Orihuela-García M Andrea, Bolado-Penagos Marina, Sala Iria, Tovar-Sánchez Antonio, García Carlos M, Bruno Miguel, Echevarría Fidel, Laiz Irene
Departamento de Física Aplicada, Facultad de Ciencias del Mar y Ambientales, Instituto Universitario de Investigación Marina (INMAR), Campus de Excelencia Internacional/Global del Mar (CEI·MAR), Universidad de Cádiz, Puerto Real, Cadiz, Spain; Departamento de Ciencias de la Tierra, Centro Nacional de Supercomputación (CNS), Barcelona, Spain.
Departamento de Física Aplicada, Facultad de Ciencias del Mar y Ambientales, Instituto Universitario de Investigación Marina (INMAR), Campus de Excelencia Internacional/Global del Mar (CEI·MAR), Universidad de Cádiz, Puerto Real, Cadiz, Spain.
Sci Total Environ. 2023 Feb 1;858(Pt 2):159662. doi: 10.1016/j.scitotenv.2022.159662. Epub 2022 Oct 24.
This study was conducted to address the changes in the surface distribution of trace metals (cobalt, copper, iron, cadmium, nickel, zinc, lead and molybdenum) as they are advected from the Gulf of Cadiz to the Alboran Sea, through the Strait of Gibraltar (south Iberian Peninsula), regions of great ecosystemic importance. Trace metals concentrations were measured in samples collected during two oceanographic cruises, together with the main factors affecting their spatial distribution and temporal variability (i.e., wind and surface currents). Several rivers, the main source of trace metals in this region, flow into the Gulf of Cadiz which is connected with the Alboran Sea through the Strait of Gibraltar by the general circulation pattern. The surface circulation pattern leads to an offshore-eastward gradient that is highly influenced by wind variability. An increase in vertical turbulence induced by the winds or the tidal cycle causes the dilution of trace metals' concentration by mixing rich-metal superficial waters with poor-metal subsurface waters. Additionally, along the eastward displacement of surface waters, several water retention zones have been described (Trafalgar, Camarinal, the Coastal Cyclonic Gyre) that imply an increase in trace metals concentration close to the coast. In addition, our results suggest that the coastal edges of the Strait of Gibraltar also act as a source of certain metals to the Alboran Sea, probably due to the industries in the proximity areas.
本研究旨在探讨痕量金属(钴、铜、铁、镉、镍、锌、铅和钼)在从加的斯湾经直布罗陀海峡(伊比利亚半岛南部)平流至阿尔沃兰海的过程中,其在表层分布的变化情况,这些区域具有重要的生态系统意义。在两次海洋学巡航期间采集的样本中测量了痕量金属浓度,并分析了影响其空间分布和时间变化的主要因素(即风和表层洋流)。该区域痕量金属的主要来源是几条河流,它们流入加的斯湾,加的斯湾通过总体环流模式经直布罗陀海峡与阿尔沃兰海相连。表层环流模式导致一个离岸向东的梯度,该梯度受风向变化的影响很大。风或潮汐周期引起的垂直湍流增加,会通过将富含金属的表层水与贫金属的次表层水混合,导致痕量金属浓度稀释。此外,沿着表层水向东的位移,已描述了几个水体滞留区(特拉法尔加、卡马里纳尔、沿岸气旋式环流),这意味着靠近海岸的痕量金属浓度增加。此外,我们的结果表明,直布罗陀海峡的海岸边缘也可能由于附近地区的工业活动,而成为阿尔沃兰海某些金属的来源。