Samples historically collected and analysed by the Continuous Plankton
Recorder survey in the North Atlantic and adjacent seas were used to
examine temporal patterns in the near-surface abundance of copepodite
stages V and VI Calanus hyperboreus (n = a total of 32836 samples; mea
n latitude of samples = 54 degrees N, SD = 6.7 degrees). The occurrenc
e of CV and VI C. hyperboreus was largely restricted to samples collec
ted in April, May and June. During this period there was a diel cycle
in near-surface abundance which was consistent with a normal pattern o
f diel vertical migration. For example, CV-VI C. hyperboreus were 1.9
times more abundant at night than during the day, a difference which w
as highly significant (t-test, t(5072) = 3.9, P < 0.001). The ratio of
night:day abundance was similar in CV-VI C. finmarchicus (night:day a
bundance = 1.4), but markedly higher in CV-VI Metridia lucens (night:d
ay abundance = 12.3) and CV-VI M. longa (night:day abundance = 15.0).