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The effects of green shelled mussel mariculture on benthic communities in Hauraki Gulf

机译:绿壳贻贝海水养殖对豪拉基湾底栖生物群落的影响

摘要

Sea-bed benthic-invertebrate assemblages of species within and proximal to an existing mussel farm off Taniwhanui Point, eastern Waiheke Island, are reported. Substratum type, whether predominantly mud, gravels or an admixture of the two, mud/gravels, is shown to influence infaunal species assemblage composition; the bivalve Theora lubrica, ostracods, amphipods and polychaetes characterise muddy substrata; polychaetes, particularly spionids and syllids, ostracods, amphipods, bivalves and ophiuroids characterise mud/gravel substrata; and diverse assemblages of polychaetes, bivalves, pagurid crabs, gastropods, ostracods, ophiuroids and nemertean worms characterise gravel substrata. Significant differences in sea-bed assemblages are reported along one transect inside and outside the farm over the three seasons during which surveys were conducted, summer, autumn, winter of 2008. Along the northern side of the mussel farm those sediments beneath the farm are characterised by greater abundances of polychaetes and crustaceans (Malacostraca), whereas sediments outside the farm are characterised by greater abundances of bivalves and ostracods. Sediments both inside and outside the north-eastern border of the farm during summer are characterised by similar abundances of polychaetes, bivalves and ostracods. Similarly, those sediments within and outside the farm along its southern border during summer are characterised by abundances of polychaetes, bivalves, crustaceans (Malacostraca) and gastropods. Measures of relative abundance, rarity and species richness are applied to sea-bed assemblages off eastern Waiheke Island to enable an appraisal of the spatial distribution of each within and outside the farm, and throughout the eastern Waiheke Island region. One of these measures, relative abundance, is then compared with other, albeit limited abundance data from previous soft-sediment surveys conducted throughout Hauraki Gulf. The most species rich and abundant sites off eastern Waiheke Island occur in gravelly substrata between Waiheke Island and Pakatoa Island, and between Rotoroa and Ponui Islands, in addition to beneath the southern portion of the existing mussel farm. Gravel-based substrata are recognised to be the most species rich and densely populated with invertebrates for this sediment type in Hauraki Gulf. Similarly, the muddy substrata off eastern Waiheke Island region appear to host more individuals and species than any other reported muddy substratum in Hauraki Gulf. The existing mussel farm is shown to significantly affect sea-bed communities, but in a manner that has not been previously reported in New Zealand. Species richness and abundance are greater beneath the farm, as are the proportions of very rare and uncommon taxa to more common and ubiquitous taxa. Sediments beneath the farm are not characterised by elevated abundances and richness of opportunistic species; and no obvious difference in sediment grain size is apparent along a transect extending from 20 m inside the farm to at least 110 m outside it. The biological footprint of the farm is limited, appearing to extend no further than 20 metres from the northern physical boundary of the farm; the gross sedimentary characteristics (grain size) do not differ significantly within and outside the farm. Within and immediately outside the farm species richness and abundance tend to increase during colder seasons; beneath the farm, species richness (d), abundance (N), Shannon index (H’) and Simpson index (1-λ’) were higher during May (autumn) and August (winter) than during February (summer); diversity values outside the farm were similar during summer and autumn, but species richness (d), evenness (J’), Shannon index (H’) and Simpson index (1-λ’) were all greater during winter. No opportunistic taxa are considered to be appropriate indicators of organically enriched environments, at least enrichment that can be intuitively linked to any direct effect of the existing mussel farm. One species, the heart urchin Echinocardium cordatum, only rarely occurs inside the physical farm boundary, so its relative abundance renders it an appropriate indicator species of mussel-farm impacts.
机译:据报道,在怀赫科岛东部的塔尼瓦哈努伊角(Taniwhanui Point)附近,一个现有的贻贝养殖场内及其附近的海底底栖无脊椎动物组合。基质类型,主要是泥土,砾石或两者的混合物,已显示出会影响不育物种组合的组成;双壳类Theora lubrica,原脚类,两栖类和多毛类是泥质基质的特征。多壳类动物,特别是孢子和突足类,成龙类,两栖类动物,双壳类和类蛇类是泥/砾石基质的特征。砾石基质的特征包括多种多样的多毛类,双壳类,pagurid蟹,腹足类,成骨类,蛇类和nemertean蠕虫。据报道,在2008年夏季,秋季,冬季的三个季节中,在该农场内外的一个样带上,海床组合的显着差异在2008年的夏季,秋季,冬季进行了调查。在贻贝农场的北侧,对该农场下方的沉积物进行了表征。其特点是多壳类和甲壳类(Malacostraca)的丰度较高,而农场外的沉积物则以双壳类和类动物的丰度较高为特征。夏季,农场东北边界内外的沉积物都以类似的多毛类,双壳类和成骨类动物为特征。同样,在夏季,沿农场南部边界在农场内外的沉积物以多毛鱼类,双壳类,甲壳类(Malacostraca)和腹足动物为特征。将相对丰度,稀有性和物种丰富度的度量应用于怀赫科岛东部沿海海床组合,以评估农场内外以及整个怀赫科岛东部区域的空间分布。然后,将这些量度中的一种,即相对丰度,与其他数据进行了比较,尽管以前整个豪拉基湾进行的软沉积调查的数据有限。怀赫科岛东部以外物种最多,最丰富的地点是在怀赫科岛与帕卡托亚岛之间,罗托鲁瓦与波努伊岛之间的砾石底层,以及现有贻贝养殖场的南部。在豪拉基湾,基于砾石的地层是这种沉积物类型中最丰富且无脊椎动物密集的物种。同样,东豪伊赫克岛地区外的泥质基质似乎比豪拉基湾任何其他已报道的泥质基质拥有更多的个体和物种。现有的贻贝养殖场已显示出对海床社区的重大影响,但其方式以前在新西兰尚未见报道。农场下的物种丰富度和丰富度更高,非常罕见和罕见的生物分类与更普遍和普遍存在的生物分类的比例也更高。农场下方的沉积物的特征不是丰富的数量和丰富的机会主义物种。从农场内部20 m延伸到农场外部至少110 m的样带,沉积物粒度没有明显差异。农场的生物足迹是有限的,似乎延伸到农场北部物理边界不超过20米;农场内外的总体沉积特征(粒度)没有显着差异。在寒冷季节,农场内部和外部的物种丰富度和丰度往往会增加;在农场下方,五月(秋季)和八月(冬季)的物种丰富度(d),丰度(N),香农指数(H')和辛普森指数(1-λ')高于二月(夏季);夏季和秋季,农场外部的多样性值相似,但冬季的物种丰富度(d),均匀度(J’),香农指数(H’)和辛普森指数(1-λ’)都更大。没有机会类群被认为是有机富集环境的适当指标,至少可以直观地将其与现有贻贝养殖场的任何直接影响联系在一起的富集。心脏野心棘心病一类物种很少在物理农场边界内发生,因此其相对丰度使其成为贻贝农场影响的适当指示物种。

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    Wong Clara;

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  • 年度 2009
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