| Climactic
Shifts: A Marine Biologist Studies How Sulfur Affects Our Atmosphere Dr. Ron Kiene |
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| Global warming.
Global cooling. Acid rain. Carbon dioxide emissions. Pick up a newspaper
today and you will see that the atmosphere is in the forefront of
environmental issues today. There are many factors that affect our
atmosphere; but one compound in particular has been the research focus of
the Sea Lab’s Dr. Ron Kiene. Sulfur, particularly in the form of
dimethylsulfide or DMS, has been one of his main interests. Why sulfur?
Its natural and man-made emissions are a clue to the very topical issues
in today’s headlines.
For Dr. Kiene, the road to marine biology, and particularly biogeochemistry, began with a love for the water in his native Brooklyn, New York. Growing up near the famed Verrazano Bridge, where the Hudson River enters the Atlantic Ocean, marine biology seemed a natural course of study; it wasn’t, however, his first choice of profession. With a baseball scholarship to Saint John’s University in New York, he aspired to become a professional pitcher. "It’s what I REALLY wanted to do, at first. When that didn’t pan out, marine biology came second," he mused. A college course in marine invertebrate zoology convinced him that his initial love of the seas could become a lively career. With "amazing foresight," according to Dr. Kiene, he combined his major in biology with a minor in chemistry. Not deterred by the extra coursework, he was later to bless the chemistry background that enables him to pursue his current research interests. A chance assignment to the lab of Dr. Doug Capone during graduate school at The State University of New York at Stony Brook gave Dr. Kiene the opportunity to conduct experiments in methane gas production by marsh sediments. "I wound up thinking that this was a pretty neat thing to do," he said. This biologist began to specialize in biogeochemistry. |
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| With regard to
sulfur, there are both natural and human contributions to the atmosphere.
Our endless consumption of energy, specifically in the form of burning
fossil fuels like coal, releases enormous amounts of sulfur to the
atmosphere. In bigger cities, these huge emissions of sulfur can mean a
sadly common atmospheric occurrence—acid rain.
A volatile compound, DMS is a naturally occurring sulfur that is produced by plants including microscopic marine algae, and released into the atmosphere. But in today’s world, the natural processes are far outstripped by human production. "Man is doubling, tripling sulfur additions," warned Dr. Kiene. Humans have tipped the delicate balance of sulfur emissions, and there is a balance to be maintained. Sulfur, it turns out, isn’t all bad. Once sulfur is in the atmosphere, it can oxidize to sulfate, tiny crystals of salt in the atmosphere. The sun shines on this multitude of crystals, and they reflect some of the solar heat, contributing a direct cooling effect to the global climate system. Additionally, these sulfate crystals provide water droplets with a foothold on which to grow, enabling the tiny droplets to form heavier ones, which is how clouds are formed. Clouds can |
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| careful with proposals like
that," Kiene warned. "We’ve learned that when we start to play
around with those things, there are consequences we just didn’t
perceive. We need a much better understanding of how the Earth system
works, especially the interactions of the ocean with the atmosphere."
Understanding the processes through which DMS is produced has taken Dr. Kiene to a range of research sites. To study DMS production in clear, nutrient-poor water, he has recently taken his team of researchers on cruises in the Gulf of Mexico and to the North Atlantic Ocean near Greenland. To study DMS processes in freshwater environments, he has established field sites in the sphagnum peat bogs of Alaska. By contrasting these different field sites and the data they yield, he is trying to determine how significant DMS production is in each system, and what mechanisms controls production in each environment. DMS is not only generated, but through a series of processes it is also consumed or removed from the water or sediments. Interestingly, peat bogs represent an environment where plant biomass is not particularly degraded; it just keeps building and building. There, DMS is not consumed at a rapid rate, leading to relatively high emissions. Per unit area, the bogs emit as much as the ocean does. Throw into the mix the effects of ultraviolet (UV) light on the DMS cycle, a new area of research into which Dr. Kiene is delving, and the biogeochemical processes become even more complicated. Ultraviolet light can effect organisms and microbes in clear ocean waters by inhibiting them. At the same time, UV causes a chemical reaction that destroys the DMS. "So we have a complicated interaction there—the ultraviolet is destroying the DMS, but it may also be causing it to be consumed LESS by biology, and produced more," according to Dr. Kiene. From the small scale of microbes and compounds to the global scale of the world’s atmosphere, Dr. Kiene exemplifies how science crosses boundaries and disciplines. His early studies in chemistry and biology set an example for other aspiring biologists interested in entering the field. "Don’t shy away from the hard courses. Get a good foundation in the natural sciences, mathematics, biology, chemistry and physics," he advises. And teachers also have a responsibility to make these subjects relevant to the real world. "This may be trivializing it a little, but much of the world around us can be explained by advanced calculus. For example, how NASA calculates where they have to shoot the space shuttle in order to have it meet up with the space station—it’s complicated, but it’s calculus. This kind of relevance to the real world is what would be inspiring to students. "Informing people that there is a lot of DMS in beer, corn and other foods usually gets their attention and makes the issue of natural sulfur compounds more relevant," Kiene concluded.
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