Tracking the Remnants of the Carbon Cycle: How an Ancestral Fungus May Have Influenced Coal Formation
The evolution of a lineage of mushrooms - may have had a massive impact on the carbon cycle, bringing an end to the 60-million year period during which coal deposits were formed. Coal generated nearly half of the roughly four trillion kilowatt-hours of electricity consumed in the United States in 2010, according to the U.S. Energy Information Administration. This fuel is actually the fossilised remains of plants that lived from around 360 to 300 million years ago. An international team of scientists, including researchers at the U.S. Department of Energy Joint Genome Institute (DOE JGI), has proposed a new factor that may have contributed to the end of the Carboniferous period - named after the large stores of what became coal deposits. The evidence, presented online in the June 29 edition of the journal Science, suggests that the evolution of fungi capable of breaking down the polymer lignin, which helps keep plant cell walls rigid, may have played a key role in ending the development of coal deposits. With the arrival of the new fungi, dead plant matter could be completely broken down into its basic chemical components. Instead of accumulating as peat, which eventually was transformed into coal, the great bulk of plant biomass decayed and was released into the atmosphere as carbon dioxide. Read more
With his discovery of what may be the world's oldest fossil imprint of a flying insect, R.J. Knecht is tackling a new dimension of New England historyone that dates back hundreds of millions of years. What did the ecology of the Boston area look like more than 300 million years ago? This question is what drives the work of Richard J. Knecht, a Tufts geology major. And his initial discoveries are bringing him closer to the answer.