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首页> 外文期刊>Journal of foraminiferal research >Ecological distribution of benthic foraminifera, offshore Northeast New Zealand
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Ecological distribution of benthic foraminifera, offshore Northeast New Zealand

机译:新西兰东北近海近岸Benthic Foraminifera的生态分布

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摘要

Northeast of New Zealand, nine benthic foraminiferal associations are recognized and mapped (50-3800 m depth) based on cluster analysis of faunal census data (> 63 mu m, 235 species, 56 samples). Similar associations are identified using cluster analysis based on the presence or absence of species. Canonical correspondence analysis shows that the associations correlate most strongly with factors related to water depth, especially decreasing food supply (organic carbon flux) with increasing depth. The depth-stratified distribution of lower bathyal to abyssal (> 1000 m) associations accords well with the deep water masses, and is attributed in part to lower oxygen concentrations in the bottom waters. The two deepest associations, dominated by Alabaminella weddellensis, Epistominella exigua, Bulimina marginata L aculeata, Globocassidulina subglobosa, and Oridorsalis umbonatus, underlie the oxygen minimum zone of Circumpolar Deep Water. A midlower bathyal association dominated by Cassidulina carinata, Alabaminella weddellensis, Abditodentrix pseudothalmanni, and Trifarina occidentalis, underlies Antarctic Intermediate Water. In addition to their bathymetric stratification, mid shelf to upper bathyal (50-600 m) associations also show latitudinal variation that may reflect differences in terrigenous mud (abundant Eilohedra vitrea), bottom current strength, food supply (more abundant Cassidulina carinata) and nutrient remineralization on the seafloor.
机译:新西兰东北部,九个底底传导物关联被认可和映射(50-3800米深度),基于动物群人口普查数据的聚类分析(> 63亩,235种,56种样品)。基于物种的存在或不存在,使用聚类分析来识别类似的关联。规范对应分析表明,关联与水深有关的因素相关,特别是随着深度的增加,尤其是减少食物供应(有机碳通量)。较低浴的深度分层分布到深水群(> 1000米)的关联符合深水质量,并且部分地归因于底部水中的较低氧浓度。由阿拉巴马氏菌属韦德利斯岛,Epestominella exigua,Bulimina Marginata L Aculeata,Globocassidulina subglobosa和Oridorsalis Umbonatus的两个最深的协会,利于循环深水的氧气最小区域。由Cassidulina Carinata,Alabaminella Weddellensis,Abditodentrix Pseudothalmanni和Trifarina occidentalis主导的中转浴科学协会,是南极中间水。除了它们的碱性分层外,中间搁板(50-600米)的关联还显示出纬度变异,可能反映人造泥浆(丰富的eIlohedra vitrea),底部电流强度,食品供应(更丰富的Cassidulina carinata)和营养物质的差异在海底上的再矿化。

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