首页> 外文期刊>Journal of foraminiferal research >MODERN FORAMINIFERAL FAUNAS OF THE SOUTHWESTERN TO NORTHERN ICELAND SHELF: OCEANOGRAPHIC AND ENVIRONMENTAL CONTROLS
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MODERN FORAMINIFERAL FAUNAS OF THE SOUTHWESTERN TO NORTHERN ICELAND SHELF: OCEANOGRAPHIC AND ENVIRONMENTAL CONTROLS

机译:西南至北冰岛大陆架的现代有孔虫纲:海洋学和环境控制

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摘要

Surface sediment samples for analysis of modern fo-raminiferal assemblages were collected from 32 sites on the western and northern Iceland shelf during cruise B997 of the Icelandic ship Bjarni Saemundsson. The purpose of the study is to provide a basis for interpreting the variations in foraminiferal content in late glacial through Holocene sediments from cores at the same sites. Cluster analysis and principal components analysis of the benthic foraminiferal data and associated modern environmental parameters including hydrography, water depth, and sediment characteristics show that large progressive changes in the foraminiferal assemblages coincide with changes in the dominant oceanic surface currents and water masses around Iceland. The western areas of the shelf are overlain by relatively warm and saline Atlantic Water of the Irminger Current. The western shelf fauna is dominated by Cassidulina laevigata and other boreal species, whereas the planktic fauna is dominated by dextrally coiling Neogloboquadrina pach-yderma. In Djupall, off the Northwest Peninsula, and in the shallow nearshore sites on the northern shelf, the boreal elements of the fauna diminish and arctic species become more important. However, the dominant species in these areas are Cibicides lobatulus and Astrononion gallowayi, attesting to winnowing of the shallow shelf areas by currents. In Isafjardardjup, the large fjord indenting the Northwest Peninsula, Cassidulina reniforme and Elphidium excavatum dominate the fauna as a result of cooler waters and more variable salinity conditions. A very large faunal shift is registered in the deep basins of the northern shelf. This faunal shift coincides with large changes in salinity and temperature stratification of the water column, reflecting the presence of the East Iceland Current. The fauna in the deep basins on the northern shelf are dominated by C. neoteretis, an indicator of modified Atlantic Water, and infaunal species that reflect organic fluxes to the seabed: Nonionellina labradorica and Melonis barleeanus, and the arctic species Islandiella norcrossi and I. helenae.
机译:在冰岛船Bjarni Saemundsson的B997巡游期间,从冰岛西部和北部陆架的32个地点收集了用于分析现代fo-raminiferal组合的表面沉积物样本。该研究的目的是为解释晚冰期至全新世沉积物从同一地点的岩心中有孔虫含量的变化提供基础。底栖有孔虫数据以及相关的现代环境参数(包括水文学,水深和沉积物特征)的聚类分析和主成分分析表明,有孔虫组合的大的渐进变化与冰岛周围主要海洋表面水流和水团的变化相吻合。大陆架的西部地区被相对较暖和咸的艾明格洋流大西洋水所覆盖。西部大陆架动物群主要由Cassidulina laevigata和其他北方物种主导,而浮游动物群则由右旋盘绕的新球藻(Yeogloboquadrina pach-yderma)主导。在西北半岛以外的朱帕尔(Djupall)和北部陆架的浅海近岸站点,动物群的北方元素逐渐减少,北极物种变得越来越重要。但是,这些地区的优势种是长叶蝉(Cibicides lobatulus)和盖天牛天文学(Astrononion gallowayi),这证明了洋流对浅层架子区域的风吹作用。在伊萨法加达朱普(Isafjardardjup),由于凉爽的海水和变化多端的盐度条件,缩进西北半岛的大型峡湾,龙形梭状芽孢杆菌(Cassidulina reniforme)和金缕梅(Elphidium excavtum)主导了动物区系。在北部陆架的深盆中,动物群的变化非常大。动物群的变化与水柱盐度和温度分层的大变化相吻合,反映出东冰岛洋流的存在。北部陆架深层盆地的动物区系以新孢梭菌(Cat neoteretis)和改良的大西洋藻类为主,它们是反映大西洋水质变化的不育物种:Nonionellina labradorica和Melonis barleeanus,以及北极物种Islandiella norcrossi和I. Helenae。

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