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Biodiversity and abundance patterns of rock encrusting fauna in a temperate fjord

机译:温带峡湾围岩动物的生物多样性和丰度模式

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摘要

Fjords are semi-enclosed systems often with usually strong physical and chemical gradients. These gradients provide the opportunity to test the influence of various physical and chemical factors on biodiversity. However study area of this investigation, Trondheimsfjord, is a large water body where especially salinity gradient along the fjord is not well pronounced. The goal of this study was to establish within a temperate fjord a baseline identifying encrusting fauna on rocks and determine the factors driving changes along the length of the fjord and changing depths. There was no trend in species composition change and increase or decrease in number of species, diversity and number of individuals along the fjord. This was likely due to the relative homogeneity of both substrate (rocks) and environmental parameters. Nevertheless, the influence of fresh water inflow in the vicinity of the river mouth was apparent by the presence of characteristic brackish-water species at these locations. Multidimensional scaling analysis revealed three separate assemblages: intertidal, shallow and deep subtidal (below 50 m). Intertidal assemblages were species poor (one to 11 species) but relatively abundant (six to 2374 indiv./m~2 of rocks). Number of individuals and biomass was highest in the shallow subtidal (2059-13,587 indiv./m~2 of rocks). Overall the highest species number (45) was recorded at 50 m depth which is probably result of low competition pressure yet still relatively high nutrient concentration in comparison to shallower locations. Environmental parameters (i.e., tidal currents, wave action, salinity) change more drastically with depth than along the fjord and these changes are the major driving forces in shaping encrusting assemblages in Trondheimsfjord.
机译:峡湾是半封闭的系统,通常具有强烈的物理和化学梯度。这些梯度为测试各种物理和化学因素对生物多样性的影响提供了机会。但是,本研究的研究区域Trondheimsfjord是一个大水体,在峡湾沿岸的盐度梯度并不十分明显。这项研究的目的是在温带峡湾中建立一个基线,以识别岩石上的结壳动物,并确定驱动沿峡湾长度和深度变化的因素。峡湾沿岸的物种组成没有变化,物种数量,多样性和个体数量增加或减少的趋势。这可能是由于基材(岩石)和环境参数的相对均一性造成的。尽管如此,由于这些地区存在咸淡水物种,淡水流入河口附近的影响显而易见。多维比例尺分析显示了三个单独的组合:潮间带,浅层和深层亚潮带(50 m以下)。潮间带组合的物种较弱(1至11种),但相对丰富(6至2374个人/ m〜2的岩石)。潮下浅层中个体数量和生物量最高(2059-13,587 indiv./m~2岩石)。总体上,最高物种数(45)记录在50 m深度,这可能是竞争压力低但与较浅位置相比仍相对较高的养分浓度的结果。环境参数(即潮流,波浪作用,盐度)随深度的变化比沿峡湾的变化大得多,而这些变化是在特隆赫姆峡湾塑造结壳组件的主要驱动力。

著录项

  • 来源
    《Marine Environmental Research》 |2013年第junaajula期|61-72|共12页
  • 作者

    Piotr Kuklinski;

  • 作者单位

    Institute of Oceanology, Polish Academy of Sciences, ul. Powstancow Warszawy 55, Sopot 81-712, Poland;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    North Atlantic; Trondheimsfjord; Fjord; Rocks; Biodiversity;

    机译:北大西洋;特隆赫姆峡湾峡湾岩石生物多样性;
  • 入库时间 2022-08-17 13:36:18

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