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雨影海岸花旗松林中凋落物分解四年期间,凋落物化学性质和天气对真菌群落组成的影响

Fungal Community Composition as Affected by Litter Chemistry and Weather during Four Years of Litter Decomposition in Rainshadow Coastal Douglas-Fir Forests.

作者信息

Shay Philip-Edouard, Winder Richard S, Constabel C Peter, Trofymow J A Tony

机构信息

Centre for Forest Biology, Department of Biology, University of Victoria, Victoria, BC V8W 3N5, Canada.

Pacific Forestry Centre, Canadian Forest Service, 506 West Burnside Road, Victoria, BC V8Z 1M5, Canada.

出版信息

J Fungi (Basel). 2022 Jul 16;8(7):735. doi: 10.3390/jof8070735.

DOI:10.3390/jof8070735
PMID:35887490
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9323820/
Abstract

Climate and litter chemistry are major factors influencing litter decay, a process mediated by microbes, such as fungi, nitrogen-fixing bacteria and ammonia-oxidizing bacteria. Increasing atmospheric CO concentrations can decrease nitrogen (N) and increase condensed tannin (CT) content in foliar litter, reducing litter quality and slowing decomposition. We hypothesized that reduced litter quality inhibits microbes and is the mechanism causing decomposition to slow. Litterbags of Douglas-fir needles and poplar leaves with a range of N (0.61-1.57%) and CT (2.1-29.1%) treatment and natural acid unhydrolyzable residue (35.3-41.5%) concentrations were placed along climatic gradients in mature Douglas-fir stands of coastal British Columbia rainshadow forests. The structure (diversity, richness and evenness) and composition of microbial communities were analyzed using DGGE profiles of 18S, NifH-universal and AmoA PCR amplicons in foliar litter after 7, 12, 24 and 43 months of decay. High CT and low N concentrations in leaf litter were associated with changes in microbial community composition, especially fungi. Contrary to our hypothesis, high CT and low N treatments did not inhibit microbial colonization or diversity. The joint effects of air temperature and soil moisture on microbial community composition at our sites were more important than the effects of initial litter chemistry.

摘要

气候和凋落物化学是影响凋落物分解的主要因素,凋落物分解过程由微生物介导,如真菌、固氮细菌和氨氧化细菌。大气中二氧化碳浓度增加会降低叶凋落物中的氮(N)含量并增加缩合单宁(CT)含量,从而降低凋落物质量并减缓分解。我们假设凋落物质量下降会抑制微生物,这是导致分解减缓的机制。将具有一系列氮(0.61 - 1.57%)、缩合单宁(2.1 - 29.1%)处理以及天然酸性不可水解残渣(35.3 - 41.5%)浓度的花旗松针叶和杨树叶片凋落物袋,沿着不列颠哥伦比亚省沿海雨影森林成熟花旗松林中的气候梯度放置。在凋落7、12、24和43个月后,使用18S、NifH通用和AmoA PCR扩增子的DGGE图谱分析叶凋落物中微生物群落的结构(多样性、丰富度和均匀度)和组成。叶凋落物中高缩合单宁和低氮浓度与微生物群落组成的变化有关,尤其是真菌。与我们的假设相反,高缩合单宁和低氮处理并未抑制微生物定殖或多样性。在我们的研究地点,气温和土壤湿度对微生物群落组成的联合影响比初始凋落物化学的影响更重要。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f3db/9323820/cb18e260d152/jof-08-00735-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f3db/9323820/905849c993f8/jof-08-00735-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f3db/9323820/d35f106b9b2a/jof-08-00735-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f3db/9323820/b0c7095f5025/jof-08-00735-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f3db/9323820/cb18e260d152/jof-08-00735-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f3db/9323820/905849c993f8/jof-08-00735-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f3db/9323820/d35f106b9b2a/jof-08-00735-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f3db/9323820/b0c7095f5025/jof-08-00735-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f3db/9323820/cb18e260d152/jof-08-00735-g004.jpg

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