Jm. Pinot et J. Jansa, Time variability of acoustic backscatter from zooplankton in the Ibiza Channel (western Mediterranean), DEEP-SEA I, 48(7), 2001, pp. 1651-1670
Citations number
30
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
One year of mean volume backscattering strength (MVBS) data obtained from a
n acoustic Doppler current profiler (ADCP) moored at 240 m in the Ibiza Cha
nnel is analysed. It shows the prominent effect of light on the zooplankton
distribution in the surface layer. Two communities of zooplankton can be d
ifferentiated, both of which perform diel vertical migrations (DVM). They i
nitiate descent at dawn, reach a maximum depth at noon, and finish ascent a
t dusk. Fast "primary" migrators, which quite homogeneously filled the surf
ace layer at night, generally descended below the ADCP during day-time, whe
reas slower "secondary" migrators always remained above the instrument. The
vertical motion of primary zooplankton at dawn and dusk was strong enough
to be directly measured by the ADCP ( +/- 3-4 cm s(-1)). The vertical veloc
ity of secondary zooplankton inferred from the slope of MVBS contours slid
not exceed a few tenths of cm s(-1). Variations in DVM show a great depende
nce on light intensity: (1) The depth attained by zooplankton at noon was m
odulated by the annual cycle of sunlight and was maximum/minimum around the
summer/winter solstice. (2) Some primary zooplankton remained above the AD
CP during day-time on days of heavy cloud cover in winter, (3) The preferen
tial depth of zooplankton at night followed the cycle of moonlight (29.5 da
ys). Primary zooplankton were present all year at the mooring, whereas seas
onal variations are seen in the abundance of secondary zooplankton. Maximum
abundance is found in summer with enhanced concentration in the thermoclin
e (upper 60 m), and minimum abundance in early winter after the erosion of
the thermocline. A bloom is also observed in late winter. These observation
s are discussed in the context of past zooplankton surveys in the area, Fas
t primary migrators could consist of euphausiids (alternatively, micronekto
n, e.g, myctophids). A fraction of slow secondary migrators very likely are
copepods. (C) 2001 Elsevier Science Ltd, All rights reserved.