Dept/School: School of Environmental Sciences, University of East Anglia
Project Supervisor(s): Prof P Liss, Dr G Malin
Funding Availability: Directly Funded Project (European/UK Students Only)
Application Deadline: 12 March 2010
As atmospheric carbon dioxide continues to rise the pH of seawater will get progressively less alkaline. This is likely to affect marine organisms from corals to microscopic plankton, particularly those that form their structures with calcium carbonate as a major component.
In this PhD proposal the student will study the effect of decreasing pH on the production of trace gases (dimethyl sulphide and its precursor dimethylsulphoniopropionate and a range of naturally produced organo-halogen gases) by marine microorganisms. These compounds are volatile and can cross the air-sea interface. In the atmosphere their oxidation products can lead to new particle formation of growth of existing particles to cloud condensation nuclei size. Because of this they can affect the formation of clouds and hence climate. In addition, these gases play important roles in controlling the oxidation capacity of the atmosphere by, for example, destruction of ozone and so affect air quality. The student will examine the effect of pH change on the biogenic production of the gases by microbes.
The approach we propose to studying this system is by a mixture of field work using floating and fixed mesocosms in which the pH is adjusted to mimic future conditions and in vitro studies using pH-altered natural seawaters and cultures of specific organisms. In addition, since there is growing evidence that lowered pH of seawater leads to significant changes in the type and composition of marine organic matter, the student will test whether this brings about alteration in the rate of transfer of gases across the air-sea interface. This will be done in the mesocosm studies by adding minute amounts of the tracer pair sulphur hexafluoride and 3-helium to estimate air-sea gas exchange rates. If this effect (which has never been tested previously) proves significant then the implications would be far wider than just for the gases proposed for study here. Finally, the student will use a one-dimensional model to assess the importance of pH-induced changes in the air-sea exchange of trace gases for particle formation and air quality.
Funding is available for UK/EU students. Funding awarded for this project will cover tuition fees and stipend for UK students. EU students may be eligible for full funding, or tuition fees only, depending on the funding source. International students will not be eligible for this funding however they are still welcome to apply for the project but would have to find alternative funding.
Hopkins, F.E., Turner, S.M., Nightingale, P.D., Steinke, M., Bakker, D. and Liss, P.S. (2009) Ocean acidification and marine trace gas emissions. Proceedings of the National Academy of Sciences 107(2), 760-765.
Hughes, C., Malin, G., Turley, C.T., Keely, B.J., Nightingale, P.D. and Liss, P.S. (2008) The production of volatile iodocarbons by biogenic marine aggregates. Limnology and Oceanography 53, 867-872.
Lee, P.A., Saunders, P.A., de Mora, S.J., Deibel, D. and Levasseur, M. (2003) Influence of copepod grazing on concentrations of dissolved dimethylsulphide, dimethyl-sulphoniopropionate and dimethylsulphoxide in the North Water in 1998. Deep-Sea Research II 49, 5171-5189.
Liss, P.S. (2007) Trace gas emissions from the marine biosphere. Philosophical Transactions of the Royal Society A 365, 1697-1704.
von Glasow, R., Sander, R., Bott, A. and Crutzen, P.J. (2002) Modeling halogen chemistry in the marine boundary layer 1. Cloud-free MBL. J. Geophys. Res. 107, 4341. doi: 10.1029/2001JD000942.
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