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Updated: Feb 15, 2026

Chemotactic Response of Marine Micro-Organisms to Micro-Scale Nutrient Layers
Published on: May 28, 2007
Phosphate insensitive aminophosphonate mineralisation within oceanic nutrient cycles
Jason P Chin1, John P Quinn2, John W McGrath2
1School of Biological Sciences and Institute for Global Food Security, Medical Biology Centre, Queen's University Belfast, 97 Lisburn Road, Belfast, BT9 7BL, UK. j.chin@qub.ac.uk.
Marine microbes can break down organic phosphonates using a previously unknown, substrate-inducible pathway. This finding challenges the idea that phosphonates are unusable in nutrient-poor ocean waters, impacting nutrient cycling.
Area of Science:
- Marine microbiology
- Biogeochemical cycles
Background:
- Marine environments are often nutrient-poor, leading to intense competition and nutrient recycling.
- Organic phosphonates are abundant but typically require specific enzymes for breakdown.
- Previous research indicated phosphonate-degrading genes are Pho regulon-controlled and repressed by phosphate, suggesting recalcitrance.
Purpose of the Study:
- To investigate the catabolism of 2-aminoethylphosphonate in marine bacteria.
- To challenge the prevailing paradigm of phosphonate recalcitrance in marine ecosystems.
- To identify the regulatory mechanisms governing phosphonate degradation in the ocean.
Main Methods:
- Isolation of marine bacteria capable of mineralizing 2-aminoethylphosphonate.
- Analysis of gene regulation involved in phosphonate catabolism.
- Comparison of substrate-inducible versus Pho-regulated metabolic pathways.
Main Results:
- Marine bacteria can mineralize 2-aminoethylphosphonate, a common marine aminophosphonate.
- This mineralization occurs via substrate-inducible gene regulation.
- The catabolism is independent of the Pho regulon, which is typically repressed by inorganic phosphate.
Conclusions:
- Substrate-inducible, Pho-independent catabolism of 2-aminoethylphosphonate is a significant, previously unrecognized pathway in marine environments.
- This pathway represents a novel component of oceanic carbon, nitrogen, and phosphorus cycles.
- The findings necessitate a re-evaluation of phosphonate bioavailability and nutrient cycling in the ocean.
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