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裂解性噬菌体对磷限制与氮限制海洋微生物的影响

Impact of Lytic Phages on Phosphorus- vs. Nitrogen-Limited Marine Microbes.

作者信息

Pourtois Julie, Tarnita Corina E, Bonachela Juan A

机构信息

Department of Biology, Stanford University, Stanford, CA, United States.

Department of Ecology and Evolutionary Biology, Princeton University, Princeton, NJ, United States.

出版信息

Front Microbiol. 2020 Feb 21;11:221. doi: 10.3389/fmicb.2020.00221. eCollection 2020.

Abstract

Lytic viruses kill almost 20% of marine bacteria every day, re-routing nutrients away from the higher trophic levels of the marine food web and back in the microbial loop. Importantly, the effect of this inflow of key elements on the ecosystem depends on the nutrient requirements of bacteria as well as on the elemental composition of the viruses that infect them. Therefore, the influence of viruses on the ecosystem could vary depending on which nutrient is limiting. In this paper, we considered an existing multitrophic model (nutrient, bacteria, zooplankton, and viruses) that accounts for nitrogen limitation, and developed a phosphorus-limited version to assess whether the limiting nutrient alters the role of viruses in the ecosystem. For both versions, we evaluated the stationary state of the system with and without viruses. In agreement with existing results, nutrient release increased with viruses for nitrogen-limited systems, while zooplankton abundance and export to higher trophic levels decreased. We found this to be true also for phosphorus-limited systems, although nutrient release increased less than in nitrogen-limited systems. The latter supports a nutrient-specific response of the ecosystem to viruses. Bacterial concentration decreased in the phosphorus-limited system but increased in most nitrogen-limited cases due to a switch from mostly bottom-up to entirely top-down control by viruses. Our results also show that viral concentration is best predicted by a power-law of bacterial concentration with exponent different from 1. Finally, we found a positive correlation between carbon export and viruses regardless of the limiting nutrient, which led us to suggest viral abundance as a predictor of carbon sink.

摘要

裂解性病毒每天会杀死近20%的海洋细菌,使营养物质从海洋食物网的较高营养级重新转移回微生物环中。重要的是,这种关键元素的流入对生态系统的影响取决于细菌的营养需求以及感染它们的病毒的元素组成。因此,病毒对生态系统的影响可能会因限制营养物质的不同而有所变化。在本文中,我们考虑了一个现有的多营养级模型(营养物质、细菌、浮游动物和病毒),该模型考虑了氮限制,并开发了一个磷限制版本,以评估限制营养物质是否会改变病毒在生态系统中的作用。对于这两个版本,我们评估了有病毒和无病毒情况下系统的稳态。与现有结果一致,在氮限制系统中,营养物质的释放随着病毒的存在而增加,而浮游动物的丰度以及向较高营养级的输出则减少。我们发现磷限制系统也是如此,尽管营养物质的释放增加幅度小于氮限制系统。后者支持了生态系统对病毒的营养物质特异性响应。在磷限制系统中细菌浓度降低,但在大多数氮限制情况下由于病毒从主要的自下而上控制转变为完全的自上而下控制而增加。我们的结果还表明,病毒浓度最好通过细菌浓度的幂律来预测,其指数不同于1。最后,我们发现无论限制营养物质是什么,碳输出与病毒之间都存在正相关,这使我们建议将病毒丰度作为碳汇的一个预测指标。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3757/7047511/485cef17f92c/fmicb-11-00221-g0001.jpg

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