Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, 2778564, Japan.
Department of Earth Science, Graduate School of Sciences, Tohoku University, Sendai, 9808578, Japan.
Sci Rep. 2024 Sep 20;14(1):21780. doi: 10.1038/s41598-024-72191-8.
Phosphorus and molybdenum play important roles in the formation of microbial cell structures and specific enzymes crucial for metabolic processes. Nevertheless, questions remain about the preservation of these elements within ancient microfossils. Here, we present shape-accurate ion images capturing phosphorus and molybdenum on Palaeoproterozoic filamentous microfossils by pioneering a methodology using lateral high-resolution secondary ion mass spectrometry. Introducing electrically conductive glass for mounting isolated microfossils facilitated clearer observations with increased secondary ion yields. Phosphorus was detected along the contours of microfossils, providing direct evidence of phospholipid utilization in the cell membrane. Trace amounts of molybdenum were detected within microfossil bodies, suggesting potential remnants of molybdenum-bearing proteins, such as nitrogenase. These findings align with the hypothesized cyanobacterial origin of filamentous gunflint microfossils. Our methodology introduces a groundbreaking tool for obtaining crucial insights into the cellular evolution and metabolic pathways of microorganisms, allowing comparisons of their morphological characteristics.
磷和钼在微生物细胞结构的形成以及对代谢过程至关重要的特定酶中发挥着重要作用。然而,关于这些元素在古代微生物化石中的保存问题仍存在疑问。在这里,我们通过开创性地使用侧向高分辨率二次离子质谱法,展示了对古元古代丝状微生物化石中磷和钼的精确形状离子图像。引入用于安装分离的微生物化石的导电玻璃,提高了二次离子产率,从而更清晰地观察到化石。在微生物化石的轮廓上检测到磷,这为细胞膜中磷脂的利用提供了直接证据。在微生物化石体内检测到痕量的钼,这表明可能存在含钼蛋白质的残留物,如固氮酶。这些发现与丝状燧石状微生物化石的假定蓝细菌起源一致。我们的方法为深入了解微生物的细胞进化和代谢途径提供了一个开创性的工具,允许对它们的形态特征进行比较。