首页> 外文期刊>Coral reefs: journal of the International Society for Reef Studies >Distribution and sediment production of large benthic foraminifers on reef flats of the Majuro Atoll, Marshall Islands
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Distribution and sediment production of large benthic foraminifers on reef flats of the Majuro Atoll, Marshall Islands

机译:马绍尔群岛马朱罗环礁礁滩上大型底栖有孔虫的分布和沉积物产生

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摘要

The distributions and population densities of large benthic foraminifers (LBFs) were investigated on reef flats of the Majuro Atoll, Marshall Islands. Annual sediment production by foraminifers was estimated based on population density data. Predominant LBFs were Calcarina and Amphistegina, and the population densities of these foraminifers varied with location and substratum type on reef flats. Both foraminifers primarily attached to macrophytes, particularly turf-forming algae, and were most abundant on an ocean reef flat (ORF) and in an inter-island channel near windward, sparsely populated islands. Calcarina density was higher on windward compared to leeward sides of ORFs, whereas Amphistegina density was similar on both sides of ORFs. These foraminifers were more common on the ocean side relative to the lagoon side of reef flats around a windward reef island, and both were rare or absent in nearshore zones around reef islands and on an ORF near windward, densely populated islands. Foraminiferal production rates varied with the degree to which habitats were subject to water motion and human influences. Highly productive sites (> 10(3) g CaCO3 m(-2) year(-1)) included an ORF and an inter-island channel near windward, sparsely populated islands, and a seaward area of a reef flat with no reef islands. Low-productivity sites (< 10 g CaCO3 m(-2) year(-1)) included generally nearshore zones of lagoonal reef flats, leeward ORFs, and a windward ORF near densely populated islands. These results suggest that the distribution and production of LBFs were largely influenced by a combination of natural environmental factors, including water motion, water depth, elevation relative to the lowest tidal level at spring tide, and the distribution of suitable substratum. The presence of reef islands may limit the distribution and production of foraminifers by altering water circulation in nearshore environments. Furthermore, increased anthropogenic factors (population and activities) may adversely affect foraminiferal distribution and production.
机译:在马绍尔群岛马朱罗环礁的礁滩上调查了大型底栖有孔虫(LBF)的分布和种群密度。有孔虫的年沉积物产量是根据人口密度数据估算的。主要的LBF是钙生动物和两栖动物,这些有孔虫的种群密度随礁滩的位置和基质类型而变化。两种有孔虫都主要附着在大型植物上,尤其是形成草皮的藻类,并且在大洋礁滩(ORF)以及靠近上风,人口稀少的岛屿的岛际通道中最为丰富。与风的背风侧相比,迎风时的car骨密度更高,而风的两侧的两栖动物密度相似。这些有孔虫相对于顺风礁岛周围礁滩的泻湖侧在海洋侧更为常见,并且在礁岛周围的近岸区域以及顺风,人口稠密的岛屿附近的ORF中,这两种有孔虫都很罕见或不存在。有孔虫的生产率随生境受到水运动和人类影响的程度而变化。高产地点(> 10(3)g CaCO3 m(-2)年(-1)(-1))包括ORF和靠近风向,人口稀少的岛屿的岛际通道,以及无礁岛的礁滩向海区域。低产站点(<10 g CaCO3 m(-2)年(-1))通常包括泻湖礁滩,背风ORF和靠近人口密集的岛屿的迎风ORF的近岸区域。这些结果表明,LBF的分布和产量在很大程度上受多种自然环境因素的影响,这些因素包括水运动,水深,相对于春季潮汐最低潮位的海拔高度以及合适的基质分布。礁岛的存在可能会通过改变近岸环境中的水循环来限制有孔虫的分布和生产。此外,增加的人为因素(种群和活动)可能会对有孔虫的分布和生产产生不利影响。

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