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Zurich, Switzerland (SPX) Jul 19, 2013
In an international collaborative project, scientists have recorded the times, places and concentrations of oceanic plankton occurrences worldwide. Their data has been collected in a global atlas that covers organisms from bacteria to krill.
Oceans cover 70 per cent of the earth's surface. The animal and plant species concealed within these vast expanses and almost fathomless depths have been researched relatively little in comparison with those of terrestrial ecosystems.
To date, very little is known about the distribution of plankton - those organisms that are too small to swim against the ocean currents. In a large-scale project coordinated by researchers at ETH Zurich and the University of East Anglia (UK), scientists from numerous universities joined forces to make a survey of when and where which plankton species occur and to determine how much carbon they absorb.
At 500,000 locations across the globe, they collected data on the species diversity and biomass of plankton.
From bacteria to small crustaceans
In spite of the tininess of individual organisms, plankton play a crucial role in the oceans: on the one hand, plankton are an important driver of global biogeochemical cycles, and on the other hand, they form the basis of the food chains in marine ecosystems.
For example, phytoplankton absorb CO2 for photosynthesis, release oxygen into the atmosphere and carry a good portion of the absorbed carbon into the depths of the oceans when they die and sink to the ground. In this way, phytoplankton remove CO2 from the atmosphere and contribute to the regulation of the global climate.
Plankton also control the marine nitrogen cycle and can even influence cloud formation through the sulphur cycle. Zooplankton such as krill are an important source of food for whales, fishes and other marine species higher up in the food chain, which in turn are exploited by humans.
Global puzzle out of hundreds of thousands of data entries
"Analysing data from half a million survey stations was an incredibly ambitious undertaking and would have been impossible without international collaboration," says Vogt.
The scientists combed through databases and publications and even extracted data from hand-written notes. The data were carefully quality-controlled before they were used to calculate biomass. What took especially long was persuading the various research institutes that gather such data to participate, and standardising the various contributions, some of which were historical.
Plankton data for climate science
This is why the data are also valuable for climate scientists, who now have a more solid foundation of data to validate their models. Until now, they have worked with simple ocean ecosystem models that differentiate between two kinds of zoo- and phytoplankton at most. If the scientists succeed in mapping ecological diversity more accurately by taking into account more plankton types, then this would allow more precise predictions with regard to the role of the ocean as a carbon sink.
A disrupted ecosystem
"What initial analyses of MAREDAT do show is that there are far more organisms in the deep sea than has been assumed so far. In addition, it seems that across the world's oceans, zooplankton have at least as much biomass as phytoplankton.
"This is surprising, since it is usually just the other way round in the terrestrial systems, where there are more plants than animals," says Meike Vogt. Her group also uses MAREDAT to form fundamental hypotheses about ecological diversity and to verify their models with the newly obtained data.
"At the moment, we can generate initial rudimentary distribution maps with statistical models. These maps, however, will change greatly in the next ten years, because we have too few samples from some regions to map them accurately," says Meike Vogt.
The South Pacific and some regions in the Southern Ocean have hardly been studied. This is why the scientists want to revise MAREDAT for the first time in 2015. The aim is to collect even more data in order to document changes in plankton communities later on.
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