Jm. Baker et al., Biological production of methyl bromide in the coastal waters of the NorthSea and open ocean of the northeast Atlantic, MAR CHEM, 64(4), 1999, pp. 267-285
Two separate studies in different oceanic regions provide evidence for the
production of methyl bromide (CH3Br) by the prymnesiophyte Phaeocystis. A s
ampling program to study the seasonal cycle of CH3Br in a coastal area demo
nstrated that the seawater was supersaturated with respect to CH3Br for ove
r 3 months of the year. The greatest saturation was observed during a bloom
of Phaeocystis, Also, in situ field measurements demonstrated that CH3Br w
as supersaturated over a large region of the northeast Atlantic. A positive
correlation was observed between CH3Br and dimethylsulphoniopropionate (DM
SP), indicating that there was a source common to both compounds. An access
ory pigment, hexanoyloxyfucoxanthin, which indicates the presence of prymne
siophytes, also correlated positively with CH3Br. (C) 1999 Elsevier Science
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