比格尔海峡冬季微生物食物网的陆源溶解有机质输入和营养光限制条件

IF 4.6 Q2 MATERIALS SCIENCE, BIOMATERIALS
Clara Natalia Rodríguez-Flórez , Joanna Paczkowska , Jacobo Martín , Mónica Noemí Gil , Ximena Flores-Melo , Andrea Malits
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引用次数: 7

摘要

病毒分流和微生物回路是微生物食物网中的营养途径,被认为是海洋中碳和营养循环的主要驱动因素。比格海峡位于南美洲最南端,是一个受陆地径流和冰川融水影响的亚南极海洋环境,具有高度的时间和空间变异性。海峡东部的营养途径和微生物食物网存在知识差距。本文首次对理化和生物光学参数对东比格海峡沿岸微生物食物网的影响进行了全面和空间范围的研究。这项研究是在冬季水文条件下进行的,其特征是水柱垂直分层较弱,叶绿素a浓度较低(0.13±0.07 mg m−3)。生物地球化学梯度在海峡内外(最东端)之间显著,由麦金莱海峡的浅底坎隔开。作为一种化学水团示踪剂,内通道底层水中NO3+NO2浓度最高,T-S图中的差异表明该水团起源于亚北太平洋。结构方程模型表明,水的比紫外吸收率(SUVA254,芳香碳含量的代表)和NO3+NO2是影响地表/地下水中微生物食物网的主要参数,这表明原核生物的生物量部分由河流排放的外来溶解有机物(DOM)支持。我们的研究结果表明,病毒分流在地表水/地下水中的主要作用是将营养物质保留在食物网的基本水平。我们认为,病毒在地表/地下水中的分流和麦金莱海峡以西的水停留时间允许受感染的细胞和病毒裂解产物到达底层水域,推动那里产生难降解和不稳定的DOM。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Terrigenous dissolved organic matter input and nutrient-light-limited conditions on the winter microbial food web of the Beagle Channel

Terrigenous dissolved organic matter input and nutrient-light-limited conditions on the winter microbial food web of the Beagle Channel

The viral shunt and microbial loop are trophic pathways in the microbial food web, recognized as major drivers of carbon and nutrient cycles in the sea. The Beagle Channel, located at the southernmost extreme of South America, is a subantarctic marine environment influenced by terrestrial runoff and glacial meltwater with high temporal and spatial variability. There is a knowledge gap on the trophic pathways and the microbial food web in the eastern part of the Channel. We herein present for the first time a comprehensive and spatially wide study of the effects of physicochemical and bio-optical parameters on the microbial food web along the Eastern Beagle Channel. The study took place under winter hydrographic conditions, featuring weak vertical stratification of the water column and low chlorophyll a concentrations (0.13 ± 0.07 mg m−3). Biogeochemical gradients were notable between the inner and outer (easternmost) sectors of the Channel, separated by a shallow sill at Mackinlay Strait. As a chemical water mass tracer, the presence of the highest concentrations in bottom waters of NO3 + NO2 in the inner channel and the difference in the T-S diagram indicate the Subantarctic Pacific origin of this water mass. Structural equation models showed that the specific UV absorbance of water (SUVA254, a proxy for the aromatic carbon content) and NO3 + NO2 were the main parameters affecting the microbial food web in surface/subsurface waters suggesting that prokaryotes biomass was partially supported by allochthonous dissolved organic matter (DOM) derived from river discharges. Our results show a major role of the viral shunt in surface/subsurface waters retaining nutrients in the basal levels of the food web. We suggest that the viral shunt in surface/subsurface waters and the water residence time west of Mackinlay Strait allows infected cells and viral lysis products to reach bottom waters propelling the production of recalcitrant and labile DOM there.

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来源期刊
ACS Applied Bio Materials
ACS Applied Bio Materials Chemistry-Chemistry (all)
CiteScore
9.40
自引率
2.10%
发文量
464
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