揭示北冰洋东部不同水团中上层微生物食物网的群落差异及其驱动因素

IF 3.4 2区 地球科学 Q1 OCEANOGRAPHY
Chaofeng Wang, Guangfu Luo, Xiaoyu Wang, Zhiqiang Xu, Musheng Lan, Junjian Wang, Denggani Liang, Yifei Fan, Wenfei Zhang, Meiping Feng, Li Zhao, Wuchang Zhang
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引用次数: 0

摘要

微生物食物网(MFWs)构成了海洋中上层生态系统的基本框架,但其群落结构、营养相互作用和相关的非生物驱动因素在北冰洋仍未得到充分的表征。为了填补这一空白,我们在2020年夏季进行了一项全面的船舶调查,调查了从表层到500 m层的三个MFW营养水平(picoplankton-Pico, nanoplankton-Nano, microzoplankton - micro)。各MFW分量在垂直分布上呈现一致的地下峰值。此外,还确定了五个不同的水团,每个水团都有不同的MFW组成。在这一框架下,异养原核生物在所有水体中占主导地位,太平洋起源的聚球菌成为追踪北极环境波动的有价值的生物指标。值得注意的是,营养层丰度比符合金字塔结构,Pico:Micro (3.5-12.8 × 105:1)和Nano:Micro (1.6-10.0 × 102:1)分别跨越5个和2个数量级。生物量比在Pico:Micro (0.4-1.2 × 101:1)和Nano:Micro(0.8-2.6:1)中分别为1级和0级。在生物-非生物相互作用方面,各MFW组分的丰度和生物量均随温度和Chl a浓度呈线性增加。其中,微真核生物表现出最陡的斜率,这表明它们对温度变化的敏感性更高。此外,MFW营养联系的驱动因素在不同水体之间存在显著差异,自下而上的控制(资源有效性)主导了浮游动物组成。该研究为量化和预测未来环境变化如何影响极地海洋生态系统中上层MFWs建立了基线。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Unraveling Both Community Divergences and Driving Factors of Pelagic Microbial Food Web in Different Water Masses of the Eastern Arctic Ocean

Unraveling Both Community Divergences and Driving Factors of Pelagic Microbial Food Web in Different Water Masses of the Eastern Arctic Ocean

Unraveling Both Community Divergences and Driving Factors of Pelagic Microbial Food Web in Different Water Masses of the Eastern Arctic Ocean

Unraveling Both Community Divergences and Driving Factors of Pelagic Microbial Food Web in Different Water Masses of the Eastern Arctic Ocean

Microbial food webs (MFWs) constitute the foundational framework of marine pelagic ecosystems, yet their community structure, trophic interactions, and associated abiotic driving factors remain inadequately characterized in the Arctic Ocean. To fill this gap, we conducted a comprehensive ship-based survey during summer 2020 to investigate three MFW trophic levels (picoplankton—Pico, nanoplankton—Nano, microzooplankton—Micro) from surface to 500 m layers. Each MFW component displayed a consistent subsurface peak in its vertical distribution. Additionally, five distinct water masses were identified, and each harboring a distinctive MFW composition. Within this framework, heterotrophic prokaryotes dominated numerically across all water masses, and Pacific-origin Synechococcus emerged as a valuable bioindicator for tracking Arctic environmental fluctuations. Notably, trophic-level abundance ratios conformed to a pyramidal structure, spanning five and two orders of magnitude for Pico:Micro (3.5–12.8 × 105:1) and Nano:Micro (1.6–10.0 × 102:1), respectively. Unlike biomass ratios, for which spanned one and zero order in Pico:Micro (0.4–1.2 × 101:1) and Nano:Micro (0.8–2.6:1), respectively. Concerning biotic-abiotic interactions, both abundance and biomass of each MFW component demonstrated a linear increase with both temperature and Chl a concentrations in Pacific Summer Water. Therein, picoeukaryotes exhibited the steepest slope revealed that their heightened sensitivity to temperature changes. Furthermore, the driving factors for MFW trophic linkages varied significantly among water masses, and the bottom‒up control (resource availability) predominating microzooplankton composition. This study upon trophic-level interaction establishes a baseline for quantifying and predicting how future environmental changes may affect pelagic MFWs in polar marine ecosystems.

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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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