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长期磷脉冲后河流生物膜中细胞内磷摄取的饱和和细胞外磷捕获的流行:对河流自净的影响。

Saturation of intracellular phosphorus uptake and prevalence of extracellular phosphorus entrapment in fluvial biofilms after long-term P pulses: Implications for river self-purification.

机构信息

Department of River Ecology, Helmholtz Centre for Environmental Research - UFZ, Brueckstrasse 3a, 39114 Magdeburg, Germany.

Department of River Ecology, Helmholtz Centre for Environmental Research - UFZ, Brueckstrasse 3a, 39114 Magdeburg, Germany.

出版信息

Sci Total Environ. 2024 Nov 20;952:175976. doi: 10.1016/j.scitotenv.2024.175976. Epub 2024 Sep 4.

DOI:10.1016/j.scitotenv.2024.175976
PMID:39241886
Abstract

Microbial consortia in riverbed substrates and their extracellular matrix (biofilms) play a key role in phosphorus (P) entrapment. When P entrapment saturates, the benthic compartment changes from a P sink to a P source thus increasing eutrophication risk. P entrapment saturation is expected to differ between intracellular and extracellular P entrapment and between different magnitudes and durations of P inputs. We studied biofilm P-entrapment following short (48 h) and long (14 days) P loading events in stream bypass flumes supplied with a gradient of dissolved P concentrations. This allowed us to link local biofilm processes in sediments to potential effects on river self-purification, via quantifying the P removal efficiency in the flumes. We found that in short-term events, biofilms develop intracellular mechanisms to cope with P inputs, while long-term events and high P inputs suppress the intracellular uptake mechanisms and increase the prevalence of extracellular entrapment. Specifically, long-term events lowered the threshold for intracellular P entrapment saturation, and decreased the ratio between intracellular and extracellular entrapment resulting in lower removal efficiency for dissolved phosphorus. Our results highlight the risk that aquatic ecosystems may face as the ratio of intracellular to extracellular P entrapment decreases, which may reduce their ability to deal with P inputs, thereby increasing risks of eutrophication.

摘要

河床基质中的微生物群落及其细胞外基质(生物膜)在磷(P)固定中起着关键作用。当 P 固定达到饱和时,底栖区就会从 P 汇转变为 P 源,从而增加富营养化风险。细胞内和细胞外 P 固定、P 输入的幅度和持续时间的不同,预计会导致 P 固定饱和度的差异。我们在提供溶解 P 浓度梯度的溪流旁路水槽中进行了短期(48 小时)和长期(14 天)P 加载实验,研究了生物膜的 P 固定作用。这使我们能够通过量化水槽中的 P 去除效率,将沉积物中局部生物膜过程与对河流自净的潜在影响联系起来。我们发现,在短期事件中,生物膜会发展出细胞内机制来应对 P 输入,而长期事件和高 P 输入会抑制细胞内吸收机制,并增加细胞外固定的普遍性。具体而言,长期事件降低了细胞内 P 固定饱和度的阈值,并降低了细胞内和细胞外固定之间的比例,从而导致溶解磷的去除效率降低。我们的研究结果强调了水生生态系统可能面临的风险,即细胞内与细胞外 P 固定的比例降低,这可能会降低它们处理 P 输入的能力,从而增加富营养化的风险。

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