Bm. Culik et G. Lunajorquera, SATELLITE TRACKING OF HUMBOLDT PENGUINS (SPHENISCUS-HUMBOLDTI) IN NORTHERN CHILE, Marine Biology, 128(4), 1997, pp. 547-556
During the El Nino of 1982/1983, the Humboldt penguin population dimin
ished dramatically in the whole distributional area of the species. Re
covery of the population was slow since 1983 and it has been suggested
that large numbers of Humboldt penguins die at ,sea, entangled in net
s, or starve to death, even during non-''EI Nino'' years. We were able
to determine for the first time, how Humboldt penguins on Pan de Azuc
ar Island (26 degrees S; 72 degrees W) utilize their marine habitat an
d where their feeding areas lie. For this purpose we employed two stre
amlined Argos satellite transmitters during the 1994/1995 and 1995/199
6 breeding seasons, respectively. Mean travelling speed of Humboldt pe
nguins during foraging trips was 0.94 m s(-1) and 50% of bird position
s were located within 5 km of the island (90% within 35 km). Total are
a covered by Humboldt penguins foraging from Pan de Azucar Island was
12255 km(2). Satellite transmitters also recorded dive duration; pengu
ins spent on average 7.8 to 9 h diving per foraging day but. showed no
preferences for particular feeding areas. Mean daily dive durations (
4-d mean) recorded during the 1994/1995 breeding season were positivel
y correlated between birds. Significant correlation between dive durat
ion and sea surface temperature anomalies and negative correlation bet
ween dive duration and fishery landings at nearby Caldera harbour indi
cate that the 1994/1995 increase in foraging effort was a response to
deteriorating prey availability. Sea surface temperatures during the 1
995/1996 breeding season were colder than average, and we observed no
trends in bird diving activities.