首页> 外文期刊>Progress in Oceanography >Spatial and temporal variability of microplankton and detritus, and their export to the shelf sediments in the upwelling area off Concepcion, Chile (~36°S), during 2002-2005
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Spatial and temporal variability of microplankton and detritus, and their export to the shelf sediments in the upwelling area off Concepcion, Chile (~36°S), during 2002-2005

机译:在2002-2005年期间,智利康塞普西翁(〜36°S)附近上升流区微浮游生物和碎屑的时空变化及其向陆架沉积物的出口

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Seasonal variations in diversity and biomass of diatoms, tintinnids, and dinoflagellates and the contribution of micro-plankton and faecal material to the vertical flux of particulates were investigated at one time series station T (station 18) between 2002 and 2005 and at a grid of stations during November 2004 in the coastal and oceanic area off Concepcion (36°S), Chile. The variations were analysed in relation to water column temperature, dissolved oxygen, nutrient concentration, offshore Ekman transport, and chlorophyll-a concentration. Abundance was estimated as cell numbers per litre and biomass in terms of biovolume and carbon units. A sharp decrease with depth was observed in the abundance of both phytoplankton and microzooplankton during the whole annual cycle; over 70% of their abundance was concentrated in the upper 10 m of the water column. Also, a clear seasonality in microplankton distribution was observed at station T, with maxima for diatoms, tintinnids, and dinoflagellates every summer (centred on January) from 2002 to 2005. On the grid of stations, the maximum integrated (0-50 m) micro-phytoplankton abundances ( > 1 × 10~9 cells m~(-2)) occurred at the coastal stations, an area directly influenced by upwelling. A similar spatial distribution was observed for the integrated (0-200 m) faecal carbon (with values up to 632 mg C m~(-2)). Tintinnids were distributed in all the first 300 miles from the coast and dinoflagellates were more abundant in oceanic waters. At station T, the average POC export production (below 50 m depth) was 16.6% (SD = 17%; range 2-67%; n = 16). The biological-mediated fluxes of carbon between the upper productive layer and the sediments of the continental shelf off Concepcion depend upon key groups of phytoplankton (Thalassiosira spp., Chaetoceros spp.) and zooplankton (euphausiids) through the export of either cells or faecal material, respectively.
机译:在2002年至2005年的一个时间序列T站(第18站)和一个网格上,研究了硅藻,丁香和鞭毛藻的多样性和生物量的季节性变化,以及微浮游生物和粪便对颗粒垂直通量的贡献。 2004年11月,在智利康塞普西翁(36°S)附近的沿海和大洋地区建立了气象站。分析了与水柱温度,溶解氧,养分浓度,离岸埃克曼转运和叶绿素-a浓度有关的变化。丰度估计为每升细胞数和生物量,以生物量和碳单位表示。在整个年周期中,浮游植物和微浮游动物的数量都随着深度的增加而急剧下降。他们的丰富度的70%以上集中在水柱的上方10 m。此外,在T站观察到微浮游生物分布的明显季节性,从2002年至2005年的每个夏季(1月为中心),硅藻,tintinnids和鞭毛鞭毛的最大值。在站网格中,最大积分(0-50 m)微型浮游植物的丰度(> 1×10〜9个细胞m〜(-2))发生在沿海站,该地区直接受到上升流的影响。粪便中集成的(0-200 m)粪便碳具有相似的空间分布(值高达632 mg C m〜(-2))。 tintinnids分布在距海岸的前300英里处,而鞭毛藻在海洋水域中更为丰富。在T站,平均POC出口产量(低于50 m深度)为16.6%(SD = 17%;范围2-67%; n = 16)。康塞普西翁上层生产层与大陆架沉积物之间的生物介导的碳通量取决于通过细胞或粪便物质的出口的浮游植物(Thalassiosira spp。,Chaetoceros spp。)和浮游动物(euphausiids)的关键群体。 , 分别。

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