Bryophytes attenuate anthropogenic nitrogen inputs in boreal forests

被引:175
|
作者
Gundale, Michael J. [1 ]
Deluca, Thomas H. [2 ]
Nordin, Annika [3 ]
机构
[1] Swedish Univ Agr Sci, Dept Forest Ecol & Management, SE-90183 Umea, Sweden
[2] Bangor Univ, Sch Environm Nat Resources & Geog, Environm Ctr Wales, Bangor LL57 2UW, Gwynedd, Wales
[3] Swedish Univ Agr Sci, Dept Forest Genet & Plant Physiol, Umea Plant Sci Ctr, SE-90183 Umea, Sweden
基金
瑞典研究理事会;
关键词
biological nitrogen fixation; bryophytes; carbon sequestration; carbon sink; cyanobacteria; nitrogen deposition; Pleurozium schreberi; productivity; soil nitrogen uptake; CARBON SEQUESTRATION; MOSS CARPETS; DEPOSITION; FIXATION; LITTER; VEGETATION; TEMPERATE; FERTILIZATION; DIVERSITY; INCREASES;
D O I
10.1111/j.1365-2486.2011.02407.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Productivity in boreal ecosystems is primarily limited by available soil nitrogen (N), and there is substantial interest in understanding whether deposition of anthropogenically derived reactive nitrogen (N-r) results in greater N availability to woody vegetation, which could result in greater carbon (C) sequestration. One factor that may limit the acquisition of N-r by woody plants is the presence of bryophytes, which are a significant C and N pool, and a location where associative cyanobacterial N-fixation occurs. Using a replicated stand-scale N-addition experiment (five levels: 0, 3, 6, 12, and 50 kg N ha(-1)yr(-1); n=6) in the boreal zone of northern Sweden, we tested the hypothesis that sequestration of Nr into bryophyte tissues, and downregulation of N-fixation would attenuate N-r inputs, and thereby limit anthropogenic N-r acquisition by woody plants. Our data showed that N-fixation per unit moss mass and per unit area sharply decreased with increasing N addition. Additionally, the tissue N concentrations of Pleuorzium schreberi increased and its biomass decreased with increasing N addition. This response to increasing N addition caused the P. schreberi N pool to be stable at all but the highest N addition rate, where it significantly decreased. The combined effects of changed N-fixation and P. schreberi biomass N accounted for 56.7% of cumulative N-r additions at the lowest N-r addition rate, but only a minor fraction for all other treatments. This 'bryophyte effect' can in part explain why soil inorganic N availability and acquisition by woody plants (indicated by their delta N-15 signatures) remained unchanged up to N addition rates of 12 kg ha(-1)yr(-1) or greater. Finally, we demonstrate that approximately 71.8% of the boreal forest experiences N-r deposition rates at or below 3 kg ha(-1)yr(-1), suggesting that bryophytes likely limit woody plant acquisition of ambient anthropogenic Nr inputs throughout a majority of the boreal forest.
引用
收藏
页码:2743 / 2753
页数:11
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