LABORATORY PRODUCTION OF BROMOFORM, METHYLENE BROMIDE, AND METHYL-IODIDE BY MACROALGAE AND DISTRIBUTION IN NEARSHORE SOUTHERN CALIFORNIA WATERS

Production rates of bromoform (CHBr3) methylene bromide (CH2Br2), and methyl iodide (CH3I) were measured in the laboratory for 11 species of ma ne macroalgae. Production rates of the volatile bromomethanes extrapolated to a global scale suggest that marine macroalgae produce 2 x 10(11) g Br yr-1 (1 x 10(9) mol Br yr-1), 98% of which is bromoform. Laminarians (kelps) produce 61% of this organic Br. These calculations suggest that marine macroalgae are important in the biogeochemical cycling of Br. Seawater concentrations of CHBr3, CH2Br2, and CH3I were determined from various southern California coastal locales. High concentrations were measured in seawater from the canopy and the bottom of a dense bed of Macrocystis as compared to other sites. Surface seawater concentrations of these halomethanes showed a strong cross-shore gradient with the highest concentration in the kelp canopy and the lowest at 5 km offshore. Seawater adjacent to decaying macroalgae on the bottom of a submarine canyon was not enriched in halomethanes relative to surface water. Water exiting a productive estuary was enriched only with CH2Br2, although two algal species that are abundant there (Ulva and Enteromorpha) showed high laboratory production rates of both CHBr3 and CH2Br2.