the Irish Sea; analysis of Continuous Plankton Recorder programme
data did suggest the existence of a slight temporal shift
(<1 month) in the spring increase of the colour index (an index of
phytoplankton abundance) of the two regions (Edwards and
Johns, 2004). Therefore, if jellyfish production (i.e. strobilation
of polyps) or growth is synchronised with the spring bloom (to
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