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微生物氮营养与东非湖泊溶解有机质特性有关。

Microbial nitrogen nutrition links to dissolved organic matter properties in East African lakes.

机构信息

Key Laboratory of Lake and Watershed Science for Water Security, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China; State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China.

Key Laboratory of Lake and Watershed Science for Water Security, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China; State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China; University of Chinese Academy of Sciences, Nanjing 211135, China.

出版信息

Sci Total Environ. 2024 Nov 10;950:175197. doi: 10.1016/j.scitotenv.2024.175197. Epub 2024 Jul 31.

Abstract

East African lakes, especially soda lakes, are home habitats for massive numbers of wildlife such as flamingos, mammals, and fishes. These lakes are known for their high primary production due to local high temperatures, light intensities, and alkalinity (inorganic carbon). However, these lakes, normally within remote areas, receive low nutrient inputs. Ammonium (NH) recycling and/or nitrogen fixation can become the major N supply mechanisms for phytoplankton. However, the driving forces on microbial N nutrition in lakes with minimal anthropogenic disturbance remain poorly understood. Using stable isotope tracer techniques, NH recycling rates were measured in 18 lakes and reservoirs in East Africa (Tanzania and Kenya) during the dry season in early 2020. Three functional genes (nifH, gdh, and ureC) relating to microbial N nutrition were also measured. The regeneration of NH supported up to 71 % of the NH uptake. Positive community biological NH demands (CBAD) for all lakes and reservoirs indicate an obvious N demand from microbial community. Our study provides clear evidence that microbial NH uptake rates linked closely to the dissolved organic matter (DOM) properties (e.g., the absorption coefficient at 254 nm, percents of total fluorescence intensity contributed by microbial humic-like and protein-like components) and that water residence time drives microbial NH recycling by regulating the duration of in-lake DOM processing and influencing algal growth. Phytoplankton, especially those of Cyanophyceae, showed maximum biomass and higher NH recycling rates at a certain range of water residence time (e.g., 5-8 years). However, CBAD showed a decreasing trend with longer water residence time, which may be influenced by changes in the algal community composition (e.g., % Cyanophyceae vs. % Bacillariophyceae). These results indicate that DOM dynamics and the water residence time have the potential to facilitate the understanding of microbial nitrogen supply status in East African lakes.

摘要

东非湖泊,尤其是苏打湖,是大量野生动物的栖息地,如火烈鸟、哺乳动物和鱼类。这些湖泊以其高初级生产力而闻名,这是由于当地高温、高强度光照和高碱性(无机碳)造成的。然而,这些湖泊通常位于偏远地区,营养输入较低。氨(NH)循环和/或氮固定可能成为浮游植物的主要氮供应机制。然而,在受人为干扰最小的湖泊中,微生物氮营养的驱动力仍知之甚少。本研究利用稳定同位素示踪技术,于 2020 年初旱季在东非(坦桑尼亚和肯尼亚)的 18 个湖泊和水库中测量了 NH 循环率。还测量了与微生物氮营养有关的三个功能基因(nifH、gdh 和 ureC)。NH 的再生支持了高达 71%的 NH 吸收。所有湖泊和水库的群落生物 NH 需求(CBAD)表明微生物群落存在明显的氮需求。本研究提供了明确的证据,表明微生物 NH 吸收速率与溶解有机质(DOM)特性密切相关(例如,254nm 处的吸收系数、微生物腐殖质和蛋白质样成分贡献的总荧光强度的百分比),并且水停留时间通过调节 DOM 在湖内的处理时间和影响藻类生长来驱动微生物 NH 循环。浮游植物,特别是蓝藻,在一定的水停留时间(例如 5-8 年)范围内表现出最大的生物量和更高的 NH 循环率。然而,CBAD 随着水停留时间的延长呈下降趋势,这可能受到藻类群落组成变化的影响(例如,%蓝藻与%硅藻的比例)。这些结果表明,DOM 动态和水停留时间有可能促进对东非湖泊微生物氮供应状况的理解。

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