The concentration of carbon dioxide was measured during 18 cruises in the s
urface waters of the North Atlantic European Shelf (Galician sea, Gulf of B
iscay, Armorican Sea, Celtic Sea, English Channel, North Sea), covering all
four seasons (9 out of 12 months) at interannual scale. This is the very f
irst intensive field study of continental shelves, in terms of source/sink
for atmospheric CO2, which allows to integrate fluxes on an annual basis an
d over a large surface area. Here we show that European continental shelves
are a sink of 90-170 million tons of carbon per year, which is an addition
al appreciable fraction to the presently proposed flux for the open North A
tlantic Ocean (similar to 45%). The air-sea fluxes of CO2 we obtained are s
imilar to those recently reported in the East China Sea, allowing us to con
clude that the coastal ocean plays a considerable role in the global oceani
c carbon cycle.