Carbon fixation by phytoplankton in the open ocean plays a key role in the global carbon cycle but is not fully understood. Until now researchers believed that cyanobacteria overwhelmingly accounted for phytoplankton’s role in carbon fixation in the open ocean. But now scientists at the University of Warwick and the National Oceanography Centre in Southampton have opened “the black box” of eukaryotic phytoplankton and discovered that they actually account for almost half the ocean’s carbon fixation by phytoplankton.
Blue-green algae, or cyanobacteria, grow in vast numbers in the sunlit surface waters of the oceans, the photic zone. They use sunlight to ‘fix’ carbon by converting carbon dioxide into sugars and other organic compounds through photosynthesis.
Cyanobacteria belong to the ‘picophytoplankton’, the tiniest phytoplankton. Until now they have been thought to dominate carbon fixation in the open ocean, with species belonging to the genera Prochlorococcus and Synechococcus being particularly abundant.
Like all bacteria, cyanobacteria are prokaryotes, distinguished from eukaryotes by the absence of a cell nucleus. However, although much less abundant than cyanobacteria, the photic zone also has a high biomass of small eukaryotic phytoplankton capable of carbon fixation.
“The eukaryotic phytoplankton community has long been a ‘black box’ in terms of its composition as well as contribution to carbon fixation,” says Professor Dave Scanlan of the University of Warwick; “Determining how much carbon different groups fix into biomass is required for a full understanding of the Earth’s carbon cycle,” adds Professor Mikhail Zubkov of the National Oceanography Centre.
In research, published today 15th April 2010 in the Journal of the International Society for Microbial Ecology, the scientists report how they measured carbon fixation by dominant phytoplankton groups in the subtropical and tropical northeast Atlantic Ocean, using samples collected from surface waters during a research cruise aboard the Royal Research Ship Discovery.
They discovered that eukaryotic phytoplankton actually fix significant amounts of carbon, contributing up to 44% of the total, despite being considerably less abundant than cyanobacteria. “This is most likely because eukaryotic phytoplankton cells, although small, are bigger than cyanobacteria, allowing them to assimilate more fixed carbon,” says Zubkov.
Two groups of eukaryotes were distinguished, ‘EukA’ cells being more abundant but smaller than ‘EukB’ cells. Molecular techniques revealed that EukB largely comprised photosynthetic organisms called prymnesiophytes, most of which have never been cultured in the laboratory. Many of these are probably previously unknown species.
“Prymnesiophytes accounted for up to 38 per cent of total primary production in the subtropical and tropical northeast Atlantic Ocean,” says Scanlan: “This suggests that they play a key role in oceanic carbon fixation, but this needs to be confirmed by widespread sampling from the world’s oceans.”
Zubkov recently showed that small eukaryotic phytoplankton can obtain carbon by feeding on bacteria, supplementing carbon fixed through photosynthesis.
It is likely that some of the organic carbon of prymnesiophytes and other eukaryotic phytoplankton is eventually exported from the photic zone to the deep ocean, rather than being returned to the atmosphere in the form of carbon dioxide.
“Given their clear importance, it is crucial that we now go on to understand the factors controlling growth of small eukaryotes in the oceans,” concludes Scanlan.
For more information please contact:
Peter Dunn, Head of Communications, University of Warwick
Tel: +44(0)24 76 523708 Mobile +44(0)7767 655860 firstname.lastname@example.org
NOC Press Officer Dr Rory Howlett on +44 (0)23 8059 8490 Email: email@example.com
Professor David Scanlan, University of Warwick
firstname.lastname@example.org Phone: (+44) 24 76 528363
Professor Mike Zubkov, National Oceanography Centre
email@example.com Phone: +44 (0)23 8059 6335
Notes for Editors:
The full list of researchers are Ludwig Jardillier, John Pearman and David Scanlan (University of Warwick), and Mikhail Zubkov (NOC).
The paper is entitled “Significant CO2 fixation by small prymnesiophytes in the subtropical and tropical northeast Atlantic Ocean” first published online by ISME on 15th April 2010.
The University of Warwick is one of the UK’s top 10 research universities
The National Oceanography Centre (NOC) is a new, national research organisation that went live from 1 April this year. The NOC will work in partnership with the UK marine research community to deliver integrated marine science and technology from the coast to the deep ocean
The NOC brings together into a single institution activity at the National Oceanography Centre, Southampton (NOCS) and the Proudman Oceanographic Laboratory (POL) in Liverpool. The NOC will work in close partnership with the wider marine science community to create the integrated research capability needed to tackle the big environmental issues facing the world. Research priorities will include the oceans’ role in climate change, sea level change and the future of the Arctic Ocean.
The University of Southampton and the University of Liverpool are hosting partners of the National Oceanography Centre. The University of Southampton's School of Ocean & Earth Science shares a waterfront campus with elements of the NOC, and a close collaborative relationship is maintained at both Southampton and Liverpool.