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二氧化碳浓度升高与气候变暖之间的相互作用可能会加大泥炭地集水区溶解性有机碳的输出量。

Interactions between elevated CO2 and warming could amplify DOC exports from peatland catchments.

作者信息

Fenner Nathalie, Freeman Christopher, Lock Maurice A, Harmens Harry, Reynolds Brian, Sparks Tim

机构信息

School of Biological Sciences, Memorial Building, University of Wales, Bangor, Deiniol Road, Bangor, Gwynedd, LL57 2UW, UK.

出版信息

Environ Sci Technol. 2007 May 1;41(9):3146-52. doi: 10.1021/es061765v.

Abstract

Peatlands export more dissolved organic carbon (DOC) than any other biome, contributing 20% of all terrestrial DOC exported to the oceans. Both warming and elevated atmospheric CO2 (eCO2) can increase DOC exports, but their interaction is poorly understood. Peat monoliths were, therefore, exposed to eCO2, warming and eCO2 + warming (combined). The combined treatment produced a synergistic (i.e., significant interaction) rise in DOC concentrations available for export (119% higher than the control, interaction P < 0.05) and enriched this pool with phenolic compounds (284%). We attribute this to increased plant inputs, coupled with impaired microbial degradation induced by competition with the vegetation for nutrients and inhibitory phenolics. Root biomass showed a synergistic increase (407% relative to the control, P < 0.1 only), while exudate inputs increased additively. Phenol oxidase was suppressed synergistically (58%, interaction P < 0.1 only) and beta-glucosidase (27%) additively, while microbial nutritional stress increased (51%) additively. Such results suggest intensified carbon exports from peatlands, with potentially widespread ramifications for aquatic processes in the receiving waters.

摘要

泥炭地输出的溶解有机碳(DOC)比其他任何生物群落都多,占陆地输出到海洋的所有DOC的20%。气候变暖和大气二氧化碳浓度升高(eCO2)都会增加DOC的输出,但它们之间的相互作用却鲜为人知。因此,将泥炭土柱暴露于eCO2、升温以及eCO2 + 升温(组合处理)环境中。组合处理使可供输出的DOC浓度产生了协同(即显著相互作用)升高(比对照高119%,相互作用P < 0.05),并使该库中的酚类化合物富集(增加了284%)。我们将此归因于植物输入增加,以及因与植被争夺养分和抑制性酚类物质而导致的微生物降解受损。根系生物量呈现协同增加(相对于对照增加407%,仅P < 0.1),而渗出物输入呈累加增加。酚氧化酶受到协同抑制(58%,仅相互作用P < 0.1),β-葡萄糖苷酶受到累加抑制(27%),而微生物营养胁迫呈累加增加(51%)。这些结果表明泥炭地的碳输出加剧,可能会对接收水体中的水生过程产生广泛影响。

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