南极金钟湾浅海岸带浮游生物群落结构:两个连续夏季的比较

D. R. Tenenbaum, J. J. Barrera-Alba, M. Tenório
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引用次数: 1

摘要

本研究的主要目的是研究南极半岛金钟湾浮游植物结构的年际变化,作为长期监测计划的一部分。自2009年以来,在显微分析的基础上,对浮游植物的分类组成和生物量进行了调查。本报告介绍了2009/2010年和2010/2011年夏季浮游植物大小结构和生物量调查的结果。本研究提出了4种环境条件和浮游植物群落情景:1)2009/2010年初夏;高Si:N促进硅藻生长,低N:P和低温抑制硅藻生长;低N:P和低Si:N对硅藻生长有抑制作用,高温和低N:P对鞭毛藻生长有促进作用,因为它们的最佳N:P比低于硅藻;3) 2010/2011年初夏;高N:P、高Si:N、高温和2010/2011年夏末对硅藻生长有促进作用;高Si:N和高温有利于形成链状硅藻(如海硅藻)的大量繁殖,这可以解释硝酸盐和硅酸盐的急剧减少。金钟湾浮游生物群落在研究期间表现出高度的变异性,这明显受环境因素的影响。这项研究覆盖的时间窗口只给了我们对南极环境可能正在经历的长期变化方向的一瞥。对这种趋势的更全面的了解在很大程度上依赖于长期监测计划的连续性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
MICROPLANKTON COMMUNITY STRUCTURE OF THE SHALLOW COASTAL ZONE AT ADMIRALTY BAY, ANTARCTICA: COMPARISON BETWEEN TWO CONSECUTIVE AUSTRAL SUMMERS
The main objective of this work was to investigate interannual changes of phytoplankton structure as part of a long-term monitoring program in Admiralty Bay, Antarctic Peninsula. Based on microscopic analysis, phytoplankton taxonomic composition and biomass are investigated since 2009. This report presents results from the 2009/2010 and 2010/2011 summer surveys regarding the phytoplankton size-structure and biomass. Four scenarios were proposed in our study for environmental conditions and phytoplankton community: 1) 2009/2010 Early Summer; diatom growth was promoted by high Si:N, but inhibited by low N:P and low temperature, 2) 2009/2010 Late Summer; diatom growth was inhibited by low N:P and low Si:N, and high temperature and low N:P promoted dinoflagellates growth, due to their low optimum N:P ratios compared to diatoms; 3) 2010/2011 Early Summer; diatom growth was promoted by high N:P, high Si:N and high temperature and 4) 2010/2011 Late Summer; blooms of chain-forming diatoms (e.g. Thalassiosira spp.), favoured by high Si:N and high temperature, and it could explain the drastic reduction both in nitrate and silicate. The microplankton community of Admiralty Bay presented a high variability during the studied period that was clearly dictated by environmental factors. The time window covered by this study gives us only a glimpse of the direction of long term changes that the Antarctic environment might be experiencing. A more complete picture of such trends relies heavily on the continuity of the long-term monitoring program.
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