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南大洋浮游植物水华期间微生物痕量金属转运蛋白的季节性动态。

Seasonal dynamics in microbial trace metals transporters during phytoplankton blooms in the Southern Ocean.

机构信息

School of Oceanography, Shanghai Jiao Tong University, Shanghai, China.

Laboratoire d'Océanographie Microbienne, LOMIC, Sorbonne Université, CNRS, Banyuls-sur-Mer, France.

出版信息

Environ Microbiol. 2024 Oct;26(10):e16695. doi: 10.1111/1462-2920.16695.

Abstract

Trace metals are required as cofactors in metalloproteins that are essential in microbial metabolism and growth. The microbial requirements of diverse metals and the capabilities of prokaryotic taxa to acquire these metals remain poorly understood. We present here results from metagenomic observations over an entire productive season in the region off Kerguelen Island (Indian Sector of the Southern Ocean). We observed seasonal patterns in the abundance of prokaryotic transporters of seven trace elements (zinc [Zn], manganese [Mn], nickel [Ni], molybdenum [Mo], tungsten [W], copper [Cu] and cobalt [Co]) and the consecutive spring and summer phytoplankton blooms were strong drivers of these temporal trends. Taxonomic affiliation of the functional genes revealed that Rhodobacteraceae had a broad repertoire of trace metal transporters (Mn, Zn, Ni, W and Mo) and a more restricted set was observed for other prokaryotic groups, such as Flavobacteriaceae (Zn), Nitrincolaceae (Ni and W) and Thioglobaceae (Mo). The prevalence of trace metal transporters within a prokaryotic group, as determined on the family level, was overall confirmed in representative metagenome-assembled genomes. We discuss the potential involvement of prokaryotic groups in processes related to organic matter utilisation that require these metals and the consequences on carbon and trace metal cycling in surface waters of the Southern Ocean.

摘要

痕量金属是金属蛋白的辅因子,对微生物的新陈代谢和生长至关重要。不同金属对微生物的需求以及原核生物类群获取这些金属的能力仍知之甚少。我们在此展示了在克尔格伦岛(南大洋印度海域)附近整个产季的宏基因组观测结果。我们观察到七种痕量元素(锌[Zn]、锰[Mn]、镍[Ni]、钼[Mo]、钨[W]、铜[Cu]和钴[Co])的原核转运蛋白的丰度存在季节性变化,而连续的春季和夏季浮游植物的爆发是这些时间趋势的主要驱动因素。功能基因的分类学归属表明,红杆菌科具有广泛的痕量金属转运蛋白(Mn、Zn、Ni、W 和 Mo),而其他原核生物群,如黄杆菌科(Zn)、硝化杆菌科(Ni 和 W)和硫杆菌科(Mo)则观察到更为有限的转运蛋白。在原核生物类群中,基于科水平确定的痕量金属转运蛋白的普遍性,在代表性的宏基因组组装基因组中得到了总体证实。我们讨论了这些金属在与有机物利用相关的过程中,原核生物群可能的参与情况,以及这对南大洋表层水碳和痕量金属循环的影响。

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