Associate Professor, Jason Briner (State University of New York at Buffalo), and Gifford Miller, Fellow and Associate Director of University of Colorado’s Institute of Arctic and Alpine Research, are analyzing fossilized Arctic moss that has been buried under ice for thousands of years to garner clues about the region’s climate history during the Holocene. Moss that has previously been buried is now surfacing as ice caps retreat.
The scientists’ research, which is supported by the National Science Foundation, takes them to the small ice caps ringing Baffin Bay that are now exposed each summer as they shrink in northeastern Canada and West Greenland. The team will head back into the field August, 2014, when Miller will return to Baffin Island, Canada. At the same time, Briner will travel to the Sukkertoppen ice cap region north of Nuuk, Greenland, along with two SUNY Buffalo graduate students and PolarTREC teacher, Tina Ciaramentaro, .
“Our overarching goal is to understand arctic climate structure over the Holocene,” said Briner. “Have temperatures changed slowly and steadily or are there periods where abrupt changes in temperature occur? Are there thresholds where, if crossed, Earth goes into severe cooling or severe warming?”
That information could help inform current climate models.
The methodology of using fossilized moss as a proxy for glaciations was pioneered on Baffin Island in the 1960’s when a group working there found exposed tundra at the edge of a receding ice cap. The team took a sample home and derived the moss’ age using the radiocarbon dating technique, which uses the natural radioactive decay of carbon to estimate the age of organic material.
“They showed that the ice cap first grew – and killed the moss – toward the beginning of the Little Ice Age. Although it was one sample – it was an important one, since it “proved” the method,” Briner says. “But what we do now is pretty different – methodologically the same, but our approach is to date hundreds of moss samples, and from dozens of ice caps – the real information lies in the spatial pattern of ages across many ice caps in a region.”
The method wasn’t used much until the middle 2000s when Miller had a light bulb moment while lecturing to a freshman class.
“From my recollection it was Giff that was showing an intro class that ice caps on Baffin were disappearing,” says Briner. “He looked up new satellite imagery at the time (early 2000s) and realized that the ice cap from which the moss was originally dated was now GONE! He then realized that, due to global warming, it would be a missed opportunity if we don’t visit these ice caps soon and sample the moss, since they grow back quickly after being exposed by retreating ice.”
In 2005 Briner and Miller got the go-ahead to perform their own study on Baffin Island in an attempt to replicate the initial study’s results. One of their first stops was to visit the ice cap from the initial study, but the ice cap was gone, melted, and so was the fossilized moss. New plants had grown in their place.
“Then we visited many ice caps in that region and sampled dozens and dozens of moss samples. Much of our new results did confirm the earlier finding, and then we’ve taken it to another level, I’d say. We are now expanding that first study to west Greenland to get an understanding of the broader spatial complexity of ice cap history across the north Atlantic sector of the Arctic,” Briner says.
In 2010, Briner and Miller dated two samples collected during a pilot study at Disko Island, Greenland. In 2013 they returned to expand the Disko Island study to Uummannaq fjord. This year the team will establish remote camps and hike to sampling sites each day.
Briner and Miller collect palm-sized clumps of rooted moss, which are bagged and shipped home. Back in the SUNY Buffalo lab, the moss is freeze-dried to remove moisture then rinsed with clean water or placed in a gentle sonicating bath to shake loose any clay. One strand of clean moss is placed in a glass vial and sent to the Woods Hole Oceanographic Institution’s radiocarbon lab for analysis. The remaining sample is archived at SUNY Buffalo for use by other scientists.
Briner says the method is still evolving as they, and other teams, learn more about what information they can glean from radiocarbon dating moss. The vegetation study will be complemented by geochemical studies of rocks collected near ice cap margins. Beryllium and Carbon isotopes that naturally occur in the rocks also act as clocks that tell the team when and where the ice caps were present or absent in the past.
“In the Arctic, temperature changes tend to be amplified relative to the rest of the earth. The Arctic is more sensitive to change so even small temperature changes can have a large effect on Arctic climate. Consequently, glaciers can shrink or grow rapidly in response to temperature change,” says Briner. “There is also a spatial component, hemispherically speaking. Areas with more sea ice might be different from areas with less sea ice, like Norway. With our study we may be able to tease out spatial gradients and compare Holocene climate changes in the European Arctic to North America and Greenland. We will better understand the current state of glaciers as well as gain a larger global perspective on how warming impacts the Arctic.” –Marcy Davis