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间歇性盐化溪流中凋落物微生物分解作用

Leaf litter microbial decomposition in salinized streams under intermittency.

机构信息

Centre for Functional Ecology, Department of Life Sciences, University of Coimbra, Calçada Martim de Freitas, 3000-456 Coimbra, Portugal.

Centre for Functional Ecology, Department of Life Sciences, University of Coimbra, Calçada Martim de Freitas, 3000-456 Coimbra, Portugal.

出版信息

Sci Total Environ. 2019 Feb 25;653:1204-1212. doi: 10.1016/j.scitotenv.2018.11.050. Epub 2018 Nov 6.

DOI:10.1016/j.scitotenv.2018.11.050
PMID:30759560
Abstract

Human-induced salinization of freshwaters constitutes a growing global problem, whose consequences on streams functioning are largely unknown. Climate change projections predict enhanced evaporation, as well as an increase in extreme events and in variability of precipitation. This will result in more frequent, extended and severe drought periods that may aggravate water salinization of streams and rivers. In this study we conducted a microcosm experiment to assess the combined effects of three drought regimes - abrupt (AD), slow (SD) and very slow transition to dryness (VSD) - and three levels of salinization (0, 4, 6 g L NaCl) on microbial-mediated oak leaf decomposition over ten weeks. Salinization did not affect mass loss and associated microbial respiration of colonized oak leaves but significantly reduced the biomass and eliminated the sporulating capacity of fungi. Desiccation negatively affected leaf decomposition regardless of regime. Even though microbial respiration did not react to the different treatments, lower fungal biomass, diversity, and conidial production were observed under AD; for fungal biomass these effects were amplified at higher salt concentrations (particularly at 6 g L). Our results indicate that effects of leaf litter desiccation depend on the rate of transition between wet and dry conditions and on the level of salt in the water. The two factors jointly affect decomposer survival and activity and, by extension, the dynamics of detrital food webs in streams.

摘要

人为引起的淡水盐化是一个日益严重的全球性问题,其对溪流功能的影响在很大程度上尚不清楚。气候变化预测表明蒸发量会增加,极端事件和降水变率也会增加。这将导致更频繁、持续时间更长和更严重的干旱期,可能会加剧溪流和河流的水盐化。在这项研究中,我们进行了一个微宇宙实验,以评估三种干旱制度——突然(AD)、缓慢(SD)和非常缓慢向干旱过渡(VSD)——以及三种盐度水平(0、4、6 g L NaCl)对微生物介导的栎树叶分解的综合影响,持续十周。盐度处理并没有影响被定殖栎树叶的质量损失和相关微生物呼吸作用,但显著降低了真菌的生物量并消除了真菌的产孢能力。无论干旱制度如何,干燥都会对叶片分解产生负面影响。尽管微生物呼吸作用对不同处理没有反应,但在 AD 条件下,观察到较低的真菌生物量、多样性和分生孢子产生;对于真菌生物量,这些影响在更高的盐浓度下(特别是在 6 g L 时)会加剧。我们的结果表明,凋落物干燥的影响取决于干湿条件转变的速度和水中盐度的水平。这两个因素共同影响分解者的生存和活性,并进一步影响溪流碎屑食物网的动态。

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