Thanks to a $100,000 grant from the National Science Foundation, two 澳门六合彩资料 professors are researching climate change in Alaska. Elizabeth Herndon, Ph.D., and Lauren Kinsman-Costello, Ph.D., assistant professors from 澳门六合彩资料鈥檚 College of Arts and Sciences, spent a week in Fairbanks, Alaska, in June studying how climate change affects the availability of plant nutrients in arctic and sub-arctic ecosystems.
The grant teams up two of 澳门六合彩资料鈥檚 newest researchers.
鈥淚 think it鈥檚 really great that two early-career scientists were awarded the funds to do this research,鈥 Herndon said.
Both Herndon and Kinsman-Costello joined 澳门六合彩资料 about two years ago. Herndon joined the university鈥檚 Department of Geology, while Kinsman-Costello joined the Department of Biological Sciences. Their new collaborative research effort has potential implications for understanding how high-latitude peatlands will respond to climate change.
鈥淚t鈥檚 this very cold, wet environment, but temperatures at high latitudes are actually increasing at twice the rate they鈥檙e rising anywhere else on the planet,鈥 Herndon said. 鈥淚t鈥檚 thawing the permafrost and driving shifts in vegetation and in hydrology. A lot of people are interested in how these environments will respond to the warming climate because they currently store a lot of carbon that has the potential to be released into the atmosphere and accelerate climate change.鈥
Herndon said that as the temperatures rise in the arctic, plants will grow bigger and forests will expand farther north. Shrubs and other woody plants are already replacing tundra vegetation across large areas of northern Alaska, Canada and other arctic locations.
鈥淲hat we want to know is how these factors will change the availability of nutrients, specifically phosphate, that help plants grow,鈥 Herndon said. 鈥淩ising temperatures are drying out existing wetlands, and this is causing iron that鈥檚 dissolved in the soil water to essentially rust out as iron oxide minerals in the soil.鈥
Phosphate, Herndon said, binds to iron oxides. That means that increased iron deposits could sequester phosphate, reducing the amount available to plants.
鈥淭hose plants are a sink for carbon dioxide,鈥 she said, 鈥渟o any nutrient limitation could also limit their ability to remove CO2 from the air.鈥
Soils in high-latitude regions like Alaska contain high amounts of carbon because the vegetation decomposes slowly due to cold temperatures, leaving large amounts of peat.
鈥淎s the temperatures rise, that peat is going to start decomposing more quickly and releasing more carbon dioxide,鈥 Herndon said.
While the available data leave some uncertainty for future changes in the arctic, Herndon said the conventional wisdom suggests a bleak picture.
鈥淚f the plants there aren鈥檛 growing enough, then they can鈥檛 absorb the excess CO2 released from peat decomposition,鈥 she said. 鈥淩ight now, it鈥檚 not clear what the difference will be, but the prediction is that the carbon dioxide released will be greater than what the plants can absorb from the atmosphere.鈥
The team, which also includes one graduate and one undergraduate student, spent a week at the Alaska Peatland Experiment (APEX) site, just outside Fairbanks, where a team of scientists have been using an adjusted water table in a wetland to study carbon dioxide and methane release.
The scientists flooded one-third of the wetland, while draining another one-third. The differential creates the perfect model for Herndon and Kinsman-Costello鈥檚 research into phosphate and iron.
Herndon brings her iron expertise while Kinsman-Costello is versed in phosphates.
鈥淲e鈥檙e combining our knowledge bases to understand the interactions between the two,鈥 Herndon said. 鈥淟auren is a great collaborator, so I鈥檓 really happy to be working on this project with her.鈥
Herndon said she hopes that this pilot project will yield data that can be used to develop a longer-term project, as well as integrate with what the other scientists in Fairbanks are studying.
Written by Dan Pompili