Halocarbon emissions by selected tropical seaweeds: species-specific and compound-specific responses under changing pH.
Five tropical seaweeds,Kappaphycus alvarezii(Doty) Doty ex P.C. Silva,Padina australisHauck,Sargassum binderiSonder ex J. Agardh (syn.S. aquifolium(Turner) C. Agardh),Sargassum siliquosumJ. Agardh andTurbinaria conoides(J. Agardh) Kützing, were incubated in seawater of pH 8.0, 7.8 (ambient), 7.6, 7.4 and 7.2, to study the effects of changing seawater pH on halocarbon emissions. Eight halocarbon species known to be emitted by seaweeds were investigated: bromoform (CHBr3), dibro-momethane (CH2Br2), iodomethane (CH3I), diiodomethane (CH2I2), bromoiodomethane (CH2BrI), bromochlorometh-ane (CH2BrCl), bromodichloromethane (CHBrCl2), and dibro-mochloromethane (CHBr2Cl). These very short-lived halocarbon gases are believed to contribute to stratospheric halogen concentrations if released in the tropics. It was observed that the seaweeds emit all eight halocarbons assayed, with the exception ofK. alvareziiandS. binderifor CH2I2and CH3I respectively, which were not measurable at the achievable limit of detection. The effect of pH on halocarbon emission by the seaweeds was shown to be species-specific and compound specific. The highest percentage changes in emissions for the halocarbons of interest were observed at the lower pH levels of 7.2 and 7.4 especially inPadina australisandSargassumspp., showing that lower seawater pH causes elevated emissions of some halocarbon compounds. In general the seaweed least affected by pH change in terms of types of halocarbon emission, wasP. australis. The commercially farmed seaweedK. alvareziiwas very sensitive to pH change as shown by the high increases in most of the compounds in all pH levels relative to ambient. In terms of percentage decrease in maximum quantum yield of photosynthesis (Fv∕Fm) prior to and after incubation, there were no significant correlations with the various pH levels tested for all seaweeds. The correlation between percentage decrease in the maximum quantum yield of photosynthesis (Fv∕Fm) and halocarbon emission rates, was significant only for CH2BrCl emission byP. australis(r= 0.47;p≤ 0.04), implying that photosynthesis may not be closely linked to halocarbon emissions by the seaweeds studied. Bromine was the largest contributor to the total mass of halogen emitted for all the seaweeds at all pH. The highest total amount of bromine emitted byK. alvarezii(an average of 98% of total mass of halogens) and the increase in the total amount of chlorine with decreasing seawater pH fuels concern for the expanding seaweed farming activities in the ASEAN region.
Institute of Ocean and Earth Sciences (IOES), University of Malaya, Kuala Lumpur, Malaysia.|Institute of Biological Sciences, Faculty of Science, University of Malaya, Kuala Lumpur, Malaysia.
Paramjeet Kaur
PK
Mithoo-Singh
Institute of Ocean and Earth Sciences (IOES), University of Malaya, Kuala Lumpur, Malaysia.|Institute of Graduate Studies (IGS), University of Malaya, Kuala Lumpur, Malaysia.
Fiona S-L
FS
Keng
Institute of Ocean and Earth Sciences (IOES), University of Malaya, Kuala Lumpur, Malaysia.|Institute of Biological Sciences, Faculty of Science, University of Malaya, Kuala Lumpur, Malaysia.
Siew-Moi
SM
Phang
Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich, United Kingdom.
Emma C
EC
Leedham Elvidge
Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich, United Kingdom.
William T
WT
Sturges
Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich, United Kingdom.
Gill
G
Malin
Department of Chemistry, University of Malaya, Kuala Lumpur, Malaysia.
Noorsaadah
N
Abd Rahman
Climate change; Emission rate; Halocarbons; Kappaphycus; Seawater pH; Tropical seaweeds