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首页> 外文期刊>Progress in Oceanography >Transparent exopolymer particle (TEP) distribution and in situ prokaryotic generation across the deep Mediterranean Sea and nearby North East Atlantic Ocean
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Transparent exopolymer particle (TEP) distribution and in situ prokaryotic generation across the deep Mediterranean Sea and nearby North East Atlantic Ocean

机译:透明的外聚合物颗粒(TEP)分布以及整个地中海深海和东北大西洋附近的原核生物

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Transparent exopolymer particles (TEP) play a key role in ocean carbon export and structuring microbial habitats, but information on their distribution across different ocean basins and depths is scarce, particularly in the dark ocean. We measured TEP vertical distribution from the surface to bathypelagic waters in an east-to-west transect across the Mediterranean Sea (MedSea) and the adjacent North East Atlantic Ocean (NEA), and explored their physical and biological drivers. TEP ranged from 0.6 to 81.7 mu g XG eq L-1, with the highest values in epipelagic waters above the deep chlorophyll maximum, and in areas near the Gibraltar and Sicily Straits. TEP were significantly related to particulate organic carbon (POC) in all basins and depth layers (epipelagic vs. deep), but the contribution of TEP to POC was higher in the NEA (85%, 79% and 67% in epi-, meso- and bathypelagic waters, respectively) than in the MedSea (from 53% to 62% in epipelagic waters, and from 45% to 48% in mesoand bathypelagic waters), coinciding with higher carbon to nitrogen particulate organic matter ratios in the NEA. The TEP connectivity between epipelagic waters and mesopelagic waters was less straightforward than between mesopelagic waters and bathypelagic waters, with a 23% and 55% of the variance in the relationship between layers explained respectively. Prokaryotes were found to be a likely net source of TEP as inferred by the significant direct relationship observed between prokaryotic heterotrophic abundance and TEP. This assumption was confirmed using experimental incubations, where prokaryotes produced TEP in concentrations ranging from 0.7 (Western Mediterranean, bathypelagic) to 232 (Western Mediterranean, mesopelagic) mu g XG eq. L-1 day(-1).
机译:透明的外聚合物颗粒(TEP)在海洋碳出口和构造微生物栖息地中起着关键作用,但缺乏有关其在不同海洋盆地和深度的分布的信息,尤其是在暗海中。我们测量了横跨地中海(MedSea)和邻近的东北大西洋(NEA)的东西向样带中,TEP从地表水到深海水的垂直分布,并探讨了它们的物理和生物驱动力。 TEP的范围为0.6到81.7μgXG eq L-1,在深层叶绿素最大值以上的上层水域以及直布罗陀和西西里海峡附近的地区,其最高值。 TEP与所有盆地和深层中的颗粒有机碳(POC)显着相关(远洋层与深层),但NEA中TEP对POC的贡献较高(表观,中观分别为85%,79%和67%) -和深海水域分别比MedSea(上层水域中的53%至62%,中层和深水域中的45%至48%)要高,这与NEA中较高的碳氮颗粒有机物比率相吻合。上层水和中上水之间的TEP连通性不如中上水和深层水之间的TEP连通性简单,层之间关系的差异分别解释了23%和55%。根据原核生物异养菌丰度与TEP之间的显着直接关系推断,原核生物可能是TEP的净来源。通过实验温育证实了这一假设,其中原核生物产生TEP的浓度范围为0.7(西地中海,深浮的)至232(西地中海,中生的)μgXG当量。 L-1天(-1)。

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