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北太平洋亚热带海域溶解态不稳定磷酸单酯和二酯的纵向与垂直变化

Longitudinal and Vertical Variations of Dissolved Labile Phosphoric Monoesters and Diesters in the Subtropical North Pacific.

作者信息

Yamaguchi Tamaha, Sato Mitsuhide, Hashihama Fuminori, Kato Haruka, Sugiyama Takanori, Ogawa Hiroshi, Takahashi Kazutaka, Furuya Ken

机构信息

Fisheries Resources Institute, Japan Fisheries Research and Education Agency, Yokohama, Japan.

Department of Aquatic Bioscience, Graduate School of Agricultural and Life Sciences, The University of Tokyo, Tokyo, Japan.

出版信息

Front Microbiol. 2021 Jan 20;11:570081. doi: 10.3389/fmicb.2020.570081. eCollection 2020.

Abstract

The labile fraction of dissolved organic phosphorus (DOP) - predominantly consisting of phosphoric esters - is an important microbial P source in the subtropical oligotrophic ocean. However, unlike phosphate, knowledge for labile DOP is still limited due to the scarcity of broad and intensive observations. In this study, we examined the concentrations and size-fractionated hydrolysis rates of labile phosphoric monoesters and diesters along a >10,000 km longitudinal transect in the North Pacific (23°N; upper 200-m layer). Depth-integrated monoesters decreased westward with a maximum difference of fivefold. Vertical profiles of monoesters in the eastern and western basins showed decreasing and increasing trends with depth, respectively. The monoester-depleted shallow layer of the western basin was associated with phosphate depletion and monoesterase activity was predominant in the large size fraction (>0.8 μm), suggesting that monoesters are significant P sources particularly for large microbes. In contrast, diester concentrations were generally lower than monoester concentrations and showed no obvious horizontal or vertical variation in the study area. Despite the unclear distribution pattern of diesters, diesterase activity in the particulate fraction (>0.2 μm) increased in the phosphate-depleted shallow layer of the western basin, suggesting that the targeted diesters in the assay were also important microbial P sources. Diesterase activities in the dissolved fraction (<0.2 μm) were not correlated with ambient phosphate concentrations; however, cell-free diesterase likely played a key role in P cycling, as dissolved diesterase activities were substantially higher than those in the particulate fraction. The horizontal and vertical variability of labile monoesters in the subtropical North Pacific were therefore predominantly regulated by P stress in particularly large microbes, whereas the distributions of labile diesters and diesterase activities were generally independent of microbial P stress, indicating a more complex regulation of diesters to that of monoesters.

摘要

溶解有机磷(DOP)的不稳定部分——主要由磷酸酯组成——是亚热带贫营养海洋中重要的微生物磷源。然而,与磷酸盐不同,由于缺乏广泛而密集的观测,关于不稳定DOP的认识仍然有限。在本研究中,我们沿着北太平洋(北纬23°;上层200米)超过10000公里的纵向断面,研究了不稳定磷酸单酯和二酯的浓度以及按粒径分级的水解速率。深度积分的单酯向西递减,最大差异为五倍。东、西盆地单酯的垂直剖面分别显示出随深度递减和递增的趋势。西盆地单酯耗尽的浅层与磷酸盐耗尽有关,且单酯酶活性在大粒径部分(>0.8μm)占主导,这表明单酯是重要的磷源,特别是对大型微生物而言。相比之下,二酯浓度通常低于单酯浓度,且在研究区域内没有明显的水平或垂直变化。尽管二酯的分布模式尚不清楚,但在西盆地磷酸盐耗尽的浅层中,颗粒部分(>0.2μm)的二酯酶活性增加,这表明分析中的目标二酯也是重要的微生物磷源。溶解部分(<0.2μm)的二酯酶活性与环境磷酸盐浓度无关;然而,无细胞二酯酶可能在磷循环中起关键作用,因为溶解态二酯酶活性显著高于颗粒部分。因此,亚热带北太平洋不稳定单酯的水平和垂直变异性主要受大型微生物中磷胁迫的调节,而不稳定二酯和二酯酶活性的分布通常与微生物磷胁迫无关,这表明二酯的调节比单酯更为复杂。

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