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早期山毛榉凋落物分解的特写研究:变化底物上的潜在驱动因素及微生物相互作用

A closeup study of early beech litter decomposition: potential drivers and microbial interactions on a changing substrate.

作者信息

Brandstätter Christian, Keiblinger Katharina, Wanek Wolfgang, Zechmeister-Boltenstern Sophie

机构信息

BFW - Federal Research and Training Centre for Forests, Natural Hazards and Landscape, Seckendorff-Gudent Weg 8, 1131 Vienna, Austria ; Institute for Water Quality, Resources and Waste Management, Vienna University of Technology, Karlsplatz 13/226, 1040 Vienna, Austria.

Institute of Soil Research, University of Natural Resources and Life Sciences, Peter-Jordan-Straße 82, 1190 Vienna, Austria.

出版信息

Plant Soil. 2013;371(1-2):139-154. doi: 10.1007/s11104-013-1671-7. Epub 2013 Mar 17.

Abstract

AIMS

Litter decomposition and subsequent nutrient release play a major role in forest carbon and nutrient cycling. To elucidate how soluble or bulk nutrient ratios affect the decomposition process of beech ( L.) litter, we conducted a microcosm experiment over an 8 week period. Specifically, we investigated leaf-litter from four Austrian forested sites, which varied in elemental composition (C:N:P ratio). Our aim was to gain a mechanistic understanding of early decomposition processes and to determine microbial community changes.

METHODS

We measured initial litter chemistry, microbial activity in terms of respiration (CO), litter mass loss, microbial biomass C and N (C and N), non purgeable organic carbon (NPOC), total dissolved nitrogen (TDN), NH, NO and microbial community composition (phospholipid fatty acids - PLFAs).

RESULTS

At the beginning of the experiment microbial biomass increased and pools of inorganic nitrogen (N) decreased, followed by an increase in fungal PLFAs. Sites higher in NPOC:TDN (C:N of non purgeable organic C and total dissolved N), K and Mn showed higher respiration.

CONCLUSIONS

The C:N ratio of the dissolved pool, rather than the quantity of N, was the major driver of decomposition rates. We saw dynamic changes in the microbial community from the beginning through the termination of the experiment.

摘要

目的

凋落物分解及随后的养分释放对森林碳和养分循环起着重要作用。为阐明可溶性或大量养分比例如何影响山毛榉(L.)凋落物的分解过程,我们进行了为期8周的微观实验。具体而言,我们研究了来自奥地利四个森林地点的凋落叶,这些凋落叶的元素组成(碳:氮:磷比例)各不相同。我们的目的是对早期分解过程有一个机理上的理解,并确定微生物群落的变化。

方法

我们测量了初始凋落物化学性质、以呼吸作用(CO)衡量的微生物活性、凋落物质量损失、微生物生物量碳和氮(C和N)、不可吹扫有机碳(NPOC)、总溶解氮(TDN)、NH、NO以及微生物群落组成(磷脂脂肪酸 - PLFAs)。

结果

在实验开始时,微生物生物量增加,无机氮(N)库减少,随后真菌PLFAs增加。NPOC:TDN(不可吹扫有机碳与总溶解氮的碳:氮比)、钾和锰含量较高的地点显示出较高的呼吸作用。

结论

溶解态库的碳:氮比而非氮的数量是分解速率的主要驱动因素。从实验开始到结束,我们观察到微生物群落的动态变化。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ee8b/4372839/fdc70aa163bc/11104_2013_1671_Fig1_HTML.jpg

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