The ocean's dead zones teem with microbes, studies show. Frank Stewart explains the research.
EDITOR’S NOTE: This item first appeared as a blog post in the Amplifier.
Oceanic dead zones are natural laboratories for exploring biological diversity. In a study published this year in the journal Nature, scientists at Georgia Tech discovered new species of the world's most abundant organism group, a bacterial clade called SAR11, which have adapted to life in dead zones by acquiring genes necessary to breath the chemical nitrate. Other work by Tech scientists shows that dead zones in the Pacific, which contain the largest pools of the greenhouse gas methane (CH4) in the open ocean, support microbes adapted to consume methane, potentially through a process that requires these microbes to make their own oxygen. Research on dead zones is challenging scientists to devise new tools to collect and manipulate ocean microbes while maintaining the exact environmental conditions the cells experience in nature. Frank Stewart, of the School of Biological Sciences, explains:
The oceans are losing oxygen. A poignant example is the "dead zone" that forms each summer in the Gulf of Mexico. Each spring, fertilizers from farms and lawns wash into the rivers feeding the Gulf. This influx of nutrients, primarily nitrogen and phosphorus from the Mississippi River, fuels expansive blooms of photosynthetic algae near the river mouths. When these algae die, they are eaten by single-celled microbes (bacteria) that consume oxygen during growth. If oxygen removal exceeds replenishment, as occurs in the Gulf during high microbial growth in the calm of summer, seawater oxygen levels can fall nearly to zero, creating a "dead zone" devoid of larger marine life. Dead zones like those in the Gulf can span thousands of square miles and, by altering the distributions of animals such as shrimp and fish, compromise the health of the ocean's most productive and biodiverse ecosystems.
But not all life deplores a dead zone. Indeed, thousands of microbial species thrive under the low-oxygen conditions of the dead zone, occurring at densities of millions of cells per milliliter (~1/5 of a teaspoon). These microbes employ a wide spectrum of biochemical solutions to life without oxygen, many of which remain poorly understood but are critical for ocean processes. For example, many of the microbes responsible for controlling the bioavailability of nitrogen, an essential component of proteins and DNA, grow only under low-oxygen conditions by using nitrogen-containing compounds, such as nitrite (NO2-), in place of oxygen. In metabolizing such compounds, these microbes produce nitrogen-containing gases, including the potent greenhouse gas nitrous oxide (N2O).
Studies of dead zone microbes are transforming our knowledge of ocean ecosystems. By collecting water at different depths through a dead zone, researchers can sample microbes exposed to vastly different oxygen and chemical conditions, thereby testing predictions of how ecosystem-level processes, such as the cycling of nutrients or greenhouse gases, may change as human activities influence ocean parameters.
Dead zones, in addition to exerting critical effects on the function of marine ecosystems, are breathing life into a broader understanding of microbes in the oceans.