Isn't this also relevant to sequestration strategies? It sounds as if
increased concentrations could create different results than currently
anticipated.
ᐧ

On Mon, Mar 30, 2015 at 9:45 AM, Andrew Lockley <andrew.lock...@gmail.com>
wrote:

> Poster's note : of interest to OIF researchers
>
> http://m.sciencemag.org/content/early/2015/03/18/science.1258955.abstract
>
> Science
> DOI: 10.1126/science.1258955
> Report
>
> OCEAN CHEMISTRY
>
> Dilution limits dissolved organic carbon utilization in the deep ocean
>
>
> Abstract
>
> Oceanic dissolved organic carbon (DOC) is the second largest reservoir of
> organic carbon on Earth. About 72% of the global DOC inventory is stored in
> deep oceanic layers for years to centuries, supporting the current view
> that it consists of materials resistant to microbial degradation. An
> alternative hypothesis is that deep-water DOC consists of many different,
> intrinsically labile compounds at concentrations too low to compensate for
> the metabolic costs associated to their utilization. Here we present
> experimental evidence showing that low concentrations rather than
> recalcitrance preclude consumption of a significant fraction of DOC leading
> to slow microbial growth in the deep ocean. These findings demonstrate an
> alternative mechanism for the long-term storage of labile DOC in the deep
> ocean, which has been hitherto largely ignored.
>
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