Phosphorus plays a key role in all life (1), from providing the energy that runs the cell machinery, linking nucleotides in RNA and DNA that form the “blueprint” of life, to being an integral part of the cell membrane lipid bilayer, making life possible by compartmentalizing biochemical processes. Polyphosphates (poly-P) are linear or cyclical polymers of a few to many hundreds of phosphate molecules linked with the same type of high-energy bond found in ATP, the key molecule in energy transactions within living cells, and poly-P may in fact act as a substitute for ATP in some enzymatic reactions (2). Poly-P was most likely present in prebiological times of the Earth’s history as these polymers spontaneously form during volcanic, or hydrothermal vent, activity (3). Additionally, it has been speculated that poly-P may have played a role in the origins of life on our planet (4). Although, poly-P appears to be ubiquitous throughout the natural world (5) and has long been recognized as a storage molecule for phosphate, relatively little has been known about its role and function in cells until quite recently (6). As a result, poly-P has sometimes been called a molecular “fossil” (7) due to its obscure and presumably pedestrian role in cell metabolism and hence has not garnered much scientific interest in the past. Nevertheless, over the last decades, it has become increasingly clear that poly-P may in fact be essential for a multitude of cellular functions, including, but not limited to, gene expression regulation, energy storage, motility, and ultimately the survival of the cell (4). However, the presence, distribution, and significance of poly-P in the marine environment and to its microbial inhabitants have been largely lacking, although recent metagenomic studies have suggested their potential importance to microorganisms in the oligotrophic oceans (8). Here, Martin et al. (9) present, to date, the most comprehensive study of poly-P content and distribution in particulate material in the marine environment. Their study transects the temperate western North Atlantic (TWNA) Ocean, which is relatively rich in nutrients, across the Gulf Stream and into the severely phosphorus-limited subtropical Sargasso Sea. Along this transect, which provides a natural gradient in nutrient regimes, they measure the poly-P content, among other phosphorus-relevant parameters, of the microbial communities in the upper water column, as well as the amount of poly-P in particles sinking out of the upper ocean into its deep interior.
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