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首页> 外文期刊>Global change biology >Bryophytes attenuate anthropogenic nitrogen inputs in boreal forests
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Bryophytes attenuate anthropogenic nitrogen inputs in boreal forests

机译:苔藓植物减弱了北方森林的人为氮输入

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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.
机译:北方生态系统的生产力主要受到可用土壤氮(N)的限制,并且人们对于了解人为衍生的反应性氮(Nr)的沉积是否会导致木本植物获得更多的氮,从而导致更多的碳(C)感兴趣。隔离。可能限制木本植物获取N-r的一个因素是苔藓植物的存在,苔藓植物是一个重要的C和N池,并且是发生关联的蓝细菌N-固定的位置。在瑞典北部的北方地区,使用重复的标准规模的N加法实验(五个级别:0、3、6、12和50 kg N ha(-1)yr(-1); n = 6),我们验证了Nr螯合到苔藓植物组织中以及N固定下调会减弱Nr输入的假设,从而限制了木本植物对人为Nr的吸收。我们的数据表明,每增加苔藓的质量和每单位面积的固氮率,都会随着添加氮的增加而急剧下降。另外,随着氮素添加量的增加,schleuberi的组织氮浓度增加,生物量减少。这种对增加的氮添加的响应使施氏假单胞菌的氮库几乎保持稳定,但氮添加率最高,但显着下降。在最低的N-r添加速率下,改变的N-固着和schreberi生物量N的组合效应占累积N-r添加的56.7%,但在所有其他处理中仅占很小的比例。这种“苔藓植物效应”可以部分解释为什么直到12 kg ha(-1)yr(-1)的氮添加量时,木本植物的土壤无机氮的有效性和获取(由其N-15三角洲指示)仍保持不变。更大。最后,我们证明了大约71.8%的北方森林在3 kg ha(-1)yr(-1)或低于3 kg ha(-1)yr(-1)时经历了Nr沉积速率,这表明苔藓植物可能会限制大多数人的木本植物对环境人为Nr输入的获取。针叶林。

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