Be. Lavaniegos et al., LONG-TERM CHANGES IN ZOOPLANKTON VOLUMES IN THE CALIFORNIA CURRENT SYSTEM - THE BAJA-CALIFORNIA REGION, Marine ecology. Progress series, 169, 1998, pp. 55-64
A retrospective analysis of zooplankton volumes (1951 to 1996) was per
formed for the area between Punta Baja (30 degrees N) and Punta Abreoj
os (26.7 degrees N) in relation to the warming anomaly that has taken
place in the California Current System during the last 2 decades. The
seasonal cycle of median standing stock of zooplankton in this area sh
owed a moderate alternation between high values from June to October (
median monthly volumes between 86 and 108 ml/1000 m(3)) and low values
from November to May (58 to 77 ml/1000 m(3)). The quarterly long-term
means of zooplankton volumes were the lowest in winter, as were wind
speeds. The standard deviations associated with the long-term means in
dicated interannual variability was higher than seasonal variability.
The time series showed an interval of high zooplankton volume between
1952 and 1957. Following the strong ENSO (El Nino Southern Oscillation
) of 1957-1958, a period of low values occurred which extended into th
e early 1960s. There was a slow recovery of zooplankton biomass throug
h the rest of the 1960s, but it did not reach the earlier high values.
Available data suggest the increasing trend reached a peak in 1975. S
ubsequently, from 1976 to the ENSO of 1982-1983, the biomass decreased
. For the remainder of the 1980s, the few existing data showed an erra
tic behavior of the biomass. In the 1990s, there has been a decrease t
o values even lower than those observed during the 1957-1958 ENSO. Non
seasonal anomalies for zooplankton and environmental variables were si
gnificantly different (p < 0.001) among decades but not between the no
rthern (30 degrees to 28 degrees N) and southern (28 degrees to 26 deg
rees N) areas. The decrease in zooplankton volume in this region over
the last 2 decades is less than that reported for the Southern Califor
nia Eight. This may be partly caused by seasonal northward movements o
f tropical zooplankton species along the Baja California coast, Mexico
.