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首页> 外文期刊>Deep-Sea Research >Live and dead deep-sea benthic foraminiferal macrofauna of the Levantine basin (SE Mediterranean) and their ecological characteristics
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Live and dead deep-sea benthic foraminiferal macrofauna of the Levantine basin (SE Mediterranean) and their ecological characteristics

机译:黎凡特盆地(地中海南部)的生死深海底栖有孔虫大型动物及其生态特征

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摘要

The present study sought to quantitatively characterize the live and dead benthic foraminifera communities of the deep southeastern Levantine basin of the Mediterranean Sea (33.4 degrees-31.7 degrees N, 31.3 degrees-34.9 degrees E; 100-1900 m water depth) and their relationships to environmental conditions. Box corer samples were collected at 50 sites between June and July 2013. The foraminiferal macrofauna ( 250 mu m) were enumerated and identified (76% to the species level). Six live foraminiferal assemblages were identified, inhabiting six biotopes, the shelf margin (SM), two upper continental slopes (UCS1 and UCS2), the lower continental slope (LCS), the eastern bathyal plain (EBP) and the western bathyal plain (WBP). The dead communities were divided into four biotopes, generally compatible with the live ones, excluding the UCS2 and the EBP. The foraminiferal density in the various live biotopes was relatively stable across the studied area, excluding the UCS2 and EBP, unlike the density of the dead shells, which increased with depth. The number of taxa per biotope was estimated by rarefaction curves and compared to the observed numbers, with a decreasing number of live taxa with water depth. The alpha-diversity, which was evaluated in relation to the number of sampled individuals, reached an asymptote in all biotopes, with very low values in the WBP. The within-biotope heterogeneity was evaluated by the average Chao-Sorensen similarity index and by a beta-diversity index (exp(gamma diversity) - exp(alpha diversity)), revealing variable heterogeneities in both assemblages. Water depth, sediment grain size mode, CaCO3 (wt%), and clay fraction (wt%) were jointly but feebly correlated with live faunal composition.
机译:本研究试图定量表征地中海黎凡特东南部深海(北纬33.4度至31.7度,东经31.3度至34.9度;水深100至1900 m)的活底栖有孔有孔虫群落和它们的关系。环境条件。在2013年6月至7月期间,在50个地点收集了箱型箱虫样品。对有孔虫大型动物(> 250微米)进行了计数和鉴定(占物种水平的76%)。确定了六个活的有孔虫组合,栖息在六个生物群落,架子边缘(SM),两个上大陆斜坡(UCS1和UCS2),下大陆斜坡(LCS),东部海底平原(EBP)和西部海底平原(WBP) )。死者社区被划分为四个生物群落,除了UCS2和EBP,它们通常与活生物群落兼容。在整个研究区域中,除UCS2和EBP外,各种活生物群落中的有孔虫密度相对稳定,这与死壳的密度不同,死壳的密度随深度而增加。通过稀疏曲线估计每个生物群落的分类单元数量,并将其与观察到的数量进行比较,随着水深的增加,活分类单元的数量减少。相对于采样个体的数量进行评估的α多样性在所有生物群落中都达到了渐近线,而WBP中的值非常低。通过平均Chao-Sorensen相似性指数和β多样性指数(exp(γ多样性)-exp(α多样性))评估了生物群落内异质性,揭示了两种组合中的可变异质性。水深,沉积物粒度模式,CaCO3(wt%)和黏土分数(wt%)共同但与动物区系组成微弱相关。

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