Soil organic matter molecular composition with long-term detrital alterations is controlled by site-specific forest properties

被引:17
|
作者
Castaneda-Gomez, Laura [1 ]
Lajtha, Kate [2 ]
Bowden, Richard [3 ]
Jauhar, Fathima Nahidha Mohammed [1 ]
Jia, Juan [4 ]
Feng, Xiaojuan [4 ]
Simpson, Myrna J. [1 ]
机构
[1] Univ Toronto, Dept Phys & Environm Sci, Toronto, ON, Canada
[2] Oregon State Univ, Dept Crop & Soil Sci, Corvallis, OR 97331 USA
[3] Allegheny Coll, Dept Environm Sci & Sustainabil, Meadville, PA 16335 USA
[4] Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing, Peoples R China
基金
加拿大自然科学与工程研究理事会;
关键词
cutin; DIRT; lignin; nuclear magnetic resonance; phospholipid fatty acids; radiocarbon; soil carbon; suberin; MICROBIAL COMMUNITY STRUCTURE; PACIFIC SILVER FIR; ELEVATED CO2; LEAF-LITTER; CARBON STORAGE; ABOVEGROUND LITTER; AGRICULTURAL SOIL; NUTRIENT RELEASE; LIGNIN OXIDATION; N FERTILIZATION;
D O I
10.1111/gcb.16456
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Forest ecosystems are important global soil carbon (C) reservoirs, but their capacity to sequester C is susceptible to climate change factors that alter the quantity and quality of C inputs. To better understand forest soil C responses to altered C inputs, we integrated three molecular composition published data sets of soil organic matter (SOM) and soil microbial communities for mineral soils after 20 years of detrital input and removal treatments in two deciduous forests: Bousson Forest (BF), Harvard Forest (HF), and a coniferous forest: H.J. Andrews Forest (HJA). Soil C turnover times were estimated from radiocarbon measurements and compared with the molecular-level data (based on nuclear magnetic resonance and specific analysis of plant- and microbial-derived compounds) to better understand how ecosystem properties control soil C biogeochemistry and dynamics. Doubled aboveground litter additions did not increase soil C for any of the forests studied likely due to long-term soil priming. The degree of SOM decomposition was higher for bacteria-dominated sites with higher nitrogen (N) availability while lower for the N-poor coniferous forest. Litter exclusions significantly decreased soil C, increased SOM decomposition state, and led to the adaptation of the microbial communities to changes in available substrates. Finally, although aboveground litter determined soil C dynamics and its molecular composition in the coniferous forest (HJA), belowground litter appeared to be more influential in broadleaf deciduous forests (BH and HF). This synthesis demonstrates that inherent ecosystem properties regulate how soil C dynamics change with litter manipulations at the molecular-level. Across the forests studied, 20 years of litter additions did not enhance soil C content, whereas litter reductions negatively impacted soil C concentrations. These results indicate that soil C biogeochemistry at these temperate forests is highly sensitive to changes in litter deposition, which are a product of environmental change drivers.
引用
收藏
页码:243 / 259
页数:17
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