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波罗的海氧化还原梯度中病毒衰变率低导致病毒丰度高。

High viral abundance as a consequence of low viral decay in the Baltic Sea redoxcline.

作者信息

Köstner Nicole, Scharnreitner Lisa, Jürgens Klaus, Labrenz Matthias, Herndl Gerhard J, Winter Christian

机构信息

Department of Limnology and Bio-Oceanography, University of Vienna, Vienna, Austria.

Department of Biological Oceanography, Leibniz Institute for Baltic Sea Research (IOW), Rostock-Warnemünde, Germany.

出版信息

PLoS One. 2017 Jun 8;12(6):e0178467. doi: 10.1371/journal.pone.0178467. eCollection 2017.

Abstract

Throughout the Baltic Sea redoxcline, virus production and the frequency of lytically-infected prokaryotic cells were estimated from parallel incubations of undiluted seawater and seawater that contained prokaryotes with substantially reduced numbers of viruses (virus dilution approach), effectively preventing viral reinfection during the incubation period. Undiluted seawater incubations resulted in much higher estimates of virus production (6-35×104 mL-1 h-1) and the frequency of infected cells (5-84%) than the virus dilution approach (virus production: 1-3×104 mL-1 h-1; frequency of infected cells: 1-11%). Viral production and the frequency of infected cells from both approaches, however, cannot be directly compared, as data obtained from undiluted incubations were biased by viral reinfection and other uncontrollable processes during the incubation period. High in situ viral abundance (1-2×107 mL-1) together with low virus production rates based on the virus dilution approach resulted in some of the longest viral turnover times (24-84 d) ever reported for the epipelagial. Throughout a wide range of environmental conditions, viral turnover time and burst size were negatively correlated. Given that viral decay estimated in ultra-filtered water was below the detection limit and the burst size was low (1-17), we conclude that prokaryotic viruses in the Baltic Sea redoxcline are investing most of their resources into stress defense (strong capsids) rather than proliferation (high burst size). In summary, the Baltic Sea redoxcline constitutes an environment where low virus production is found in combination with low viral decay, resulting in high viral abundance.

摘要

在整个波罗的海氧化还原跃层,通过对未稀释海水和含有数量大幅减少的病毒的海水(病毒稀释法)进行平行培养,估算病毒产生量和溶菌感染原核细胞的频率,这有效地防止了培养期间的病毒再感染。未稀释海水培养得出的病毒产生量(6 - 35×10⁴ mL⁻¹ h⁻¹)和感染细胞频率(5 - 84%)比病毒稀释法(病毒产生量:1 - 3×10⁴ mL⁻¹ h⁻¹;感染细胞频率:1 - 11%)高得多。然而,由于未稀释培养获得的数据在培养期间受到病毒再感染和其他不可控过程的影响而存在偏差,因此两种方法得出的病毒产生量和感染细胞频率无法直接比较。基于病毒稀释法,原位病毒丰度高(1 - 2×10⁷ mL⁻¹)且病毒产生率低,导致了一些在海洋上层报道过的最长病毒周转时间(24 - 84天)。在广泛的环境条件下,病毒周转时间和爆发大小呈负相关。鉴于超滤水中估计的病毒衰减低于检测限且爆发大小较低(1 - 17),我们得出结论,波罗的海氧化还原跃层中的原核病毒将其大部分资源投入到应激防御(强衣壳)而非增殖(高爆发大小)中。总之,波罗的海氧化还原跃层构成了一个病毒产生量低且病毒衰减低相结合,从而导致病毒丰度高的环境。

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