
10.1016/j.soilbio.2017.04.021
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The importance of rhizodeposit C and associated microbial communities in deep soil C stabilization is relatively unknown. Phenotypic variability in plant root biomass could impact C cycling through belowground plant allocation, rooting architecture, and microbial community abundance and composition. We used a pulse-chase C-13 labeling experiment with compound-specific stable-isotope probing to investigate the importance of rhizodeposit C to deep soil microbial biomass under two switchgrass ecotypes (Panicum virgatum L, Kanlow and Summer) with contrasting root morphology. We quantified root phenology, soil microbial biomass (phospholipid fatty acids, PLFA), and microbial rhizodeposit uptake (C-13-PLFAs) to 150 cm over one year during a severe drought. The lowland ecotype, Kanlow, had two times more root biomass with a coarser root system compared to the upland ecotype, Summer. Over the drought, Kanlow lost 78% of its root biomass, while Summer lost only 60%. Rhizosphere microbial communities associated with both ecotypes were similar. However, rhizodeposit uptake under Kanlow had a higher relative abundance of gram-negative bacteria (44.1%), and Summer rhizodeposit uptake was primarily in saprotrophic fungi (48.5%). Both microbial community composition and rhizodeposit uptake shifted over the drought into gram-positive communities. Rhizosphere soil C was greater one year later under Kanlow due to turnover of unlabeled structural root C. Despite a much greater root biomass under Kanlow, rhizosphere delta C-13 was not significantly different between the two ecotypes, suggesting greater microbial C input under the finer rooted species, Summer, whose microbial associations were predominately saprotrophic fungi. Ecotype specific microbial communities can direct rhizodeposit C flow and C accrual deep in the soil profile and illustrate the importance of the microbial community in plant strategies to survive environmental stress such as drought. Published by Elsevier Ltd.
引用
收藏
页码:191 / 203
页数:13
相关论文
共 52 条
[11]   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
[12]   Variation in root architecture among switchgrass cultivars impacts root decomposition rates [J].
de Graaff, Marie-Anne ;
Six, Johan ;
Jastrow, Julie D. ;
Schadt, Christopher W. ;
Wullschleger, Stan D. .
SOIL BIOLOGY & BIOCHEMISTRY, 2013, 58 :198-206
[13]  
De Micco V., 2012, PLANT RESPOSNES DROU, P37, DOI [DOI 10.1007/978-3-642-32653-0_2, 10.1007/978-3-642-32653-02]
[14]  
de Vries FT, 2012, NAT CLIM CHANGE, V2, P276, DOI [10.1038/NCLIMATE1368, 10.1038/nclimate1368]
[15]   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
[16]  
Fenchel T, 2012, BACTERIAL BIOGEOCHEMISTRY: THE ECOPHYSIOLOGY OF MINERAL CYCLING, 3RD EDITION, P89, DOI 10.1016/B978-0-12-415836-8.00006-2
[17]   Do high-tannin leaves require more roots? [J].
Fischer, D. G. ;
Hart, S. C. ;
Rehill, B. J. ;
Lindroth, R. L. ;
Keim, P. ;
Whitham, T. G. .
OECOLOGIA, 2006, 149 (04) :668-675
[18]   Use and misuse of PLFA measurements in soils [J].
Frostegard, Asa ;
Tunlid, Anders ;
Baath, Erland .
SOIL BIOLOGY & BIOCHEMISTRY, 2011, 43 (08) :1621-1625
[19]   Drought history affects grassland plant and microbial carbon turnover during and after a subsequent drought event [J].
Fuchslueger, Lucia ;
Bahn, Michael ;
Hasibeder, Roland ;
Kienzl, Sandra ;
Fritz, Karina ;
Schmitt, Michael ;
Watzka, Margarete ;
Richter, Andreas .
JOURNAL OF ECOLOGY, 2016, 104 (05) :1453-1465
[20]   Experimental drought reduces the transfer of recently fixed plant carbon to soil microbes and alters the bacterial community composition in a mountain meadow [J].
Fuchslueger, Lucia ;
Bahn, Michael ;
Fritz, Karina ;
Hasibeder, Roland ;
Richter, Andreas .
NEW PHYTOLOGIST, 2014, 201 (03) :916-927