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Transient fertilizing effect of dust in P-deficient LNLC surface ocean

机译:缺磷LNLC表层海洋粉尘的短暂施肥效应

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[1] In much of the world's low-nutrient low-chlorophyll(LNLC) oceans, including the Mediterranean Sea, surfacedissolved inorganic phosphorus (DIP) is below the detectionlimit of conventional techniques. Although dust depositionhas been generally recognized as a major source of P to theMediterranean Sea, the lack of DIP data at nanomolar levelshas so far precluded a quantification of this effect. Thiswork reports the first one-year time series of surfacenanomolar DIP in the Mediterranean Sea. Moreover, bycombining nanomolar DIP data from two field studies (theabove cited time-series and an experimental addition ofSaharan dust to large mesocosms) and one in vitro dustdissolution experiment, we show that dust pulses mayindeed provoke transient increases in DIP concentration (upto 80 nM) in P-starved surface waters of this LNLC region.
机译:[1]在包括地中海在内的世界许多低营养低叶绿素(LNLC)海洋中,表面溶解的无机磷(DIP)低于常规技术的检测极限。尽管尘埃沉积已被普遍认为是地中海磷的主要来源,但到目前为止,由于缺乏纳摩尔级DIP数据,因此无法对此效果进行量化。这项工作报告了地中海地表纳米摩尔DIP的第一个一年时间序列。此外,通过结合两项现场研究(上文引用的时间序列和将撒哈拉尘埃加入大型中观的实验性添加)和一项体外尘埃溶解实验的纳摩尔DIP数据,我们表明尘埃脉冲确实会引起DIP浓度的瞬时增加(最高80 nM)。在该LNLC地区的P饥饿地表水中。

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