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气候变化与上升流系统中的赤潮甲藻

Climate variability and Dinophysis acuta blooms in an upwelling system.

机构信息

Instituto Español de Oceanografía (IEO), Centro Oceanográfico de Vigo, Subida a Radio Faro 50, 36390 Vigo, Spain; Programa de Investigación Pesquera & Instituto de Acuicultura, Universidad Austral de Chile, PO Box 1327, Los Pinos s/n, Balneario Pelluco, Puerto Montt, Chile.

Instituto Español de Oceanografía (IEO), Centro Oceanográfico de A Coruña, Muelle das Ánimas s/n, 15001 A Coruña, Spain.

出版信息

Harmful Algae. 2016 Mar;53:145-159. doi: 10.1016/j.hal.2015.11.007. Epub 2016 May 3.

Abstract

Dinophysis acuta is a frequent seasonal lipophilic toxin producer in European Atlantic coastal waters associated with thermal stratification. In the Galician Rías, populations of D. acuta with their epicentre located off Aveiro (northern Portugal), typically co-occur with and follow those of Dinophysis acuminata during the upwelling transition (early autumn) as a result of longshore transport. During hotter than average summers, D. acuta blooms also occur in August in the Rías, when they replace D. acuminata. Here we examined a 30-year (1985-2014) time series of D. acuta from samples collected by the same method in the Galician Rías. Our main objective was to identify patterns of distribution and their relation with climate variability, and to explain the exceptional summer blooms of D. acuta in 1989-1990. A dome-shaped relationship was found between summer upwelling intensity and D. acuta blooms; cell maxima were associated with conditions where the balance between upwelling intensity and heating, leading to deepened thermoclines, combined with tidal phase (3 days after neap tides) created windows of opportunity for this species. The application of a generalized additive model based on biological (D. acuta inoculum) and environmental predictors (Cumulative June-August upwelling CUI, average June-August SST and tidal range) explained more than 70% of the deviance for the exceptional summer blooms of D. acuta, through a combination of moderate (35,000-50,000mskm) summer upwelling (CUI), thermal stratification (SST>17°C) and moderate tidal range (∼2.5m), provided D. acuta cells (inoculum) were present in July. There was no evidence of increasing trends in D. acuta bloom frequency/intensity nor a clear relationship with NAO or other long-term climatic cycles. Instead, the exceptional summer blooms of 1989-1990 appeared linked to extreme hydroclimatic anomalies (high positive anomalies in SST and NAO index), which affected most of the European Atlantic coast.

摘要

短沟藻是一种常见的季节性脂溶性毒素生产者,存在于与热分层相关的欧洲大西洋沿海水域。在加利西亚里阿斯,短沟藻的种群中心位于阿威罗(葡萄牙北部)附近,通常与 Dinophysis acuminata 种群一起出现,并在上升流过渡期间(初秋)随着沿岸运输而出现。在比平均温度高的夏季,里阿斯也会在 8 月出现短沟藻水华,此时它们会取代 Dinophysis acuminata。在这里,我们研究了来自加利西亚里阿斯的同一方法采集的 30 年(1985-2014 年)短沟藻时间序列。我们的主要目标是确定分布模式及其与气候变率的关系,并解释 1989-1990 年短沟藻异常夏季水华的原因。发现夏季上升流强度与短沟藻水华之间存在圆顶形关系;细胞最大值与上升流强度与加热之间的平衡有关,这导致了温跃层加深,并与潮汐阶段(小潮后的第 3 天)相结合,为该物种创造了机会窗口。应用基于生物(短沟藻接种物)和环境预测因子(6 月至 8 月累积上升流 CUI、6 月至 8 月平均 SST 和潮汐范围)的广义加性模型,通过适度(35,000-50,000mskm)夏季上升流(CUI)、热分层(SST>17°C)和适度潮汐范围(~2.5m)的组合,解释了异常夏季短沟藻水华超过 70%的离差,前提是 7 月存在短沟藻细胞(接种物)。没有证据表明短沟藻水华频率/强度呈上升趋势,也没有明确的与 NAO 或其他长期气候周期的关系。相反,1989-1990 年的异常夏季水华似乎与极端水文气候异常(SST 和 NAO 指数的高正异常)有关,这些异常影响了欧洲大西洋沿岸的大部分地区。

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