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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Intrabasinal conditions promoting the development of a blogenic carbonate sedimentary facies associated with the seagrass Posidonia oceanica
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Intrabasinal conditions promoting the development of a blogenic carbonate sedimentary facies associated with the seagrass Posidonia oceanica

机译:碱性条件促进与海草波塞冬大洋洲有关的生成碳酸盐沉积相的发展

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This paper aims to elucidate the spatial relationships between the distribution and growth dynamics of Posidonia oceanica, the sedimentary depositional facies (carbonate vs. siliciclastic), and the hydrodynamic features of the Gulf of Oristano (Western Sardinia, Mediterranean sea), a complex depositional system characterized by multiple sources of sediments and a marked hydrodynamic gradient. Three depositional environments were identified: (i) a poorly vegetated sector characterized by muddy sediments derived from the river input; (ii) a sector colonized by P. oceanica meadows characterized by biogenic carbonate sediments derived from the sediment production associated with the seagrass ecosystem and (iii) a sector colonized by P. oceanica meadows characterized by coarse siliciclastic sediments, possibly relict sediments. The sedimentary depositional environments are heavily influenced by the spatial distribution of the wind wave energy. Biogenic carbonate reels associated with P. oceanica meadows develop in sheltered areas characterized by low amplitude of waves generated by the main wind regime. In the exposed sectors, characterized by a higher wave height, the meadows colonize relict siliciclastic sediments, without promoting carbonate particle deposition. Posidonia oceanica meadows in sheltered areas, associated with biogenic sedimentary facies, exhibit higher rhizome growth rate values (1.1 and 1.2cm year(-1) vs. 0.7 cm year(-1)) and a lower percentage of horizontal shoots (1.1%, and 4.1% vs. 18%) in comparison to P. oceanica meadows in exposed areas, associated with siliciclastic sedimentary facies. The former tend to develop in a vertical direction, thus contrasting the sediment deposition rate, the latter tend to expand laterally due to the absence of sediment deposition. These results highlight that wave amplitude is the intrabasinal factor which influences the deposition of biogenic sediments and the growth dynamics of P. oceanica meadows. (C) 2008 Elsevier Ltd. All rights reserved.
机译:本文旨在阐明大洋波西多尼亚的分布和生长动力学,沉积沉积相(碳酸盐岩与硅质碎屑)以及奥里斯塔诺湾(西撒丁岛,地中海)的水动力特征之间的空间关系。具有多种沉积物来源和明显的水动力梯度。确定了三种沉积环境:(i)植被贫瘠的地区,其特征是河流输入物产生了泥泞的沉积物; (ii)洋红松草甸所定殖的一个区域,其特征是源自与海草生态系统相关的沉积物产生的生物碳酸盐沉积物;以及(iii)洋红松草甸所定殖的一个区域,其特征是较粗的硅质碎屑沉积物,可能是残渣沉积物。沉积沉积环境受到风波能量的空间分布的严重影响。与P. oceanica草甸相关的生物碳酸盐卷盘在庇护区发展,其特征是主要风态产生的波幅较低。在以较高波高为特征的裸露部分,草甸定居在残存的硅质碎屑沉积物中,而不会促进碳酸盐颗粒的沉积。与生物成因的沉积相相关的庇护区的波西多尼亚大洋洲草地表现出较高的根茎生长速率值(1.1和1.2cm年(-1)对0.7 cm年(-1)),而水平枝的百分比较低(1.1%,相较于裸露的大洋山地草甸,与硅质碎屑沉积相相关,分别为4.1%和18%)。前者倾向于在垂直方向上发展,从而形成沉积物沉积速率的对比,而后者则由于缺乏沉积物而倾向于横向扩展。这些结果表明,波幅是影响生物成因沉积物沉积和海洋运动草地生长动态的基本因素。 (C)2008 Elsevier Ltd.保留所有权利。

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