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首页> 外文期刊>Sedimentology: Journal of the International Association of Sedimentologists >Dolomite formation within microbial mats in the coastal sabkha of Abu Dhabi (United Arab Emirates)
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Dolomite formation within microbial mats in the coastal sabkha of Abu Dhabi (United Arab Emirates)

机译:阿布扎比沿海阿布扎比(阿拉伯联合酋长国)微生物垫内的白云岩形成

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Microbial mediation is the only demonstrated mechanism to precipitate dolomite under Earth surface conditions. A link between microbial activity and dolomite formation in the sabkha of Abu Dhabi has, until now, not been evaluated, even though this environment is cited frequently as the type analogue for many ancient evaporitic sequences. Such an evaluation is the purpose of this study, which is based on a geochemical and petrographic investigation of three sites located on the coastal sabkha of Abu Dhabi, along a transect from the intertidal to the supratidal zone. This investigation revealed a close association between microbial mats and dolomite, suggesting that microbes are involved in the mineralization process. Observations using scanning electron microscopy equipped with a cryotransfer system indicate that authigenic dolomite precipitates within the exopolymeric substances constituting the microbial mats. In current models, microbial dolomite precipitation is linked to an active microbial activity that sustains high pH and alkalinity and decreased sulphate concentrations in pore waters. Such models can be applied to the sabkha environment to explain dolomite formation within microbial mats present at the surface of the intertidal zone. By contrast, these models cannot be applied to the supratidal zone, where abundant dolomite is present within buried mats that no longer show signs of intensive microbial activity. As no abiotic mechanism is known to form dolomite at Earth surface conditions, two different hypotheses can reconcile this result. In a first scenario, all of the dolomite present in the supratidal zone formed in the past, when the mats were active at the surface. In a second scenario, dolomite formation continues within the buried and inactive mats. In order to explain dolomite formation in the absence of active microbial metabolisms, a revised microbial model is proposed in which the mineral-template properties of exopolymeric substances play a crucial role.
机译:微生物调解是在地球表面条件下沉淀白云石的唯一证明机制。迄今为止,尚未评估微生物活动与阿布扎比萨卜哈地区白云岩形成之间的联系,尽管该环境经常被许多古老的蒸发序列的类型类似物引用。这种评估是这项研究的目的,该研究基于对阿布扎比沿海萨布哈沿沿潮间带至上地带的一条断面的三个地点的地球化学和岩石学调查。这项调查揭示了微生物席与白云石之间的紧密联系,表明微生物参与了矿化过程。使用配备有低温传递系统的扫描电子显微镜进行的观察表明,自生的白云石在构成微生物垫的外聚合物质中沉淀。在当前模型中,微生物白云石沉淀与活跃的微生物活动有关,该活动维持高pH和碱度并降低了孔隙水中的硫酸盐浓度。可以将这种模型应用于sabkha环境,以解释潮间带表面微生物垫中白云石的形成。相比之下,这些模型不能应用于上层地带,在该上层地带中存在大量白云岩,这些地层不再显示出强烈的微生物活性迹象。由于尚无非生物机制在地球表面形成白云石,因此有两种不同的假设可以调和这一结果。在第一种情况下,当垫子在地表活动时,存在于上地带中的所有白云岩都是过去形成的。在第二种情况下,白云石的形成在埋入的和非活动的垫层中继续进行。为了解释在没有活跃的微生物代谢的情况下白云石的形成,提出了一种修正的微生物模型,其中外聚合物质的矿物模板特性起着至关重要的作用。

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