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Biogeochemical cycling and phyto- and bacterioplankton communities in a large and shallow tropical lagoon (Términos Lagoon, Mexico) under 2009–2010 El Ni?o Modoki drought conditions

机译:在2009-2010 El Ni的大型浅层热带泻湖(Términos泻湖,墨西哥)中的生物地球化学循环和植物和菌株组织社区在2009-2010 El Ni?O Modoki干旱条件下

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The 2009–2010 period was marked by an episode of intense drought known as the El Ni?o Modoki event. Sampling of the Términos Lagoon (Mexico) was carried out in November 2009 in order to understand the influence of these particular environmental conditions on organic matter fluxes within the lagoon's pelagic ecosystem and, more specifically, on the relationship between phyto- and bacterioplankton communities. The measurements presented here concern biogeochemical parameters (nutrients, dissolved and particulate organic matter [POM], and dissolved polycyclic aromatic hydrocarbons [PAHs]), phytoplankton (biomass and photosynthesis), and bacteria (diversity and abundance, including PAH degradation bacteria and ectoenzymatic activities). During the studied period, the water column of the Términos Lagoon functioned globally as a sink and, more precisely, as a nitrogen assimilator. This was due to the high production of particulate and dissolved organic matter (DOM), even though exportation of autochthonous matter to the Gulf of Mexico was weak. We found that bottom-up control accounted for a large portion of the variability of phytoplankton productivity. Nitrogen and phosphorus stoichiometry mostly accounted for the heterogeneity in phytoplankton and free-living prokaryote distribution in the lagoon. In the eastern part, we found a clear decoupling between areas enriched in dissolved inorganic nitrogen near the Puerto Real coastal inlet and areas enriched in phosphate (PO4) near the Candelaria estuary. Such a decoupling limited the potential for primary production, resulting in an accumulation of dissolved organic carbon and nitrogen (DOC and DON, respectively) near the river mouths. In the western part of the lagoon, maximal phytoplankton development resulted from bacterial activity transforming particulate organic phosphorus (PP) and dissolved organic phosphorus (DOP) to available PO4 and the coupling between Palizada River inputs of nitrate (NO3) and PP. The Chumpan River contributed only marginally to PO4 inputs due to its very low contribution to overall river inputs. The highest dissolved total PAH concentrations were measured in the El Carmen Inlet, suggesting that the anthropogenic pollution of the zone is probably related to the oil-platform exploitation activities in the shallow waters of the southern of the Gulf of Mexico. We also found that a complex array of biogeochemical and phytoplanktonic parameters were the driving force behind the geographical distribution of bacterial community structure and activities. Finally, we showed that nutrients brought by the Palizada River supported an abundant bacterial community of PAH degraders, which are of significance in this important oil-production zone.
机译:2009 - 2010年期间由被称为EL NI的激烈的干旱活动是标志的。 Términos泻湖(墨西哥)的抽样于2009年11月进行,以了解这些特定环境条件对泻湖的岩浆生态系统内有机质通量的影响,更具体地说,培养植物和菌属组合社区之间的关系。这里介绍了生物地球化学参数(营养,溶解和颗粒物质[POM],溶解多环芳烃[PAHS]),浮游植物(生物质和光合作用)和细菌(包括PAH降解细菌和胞外酶活性,溶解多环芳烃[POM]) )。在研究期间,Términos泻湖的水柱作为水槽全球发挥作用,更精确地作为氮同化器。这是由于颗粒状和溶解有机物(DOM)的高生产率,即使向墨西哥湾出口到墨西哥湾的出口是薄弱的。我们发现自下而上的控制占Phytoplankton生产率的大部分变异性。氮和磷的化学计量主要占盐水植物中浮游植物的异质性和泻湖中的自由生物原核生物分布。在东部,我们发现在坎塔利亚河口附近的波多真正的沿海入口附近富含溶解无机氮的区域之间的清晰分离。这种去耦限制了初级产量的可能性,导致河口附近的溶解有机碳和氮气(分别)积累。在泻湖的西部,最大植物植物发育从细菌活性转化为颗粒状有机磷(PP)和溶解的有机磷(DOP)到可用的PO4,硝酸盐(NO3)和PP的Palizada河流进口之间的耦合。 Chumpan River由于对整个河流投入的贡献非常低,因此仅略微贡献到PO4投入。在EL Carmen入口中测量了最高溶解的总PAH浓度,表明该区域的人为污染可能与墨西哥湾南部浅水区的石油平台剥削活动有关。我们还发现,一种复杂的生物地理化学和浮游植物参数是细菌群落结构和活动地理分布背后的驱动力。最后,我们展示了Palizada River带来的营养素支持一种丰富的Pah降解细菌群体,这在这一重要的石油生产区具有重要意义。
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