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Unlike carbon, water, and nitrogen, phosphorus is not present in the atmosphere as a gas. Instead, most phosphorus in the ecosystem exists as compounds, such as phosphate ions (PO43-), found in soil, water, sediment and rocks. Phosphorus is often a limiting nutrient (i.e., in short supply). Consequently, phosphorus is added to most agricultural fertilizers, which can cause environmental problems related to runoff in aquatic ecosystems.
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Buffers02:56

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A solution containing appreciable amounts of a weak conjugate acid-base pair is called a buffer solution, or a buffer. Buffer solutions resist a change in pH when small amounts of a strong acid or a strong base are added. A solution of acetic acid and sodium acetate is an example of a buffer that consists of a weak acid and its salt: CH3COOH (aq) + CH3COONa (aq). An example of a buffer that consists of a weak base and its salt is a solution of ammonia and ammonium chloride: NH3 (aq) + NH4Cl...
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Microorganisms play a critical role in the transformation and immobilization of uranium in contaminated environments through four main pathways: bioreduction, biosorption, bioaccumulation, and biomineralization. These mechanisms reduce uranium’s toxicity and prevent its migration through groundwater systems, offering sustainable approaches for in situ bioremediation.Bioreduction of UraniumBioreduction is driven by anaerobic bacteria such as certain strains of Geobacter and Shewanella,...
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Assaying for Inorganic Polyphosphate in Bacteria
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Dominant oceanic bacteria secure phosphate using a large extracellular buffer.

Mikhail V Zubkov1, Adrian P Martin1, Manuela Hartmann1

  • 1National Oceanography Centre, Ocean Biogeochemistry &Ecosystems Research Group, European Way, Southampton SO14 3ZH, UK.

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|July 23, 2015
PubMed
Summary
This summary is machine-generated.

SAR11 and Prochlorococcus bacteria use an extracellular phosphate buffer to secure growth in low-nutrient waters. This buffer strategy reduces their reliance on ambient phosphate, even in productive tropical seas.

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Area of Science:

  • Marine microbiology
  • Biogeochemistry
  • Oceanography

Background:

  • SAR11 and Prochlorococcus are abundant marine bacteria crucial for nutrient cycling.
  • These microbes inhabit phosphate-limited environments like the North Atlantic subtropical gyre.
  • Their phosphate uptake mechanisms in varying oceanic productivity zones remain incompletely understood.

Purpose of the Study:

  • To investigate how SAR11 and Prochlorococcus bacteria manage phosphate acquisition in different oceanic conditions.
  • To determine the role of extracellular phosphate buffering in bacterial growth and survival.
  • To elucidate the relationship between phosphate availability, cellular demand, and uptake kinetics.

Main Methods:

  • Utilized flow sorting to isolate and analyze phosphate-pulsed and chased cells.
  • Quantified labile extracellular phosphate buffers in Prochlorococcus and SAR11.
  • Employed mathematical modeling to interpret phosphate uptake dynamics and buffer saturation.

Main Results:

  • Demonstrated that Prochlorococcus and SAR11 maintain large extracellular phosphate buffers (5-40 times chromosome replication needs).
  • Observed that buffer size inversely correlates with cellular phosphate uptake rates.
  • Found that phosphate uptake becomes marginal in phosphate-replete tropical waters due to buffer saturation.

Conclusions:

  • Extracellular buffer stocking is a key adaptation for SAR11 and Prochlorococcus, ensuring growth by reducing dependency on fluctuating ambient phosphate.
  • This strategy allows these bacteria to thrive in oligotrophic environments and manage phosphate acquisition effectively.
  • Buffer saturation explains counter-intuitive lower phosphate uptake in more productive tropical waters.