Natural Resources Institute Finland (Luke), Latokartanonkaari 9, FI-00790 Helsinki, Finland.
Natural Resources Institute Finland (Luke), Latokartanonkaari 9, FI-00790 Helsinki, Finland.
Sci Total Environ. 2019 Feb 25;653:995-1004. doi: 10.1016/j.scitotenv.2018.10.364. Epub 2018 Oct 29.
Biological fixation of atmospheric nitrogen (N) by bryophyte-associated cyanobacteria is an important source of plant-available N in the boreal biome. Information on the factors that drive biological N fixation (BNF) rates is needed in order to understand the N dynamics of forests under a changing climate. We assessed the potential of several cryptogam species (the feather mosses Hylocomium splendens and Pleurozium schreberi, a group of Dicranum bryophytes, two liverworts, and Cladina lichens) to serve as associates of cyanobacteria or other N-fixing bacteria (diazotrophs) using acetylene reduction assay (ARA). We tested the hypotheses that the legacy of chronic atmospheric N deposition reduces BNF in the three bryophyte species, sampled from 12 coniferous forests located at latitudes 60-68° N in Finland. In addition, we tested the effect of moisture and temperature on BNF. All species studied showed a BNF signal in the north, with the highest rates in feather mosses. In moss samples taken along the north-south gradient with an increasing N bulk deposition from 0.8 to 4.4 kg ha year, we found a clear decrease in BNF in both feather mosses and Dicranum group. BNF turned off at N deposition of 3-4 kg ha year. Inorganic N (NH-N + NO-N) best predicted the BNF rate among regression models with different forms of N deposition as explanatory variables. However, in southern spruce stands, tree canopies modified the N in throughfall so that dissolved organic N (DON) leached from canopies compensated for inorganic N retained therein. Here, both DON and inorganic N negatively affected BNF in H. splendens. In laboratory experiments, BNF increased with increasing temperature and moisture. Our results suggest that even relatively low N deposition suppresses BNF in bryophyte-associated diazotrophs. Further, BNF could increase in northern low-deposition areas, especially if climate warming leads to moister conditions, as predicted.
苔藓植物相关蓝藻的生物固氮(BNF)是北方生物群中植物可用氮的重要来源。为了了解气候变化下森林的氮动态,需要了解驱动生物固氮(BNF)速率的因素。我们使用乙炔还原测定法(ARA)评估了几种隐花植物物种(华丽羽藓、粗枝羽藓、一组角苔、两种地钱和石地钱)作为蓝藻或其他固氮细菌(固氮菌)伴生物的潜力。我们检验了以下假设:慢性大气氮沉降减少了从纬度 60-68° N 的芬兰 12 个针叶林采集的三种苔藓植物的 BNF。此外,我们还测试了水分和温度对 BNF 的影响。所有研究的物种在北方都显示出 BNF 信号,羽藓的速率最高。在沿着南北梯度的苔藓样本中,随着氮总沉积从 0.8 到 4.4kg/公顷的增加,我们发现羽藓和角苔组的 BNF 明显减少。当氮沉积达到 3-4kg/公顷时,BNF 关闭。在具有不同形式氮沉积作为解释变量的回归模型中,无机氮(NH-N+NO-N)最好地预测了 BNF 速率。然而,在南部云杉林分中,树冠改变了穿透雨的氮,使得从树冠中淋滤出的溶解有机氮(DON)补偿了其中保留的无机氮。在这里,DON 和无机氮都对 H. splendens 的 BNF 产生负面影响。在实验室实验中,BNF 随温度和水分的增加而增加。我们的结果表明,即使是相对较低的氮沉积也会抑制苔藓植物相关固氮菌的 BNF。此外,如果气候变暖导致条件更加湿润,正如预测的那样,北方低氮沉积区的 BNF 可能会增加。