Iron plays a crucial role in the cycling of organic carbon in the Southern Ocean, but the strategies of diverse microbes in acquiring different forms of iron under seasonally changing organic carbon regimes are poorly understood. High-resolution seasonal metagenomic observations near Kerguelen Island revealed distinct seasonal patterns in the abundance of genes related to iron and organic substrate transport, siderophore biosynthesis, and carbohydrate-active enzymes. This study provides insights into the ecological strategies of iron acquisition and their potential impact on the microbial community composition and organic matter transformations in the Southern Ocean.
Iron (Fe) governs the cycling of organic carbon in large parts of the Southern Ocean. The strategies of diverse microbes to acquire the different chemical forms of Fe under seasonally changing organic carbon regimes remain, however, poorly understood. Here, we report high-resolution seasonal metagenomic observations from the region off Kerguelen Island (Indian Sector of the Southern Ocean) where natural Fe-fertilization induces consecutive spring and summer phytoplankton blooms. Our data illustrate pronounced, but distinct seasonal patterns in the abundance of genes implicated in the transport of different forms of Fe and organic substrates, of siderophore biosynthesis and carbohydrate-active enzymes. The seasonal dynamics suggest a temporal decoupling in the prokaryotic requirements of Fe and organic carbon during the spring phytoplankton bloom and a concerted access to these resources after the summer bloom. Taxonomic assignments revealed differences in the prokaryotic groups harbouring genes of a given Fe-related category and pronounced seasonal successions were observed. Using MAGs we could decipher the respective Fe- and organic substrate-related genes of individual taxa assigned to abundant groups. The ecological strategies related to Fe-acquisition provide insights on how this element could shape microbial community composition with potential implications on organic matter transformations in the Southern Ocean.
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