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Unexpected interaction between ocean currents and bacteria may weaken ocean's ability to absorb carbon dioxide

Date:
September 13, 2013
Source:
University of Southern Denmark
Summary:
For the first time, researchers have successfully demonstrated an interaction between ocean currents and bacteria: The unexpected interaction leads to the production of vast amounts of nitrogen gas in the Pacific Ocean. This takes place in one of the largest oxygen free water masses in the world -- and these zones are expanding. This can ultimately weaken the ocean's ability to absorb CO2.

Illustration. Purple area: This ocean water holds less than 10 per cent oxygen. Blue area: The Oxygen Free Zone off Peru/Chile, where bacteria produce huge amount of nitrogen. Black Arrow: Ocean current that transports the bacteria through the Oxygen Minimum Zone.
Credit: Illustration: Bo Thamdrup/SDU

For the first time, researchers have successfully demonstrated an interaction between ocean currents and bacteria: The unexpected interaction leads to the production of vast amounts of nitrogen gas in the Pacific Ocean. This takes place in one of the largest oxygen free water masses in the world -- and these zones are expanding. This can ultimately weaken the ocean's ability to absorb CO2.

Three places in the world harbor extensive oxygen free water masses, called Oxygen Minimum Zones. In these zones, microbes produce atmospheric nitrogen gas -- the gas that accounts for almost 80 per cent of Earth's atmosphere. Researchers from the University of Southern Denmark now report to have found the reason behind the huge nitrogen gas production in the largest of the three Minimum Oxygen Zones, located in the Pacific Ocean off Chile and Peru. The nitrogen gas is produced by a steady stream of bacteria who, when they feed, produce lots of nitrogen gas.

"The bacteria flow with an ocean current, that comes from the Equator and is heading towards the South Pole. On their way south the bacteria rid the water of ammonia, which they eat and transform into nitrogen gas in the Oxygen Minimum Zone," explain the scientists, postdoc Loreto De Brabandere and Professor Bo Thamdrup from the Nordic Center for Earth Evolution at the University of Southern Denmark.

Behind the research are also colleagues from Aarhus University, Monterey Bay Aquarium Research Institute, USA, and Universidad de Concepciσn, Chile.

In the western Pacific off New Zealand heavy and nutrient-rich water sinks below the surface and begins to flow as an underwater current; first towards and along the Equator and then it changes course and heads south, when it approaches the coast of South America. During this long journey oxygen disappears from the current's water, and off Peru and Chile the hungry bacteria go to work.

The hungry bacteria in the ocean current from the Equator are called anammox bacteria; they get energy to grow by allowing nitrite to react with ammonia and form nitrogen gas. Anammox bacteria and their impact on the global nitrogen cycle were only discovered a few years ago.

The scientists are surprised, that this type of bacteria is responsible for the production of nitrogen gas in the giant Oxygen Minimum Zone in the Pacific Ocean.

"In the other zones we find that another nitrogen gas producing type of bacteria is responsible, namely the so-called denitrifying bacteria," says Loreto De Brabandere.

Denitrifying bacteria also produce nitrogen gas, but they do it from nitrate and nitrite when combusting organic material -- not from ammonia as anammox bacteria do.

"But here we show that the denitrifying bacteria simply do not get enough organic food to form nitrogen gas, so they are virtually pushed out of the way by anammox bacteria that come with the water from the Equator. The result is that anammox bacteria account for almost the entire nitrogen gas production," explains Bo Thamdrup.

If the anammox bacteria did not come with ocean currents along the coast of South America, significantly less nitrogen gas would be produced in the oceans as a whole. The denitrifying bacteria would probably never be able to find enough nutrients to produce the same amount of nitrogen gas.

"The exciting news is that the explanation for the large production of nitrogen gas off Chile is found near the Equator, over a thousand kilometers further north. It is the first time we see such an interaction between ocean currents, bacteria, and nutrient cycling," says Bo Thamdrup.

There are no indications that the ocean current may be disturbed by climate change or other factors, and thus there will probably be no changes in its cargo of anammox bacteria.

"However there are signs that the Oxygen Minimum Zones around the world are expanding, and this can lead to an increased production of atmospheric nitrogen. An increase in nitrogen gas emission leads to fewer algae in the water, and thus there is less food for marine microorganisms. Ultimately, it means less food for the fish," explains Bo Thamdrup.

Expanding Minimum Oxygen Zones may also weaken the ocean's capacity to absorb CO2, explains Loreto De Brabandere: "It gives more room for the nitrate-eating bacteria, and thus there is less nitrate available to marine plankton. Plankton is effective at absorbing CO2, and if there is less plankton there will be less CO2 absorbed."

The Minimum Oxygen Zones

There are three Minimum Oxygen Zones in the world: in the Pacific Ocean off Peru/Chile, north of the Equator off Mexico/Guatemala and in the Arabian Sea. The zones are underwater pools, not in contact with the surrounding seawater, and they do not contain any oxygen. The zones are located app. 100 -- 500 meters below the surface and they make up app. two per cent of the oceans. They are nevertheless very important, as they account for a third of the oceans' removal of nitrogen. Just a little variation in their size will have great impact on how much nitrogen is removed. No animals can live in the Minimum Oxygen Zones. Only bacteria that do not need oxygen, can thrive here.


Story Source:

The above story is based on materials provided by University of Southern Denmark. The original article was written by Birgitte Svennevig. Note: Materials may be edited for content and length.


Journal Reference:

  1. Loreto De Brabandere, Don E. Canfield, Tage Dalsgaard, Gernot E. Friederich, Niels Peter Revsbech, Osvaldo Ulloa, Bo Thamdrup. Vertical partitioning of nitrogen-loss processes across the oxic-anoxic interface of an oceanic oxygen minimum zone. Environmental Microbiology, 2013; DOI: 10.1111/1462-2920.12255

Cite This Page:

University of Southern Denmark. "Unexpected interaction between ocean currents and bacteria may weaken ocean's ability to absorb carbon dioxide." ScienceDaily. ScienceDaily, 13 September 2013. <www.sciencedaily.com/releases/2013/09/130913101817.htm>.
University of Southern Denmark. (2013, September 13). Unexpected interaction between ocean currents and bacteria may weaken ocean's ability to absorb carbon dioxide. ScienceDaily. Retrieved October 1, 2014 from www.sciencedaily.com/releases/2013/09/130913101817.htm
University of Southern Denmark. "Unexpected interaction between ocean currents and bacteria may weaken ocean's ability to absorb carbon dioxide." ScienceDaily. www.sciencedaily.com/releases/2013/09/130913101817.htm (accessed October 1, 2014).

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