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Distribution of meiofauna in bathyal sediments influenced by the oxygen minimum zone off Costa Rica

机译:哥斯达黎加近海最小氧气区影响海底沉积物中鱼类的分布

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Ocean deoxygenation has become a topic of increasing concern because of its potential impacts on marine ecosystems, including oxygen minimum zone (OMZ) expansion and subsequent benthic effects. We investigated the influence of oxygen concentration and organic matter (OM) availability on metazoan meiofauna within and below an OMZ in bathyal sediments off Costa Rica, testing the hypothesis that oxygen and OM levels are reflected in meiofaunal community structures and distribution. Mean total densities in our sampling cores (400-1800 m water depth) were highest with 3688 ind. 10 cm-2 at the OMZ core at 400 m water depth, decreasing rapidly downslope. Nematodes were overall dominant, with a maximum of 99.9% in the OMZ core, followed by copepods (13%), nauplii (4.8%), and polychaetes (3%). Relative copepod and nauplii abundance increased consistently with depth and increasing bottom-water O2. Meiofaunal composition was significantly different among sites, with lower taxonomic diversity at OMZ sites relative to deeper, oxygenated sites. Vertical distribution patterns within sediments showed that in strongly oxygen-depleted sites less meiofauna was concentrated in the surface sediment than at deeper slope sites. Highest meiofaunal abundance and lowest diversity occurred under lowest oxygen and highest pigment levels, whereas highest diversity occurred under highest oxygen-concentrations and low CPE, as well as high quality of sedimentary pigment (chl a/phaeo) and organic carbon (C/N). The lower meiofaunal diversity, and hence lower structural and trophic complexity, at oxygen-depleted sites raises concerns about changes in the structure and function of benthic marine ecosystems in the face of OMZ expansions.
机译:海洋脱氧已经成为人们日益关注的话题,因为它对海洋生态系统的潜在影响,包括最小氧区(OMZ)扩展和随后的底栖影响。我们调查了氧气浓度和有机质(OM)的可用性对哥斯达黎加海底沉积物中OMZ内和以下的后生动物微动动物的影响,检验了氧和OM水平反映在动植物群落结构和分布中的假设。我们采样岩心的平均总密度(水深为400-1800 m)最高,为3688 ind。在水深400 m的OMZ岩心处10 cm-2,迅速降低了下坡。线虫总体上占优势,在OMZ核心中最大为99.9%,其次是co足类(13%),无节幼体(4.8%)和多壳类(3%)。相对co足和无节幼体的丰度随着深度和底水O2的增加而持续增加。各个部位的角茴香成分显着不同,与较深的含氧部位相比,OMZ部位的分类多样性较低。沉积物内的垂直分布模式表明,在氧气严重耗竭的地区,与深坡地区相比,较少的动物群落集中在地表沉积物中。在最低的氧气和最高的色素水平下,最高的金黄色金属丰度和最低的多样性发生,而在最高的氧气浓度和较低的CPE,以及高品质的沉积色素(chl a / phaeo)和有机碳(C / N)下,最高的多样性发生。在缺氧的地区,较低的动植物多样性,从而降低了结构和营养的复杂性,这引起了人们对OMZ扩张下底栖海洋生态系统结构和功能变化的担忧。

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