Pelagic ecosystem dynamics between late autumn and the post spring bloom in a sub-Arctic fjord

IF 4.7 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
E. Walker, I. Wiedmann, A. Nikolopoulos, J. Skarðhamar, E. M. Jones, A. Renner
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引用次数: 1

Abstract

Marine ecosystems, and particularly fjords, are experiencing an increasing level of human activity on a year-round basis, including the poorly studied winter period. To improve the knowledge base for environmentally sustainable management in all seasons, this study provides hydrographic and biological baseline data for the sub-Arctic fjord Kaldfjorden, Northern Norway (69.7° N, 18.7° E), between autumn 2017 and spring 2018. Field observations are integrated with results of a numerical ocean model simulation, illustrating how pelagic biomass, represented by chlorophyll a (Chl a), particulate organic carbon (POC), and zooplankton, is affected by stratification and circulation from October to May. We observed an unusually warm autumn that likely delayed the onset of cooling and may have supported the high abundances of holoplankton and meroplankton (5768 individuals m–3). With the onset of winter, the water column cooled and became vertically mixed, while suspended Chl a concentrations declined rapidly (< 0.12 mg Chl a m–3). In January and February, suspended POC concentrations and downward flux were elevated near the seafloor. The hydrodynamic model results indicate that the strongest currents at depth occurred in these months, potentially inducing resuspension events close to the seafloor. In spring (April), peak abundances of suspended biomass were observed (6.9–7.2 mg Chl a m–3 at 5–15 m; 9952 zooplankton ind. m–3 at 0–100 m), and field observations and model results suggest that zooplankton of Atlantic origin were probably advected into Kaldfjorden. During all investigated seasons, the model simulation suggests a complex circulation pattern, even in such a small fjord, which can have implications for environmental management of the fjord. We conclude that the pelagic system in Kaldfjorden changes continually from autumn to spring and that winter must be seen as a dynamic period, not a season where the fjord ecosystem is ‘at rest’.
亚北极峡湾深秋至春后水华之间的远洋生态系统动态
海洋生态系统,特别是峡湾,全年都在经历越来越多的人类活动,包括对冬季的研究很少。为了完善四季环境可持续管理的知识库,本研究提供了2017年秋季至2018年春季挪威北部卡德约登亚北极峡湾(69.7°N, 18.7°E)的水文和生物基线数据。将野外观测结果与数值海洋模式模拟结果相结合,说明了10 - 5月分层和环流如何影响以叶绿素a (Chl a)、颗粒有机碳(POC)和浮游动物为代表的远洋生物量。我们观察到一个异常温暖的秋季,这可能推迟了降温的开始,并可能支持了整体浮游生物和浮游生物的高丰度(5768个m-3)。随着冬季的到来,水柱冷却并垂直混合,悬浮Chl a浓度迅速下降(< 0.12 mg Chl a m-3)。1月和2月,海底附近悬浮POC浓度和向下通量升高。水动力模型结果表明,这几个月发生了最强烈的深海洋流,可能会引起靠近海底的再悬浮事件。春季(4月),悬浮物丰度最高(5 ~ 15 m, 6.9 ~ 7.2 mg Chl a m - 3;9952浮游动物(m - 3, 0-100 m),野外观测和模式结果表明,来自大西洋的浮游动物可能平流到Kaldfjorden。在所有被调查的季节,模型模拟显示了一个复杂的环流模式,即使在这样一个小峡湾,这可能对峡湾的环境管理产生影响。我们的结论是,从秋天到春天,卡尔德约登的海洋系统不断变化,冬季必须被视为一个动态的时期,而不是峡湾生态系统“休息”的季节。
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来源期刊
Elementa-Science of the Anthropocene
Elementa-Science of the Anthropocene Earth and Planetary Sciences-Atmospheric Science
CiteScore
6.90
自引率
5.10%
发文量
65
审稿时长
16 weeks
期刊介绍: A new open-access scientific journal, Elementa: Science of the Anthropocene publishes original research reporting on new knowledge of the Earth’s physical, chemical, and biological systems; interactions between human and natural systems; and steps that can be taken to mitigate and adapt to global change. Elementa reports on fundamental advancements in research organized initially into six knowledge domains, embracing the concept that basic knowledge can foster sustainable solutions for society. Elementa is published on an open-access, public-good basis—available freely and immediately to the world.
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