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Latitudinal variation in virus-induced mortality of phytoplankton across the North Atlantic Ocean

机译:北大西洋海洋病毒引起的浮游植物死亡率的纬度变化

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摘要

Viral lysis of phytoplankton constrains marine primary production, food web dynamics and biogeochemical cycles in the ocean. Yet, little is known about the biogeographical distribution of viral lysis rates across the global ocean. To address this, we investigated phytoplankton group-specific viral lysis rates along a latitudinal gradient within the North Atlantic Ocean. The data show large-scale distribution patterns of different virus groups across the North Atlantic that are associated with the biogeographical distributions of their potential microbial hosts. Average virus-mediated lysis rates of the picocyanobacteria Prochlorococcus and Synechococcus were lower than those of the picoeukaryotic and nanoeukaryotic phytoplankton (that is, 0.14 per day compared with 0.19 and 0.23 per day, respectively). Total phytoplankton mortality (virus plus grazer-mediated) was comparable to the gross growth rate, demonstrating high turnover rates of phytoplankton populations. Virus-induced mortality was an important loss process at low and mid latitudes, whereas phytoplankton mortality was dominated by microzooplankton grazing at higher latitudes (>56°N). This shift from a viral-lysis-dominated to a grazing-dominated phytoplankton community was associated with a decrease in temperature and salinity, and the decrease in viral lysis rates was also associated with increased vertical mixing at higher latitudes. Ocean-climate models predict that surface warming will lead to an expansion of the stratified and oligotrophic regions of the world's oceans. Our findings suggest that these future shifts in the regional climate of the ocean surface layer are likely to increase the contribution of viral lysis to phytoplankton mortality in the higher-latitude waters of the North Atlantic, which may potentially reduce transfer of matter and energy up the food chain and thus affect the capacity of the northern North Atlantic to act as a long-term sink for CO2.
机译:浮游植物的病毒裂解会限制海洋的初级生产,食物网动态和海洋中的生物地球化学循环。然而,关于全球海洋中病毒裂解率的生物地理分布知之甚少。为了解决这个问题,我们调查了北大西洋内沿纬度梯度的浮游植物特异性病毒裂解率。数据显示了北大西洋地区不同病毒群的大规模分布模式,与其潜在微生物宿主的生物地理分布有关。微病毒蓝藻原球菌和聚球菌的平均病毒介导裂解率低于微核真核和纳米真核浮游植物(分别为每天0.14和每天0.19和0.23)。浮游植物总死亡率(病毒加放牧媒介介导的死亡率)与总增长率相当,表明浮游植物种群的高周转率。在低纬度和中纬度地区,病毒引起的死亡率是重要的损失过程,而在较高纬度(> 56°N)时,浮游植物的死亡率以放生的微浮游藻为主。从病毒裂解为主到浮游植物为主的浮游植物群落的这种转变与温度和盐度的降低有关,病毒裂解速率的降低也与高纬度地区的垂直混合增加有关。海洋气候模型预测,地表变暖将导致世界海洋的分层和贫营养区域扩大。我们的发现表明,未来这些海表层区域气候变化将可能增加病毒裂解对北大西洋高纬度水域浮游植物死亡率的贡献,从而有可能减少物质和能量在北大西洋的转移。食物链,从而影响北大西洋北部作为长期吸收二氧化碳的能力。

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