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凋落针叶分解与根际活性之间的反馈相互作用。

Feedback interactions between needle litter decomposition and rhizosphere activity.

作者信息

Subke Jens-Arne, Hahn Volker, Battipaglia Giovanna, Linder Sune, Buchmann Nina, Cotrufo M Francesca

机构信息

Department of Environmental Sciences, Second University of Naples, Via Vivaldi 43, 81100 Caserta, Italy.

出版信息

Oecologia. 2004 May;139(4):551-9. doi: 10.1007/s00442-004-1540-4. Epub 2004 Mar 20.

Abstract

The aim of our study was to identify interactions between the decomposition of aboveground litter and rhizosphere activity. The experimental approach combined the placement of labelled litter (delta13C=-37.9 per thousand ) with forest girdling in a 35-year-old Norway spruce stand, resulting in four different treatment combinations: GL (girdled, litter), GNL (girdled, no litter), NGL (not girdled, litter), and NGNL (not girdled, no litter). Monthly sampling of soil CO2 efflux and delta13C of soil respired CO2 between May and October 2002 allowed the partitioning of the flux into that derived from the labelled litter, and that derived from native soil organic matter and roots. The effect of forest girdling on soil CO2 efflux was detectable from June (girdling took place in April), and resulted in GNL fluxes to be about 50% of NGNL fluxes by late August. The presence of litter resulted in significantly increased fluxes for the first 2 months of the experiment, with significantly greater litter derived fluxes from non-girdled plots and a significant interaction between girdling and litter treatments over the same period. For NGL collars, the additional efflux was found to originate only in part from litter decomposition, but also from the decay of native soil organic matter. In GL collars, this priming effect was not significant, indicating an active role of the rhizosphere in soil priming. The results therefore indicate mutual positive feedbacks between litter decomposition and rhizosphere activity. Soil biological analysis (microbial and fungal biomass) of the organic layers indicated greatest activity below NGL collars, and we suppose that this increase indicates the mechanism of mutual positive feedback between rhizosphere activity and litter decomposition. However, elimination of fresh C input from both above- and belowground (GNL) also resulted in greater fungal abundance than for the NGNL treatment, indicating likely changes in fungal community structure (i.e. a shift from symbiotic to saprotrophic species abundance).

摘要

我们研究的目的是确定地上凋落物分解与根际活动之间的相互作用。实验方法是在一片35年生的挪威云杉林中,将标记凋落物(δ¹³C = -37.9‰)的放置与环剥处理相结合,产生四种不同的处理组合:GL(环剥,有凋落物)、GNL(环剥,无凋落物)、NGL(未环剥,有凋落物)和NGNL(未环剥,无凋落物)。在2002年5月至10月期间,每月对土壤二氧化碳通量和土壤呼吸二氧化碳的δ¹³C进行采样,从而将通量划分为来自标记凋落物的通量以及来自原生土壤有机质和根系的通量。森林环剥对土壤二氧化碳通量的影响从6月开始可检测到(环剥在4月进行),到8月底,GNL通量约为NGNL通量的50%。在实验的前两个月,凋落物的存在导致通量显著增加,非环剥地块来自凋落物的通量显著更大,并且在同一时期环剥和凋落物处理之间存在显著的相互作用。对于NGL处理区,额外的通量被发现仅部分源自凋落物分解,还源自原生土壤有机质的分解。在GL处理区,这种激发效应不显著,表明根际在土壤激发中发挥了积极作用。因此,结果表明凋落物分解与根际活动之间存在相互的正反馈。对有机层进行的土壤生物学分析(微生物和真菌生物量)表明,NGL处理区下方的活性最高,我们推测这种增加表明了根际活动与凋落物分解之间相互正反馈的机制。然而,地上和地下新鲜碳输入的消除(GNL)也导致真菌丰度高于NGNL处理,表明真菌群落结构可能发生了变化(即从共生物种到腐生物种丰度的转变)。

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