News Release

Amazon outflow is found to power ocean capture of carbon dioxide

River nourishes unexpected plant life, trapping greenhouse gas

Peer-Reviewed Publication

Columbia Climate School

River Plume

image: True-color image of the Amazon outflow, which nourishes plant life thousand of kilometers into the Atlantic Ocean. view more 

Credit: Norman Kuring/NASA

Nutrients washed out of the Amazon River are powering huge amounts of previously unexpected plant life far out to sea, thus trapping atmospheric carbon dioxide, according to a new study. Until now, the areas around the Amazon and other great rivers had been thought to be emitting CO2, so the study may affect climate scientists' calculations of how the greenhouse gas acts. The study appears in this week's Proceedings of the National Academy of Sciences. http://www.pnas.org/

"This new understanding allows us to better think about how carbon dioxide is cycled between the atmosphere and the oceans, and how this might change in the future," said lead author Ajit Subramaniam, a biological oceanographer at Columbia University's Lamont-Doherty Earth Observatory. Lamont is part of The Earth Institute.

The Amazon River is the world's largest, accounting for nearly a fifth of earth's river input to the oceans. Using satellite imagery and samples taken at sea over three years, Subramaniam and colleagues outlined a rich plume of microscopic phytoplankton nourished by its outflow, covering 1.3 million square kilometers (500,000 square miles), an area about twice the size of Texas. Tropical waters are generally considered poor because they lack nitrogen, a nutrient essential for plants, so the scientists were surprised to find so much life. The secret: a predominance of diazotrophs, photosynthetic microorganisms that fix nitrogen directly from the air. They were able to bloom far from shore because the Amazon also washes other needed nutrients eroded from land: phosphorus, iron and silicon. Plants use large amounts of carbon dioxide for photosynthesis, so the region, previously estimated to emit a yearly 30 million tons of CO2, is probably soaking that amount back up, said Subramaniam. Furthermore, once the diazotrophs bloom, they tend to sink quickly to the bottom, more or less permanently removing the CO2 from the air. Because excess human-generated CO2 is warming the atmosphere, artificial trapping of CO2, or "sequestration," has become a subject of rising interest. Here, the scientists showed, it is happening naturally on an unexpected scale.

Each year the world's oceans are thought to absorb about 2 billion tons of CO2 from the atmosphere, but the amount permanently sequestered by sinkage is unclear. The new discovery may tilt the estimated balance between air and oceans by only about 2%, said Subramaniam. However, he said, "it alters our view about the processes that we think are going on. There may be other surprises out there." Studies of other large rivers including the Congo, Orinoco and Mekong suggest that similar processes may be taking place there.

Subramaniam said that climate change, booming human populations and intensified land uses could alter the workings of the great river basins. For instance, ongoing conversion of Amazonian rainforest into farmland may increase outwash of nutrients; in some regions, future warming could greatly increase rainfall, and thus river flows. On the other hand, proposed large dam projects on rivers like the Orinoco could cut flow by as much as half. "The whole process could change," said Subramaniam. "But we can't predict how it will change, or what the outcome will be."

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Subramaniam and coauthor Doug Capone of the University of Southern California discuss their findings in a video presented by the National Science Foundation, which funded much of the project: http://www.nsf.gov/news/news_videos.jsp?cntn_id=111904&media_id=62649&org=NSF

Maps and photos are also available on the NSF site: http://www.nsf.gov/news/news_summ.jsp?cntn_id=111904&org=NSF&from=news

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Copies of the paper, "Amazon River enhances diazotrophy and carbon sequestration in the tropical North Atlantic Ocean," are available from the authors, the PNAS news office, or the Earth Institute.

Lead author: Ajit Subramaniam 646-546-0367, ajit@ldeo.columbia.edu
PNAS News Office: 202-334-1310, PNASNews@nas.edu
Earth Institute: Kevin Krajick, Senior Science Writer 212-854-9729, kkrajick@ei.columbia.edu

Lamont-Doherty Earth Observatory, a member of The Earth Institute at Columbia University, is one of the world's leading research centers seeking fundamental knowledge about the origin, evolution and future of the natural world. More than 300 research scientists study the planet from its deepest interior to the outer reaches of its atmosphere, on every continent and in every ocean. From global climate change to earthquakes, volcanoes, nonrenewable resources, environmental hazards and beyond, Observatory scientists provide a rational basis for the difficult choices facing humankind in the planet's stewardship. http://www.ldeo.columbia.edu/

The Earth Institute at Columbia University mobilizes the sciences, education and public policy to achieve a sustainable earth. Through interdisciplinary research among more than 500 scientists in diverse fields, the Institute is adding to the knowledge necessary for addressing the challenges of the 21st century and beyond. With over two dozen associated degree curricula and a vibrant fellowship program, the Earth Institute is educating new leaders to become professionals and scholars in the growing field of sustainable development. We work alongside governments, businesses, nonprofit organizations and individuals to devise innovative strategies to protect the future of our planet. http://www.earth.columbia.edu/sections/view/9


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