Held Noelle A, Sutherland Kevin M, Webb Eric A, McIlvin Matthew R, Cohen Natalie R, Devaux Alexander J, Hutchins David A, Waterbury John B, Hansel Colleen M, Saito Mak A
Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA, USA.
Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA.
ISME Commun. 2021 Jul 13;1(1):35. doi: 10.1038/s43705-021-00034-y.
The keystone marine nitrogen fixer Trichodesmium thrives in high-dust environments. While laboratory investigations have observed that Trichodesmium colonies can access the essential nutrient iron from dust particles, less clear are the biochemical strategies underlying particle-colony interactions in nature. Here we demonstrate that Trichodesmium colonies engage with mineral particles in the wild with distinct molecular responses. We encountered particle-laden Trichodesmium colonies at a sampling location in the Southern Caribbean Sea; microscopy and synchrotron-based imaging then demonstrated heterogeneous associations with iron oxide and iron-silicate minerals. Metaproteomic analysis of individual colonies by a new low-biomass approach revealed responses in biogeochemically relevant proteins including photosynthesis proteins and metalloproteins containing iron, nickel, copper, and zinc. The iron-storage protein ferritin was particularly enriched implying accumulation of mineral-derived iron, and multiple iron acquisition pathways including Fe(II), Fe(III), and Fe-siderophore transporters were engaged. While the particles provided key trace metals such as iron and nickel, there was also evidence that Trichodesmium was altering its strategy to confront increased superoxide production and metal exposure. Chemotaxis regulators also responded to mineral presence suggesting involvement in particle entrainment. These molecular responses are fundamental to Trichodesmium's ecological success and global biogeochemical impact, and may contribute to the leaching of particulate trace metals with implications for global iron and carbon cycling.
关键的海洋固氮蓝藻束毛藻在高沙尘环境中茁壮成长。虽然实验室研究观察到束毛藻群体可以从沙尘颗粒中获取必需营养元素铁,但自然界中颗粒与群体相互作用背后的生化策略尚不清楚。在这里,我们证明束毛藻群体在野外与矿物颗粒相互作用时具有独特的分子反应。我们在加勒比海南部的一个采样点遇到了附着颗粒的束毛藻群体;显微镜检查和基于同步加速器的成像随后显示了与氧化铁和铁硅酸盐矿物的异质关联。通过一种新的低生物量方法对单个群体进行的元蛋白质组分析揭示了生物地球化学相关蛋白质的反应,包括光合作用蛋白质以及含铁、镍、铜和锌的金属蛋白。铁储存蛋白铁蛋白特别富集,这意味着矿物来源的铁在积累,并且多种铁获取途径,包括亚铁离子(Fe(II))、铁离子(Fe(III))和铁载体转运蛋白都在发挥作用。虽然颗粒提供了关键的痕量金属,如铁和镍,但也有证据表明束毛藻正在改变其策略以应对超氧化物产生增加和金属暴露。趋化性调节因子也对矿物的存在做出反应,表明其参与了颗粒夹带。这些分子反应对于束毛藻的生态成功和全球生物地球化学影响至关重要,并且可能有助于颗粒痕量金属的淋溶,对全球铁和碳循环产生影响。