Funded Research

Evaluating the Controls of Dissolved Organic Matter Accumulation, its Availability to Bacterioplankton, its Subsequent Diagenetic Alteration and Contribution to Export Flux

Carlson, Craig: University of California-Santa Barbara (Project Lead)

NRA: 2016 NASA: Ocean Biology and Biogeochemistry   

Food web dynamics play an important role in partitioning the pelagic net community production (NCP) between particulate (POM) and dissolved organic matter (DOM). Approximately 50% of the DOM produced is rapidly consumed to meet bacterial carbon demand. However, biotic and abiotic transformation of organic matter can lead to the accumulation of carbon-rich DOM resistant to rapid microbial degradation in the surface ocean; a fraction of this persists long enough to be entrained during overturn such that it impacts the efficiency and magnitude of the biological carbon pump. The vertical redistribution of DOM results in the global ocean export of ~1.8 Pg C from the euphotic zone, or ~20% of the total export production. Thus, vertical export of DOM represents one of the five major flux pathways central to the EXPORT program. The contribution of DOM to export flux is most pronounced at high latitudes where convective mixing and submesoscale processes deliver dissolved and suspended materials to the depth, whereby the carbon is sequestered for decades to millennia. To resolve the contribution DOM to export it is critical to obtain high quality DOM data, assess the controls on its net production, chemically characterize the accumulated pool, and quantify export; it is critical to assess the microbial bioavailability at each ecosystem / carbon cycling (ECC) state observed by the EXPORTS field campaigns in the North Pacific and North Atlantic. The guiding Hypotheses of this proposed project are: H1: Given quantification of NCP, the net production (accumulation) of DOC is a predictable process for these subarctic systems. H2: Given measures of vertical overturn, DOC export to the twilight zone is a predictable process. The Carlson (UCSB) and Hansell (RSMAS) team has over two decades of experience resolving temporal and basin scale distributions bulk DOC and DON across the global ocean and, from those, their contributions to vertical flux. They have experience determining the diagenetic characterization of DOM through the measure of specific compounds such as the dissolved combined neutral sugar component. They have optimized the microbial remineralization bioassays necessary to assess the bioavailability / persistence (i.e. export potential) of the accumulated DOM. The team is poised to generate mission-critical data for EXPORTS (Table 2 of the Implementation Plan) that address components of Scientific Questions SQ1 and SQ2. Specifically, this proposed work aims to: A. Understand controls on the fractions of net primary production and net community production partitioned as DOC and DON B. Determine the flux of the most labile fraction of DOM required to meet carbon demand of heterotrophic bacterial production (i.e. bacterial carbon demand) C. Determine DOM bioavailability to microbes and the fraction of the seasonally accumulated pool that persists for weeks to months D. Assess DOM diagenetic state (compositional variations) over varying ecosystem / carbon cycling (ECC) states. E. Evaluate physical mixing of DOM out of the euphotic zone, its contribution to export and its fate