强烈冬季风暴对地中海大陆架地点物理和生物变量的影响

Antoine Grémare , Jean-Michel Amouroux , Gustave Cauwet , François Charles , Claude Courties , Francis De Bovée , Alain Dinet , Jean Luc Devenon , Xavier Durrieu De Madron , Béatrice Ferre , Philippe Fraunie , Fabien Joux , François Lantoine , Philippe Lebaron , Jean-Jacques Naudin , Albert Palanques , Mireille Pujo-Pay , Laurent Zudaire
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引用次数: 71

摘要

1999年秋,在滨海巴纽尔斯湾进行了一项调查,包括永久系泊和高频采样,以评估强烈和不可预测的气象事件对地中海沿岸生态系统功能的影响。11月12日发生了一场严重的冬季风暴,产生了7米高的海浪,海面上升了约0.5米。近底流速在24 m处达到30 cm s-1。这次风暴通过再悬浮导致了总悬浮物的显著增加,随后总沉积速率增加。这也导致水柱中难降解颗粒有机物的比例增加。它还倾向于通过再悬浮和解吸过程增加水柱中的养分有效性。这种增长的动力因营养物质而异。该风暴显著提高了细菌生物量和产量。这些影响是暂时的,可能不仅仅是由于再悬浮。在水-沉积物界面附近,由于不同的再悬浮和沉积作用,植物色素的分布发生了变化,但风暴对浮游植物生物量的影响不大。这种缺乏响应可能与低降水量和/或光照限制有关。风暴导致了水-沉积物界面细颗粒丰度的短暂增加。这些颗粒被难熔的有机物包裹着。风暴导致了稀有动物丰度的显著减少。松弛期的持续时间因参数而异。总悬浮物、表层沉积物粒度测定和碳水化合物含量测定持续2周。
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The effects of a strong winter storm on physical and biological variables at a shelf site in the Mediterranean

A survey involving both permanent mooring and high frequency sampling was carried in the Bay of Banyuls-sur-Mer during the fall of 1999 to assess the effect of strong and unpredictable meteorological events on the functioning of a coastal Mediterranean ecosystem. A severe winter storm took place on 12 November, which generated waves with a significant height of 7 m and a sea surface rise of about 0.5 m. The near-bottom current speed at 24 m reached 30 cm s–1. This storm induced a significant increase in total suspended matter through resuspension and then a subsequent increase in gross sedimentation rates. It also resulted in an increase of the proportion of refractory particulate organic matter in the water column. It also tended to increase nutrient availability in the water column through resuspension and desorption processes. The kinetic of this increase differed among nutrients. Bacterial biomass and production were significantly enhanced by the storm. These effects were transitory and probably not due to resuspension alone. The distribution of plant pigments was modified at the immediate vicinity of the water-sediment interface due to differential resuspension and sedimentation but the storm had no effect on integrated phytoplanktonic biomass. Such a lack of response may be linked to low precipitations and/or light limitation. The storm resulted in a transitory increase of the abundance of fine particles at the water-sediment interface. These particles were coated with refractory organic matter. The storm induced a significant decrease of meiofauna abundance. The duration of the relaxation periods varied among parameters. It lasted 2 weeks for total suspended matter, surface sediment granulometry and carbohydrate contents.

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