Cambridge, Md. (November 24, 2009) – New research on bacterial communities throughout six large Arctic river ecosystems reveals predictable temporal patterns, suggesting that scientists could use these communities as markers for monitoring climate change in the polar regions. The study, published this week in the Proceedings of the National Academy of Sciences Early Edition, shows that bacterial communities in the six rivers shifted synchronously over time, correlating with seasonal shifts in hydrology and biogeochemistry.
The research team documents these patterns through a three-year, circumpolar study of planktonic bacterial communities in the six largest rivers of the pan-arctic watershed: the Ob’, Yenisey, Lena, Kolyma, Yukon, and Mackenzie Rivers.
“Our results demonstrate that synchrony, seasonality and annual reassembly in planktonic bacterial communities occur on global scales,” said lead author Dr. Byron Crump of the University of Maryland Center for Environmental Science. “Since bacterial communities in big arctic rivers shift predictably with circumpolar seasonal changes in environmental conditions, they may serve as sensitive indicators of climate change in the Arctic.”
“The six river systems studied are comparable in size to the Mississippi River in the United States,” said coauthor Rainer Amon of Texas A&M University at Galveston. “One of the things we learned is the bacteria communities in all six of them seem to be very similar. There are many questions still to be answered, such as how these bacteria communities might respond to a continued increase in temperature.”
This synchrony indicates that hemisphere-scale variation in seasonal climate sets the pace of variation in microbial diversity. Moreover, these seasonal communities reassembled each year in all six rivers, suggesting a long-term, predictable succession in the composition of big river bacterial communities.
Divergence from this synchronous pattern may provide an early signal of climate change in some regions of the Arctic, and may result in changes to river microbial communities and the biogeochemical transformations that they carry out.
"Researchers already recognize that changes in river discharge and chemistry can be used to detect climate-induced changes in Arctic watersheds," said co-author R. Max Holmes of the Woods Hole Research Center. "Now microbial community structure can be added to the list of diagnostic variables."
Data for this study was collected through the PARTNERS program, a collaboration among scientists from the U.S., Canada and Russia examining the largest rivers of the pan-arctic watershed. By including five of the world’s 25 largest rivers in the study, the results provide a unique perspective on global-scale patterns in bacterial diversity.
The article, “Circumpolar synchrony in big river bacterioplankton,” appears in the PNAS Early Edition the week of November 23, 2009 and is authored by Drs. Byron Crump, Bruce Peterson, Peter Raymond, Rainer Amon, Amanda Rinehart, James W. McClelland and R. Max Holmes. This research was supported by the National Science Foundation.
The University of Maryland Center for Environmental Science is the University System of Maryland’s environmental research institution. UMCES researchers are helping improve our scientific understanding of Maryland, the region and the world through its three laboratories – Chesapeake Biological Laboratory in Solomons, Appalachian Laboratory in Frostburg, and Horn Point Laboratory in Cambridge – and the Maryland Sea Grant College.
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