Abstract
Arrieta et al. (Reports, 17 April 2015, p. 331) propose that low concentrations of labile dissolved organic carbon (DOC) preclude prokaryotic consumption of a substantial fraction of DOC in the deep ocean and that this dilution acts as an alternative mechanism to recalcitrance for long-term DOC storage. Here, we show that the authors’ data do not support their claims.
Original language | English |
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Pages (from-to) | 1483a |
Number of pages | 2 |
Journal | Science |
Volume | 350 |
Issue number | 6267 |
DOIs | |
Publication status | Published - 18 Dec 2015 |
Profiles
-
Carol Robinson
- School of Environmental Sciences - Professor of Marine Sciences
- Centre for Ecology, Evolution and Conservation - Member
- Centre for Ocean and Atmospheric Sciences - Member
- Collaborative Centre for Sustainable Use of the Seas - Member
- Environmental Biology - Member
- ClimateUEA - Member
Person: Research Group Member, Research Centre Member, Academic, Teaching & Research