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Bacterial-viral interactions in the sea surface microlayer of a black carbon-dominated tropical coastal ecosystem (Halong Bay, Vietnam)

机译:黑色碳为主的热带沿海生态系统(越南下龙湾)海表微层中的细菌-病毒相互作用

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Increasing human activity has raised concerns about the impact of deposition of anthropogenic combustion aerosols (i.e., black carbon; BC) on marine processes. The sea surface microlayer (SML) is a key gate for the introduction of atmospheric BC into the ocean; however, relatively little is known of the effects of BC on bacteria-virus interactions, which can strongly influence microbially mediated processes. To study the impact of BC on bacteria-virus interactions, field investigations involving collection from the SML and underlying water were carried out in Halong Bay (Vietnam). Most inorganic nutrient concentrations, as well as dissolved organic carbon, were modestly but significantly higher ( p = 0.02–0.05) in the SML than in underlying water. The concentrations of particulate organic carbon (though not chlorophyll a ) and of total particulate carbon, which was composed largely of particulate BC (mean = 1.7 ± 6.4 mmol L~(–1)), were highly enriched in the SML, and showed high variability among stations. On average, microbial abundances (both bacteria and viruses) and bacterial production were 2- and 5fold higher, respectively, in the SML than in underlying water. Significantly lower bacterial production ( p 0.01) was observed in the particulate fraction (3 μm) compared to the bulk sample, but our data overall suggest that bacterial production in the SML was stimulated by particulate BC. Higher bacterial production in the SML than in underlying water supported high viral lytic infection rates (from 5.3 to 30.1%) which predominated over percent lysogeny (from undetected to 1.4%). The sorption of dissolved organic carbon by black carbon, accompanied by the high lytic infection rate in the black carbon-enriched SML, may modify microbially mediated processes and shift the net ecosystem metabolism (ratio of production and respiration) to net heterotrophy and CO_(2 )production in this critical layer between ocean and atmosphere.
机译:人类活动的增加引起了对人为燃烧气溶胶(即黑碳; BC)沉积对海洋过程的影响的关注。海面微层(SML)是将大气BC引入海洋的关键大门。然而,关于细菌-病毒相互作用的影响,细菌污染的影响知之甚少,而细菌与病毒的相互作用会强烈影响微生物介导的过程。为了研究BC对细菌-病毒相互作用的影响,在越南下龙湾进行了现场调查,涉及从SML和下层水收集。在SML中,大多数无机营养物浓度以及溶解的有机碳均适度但显着高于底层水中(p = 0.02-0.05)。 SML中高度富集了颗粒有机碳(尽管不是叶绿素a)和总颗粒碳的浓度,其中大部分由BC颗粒组成(平均值= 1.7±6.4 mmol L〜(-1))。站之间的变异性。平均而言,SML中的微生物丰度(细菌和病毒)和细菌产量分别比底层水高2到5倍。与散装样品相比,在颗粒级分(> 3μm)中观察到明显更低的细菌产生(p <0.01),但我们的数据总体表明,SML中的细菌产生受到颗粒BC的刺激。 SML中细菌的产生高于底层水中的细菌产生,支持较高的病毒裂解感染率(从5.3%到30.1%),而溶菌性百分比则占主导地位(从未发现到1.4%)。黑碳对溶解有机碳的吸附,以及富含黑碳的SML的高裂解感染率,可能会改变微生物介导的过程,并将净生态系统代谢(生产和呼吸比)转变为净异养和CO_(2 )在海洋和大气之间的这一关键层中进行生产。

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