Fertilized by nutrients that have built up during the winter, the cool waters of the North Atlantic come alive every spring and summer with a vivid display of color that stretches across hundreds of miles. In what’s known as the North Atlantic Bloom, millions of phytoplankton use sunlight and carbon dioxide to grow and reproduce at the ocean’s surface.
According to Melissa Omand, assistant professor of oceanography at the University of Rhode Island’s Graduate School of Oceanography, phytoplankton remove carbon dioxide from seawater during photosynthesis and release oxygen as a by-product. That allows the oceans to absorb additional carbon dioxide from the atmosphere.
Flowers ultimately wither and fade, but what eventually happens to these tiny plants produced in the sea? When phytoplankton die, the carbon in their cells sinks to the deep ocean. This so-called biological pump makes the North Atlantic Ocean efficient at soaking up CO2 from the air.
“Much of this particulate organic carbon, especially the larger, heavier particles, sinks,” said Omand, co-author of a paper on the North Atlantic Bloom published last week in the journal Science.
“But we wanted to find out what’s happening to the smaller, non-sinking phytoplankton cells from the bloom. Understanding the dynamics of the bloom and what happens to the carbon produced by it is important, especially for being able to predict how the oceans will affect atmospheric CO2 and ultimately climate.”
In addition to Omand, other authors of the paper are Amala Mahadevan of the Woods Hole Oceanographic Institution, Eric D’Asaro and Craig Lee of the University of Washington, and Mary Jane Perry, Nathan Briggs and Ivona Cetinic of the University of Maine. Their research was funded by the National Science Foundation.
During their fieldwork, the scientists used a float to follow a patch of seawater off Iceland. They observed the progression of the bloom by taking measurements from multiple platforms. Autonomous gliders outfitted with sensors were used to gather data such as temperature, salinity and information about the chemistry and biology of the bloom – oxygen, nitrate, chlorophyll and the optical signatures of the particulate matter.
At the onset of the bloom and over the next month, four teardrop-shaped seagliders gathered 774 profiles to depths of up to 1,000 meters. Analysis of the profiles showed that about 10 percent had unusually high concentrations of phytoplankton bloom properties, even in deep waters, as well as high oxygen concentrations usually found at the surface.
“These profiles were showing what we initially described as ‘bumps’ at depths much deeper than phytoplankton can grow,” said Omand.
Using information collected at sea, Omand and Mahadevan modeled ocean currents and eddies and their effects on the spring bloom.
“What we were seeing was surface water, rich with phytoplankton carbon, being transported downward by currents on the edges of eddies,” Mahadevan said. “Eddies hadn’t been thought of as a major way organic matter is moved into the deeper ocean. But this type of eddy-driven ‘subduction’ could account for a significant downward movement of phytoplankton from the bloom.”
In related work published in Science in 2012, the researchers found that eddies act as early triggers of the North Atlantic Bloom. Eddies help keep phytoplankton in shallower water where they can be exposed to sunlight to fuel photosynthesis and growth.
Learning more about eddies and their link with plankton blooms will allow for more accurate global models of the ocean’s carbon cycle, the researchers say, and improve the models’ predictive capabilities.