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Response of the Eastern Mediterranean Microbial Ecosystem to Dust and Dust Affected by Acid Processing in the Atmosphere

机译:东地中海微生物生态系统对大气尘埃和尘埃的反应

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Acid processes in the atmosphere, particularly those caused by anthropogenic acid gases, increase the amount of bioavailable P in dust and hence are predicted to increase microbial biomass and primary productivity when supplied to oceanic surface waters. This is likely to be particularly important in the Eastern Mediterranean Sea (EMS), which is P limited during the winter bloom and N&P co-limited for phytoplankton in summer. However, it is not clear how the acid processes acting on Saharan dust will affect the microbial biomass and primary productivity in the EMS. Here, we carried out bioassay manipulations on EMS surface water on which Saharan dust was added as dust (Z), acid treated dust (ZA), dust plus excess N (ZN) and acid treated dust with excess N (ZNA) during springtime (May 2012) and measured bacterioplankton biomass, metabolic and other relevant chemical and biological parameters. We show that acid treatment of Saharan dust increased the amount of bioavailable P supplied by a factor of ~40 compared to non-acidified dust (18.4 nmoles P mg-1 dust vs. 0.45 nmoles P mg-1 dust, respectively). The increase in chlorophyll, primary and bacterial productivity for treatments Z and ZA were controlled by the amount of N added with the dust while those for treatments ZN and ZNA (in which excessive N was added) were controlled by the amount of P added. These results confirm that the surface waters were N&P co-limited for phytoplankton during springtime. However, total chlorophyll and primary productivity in the acid treated dust additions (ZA and ZNA) were less than predicted from that calculated from the amount of the potentially limiting nutrient added. This biological inhibition was interpreted as being due to labile trace metals being added with the acidified dust. A probable cause for this biological inhibition was the addition of dissolved Al, which forms potentially toxic Al nanoparticles when added to seawater. Thus, the effect of anthropogenic acid processes in the atmosphere, while increasing the flux of bioavailable P from dust to the surface ocean, may also add toxic trace metals such as Al, which moderate the fertilizing effect of the added nutrients.
机译:大气中的酸过程,特别是由人为酸性气体引起的酸过程,增加了粉尘中生物利用磷的含量,因此,预测将其供应到海洋地表水中后,会增加微生物的生物量和初级生产力。这在东地中海(EMS)中尤为重要,该区域冬季盛放时限磷,夏季浮游植物则限N&P限。但是,尚不清楚作用在撒哈拉尘埃上的酸过程如何影响EMS中的微生物生物量和初级生产力。在这里,我们对EMS地表水进行了生物测定操作,在春季,在地表水上添加了撒哈拉粉尘(Z),酸处理粉尘(ZA),粉尘加过量的N(ZN)和酸处理的粉尘和过量N(ZNA)。 2012年5月),并测量了浮游细菌的生物量,代谢和其他相关的化学和生物学参数。我们显示,与未酸化的粉尘(分别为18.4 nmoles P mg-1尘粉和0.45 nmoles P mg-1粉尘)相比,酸处理撒哈拉沙漠粉尘可提供的生物利用磷数量增加约40倍。处理Z和ZA的叶绿素,初级生产力和细菌生产力的提高是由粉尘中添加的N量控制的,而处理ZN和ZNA(其中添加了过量的N)的叶绿素,初级和细菌生产力的提高则由P的添加量控制。这些结果证实,春季浮游植物的地表水受到N&P共同限制。但是,酸处理过的粉尘添加物(ZA和ZNA)中的总叶绿素和初级生产力低于根据潜在添加的有限养分量计算得出的预测值。这种生物抑制作用被解释为是由于不稳定的痕量金属与酸化粉尘一起添加的缘故。这种生物抑制的可能原因是溶解的铝的添加,当添加到海水中时,铝会形成有毒的铝纳米颗粒。因此,人为酸过程在大气中的作用,虽然增加了从粉尘到海洋表层的生物利用磷的通量,但可能还会添加有毒的微量金属(例如Al),从而缓和所添加养分的施肥作用。

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