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Arsenate and microbial dynamics in different phosphorus regimes of the subtropical Pacific Ocean

机译:亚热带太平洋不同磷形态下的砷和微生物动力学

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Biologically toxic arsenate is physicochemically similar to biologically essential phosphate. Because arsenate and phosphate are indiscriminately incorporated by microbes, their ambient concentration ratios can be an important factor controlling microbial growth and metabolism. This study investigated the spatial distributions of arsenate and phosphate and the associated biogeochemical dynamics in the subtropical North and South Pacific Ocean. Vertical arsenate and phosphate profiles (<= 150 m) in most of the study areas showed a nutrient-type distribution where the concentrations increased below the euphotic zone. The arsenate and phosphate concentrations in the surface waters ranged from the detection limits (5 nM and 4 nM, respectively) to approximately 40 nM and 400 nM, respectively. The surface arsenate:phosphate ratios were typically lower than 1, but those in the western subtropical North Pacific (WSNP) were frequently higher than 1 due to phosphate depletion. In the WSNP surface waters, Prochlorococcus and Pelagibacter arsenic detoxification and phosphorus acquisition genes were abundant. Results of the onboard bioassays involving the addition of arsenate or phosphate to the surface water indicated that microbes throughout the study areas possessed arsenate resistance and those in the WSNP during summer were under serious phosphate limitation. Although phosphate limitation likely accelerates the relative cellular accumulation of toxic arsenate, the lowest particulate As:P ratios were observed in the summer WSNP, concurrent with the lowest dissolved organic P (DOP) concentrations and the highest alkaline phosphatase activities. These results imply that active As excretion and/or DOP utilization could alleviate As accumulation while maintaining the cellular P quota.
机译:具有生物毒性的砷酸盐在物理化学上类似于生物学必需的磷酸盐。由于砷和磷酸盐被微生物不加选择地掺入,它们的环境浓度比可能是控制微生物生长和代谢的重要因素。这项研究调查了亚热带北太平洋和南太平洋中砷酸盐和磷酸盐的空间分布以及相关的生物地球化学动力学。大多数研究区域中的垂直砷酸盐和磷酸盐剖面(<= 150 m)显示出一种营养类型的分布,其中浓度在富营养区以下增加。地表水中砷和磷酸盐的浓度范围从检测极限(分别为5 nM和4 nM)到大约40 nM和400 nM。表面砷酸盐:磷酸盐的比率通常低于1,但由于磷酸盐消耗,西亚热带北太平洋(WSNP)中的砷酸盐:磷酸盐的比率通常高于1。在WSNP地表水中,原球菌和Pelagibacter砷的解毒和磷获取基因丰富。船上涉及向地表水中添加砷酸盐或磷酸盐的生物测定结果表明,整个研究区域的微生物均具有砷酸盐抗性,而夏季WSNP中的微生物处于严重的磷酸盐限制之下。尽管磷酸盐的限制可能会加速有毒砷酸盐的相对细胞积累,但在夏季WSNP中观察到最低的颗粒As:P比,同时具有最低的溶解有机P(DOP)浓度和最高的碱性磷酸酶活性。这些结果暗示活跃的As排泄和/或DOP利用可以减轻As的积累,同时保持细胞的P配额。

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