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Additional nutrients intensify dead zones in oceans, researchers find

Additional nutrients intensify dead zones in oceans
First author Zoe van Kemenade filtering sea water on board the Dutch research vessel RV Pelagia. Credit: NIOZ

As more and more nutrients from land and air enter the world's oceans, the dead zones without oxygen in the water will increase in size and intensity. That is the warning that Ph.D. student Zoë van Kemenade, an organic geochemist at NIOZ, draws from her analysis of drill cores from the ocean floor off the coast of California.

The results of this research are published in the journal Biogeosciences.

Van Kemenade and colleagues looked at drill cores that were taken from the Pacific Ocean floor off the coast of California as early as 1997. "There is a very interesting, natural 'dead zone' there that is relatively low in oxygen due to specific ocean currents from the poles and from the Equator," Van Kemenade says.

"By looking at how that lack of oxygen over the past 2.5 million years has correlated with warmer and colder periods, we wanted to learn how that lack of oxygen might continue to evolve in the future under the influence of changing climate."

Oxygen depletion can occur as the water gets warmer. This is because warmer water can hold less dissolved gases. Because of the current warming of the oceans, they already contain 2 percent less oxygen than they did half a century ago. But can also be caused by an extra supply of nutrients, Van Kemenade explains.

"Extra nitrogen causes extra growth of algae. Initially, all those little plants in the upper layer of the water produce oxygen, but when they die and are 'eaten' by bacteria at the bottom of the ocean, the scale tips and more oxygen is consumed than produced."

For her reconstruction of oxygen levels, Van Kemenade used a very specific molecule from the drill core. "A distinct group of bacteria can break down nitrogen compounds under oxygen-free conditions. These so-called anammox bacteria produce very special molecules in the process, ladderanes."

"These should protect the cell from the extremely reactive metabolites in that chemical process. An additional advantage for us as researchers is that we can find those characteristic ladderanes literally hundreds of thousands of years later as traces of these bacterial processes under oxygen-free conditions."

Whereas Van Kemenade had expected to see the conditions with low oxygen in the 'history book' of the going up and down with warmer and colder periods in the past, she saw that ladderanes were quite common during both the ice ages and interglacials. "So, for this particular spot, we have to conclude that oxygen depletion was related not only to the fluctuations in temperature but, more importantly, to the amount of nutrients in the water," Van Kemenade said.

This study was one of the first to use information from ladderanes on this scale. "We should, therefore, not immediately translate the results to all seas where oxygen-free conditions can occur," Van Kemenade warns.

"At the same time, it does serve as a warning that extra nutrients in the water can cause major problems for ocean biodiversity. Oxygen-less conditions can have major consequences for the ecosystem, but also for fisheries, for example."

More information: Zoë Rebecca van Kemenade et al, Loss of nitrogen via anaerobic ammonium oxidation (anammox) in the California Current system during the late Quaternary, Biogeosciences (2024). DOI: 10.5194/bg-21-1517-2024

Journal information: Biogeosciences

Citation: Additional nutrients intensify dead zones in oceans, researchers find (2024, March 25) retrieved 27 April 2024 from https://phys.org/news/2024-03-additional-nutrients-dead-zones-oceans.html
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