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Community Structure of Soft‐Bottom Macrobenthos of the Newport Submarine Canyon, California

机译:加利福尼亚州纽波特海底峡谷软底大型底栖动物的群落结构

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Abstract.The hypothesis that benthic community structure of soft‐bottom macrobenthos does not change throughout the Newport Submarine Canyon, California was tested with a set of quantitative VanVeen(0.1 m2) samples down the canyon axis. There was a marked break in community structure between Station C4 (187 m) and Station C5 (324 m). Comparison of the present study with work conducted earlier indicates that mean number of species, abundance, and biomass were not significantly different between 1962 and 1978. Within the canyon, species diversity was high compared to 12 other southern California canyons. This difference was mainly due to sampling effort and the inactive nature of the Newport Canyon.SummaryOver 500 species are identified from Newport Canyon, California from 1978 to 1990. The diversity of soft‐bottom macrobenthos in shallow to intermediate depths of Newport Canyon is much higher than in other southern California canyons (Hartman, 1963). This difference is mainly due to sampling effort and the inactive nature of Newport Canyon which facilitates the maturation of soft‐bottom communities; in contrast to active canyons which through turbidity currents frequently disrupt the water‐sediment interface. Conditions within Newport Canyon have been stable for benthic community structure for at least 16 years and probably closer to 25 years. The hypothesis examined here shows that community structure is not homogeneous with depth along its axis, but has a marked break between 187 m and 324 m. Finally, we are now in a position to examine hypotheses concerning the effects of an ocean outfall on benthic community structure between the shelf and the
机译:摘要:在加利福尼亚州纽波特海底峡谷中,采用一组定量VanVeen(0.1 m2)样品,沿峡谷轴线测试了软底大型底栖动物底栖动物群落结构不变的假设。C4站(187 m)和C5站(324 m)之间的社区结构明显断裂。本研究与早期工作的比较表明,1962 年至 1978 年间物种的平均数量、丰度和生物量没有显着差异。在峡谷内,与其他 12 个南加州峡谷相比,物种多样性很高。从1978年到1990年,加利福尼亚州纽波特峡谷发现了500多个物种。纽波特峡谷中浅层至中层软底大型底栖动物的多样性远高于其他南加州峡谷(Hartman,1963)。这种差异主要是由于采样工作和纽波特峡谷的非活动性质,这促进了软底群落的成熟;与活跃的峡谷相反,活跃的峡谷经常通过浊流破坏水-沉积物界面。纽波特峡谷内的底栖群落结构条件已经稳定了至少16年,可能接近25年。本文研究的假设表明,群落结构与其轴线的深度不均匀,但在 187 m 和 324 m 之间有明显的断裂。最后,我们现在能够研究有关海洋排污口对大陆架和大陆架之间底栖群落结构影响的假设。

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