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Phosphorus Cycling in the Red Tide Incubator Region of Monterey Bay in Response to Upwelling

机译:上升流对蒙特雷湾赤潮孵化区磷循环的影响

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摘要

This study explores the cycling of phosphorus (P) in the euphotic zone following upwelling in northeastern Monterey Bay (the Red Tide Incubator region) of coastal California, with particular emphasis on how bacteria and phytoplankton that form harmful algal blooms mediate and respond to changes in P availability. In situ measurements of nutrient concentrations, phytoplankton community composition, and cell-specific alkaline phosphatase (AP) activity (determined via enzyme-labeled fluorescence assay) were measured during three cruises. Upwelling led to a 10-fold increase in dissolved inorganic (DIP) in surface waters, reaching ∼0.5 μmol L−1. This DIP was drawn down rapidly as upwelling relaxed over a period of 1 week. Ratios of nitrate to DIP drawdown (∼5:1, calculated as the change in nitrate divided by the change in DIP) were lower than the Redfield ratio of 16:1, suggesting that luxury P uptake was occurring as phytoplankton bloomed. Dissolved organic (DOP) remained relatively constant (∼0.3 μmol L−1) before and immediately following upwelling, but doubled as upwelling relaxed, likely due to phytoplankton excretion and release during grazing. This transition from a relatively high DIP:DOP ratio to lower DIP:DOP ratio was accompanied by a decline in the abundance of diatoms, which had low AP activity, toward localized, spatially heterogeneous blooms of dinoflagellates in the genera Prorocentrum, Ceratium, Dinophysis, Alexandrium, and Scrippsiella that showed high AP activity regardless of ambient DIP levels. A nutrient addition incubation experiment showed that phytoplankton growth was primarily limited by nitrate, followed by DIP and DOP, suggesting that P regulates phytoplankton physiology and competition, but is not a limiting nutrient in this region. AP activity was observed in bacteria associated with lysed cell debris and aggregates of particulate organic material, where it may serve to facilitate P regeneration, as well as affixed to the surfaces of intact phytoplankton cells, possibly indicative of close, beneficial phytoplankton–bacteria interactions.
机译:这项研究探索了加利福尼亚沿海蒙特雷湾(红潮孵化器地区)东北部上升后富营养区中磷(P)的循环,特别着重于形成有害藻华的细菌和浮游植物如何介导和响应藻类的变化。 P可用性。在三轮航行中对营养物浓度,浮游植物群落组成和细胞特异性碱性磷酸酶(AP)活性(通过酶标记的荧光测定法测定)进行了现场测量。上升流导致地表水中的溶解性无机(DIP)增加了10倍,达到〜0.5μμmol·L-1。随着上流在1周内的放松,该DIP迅速下降。硝酸盐与DIP下降的比率(〜5:1,用硝酸盐的变化除以DIP的变化计算)低于Redfield的16:1比率,这表明浮游植物开花时会吸收大量的P。在上涌之前和之后,溶解的有机物(DOP)保持相对恒定(〜0.3μμmol·L-1),但由于上浮过程中的浮游植物排泄和释放,上溢放松而翻倍。从相对较高的DIP:DOP比值降低到较低的DIP:DOP比值的转变是伴随着具有低AP活性的硅藻丰度的下降,向原核,角膜蕨属,恐龙,无论周围的DIP浓度如何,亚历山大和镰孢菌均具有较高的AP活性。营养物添加温育实验表明,浮游植物的生长主要受硝酸盐限制,其次是DIP和DOP,这表明磷调节浮游植物的生理和竞争,但不是该区域的限制性营养物。在与裂解的细胞碎片和颗粒状有机物质聚集体相关的细菌中观察到了AP活性,它可以促进磷的再生,并附着在完整的浮游植物细胞表面,这可能表明浮游植物与细菌之间存在紧密而有益的相互作用。

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