Document Type
Article
Department/Program
Virginia Institute of Marine Science
Publication Date
5-2004
Journal
Aquatic Microbial Ecology
Volume
35
Issue
3
First Page
229
Last Page
241
Abstract
The majority of bacterial growth and respiration in the upper ocean is thought to result from coupling between microheterotrophic populations and the reactive soluble components of planktonic primary and secondary production. However, we know little about the potential turnover of these components and the concomitant growth of bacteria under conditions of intermittent or transient inputs of natural dissolved organic matter (DOM) compared to quasi-steady state, low DOM conditions. The present study evaluated the short-term (similar to3 d) rates and net extents of utilization (as measured losses) of selected constituents of plankton-derived DOM (DOMPD) by indigenous bacterioplankton populations in eastern North Pacific surface waters, and assessed bacterial growth efficiencies (BGE) during temporarily non-limiting DOM conditions. Approximately 28% of the starting dissolved organic carbon (DOC) and 34% of the dissolved organic nitrogen (DON) in incubations supplemented with DOMPD could be characterized as dissolved free and combined amino acids (DFAA and DCAA, respectively) and monosaccharides (MCHO). Up to 31% of the added DOC and 26% of the added DON was utilized in +DOMPD incubations; however, BGE under supplemented conditions (similar to4 to 5%) was similar to estimates for ambient oligotrophic waters. Of the net DOC consumed, 75% was accounted for by DFAA (which alone was 61% of the total), DCAA, and MCHO, while the remaining non-characterizable 25% may represent an inherent or rapidly formed component of lower reactivity. In contrast to DOC, net DON utilization was supported entirely by DFAA and DCAA, with DFAA alone accounting for the vast majority (up to 99%). Together, DCAA and MCHO accounted for only similar to13% of the DOC consumed and less than or equal tosimilar to5% of the DON (i.e. as DCAA) utilized. These findings are consistent with bacterial growth in the open ocean being controlled predominantly by inputs of a small fraction of bulk DOM, and further suggest that bacteria may function primarily as remineralizers even during transient periods where labile DOC and DON is relatively available.
DOI
10.3354/ame035229
Keywords
plankton-derived DOM; bacterial growth efficiency; DOC; DON; dissolved free amino acids; dissolved combined amino acids; monosaccharides
Recommended Citation
Cherrier, J and Bauer, JE, Bacterial utilization of transient plankton-derived dissolved organic carbon and nitrogen inputs in surface ocean waters (2004). Aquatic Microbial Ecology, 35(3), 229-241.
10.3354/ame035229
