DURHAM, N.C. – A new Duke University-led study has documented dramatic, natural short-term increases in the acidity of a North Carolina estuary.
"The natural short-term variability in acidity we observed over the course of one year exceeds 100-year global predictions for the ocean as a whole and may already be exerting added pressure on some of the estuary's organisms, particularly shelled organisms that are especially susceptible to changes in pH," said Zackary I. Johnson, Arthur P. Kaupe Assistant Professor of Molecular Biology at Duke's Nicholas School of the Environment.
The short-term spikes in the acidity of the estuary were driven by changes in temperature, water flow, biological activity and other natural factors, the researchers said. And they are occurring in addition to the long-term acidification taking place in Earth's oceans as a result of human-caused climate change.
"For vulnerable coastal marine ecosystems, this may be adding insult to injury," said Johnson, who was lead author of the study.
When the effects of long-term ocean acidification and short-term natural variation combine, they can create "extreme events" which may be especially harmful to coastal marine life, he said.
The study was conducted at the Pivers Island Coastal Observatory at the Duke Marine Lab in Beaufort, N.C., as part of a long-term coastal monitoring program. Researchers collected seawater samples from Beaufort Inlet weekly for a year and on a daily and hourly basis for shorter periods to track changes in the water's pH and dissolved inorganic carbon on multiple time scales.
Numerous studies have shown that increasing amounts of atmospheric carbon dioxide from human sources are finding their way into the world's oceans. When the carbon dioxide dissolves in seawater, it reduces the water's pH and the ability of organisms to form calcium carbonate minerals that are the building blocks of many species' shells and skeletons. This process is known as ocean acidification.
If current trends continue, experts predict that the mean ocean pH will decrease by about 0.2 units over the next 50 years. A drop of that magnitude could have far-reaching effects on ocean ecosystems and organisms.
"We may see significant changes in biological processes such as primary production," said Dana Hunt, assistant professor of microbial ecology, who co-authored the new study. "Some organisms, such as phytoplankton, may benefit. Many others, including shelled organisms and corals, will not."
The Duke team's analysis showed that a wide range of natural variables, including changes in temperature, algal production and respiration, and water movement caused by tides and storms, triggered sharp spikes in the inlet's acidity. Some changes occurred over the course of a season; others took place on a daily or hourly basis.
"Understanding to what extent pH naturally varies in coastal ecosystems worldwide will be essential for predicting where and when the effects of increasing ocean acidity will be most profound, and what organisms and ecosystems may be most affected," Hunt said. "Our research demonstrates we have to take into account a wide range of environmental variables, not just pH."
The study appears in the peer-reviewed open-access journal PLOS ONE.
Johnson and Hunt's co-authors were research technician Benjamin Wheeler, doctoral student Christopher Ward and former undergraduate Christina Carlson, all of Duke; and Sara Blinebry, a student intern from Carteret County Community College. Blinebry is now a research technician in Johnson's lab. Carlson is now a policy research assistant at the Union of Concerned Scientists.
The study was funded by National Science Foundation grants to Johnson and Hunt and through private support through Duke's Nicholas School.
CITATION: "Dramatic Variability of the Carbonate System at a Temperate Coastal Ocean Site (Beaufort, North Carolina) is Regulated by Physical and Biogeochemical Processes on Multiple Timescales," by Zackary I. Johnson, Benjamin J. Wheeler, Sara K. Blinebry, Christina M. Carlson, Christopher S. Ward, Dana E. Hunt. PLOS ONE, Dec. 17, 2013. DOI:10.1371/journal.pone.0085117
Journal
PLOS ONE