Molecular mechanisms underlying iron and phosphorus co-limitation responses in the nitrogen-fixing cyanobacterium Crocosphaera
Molecular mechanisms underlying iron and phosphorus co-limitation responses in the nitrogen-fixing cyanobacterium Crocosphaera
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DOI:
10.1038/s41396-022-01307-7
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发表时间:
2022-08
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通讯作者:
Nina Yang;Yu-An Lin;C. Merkel;Michelle A. DeMers;Ping-Ping Qu-Ping;E. Webb;Feixue Fu;D. Hutchins
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作者:
Nina Yang;Yu-An Lin;C. Merkel;Michelle A. DeMers;Ping-Ping Qu-Ping;E. Webb;Feixue Fu;D. Hutchins
In the nitrogen-limited subtropical gyres, diazotrophic cyanobacteria, includingCrocosphaera, provide an essential ecosystem service by converting dinitrogen (N2) gas into ammonia to support primary production in these oligotrophic regimes. Natural gradients of phosphorus (P) and iron (Fe) availability in the low-latitude oceans constrain the biogeography and activity of diazotrophs with important implications for marine biogeochemical cycling. Much remains unknown regardingCrocosphaera’s physiological and molecular responses to multiple nutrient limitations. We culturedC. watsoniiunder Fe, P, and Fe/P (co)-limiting scenarios to link cellular physiology with diel gene expression and observed unique physiological and transcriptional profiles for each treatment. Counterintuitively, reduced growth and N2fixation resource use efficiencies (RUEs) for Fe or P under P limitation were alleviated under Fe/P co-limitation. Differential gene expression analyses show that Fe/P co-limited cells employ the same responses as single-nutrient limited cells that reduce cellular nutrient requirements and increase responsiveness to environmental change including smaller cell size, protein turnover (Fe-limited), and upregulation of environmental sense-and-respond systems (P-limited). Combined, these mechanisms enhance growth and RUEs in Fe/P co-limited cells. These findings are important to our understanding of nutrient controls on N2fixation and the implications for primary productivity and microbial dynamics in a changing ocean.