A shocking amount of nitrous oxide off the western coast of India is causing scientists to take another look at laughing gas. Researchers at the National Institute of Oceanography in Goa found three times more nitrous oxide in the Arabian Sea than previously found anywhere else in the world.

“The actual magnitude of the concentrations really blew me away,” says Louis Codispoti of Horn Point Laboratory in Cambridge, Md., who read the report in the Nov. 16 Nature. The findings also suggest nitrous oxide plays a stronger role in global warming than originally thought.

“We are talking about a fairly large and globally significant source,” says Wajih Naqvi, the primary author of the report. The contribution of the Arabian Sea to the total amount of nitrous oxide into the atmosphere may be as much as one million tons per year or 25 percent of all anthropogenic sources of nitrous oxide, he says. This complicates the picture of global warming even further. “On a per molecule basis, nitrous oxide is over 200 times more effective in absorbing infrared radiation as carbon dioxide.” Even small increases in nitrous oxide inventory of the atmosphere could bring about relatively large changes in climate.

[Wajih Naqvi (left) and assistant prepare a water trap while on board the Research Vessel Sagar Kanya (below right). Photos courtesy of W. Naqvi.]

A 1992 report of nitrous oxide concentrations of 173 nanomoles off the coast of Peru held the record. Naqvi’s report, with nitrous oxide concentrations reaching 533 nanomoles in the Arabian Sea, triples that number.  During the summer monsoon season, an undercurrent off the coastal shelf of western India brings an upwelling of cold, saline, nutrient rich and oxygen depleted water to the country’s shores. But freshwater runoff during the heavy monsoon rains bleeds out over the colder seawater — covering it with a 5- to 10-meter-thick, warm cap. Planktonic algae thrive in the upper layers of these nutrient rich waters before sinking to the bottom where bacteria, living off decaying organic matter, produce nitrous oxide in the low-oxygen environment through both nitrification and denitrification.

The three-year study also indicates fertilizer runoff into the Arabian Sea may be contributing to the production of the nitrous oxide. The increasing runoff of nutrients from land aggravate the situation by increasing eutrophication in the surface waters and thereby feeding the bacteria with further organic matter. Because the area is so shallow, 6 to 28 meters, the nitrous oxide produced can easily escape to the atmosphere, Naqvi says. More nitrous oxide could feed a vicious cycle — leading  to increased global warming, potentially stronger monsoons, an increase in the nitrogen-laden runoff from land, coastal eutrophication, and bacteria producing nitrous oxide as they munch on dead plankton cells. And nitrous oxide is but one part in the “deliciously complex” nitrogen cycle, Codispoti says.

In the open ocean, the site of past studies on nitrous oxide, scientists such as Codispoti learned that bacteria finish eating what little oxygen remains in their surroundings and then begin to consume the nitrous oxide they already produced — converting N2O to N2 using an enzyme known as nitrous oxide reductase in the denitrification process. The bacteria switch to consuming the reductase — helping to keep the level of nitrous oxide in check.

Naqvi and colleagues have found that in shallow waters with almost no oxygen, high microbial metabolic rates can lead to brief periods when nitrous oxide accumulates to extremely high levels with the chance, in the shallow environment, to escape before the bacteria can chow down on the nitrous oxide reductase. This can give a pulsing effect to the levels of nitrous oxide as the stop-and-go nature of local phenomena, such as storms, temporarily re-oxygenate the waters.

“It’s time we started looking at analogous areas more closely,” Codispoti says. He would like to investigate nitrous oxide in the Chesapeake Bay. Other areas with fluctuating nutrient zones to explore include the mouth of the Mississippi River, the Gulf of Mexico and coastal waters off Peru.

Christina Reed
 

Geotimes Home | AGI Home | Information Services | Geoscience Education | Public Policy | Programs | Publications | Careers © 2025 American Geological Institute. All rights reserved. Any copying, redistribution or retransmission of any of the contents of this service without the express written consent of the American Geological Institute is expressly prohibited. For all electronic copyright requests, visit: http://www.copyright.com/ccc/do/showConfigurator?WT.mc_id=PubLink