Biological and physical controls on dissolved dimethylsulfide over the north-eastern continental shelf of New Zealand

• Published in: Journal of sea research Vol. 43; no. 3-4; pp. 253 - 264
• Main Authors: Walker, C.F, Harvey, M.J, Bury, S.J, Chang, F.H
• Format: Journal Article
• Language: English
• Published: 01-08-2000
• Subjects: Marine; PSE, New Zealand, North I
• ISSN: 1385-1101
• DOI: 10.1016/S1385-1101(00)00017-4

Data presented in this paper are part of an extensive investigation of the physics of cross-shelf water mass exchange in the north-east of New Zealand and its effect on biological processes. Levels of dissolved dimethylsulfide (DMS) were quantified in relation to physical processes and phytoplankton biomass. Measurements were made at three main sites over the north-east continental shelf of New Zealand's North Island during a current-driven upwelling event in late spring 1996 (October) and an oceanic surface water intrusion event in summer 1997 (January). DMS concentrations in the euphotic zone ranged between 0.4 and 12.9 nmol dm super(-3). Integrated water column DMS concentrations ranged from 33 to 173 mu mol m super(-2) in late spring during the higher biomass (15-62 Chl-a mg m super(-2)) month of October, and from 25 to 38 mu mol m super(-2) in summer during the generally lower biomass (16-42 Chl-a mg m super(-2)) month of January. We observed high levels of DMS in the surface waters at an Inner Shelf site in association with a Noctiluca scintillans bloom which is likely to have enhanced lysis of DMSP-producing algal cells during phagotrophy. Integrated DMS concentrations increased three-fold at a Mid Shelf site over a period of a week in conjunction with a doubling of algal biomass. A high correlation (r super(2) = 0.911, significant <0.001) of integrated DMS and chlorophyll-a concentrations for compiled data from all stations indicated that chlorophyll-a biomass may be a reasonable predictor of DMS in this region, even under highly variable hydrographic conditions. Integrated bacterial production was inversely correlated to DMS production, indicating active bacterial consumption of DMS and/or its precursor.