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Prochlorococcus Cells Rely on Microbial Interactions Rather than on Chlorotic Resting Stages To Survive Long-Term
Dalit Roth-Rosenberg1, Dikla Aharonovich1, Tal Luzzatto-Knaan1
1Department of Marine Biology, Leon H. Charney School of Marine Sciences, University of Haifa, Haifa, Israel.
Prochlorococcus, a key marine cyanobacterium, undergoes chlorosis under stress but cannot survive alone. Instead, it relies on symbiotic heterotrophic bacteria for survival during nutrient starvation, highlighting microbial interactions in ocean cycles.
Area of Science:
- Marine microbiology
- Ocean biogeochemical cycles
- Cyanobacteria physiology
Background:
- Microorganisms survive nutrient stress via resting cells with low metabolic activity.
- Cyanobacteria and phytoplankton use chlorosis (pigment loss) to form resting stages.
- Prochlorococcus is a dominant phytoplankton globally, crucial for ocean biogeochemical cycles.
Purpose of the Study:
- Investigate chlorosis-like processes in Prochlorococcus under stress.
- Determine Prochlorococcus viability and survival mechanisms during nutrient starvation.
- Understand the ecological role of microbial interactions in Prochlorococcus survival.
Main Methods:
- Axenic laboratory cultures of Prochlorococcus strain MIT9313.
- Induction of stress conditions to observe chlorosis.
- Nanoscale secondary ion mass spectrometry (NanoSIMS) to measure carbon (C) and nitrogen (N) uptake.
- Coculture experiments with Alteromonas macleodii HOT1A3.
Main Results:
- Prochlorococcus exhibits a chlorosis-like process under multiple stress conditions.
- Chlorotic Prochlorococcus cells show reduced metabolic activity (C and N uptake).
- Chlorotic Prochlorococcus cells are not viable axenically but survive for months in coculture with Alteromonas macleodii.
Conclusions:
- Prochlorococcus survival during nutrient starvation depends on symbiotic relationships with heterotrophic bacteria.
- Reliance on bacterial symbionts, not resting cell formation, is key to Prochlorococcus's ecological success.
- Microbial interactions significantly influence ocean biogeochemical cycles at a global scale.
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