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首页> 外文期刊>Freshwater Biology >Planktonic phosphorus pool sizes and cycling efficiency in coastal and interior British Columbia lakes.
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Planktonic phosphorus pool sizes and cycling efficiency in coastal and interior British Columbia lakes.

机译:英属哥伦比亚沿海和内陆湖泊浮游生物磷池的大小和循环效率。

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Limnologists have long acknowledged the importance of phosphorus (P) in determining the organism biomass and productivity of lake ecosystems. Despite a relatively large number of studies that have examined P cycling in lake ecosystems, there remain several substantial methodological issues that have impeded our understanding of P cycling in limnetic plankton communities. Two critical issues confronting ecologists are (1) a lack of precise measurements of the dissolved inorganic phosphorus (PO43-) and (2) accurate or complete measurements of dissolved P regeneration rates by plankton communities. Here, we examine patterns of epilimnetic planktonic P pool sizes and turnover rates in eight lakes in British Columbia, Canada over a 2-year period. We determine the concentrations and turnover times of P in various planktonic compartments (dissolved and various planktonic size fractions), using recently developed methods for estimating phosphate concentration and planktonic regeneration rates. The pico- and nanoplankton size fraction (0.2-20 micro m) played a central role in planktonic P cycling in lakes examined by this study. On average across lakes, pico- and nanoplankton contained >60% of the planktonic P, accounted for >90% PO43- uptake, and contributed 50% of the plankton community dissolved P regeneration rate. PO43- concentrations determined by steady state bioassays (ssPO43-) were extremely low (87-611 pmol L-1) and were 2-3 orders of magnitude less than simultaneously measured colorimetric soluble reactive phosphorus estimates. Lake ssPO43- concentrations increased linearly with total phosphorus (TP), and the slope of this relationship was approximately 1, indicating that PO43- remained a consistent proportion of the TP pool across a range of TP concentrations. Turnover rates of the total planktonic P pool and the <20 micro m pool became more rapid with increasing lake TP, indicating that, according to this metric, planktonic P cycling efficiency increased with TP concentrations. We also detected a significant relationship between particulate phosphorus (PP) <20 micro m turnover time and seston N:P ratios, with PP<20 micro m turnover times becoming slower with increasing seston N:P. These findings suggest that long-standing conceptual models of nutrient cycling that predict slower cycling rates and decreasing cycling efficiency with increasing TP concentrations require further empirical examination. We postulate that patterns in lake P turnover and cycling efficiency are a result of complex interactions between plankton biomass and composition, and the ratios of multiple nutrients (C, N, P), rather than solely a function of the TP pool..
机译:湖泊学家早就认识到磷在确定湖泊生态系统生物量和生产力方面的重要性。尽管有大量研究检查了湖泊生态系统中的磷循环,但是仍然存在一些重大的方法论问题,这些问题阻碍了我们对黑质浮游生物群落中磷循环的理解。生态学家面临的两个关键问题是:(1)缺乏对溶解的无机磷(PO43-)的精确测量,(2)浮游生物群落对溶解的磷再生速率的精确或完全测量。在这里,我们研究了加拿大不列颠哥伦比亚省8个湖泊在2年期间的表观浮游性P池大小和周转率的模式。我们使用最近开发的估算磷酸盐浓度和浮游生物再生率的方法,确定了各个浮游生物隔室(溶解的和各种浮游生物的大小分数)中P的浓度和周转时间。这项研究研究了微微和纳米级浮游生物的大小分数(0.2-20微米)在湖泊浮游磷循环中起着重要作用。在整个湖泊中,微微和纳米级浮游生物平均包含> 60%的浮游磷,占> 43%的PO43吸收,并贡献了50%的浮游生物溶解性P再生率。通过稳态生物测定法(ssPO43-)测定的PO43-浓度极低(87-611 pmol L-1),比同时测量的比色可溶性反应性磷估计值低2-3个数量级。 Lake ssPO43-的浓度随总磷(TP)线性增加,并且这种关系的斜率约为1,这表明PO43-在一定范围的TP浓度范围内仍保持TP池的恒定比例。随着湖泊TP的增加,总浮游P池和<20 microm池的周转率变得更快,表明根据该指标,浮游P循环效率随TP浓度的增加而增加。我们还检测到颗粒磷(PP)<20微米周转时间与血浆N:P比率之间存在显着关系,PP <20微米周转时间随着血浆N:P的增加而变慢。这些发现表明,长期的营养循环概念模型需要进一步的实证检验,该模型可以预测循环速率降低和循环效率随TP浓度增加而降低。我们假设湖泊P的周转率和循环效率的模式是浮游生物生物量和组成之间复杂相互作用的结果,以及多种营养物(C,N,P)的比率,而不仅仅是TP库的函数。

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