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The Role of the Sedimentary Regime in Shaping the Distribution of Subtidal Sandbank Environments and the Associated Meiofaunal Nematode Communities: An Example from the Southern North Sea

机译:沉积制度在改变潮下沙丘环境和相关的牛源线虫群落分布中的作用:以南北海为例

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摘要

We combined sediment and faunal data to explore the role of the sedimentary regime in shaping the distribution of subtidal sandbank environments and the associated meiofaunal nematode communities at Broken Bank and Swarte Bank, in the southern North Sea. A variety of sediment transport processes occur in the area, differing in the frequency and magnitude of sediment mobility, and the continuum between erosion, translation and sediment accumulation. The seabed contained a variety of bedforms, including longitudinal furrows, and small to very large sandwaves. The bed sediments were dominated by fine and medium sands, with admixtures of silt and gravel. Based on sedimentary bedforms and grain size analysis, a total of 11 sedimentary facies were delineated, of which 8 were analysed in detail for their relationships with the meiofauna. The sedimentary facies fell clearly into groups of facies, respectively representing high, high-moderate and moderate, and episodic sediment mobility. For those sedimentary facies where daily movement of sediments and bedforms occurred (‘high’ sediment mobility), the resulting spatially homogeneous environments were dominated by an impoverished nematode community comprising small deposit feeders and large predators. Resistance to sediment movement and the ability to exploit alternative food sources were prominent functional features of the successful colonisers. Those facies characterised by relatively infrequent sediment mobility (‘episodic’ and ‘high-moderate and moderate’ sediment mobility) comprised a heterogeneous suite of benthic habitats, containing taxonomically and functionally diverse assemblages of nematodes of various sizes, feeding types and reproductive potential. Faunal distribution patterns here indicated trade-offs between the resistance to sediment movement, environmental tolerance and competitive abilities. Our focus on diverse assemblages of organisms with high turnover times, inhabiting highly dynamic sedimentary environments, has revealed new animal-sediment relationships of relevance to pure and applied science.
机译:我们结合了沉积物和动物区系数据,探讨了沉积制度在塑造潮汐沙洲环境以及北海南部Broken Bank和Swarte Bank的相关的淡紫色线虫群落分布中的作用。该地区发生了各种沉积物迁移过程,其沉积物迁移的频率和幅度以及侵蚀,平移和沉积物积累之间的连续性都不同。海床包含多种床形,包括纵向犁沟以及小到非常大的沙波。床底沉积物以细砂和中砂为主,还有粉砂和砾石的混合物。根据沉积物床形和粒度分析,共划定了11个沉积相,其中8个与沉积物的关系被详细分析。沉积相清楚地分为相相组,分别代表高,高中度和中度以及偶发性沉积物迁移率。对于那些每天发生沉积物和床状运动(“高”沉积物迁移率)的沉积相,所形成的空间均匀环境主要是一个由线虫组成的贫困线虫群落,其中包括小型沉积物饲养者和大型食肉动物。抵抗泥沙运动和开发替代食物来源的能力是成功定居者的突出功能特征。那些以相对较少的沉积物迁移(“间歇性”和“高中度和中等”沉积物迁移率)为特征的相包括不同种类的底栖生境,其中包含各种分类,功能和种类,不同摄食类型和繁殖潜力的线虫。动物的分布模式表明了在抵抗泥沙运动,环境耐受性和竞争能力之间的权衡。我们关注具有高周转时间的各种生物,在高度动态的沉积环境中居住,揭示了与纯科学和应用科学有关的新的动物-沉积关系。

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