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ABSTRACT
Due to their large body size and high
mammalian metabolic rate, blue whales
(Balaenoptera musculus) have the highest
average daily total energy requirement of any
species. Blue whales meet this energy demand by
feeding exclusively upon dense but patchy schools
of euphausiids. We used an integrated approach to
determine whether a unique combination of
seasonally high primary production supported by
coastal upwelling works in concert with topographic
breaks in the continental shelf off California to
collect and maintain large concentrations of
euphausiids that are exploited by foraging whales.
Specifically we used concurrent ship- and mooring-
based oceanographic, hydroacoustic, and net
sampling, opportunistic whale sighting records,
systematic visual surveys, and time-depth recorder
deployment to: 1) define prey patches and whale
foraging behavior within patches, 2) determine
spatial and temporal patterns in the distribution
and abundance of whale prey patches, and 3) examine
the biotic and abiotic factors important in
creating whale foraging patches in the seasonal
upwelling context of Monterey Bay, California
between 1992-1996.
Blue
whales fed exclusively upon epipelagic euphausiids
(Thysanoessa spinifera and Euphausia
pacifica) that were larger and in proportions
from that generally available in the Bay. Foraging
blue whales targeted schools of adult T. spinifera,
diving repeatedly to extremely dense patches
aggregated between 150 and 200m on the edge of the
Monterey Bay Submarine Canyon. These patches
averaged 145 g m-3, approximately two orders of
magnitude greater than the densities generally
available in the Bay (1.3 g m-3). High euphausiid
densities are supported by a combination of high
primary production between April and August
(average peak production 249 mg-C m-3 day-1) and
the presence of a deep canyon that provided deep
water downstream from the Davenport/Año
Nuevo coastal upwelling center. Peak euphausiid
densities occur in late summer/early fall, lagging
the seasonal increase in primary production by 3-4
months. This lag likely results from both the
temporal development of euphausiids spawned around
the seasonal increase in primary production in the
spring and the shoreward collapse of productivity
due to decreased intensity of coastal upwelling in
the late summer. The annual migratory movements of
the California blue whale likely reflect seasonal
patterns in productivity in other foraging areas
similar to those we have described for Monterey
Bay.
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