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Prof. Dr. Marcel Kuypers

Max Planck Institute for Marine Microbiology, Bremen
Phone:+49 421 2028-602Fax:+49 421 2028-690

Dr. Rita Dunker

Max Planck Institute for Marine Microbiology, Bremen
Phone:+49 421 2028-856Fax:+49 421 2028-790

Dr. Manfred Schlösser

Max Planck Institute for Marine Microbiology, Bremen
Phone:+49 421 2028-704Fax:+49 421 2028-790

Original publication

Tim Kalvelage, Gaute Lavik, Phyllis Lam, Sergio Contreras, Lionel Arteaga, Carolin R. Löscher, Andreas Oschlies, Aurélien Paulmier, Lothar Stramma and Marcel M. M. Kuypers
Nitrogen cycling driven by organic matter export in the South Pacific oxygen minimum zone

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Ecology

How the ocean loses nitrogen

Scientists identify key factor controlling nitrogen availability in the ocean

February 24, 2013

During an expedition to the South Pacific Ocean, scientists from the Max Planck Institute for Marine Microbiology, along with their colleagues from the GEOMAR Helmholtz Centre for Ocean Research in Kiel discovered that organic matter derived from decaying algae regulates nitrogen loss from the ocean's oxygen minimum zones.
A pump-CTD was used to sample the South Pacific oxygen minimum zones in various depths of water. Zoom Image
A pump-CTD was used to sample the South Pacific oxygen minimum zones in various depths of water.

One of the central aims of today's marine research is to better predict the response of our ocean to global warming and human activity in general. Understanding of the oceanic nitrogen cycle is of key importance in this effort as nitrogen is the limiting nutrient for life in the ocean. Its bio-available form (so-called fixed nitrogen, such as ammonium) is produced biologically from nitrogen gas by bacteria or is transported to the ocean as dust or river run-off. However, due to the activity of billions of marine microorganisms, this fixed nitrogen is rapidly converted back to nitrogen gas, which escapes from the ocean to the atmosphere. There are two processes, which are mainly responsible for this nitrogen loss: denitrification and anammox (anaerobic oxidation of ammonium with nitrite), both performed by anaerobic bacteria.

Up to 40 percent of global oceanic nitrogen loss occurs in oxygen minimum zones (OMZ), which are areas with low to non-measurable oxygen concentrations. "The eastern tropical South Pacific OMZ is one of the largest oxygen minimum zones in the world," explains Tim Kalvelage from the Max Planck Institute for Marine Microbiology, the first author of this study. "We assumed that if we could identify and constrain the parameters that regulate N loss from this OMZ, we could better predict the nitrogen loss from all OMZs, and possibly from the Ocean, as well." Andreas Oschlies from GEOMAR in Kiel adds: "This research is fundamental for the current biogeochemical models to work because so far our models cannot reliably reproduce the patterns of nitrogen loss that we measure."

As a part of a large collaborative project SFB 754 a series of expeditions onboard of the research ship Meteor from 2008 - 2009 were specifically dedicated to collect samples from the South Pacific OMZ. Further analyses and measurements followed in the laboratories of the Max Planck Institute for Marine Microbiology in Bremen, GEOMAR Helmholtz Centre for Ocean Research and Institute for General Microbiology in Kiel. The results provide a detailed overview of nutrient distributions, rates of nitrogen loss processes and abundances and identity of bacteria in the South Pacific OMZ. Furthermore, models were employed to calculate the amount of algal biomass that is exported from the surface to the deeper OMZ waters. This large-scale study resulted in the so far most comprehensive nitrogen budget for an oceanic OMZ.

"Our results will help to more realistically estimate the short- and long-term impacts of human-induced ocean de-oxygenation and changing productivity on nitrogen cycling in the OMZs, as well as the rest of the Ocean. This is critical to estimate how much CO2 can be taken up by the Ocean in the future," Marcel Kuypers concludes.

MS/BA

 
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