Texas A&M Scientists Find Trace Elements Increasing In Rapidly Changing Arctic Ocean
Oceanographers used data from a pan-Arctic survey of carbon and trace elements to better understand how climate change will affect ecosystems in one of the fastest warming regions of the world.
Apr 14, 2020
Significant quantities of carbon and trace elements are flowing across the central Arctic Ocean under the sea ice via freshwater runoff from rivers and continental shelf sediments, according to a new study by an international team of ocean scientists.
“This research is critical to understanding the current and future health of the Arctic Ocean, which is warming faster than much of the rest of the planet,” said Dr. Jessica Fitzsimmons, a co-author of the study and assistant professor in the Department of Oceanography at Texas A&M University. “The Arctic is also receiving more freshwater with its changing climate, making an understanding of the chemistry and fate of that freshwater more important than ever before.”
Texas A&M doctoral students Laramie Jensen and Tatiana Williford, and Dr. Rainer Amon, professor of marine and coastal environmental science at Texas A&M - Galveston, were also co-authors of the study. Their results were recently published in the Journal of Geophysical Research-Oceans.
Dr. Jessica Fitzsimmons, assistant professor of Oceanography at Texas A&M, on the sea ice near the North Pole, preparing to collect samples. (Photo courtesy of Dr. Jessica Fitzsimmons.)
PhD Candidate Laramie Jensen at the door to the Fitzsimmons lab clean room at Texas A&M Oceanography, where the metal samples for this study were analyzed. Due to the low metal content of some of these water samples, they were highly prone to contamination from dust and human fibers, and thus they were analyzed in Fitzsimmons’ metal-free clean room. (Photo courtesy of Dr. Jessica Fitzsimmons.)
“Our team analyzed the concentrations of six nutrient metals – like iron and zinc – and one toxic contaminant metal – lead - and found that the nutrient metals are supplied by Arctic rivers and are directly transported across the center of the Arctic Ocean within a high-speed current,“ Fitzsimmons said. “Fortunately, toxic contaminant fluxes in this study remained low and do not appear to be coming from Arctic rivers.”
The increased nutrients are carried by the Transpolar Drift — a major surface current that moves water from Siberia across the North Pole to the North Atlantic Ocean. In 2015, oceanographers conducting research in the Arctic Ocean as part of the International GEOTRACES program found much higher concentrations of trace elements in surface waters near the North Pole than in regions on either side of the current.
“Many important trace elements that enter the ocean from rivers and shelf sediments are quickly removed from the water column,” said Dr. Matthew Charette, lead author of the study and a marine chemist at Woods Hole Oceanographic Institution. “But in the Arctic they are bound with abundant organic matter from rivers, which allows the mixture to be transported into the central Arctic, over 1,000 kilometers from their source."
Trace elements, like iron, form essential building blocks for ocean life. As the Arctic warms and larger swaths of the ocean become ice-free for longer periods of time, marine algae are becoming more productive. A greater abundance of trace elements coming from rivers and shelf sediments can lead to increases in nutrients reaching the central Arctic Ocean, further fueling algal production.
“It’s difficult to say exactly what changes this might bring,” Charette said. “But we do know that the structure of marine ecosystems is set by nutrient availability.”
Nutrients fuel the growth of phytoplankton, a microscopic algae that forms the base of the marine food web. Generally speaking, more phytoplankton brings more zooplankton—small fish and crustaceans, which can then be eaten by top ocean predators like seals and whales.
Arctic Ocean sea ice operations about the USCGC Healy on the 2015 U.S. GEOTRACES cruise. (Photo courtesy of Cory Mendenhall, U.S. Coast Guard.)
A polar bear investigating the ship while on the U.S. GEOTRACES cruise in the Arctic. (Photo courtesy of Dr. Jessica Fitzsimmons.)
Higher concentrations of trace elements and nutrients previously locked up in frozen soils (permafrost) are expected to increase as more river runoff reaches the Arctic, which is warming at a much faster rate than most anywhere else on Earth. While an increase in nutrients may boost Arctic marine productivity, Charette cautioned that the continued loss of sea ice will further exacerbate climate warming, which will impact ecosystems more broadly.
“The Arctic plays an important role in regulating Earth’s climate, with the ice cover reflecting sunlight back to space, helping to mitigate rising global temperatures due to greenhouse gas emissions,” Charette added. “Once the ice is gone, the Arctic Ocean will absorb more heat from the atmosphere, which will only make our climate predicament worse.”
Funding for Arctic GEOTRACES was provided by the U.S. National Science Foundation, Swedish Research Council Formas, French Agence Nationale de la Recherche and LabexMER, Netherlands Organization for Scientific Research, and Independent Research Fund Denmark. The Arctic GEOTRACES expeditions were supported by the captains and crew of the USCGC Healy and the R/V Polarstern. Laramie Jensen was also funded by a Texas A&M Graduate Merit Fellowship.
Written in collaboration with Woods Hole Oceanographic Institution.
