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首页> 外文期刊>Journal of marine systems: journal of the European Association of Marine Sciences and Techniques >Coccolithophore and benthic foraminifera distribution patterns in the Gulf of Cadiz and Western Iberian Margin during Integrated Ocean Drilling Program (IODP) Expedition 339
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Coccolithophore and benthic foraminifera distribution patterns in the Gulf of Cadiz and Western Iberian Margin during Integrated Ocean Drilling Program (IODP) Expedition 339

机译:Coccolthophore和Benthic foraminifera分布在Cadiz和西部伊伯利亚山脉综合钻井计划(IODP)探险中的伊比利亚缘339期间

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摘要

For the first time during an Integrated Ocean Drilling Program (IODP) Expedition (Exp. 339, Mediterranean Outflow) water samples for living coccolithophore distributions and mudline samples for coccoliths, benthic foraminifera, and geochemical analyses in the underlying surface sediments were collected. In total, 14 water samples (from 5 to 20 m water depth) and 7 mudline samples were gathered at the drill sites. Coccolithophore distributions show spatial variations in species diversity. In particular, assemblages that characterize the Western Iberian Margin differ from those in the Gulf of Cadiz, indicative of oceanographic and environmental controls on the community in the upper ocean (0-20 m depth). Comparison of the living assemblages to those in surface sediments shows differences in the presence of some species, suggesting the influence of post deposition sedimentary processes. Other factors such as the season of sampling and the limited sampling depth may also have a role in the differences recorded. Benthic foraminiferal assemblages seem to be primarily determined by source, quantity and quality of available food. Sites in the Gulf of Cadiz are bathed by Mediterranean Outflow Water (MOW) and characterized by a considerable amount of advected food particles. Elevated epibenthic foraminifera exploit this niche, while arborescent epifaunal and infaunal taxa thrive on food particles falling out of MOW. The combined data suggest different flow speeds and settling of MOW suspension load in the Gulf of Cadiz. In contrast, assemblages from the Western Iberian Margin located farthest from or outside of MOW are determined by local export productivity and mirror trophic conditions in the surface waters. Both assemblages reveal variation in the composition at intermediate and deep water depths along the southern and western Iberian Margins with distance from the Strait of Gibraltar. (C) 2017 Elsevier B.V. All rights reserved.
机译:在综合海洋钻探计划(IODP)探险期间(EXP.339,地中海流出)水样中的水样和COCCOLITHS的泥土样品,底层表面沉积物中的地球化学分析和地球化学分析。总共14个水样(从5至20米水深)和7个泥浆样品在钻头。 COCCOLETHOPHORE分布显示物种多样性的空间变化。特别是,表征西伊伯利亚边缘的大会与加入斯湾的集会不同,指示上海(0-20米深度)的社区海洋和环境控制。生活组合对地表沉积物的比较显示了一些物种存在的差异,表明沉积沉积过程的影响。其他因素如采样季节和有限的采样深度也可能在记录的差异中具有作用。底栖的传染率似乎主要由可用食品的来源,数量和质量决定。 Cadiz海湾的景点由地中海流出水(割草)沐浴,并具有相当大量的加剧食品颗粒。升高的epibenthic foraminifera利用这个niche,而树脂志的epifaal和婴儿毒群在食物粒子上落下的割草。综合数据表明了加入峡湾中的不同流量速度和割草悬浮载荷。相比之下,距离割草中最远的西伊伯利亚边缘的组装由地表水域的局部出口生产力和镜子营养状况决定。两个组合都揭示了沿着南部和西部伊比塔的伊比塔距离的南部和西部伊比塔的中间和深水深度的组合物的变化。 (c)2017 Elsevier B.v.保留所有权利。

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