MESOPELAGIC MICRONEKTON AND MACROZOOPLANKTON OBSERVED BY ECHOSOUNDING, MULTIPLE-NET SAMPLING AND VIDEO PROFILING ACROSS THE ALMERIA-ORAN FRONT (W MEDITERRANEAN-SEA)
T. Baussant et al., MESOPELAGIC MICRONEKTON AND MACROZOOPLANKTON OBSERVED BY ECHOSOUNDING, MULTIPLE-NET SAMPLING AND VIDEO PROFILING ACROSS THE ALMERIA-ORAN FRONT (W MEDITERRANEAN-SEA), Annales de l'Institut oceanographique, 69(1), 1993, pp. 87-93
The daytime vertical distribution and abundance of mesopelagic microne
kton and macrozooplankton were investigated, using simultaneous echoso
unding, multiple-net sampling (EZNET) and Video Profiling across the A
lmeria-Oran front, during spring 1991. Three sites were studied: a Med
iterranean site, an Atlantic site and a frontal site lying between the
m. Observations carried out with a 38 kHz echosounder demonstrated dif
ferences in the patterns and backscattering volume of deep sound scatt
ering layers (SSL) between these sites. The two main SSL (SSL1 and SSL
2) were found more than 50 m deeper at the Mediterranean site than at
the Atlantic site, while the frontal site wal characterized by two add
itional shallow SSL (SSL3 and SSL4) situated above SSL1 and 2. These d
ifferences in acoustic patterns were reflected in the depth distributi
on and biovolumes of both micronekton and macrozooplankton from EZNET
samples and Video Profiler recordings. Fishes appear responsible for S
SL1, 2 and 3, while euphausiids are possible sources of SSL4 in the fr
ontal site. Though gelatinous zooplankton (medusae, siphonophores, app
endicularians, ctenophores) visualized by the Video Profiler was abund
ant, it seems to be transparent to 38 kHz sound. Biological productivi
ty in superficial layers probably plays a role in differences observed
in patterns across the Almeria-Oran front.