How salt and temperature ‘herd’ phytoplankton

Subtle and brief differences in ocean salinity or temperature work like physical barriers for phytoplankton, and result in a patchy distribution of the oceans’ most important food resource.

Phytoplankton are microscopic algae that live free-floating in the sea, transported around by ocean currents. Because phytoplankton constitute the base of the food web in the sea, the composition of their communities affects other microscopic organisms, fish, and whales.

“The oceans are full of invisible barriers that occur when temperature or salinity changes,” says lead author and postdoc Erik Mousing of the Center for Macroecology, Evolution and Climate at University of Copenhagen.

“Our new research shows that even short-lived barriers of just a couple of days or weeks, are enough to influence phytoplankton communities. This provides us with new insight into how the high biodiversity of phytoplankton is maintained and how the food web might be affected.”

Rise of ‘armored’ phytoplankton puzzles scientists

In recent decades, researchers have increasingly understood how small organisms are separated by relatively permanent fronts in the sea caused, for example, by large ocean currents. However, this is the first time researchers demonstrate that short-lived changes in salinity or temperature also lead to changes in the composition of algae communities.

While it is known that physical barriers on land, such as rivers and mountains, can lead to the development of new plant and animal species over time, the oceans have primarily been perceived as a homogeneous environment. Therefore, it has been difficult to explain the large biodiversity of small algae.

“Our results show that the distribution of phytoplankton is much patchier than previously assumed as a result of these commonly occurring weak fronts,” says coauthor Katherine Richardson, professor at the Center for Macroecology, Evolution and Climate. “Coupled with the short generation time of phytoplankton the local barriers caused by these fronts could help explain why phytoplankton diversity is so large. Thus, at least in terms of the overall mechanisms controlling biodiversity, the terrestrial and marine systems are not fundamentally different.”

In the study, which appears in the Journal of Ecology, the researchers analyze 30 samples of phytoplankton from 16 locations in the North Atlantic. They measured temperature and salinity in different water depths. Based on the samples, the researchers mapped out a front with different salinities on each side. The species composition of phytoplankton was significantly different on either side of the front.

“Although our results are based on samples in the North Atlantic, weak and short-lived fronts occur in oceans all over the world. Therefore, there is every reason to believe that the influence of these small scale fronts on phytoplankton is a common feature in the world’s oceans,” concludes Mousing.

Study collaborators are from the Danish ClimateLab, NASA, and the University of Maine.

Source: University of Copenhagen

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Source: Futurity