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High Molybdenum availability for evolution in a Mesoproterozoic lacustrine environment

机译:中元古代湖相环境中钼的高可用演化性

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Trace metal data for Proterozoic marine euxinic sediments imply that the expansion of nitrogen-fixing cyanobacteria and diversification of eukaryotes were delayed while the availability of bioessential metals such as molybdenum in the ocean was limited. However, there is increasing recognition that the Mesoproterozoic evolution of nitrogen fixation and eukaryotic life may have been promoted in marginal marine and terrestrial environments, including lakes, rather than in the deep ocean. Molybdenum availability is critical to life in lakes, just as it is in the oceans. It is, therefore, important to assess molybdenum availability to the lacustrine environment in the Mesoproterozoic. Here we show that the flux of molybdenum to a Mesoproterozoic lake was 1 to 2 orders of magnitude greater than typical fluxes in the modern and ancient marine environment. Thus, there was no barrier to availability to prevent evolution in the terrestrial environment, in contrast to the nutrient-limited Mesoproterozoic oceans.
机译:原生动物海洋共生沉积物的痕量金属数据表明,固氮细菌的扩展和真核生物的多样化被延迟,而海洋中诸如钼等生物必需金属的可用性却受到限制。但是,人们越来越认识到,可能在边缘湖泊和陆地环境(包括湖泊)而非深海中促进了固氮和真核生物的中元古代演化。钼的供应对湖泊中的生命至关重要,就像在海洋中一样。因此,重要的是评估中元古代的湖环境中钼的可用性。在这里,我们表明,进入中元古代湖的钼通量比现代和古代海洋环境中的典型通量大1至2个数量级。因此,与营养受限的中元古代海洋相比,没有可利用的障碍来阻止在陆地环境中的进化。

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