Moss removal facilitates decomposition and net nitrogen loss of monospecific and mixed-species litter in a boreal peatland

IF 3.9 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Xinhou Zhang, Wei Chen, Weixiang Chen, Xianwei Wang, Rong Mao
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Abstract

Litter decomposition plays an important role in biogeochemical cycling in boreal peatlands, where mosses, especially Sphagnum species, are a determinant. In recent decades, these peatlands have experienced a decline in moss cover due to abrupt climate warming and atmospheric nitrogen (N) deposition. To reveal the effect of the reduction in moss cover on litter decomposition, we adopted a field living moss removal experiment (with the senesced tissues remaining) in a Sphagnum-dominated boreal peatland, and investigated litter mass loss and net N loss of three deciduous woody species decomposing in monocultures and mixtures over 3 years. Based on the observed and predicted mass loss and net N loss of litter mixtures, we divided litter mixing effects into additive (no significant difference), synergistic (observed value greater than predicted value), and antagonistic (observed value lower than predicted value) effects. Across 3 years of decomposition, moss removal increased litter mass loss and net N loss, irrespective of single- or mixed-species compositions. Moss removal generally changed litter mixing effects on mass loss from antagonistic to additive effects in the initial 2 years, but from synergistic to additive effects after 3 years of decomposition. Regarding net N loss of litter mixtures, moss removal often resulted in a shift from additive to synergistic effects or from antagonistic to additive effects after 2 and 3 years of decomposition. Our observations suggest that the declines in living moss cover can accelerate litter decomposition and nutrient release, and highlight that living moss loss makes litter mixture decomposition predictable by reducing non-additive effects in boreal peatlands. Given the widespread occurrence of reduced moss cover in boreal peatlands, the mechanisms explaining living moss controls on litter decomposition and N cycling should receive significant attention in further studies.

Abstract Image

在北方泥炭地清除苔藓有助于单种和混种枯落物的分解和净氮损失
腐殖质分解在北方泥炭地的生物地球化学循环中发挥着重要作用,而苔藓,尤其是泥炭藓物种,是泥炭地的一个决定性因素。近几十年来,由于气候骤然变暖和大气中氮(N)的沉积,这些泥炭地的苔藓覆盖率下降。为了揭示苔藓覆盖率下降对枯落物分解的影响,我们在以泥炭藓为主的北方泥炭地进行了一次野外活体苔藓清除实验(保留衰老组织),并调查了三种落叶木本物种在单一栽培和混合栽培中三年的枯落物质量损失和净氮损失。根据观察到的和预测的枯落物混合物的质量损失和净氮损失,我们将枯落物混合效应分为相加效应(无显著差异)、协同效应(观察值大于预测值)和拮抗效应(观察值低于预测值)。在 3 年的分解过程中,不管是单一物种还是混合物种,去除苔藓都会增加枯落物的质量损失和净氮损失。在最初的 2 年中,苔藓的清除通常会使垃圾混合对质量损失的影响从拮抗作用变为相加作用,但在 3 年的分解后,则会从协同作用变为相加作用。关于枯落物混合物的净氮损失,去除苔藓通常会导致从相加效应到协同效应的转变,或在分解 2 年和 3 年后从拮抗效应到相加效应的转变。我们的观察结果表明,活苔藓覆盖率的下降会加速枯落物的分解和养分的释放,并强调活苔藓的消失会减少北方泥炭地的非相加效应,从而使枯落物混合物的分解变得可预测。鉴于北方泥炭地普遍存在苔藓覆盖率降低的情况,活苔藓对废弃物分解和氮循环的控制机制应在进一步的研究中得到重视。
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来源期刊
Biogeochemistry
Biogeochemistry 环境科学-地球科学综合
CiteScore
7.10
自引率
5.00%
发文量
112
审稿时长
3.2 months
期刊介绍: Biogeochemistry publishes original and synthetic papers dealing with biotic controls on the chemistry of the environment, or with the geochemical control of the structure and function of ecosystems. Cycles are considered, either of individual elements or of specific classes of natural or anthropogenic compounds in ecosystems. Particular emphasis is given to coupled interactions of element cycles. The journal spans from the molecular to global scales to elucidate the mechanisms driving patterns in biogeochemical cycles through space and time. Studies on both natural and artificial ecosystems are published when they contribute to a general understanding of biogeochemistry.
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