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MEPS 289:117-130 (2005)
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Abstract
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From wind to whales: trophic links in acoastal upwelling system
Donald A. Croll1,*, Baldo Marinovic1, Scott Benson2, Francisco P. Chavez3, Nancy Black4, Richard Ternullo4, Bernie R. Tershy1
1Center for Ocean Health, Long Marine Laboratory, 100 Shaffer Road, University of California Santa Cruz, Santa Cruz, California 95060, USA 2Moss Landing Marine Laboratories, PO Box 450, Moss Landing, California 95039,
USA 3Monterey Bay Aquarium Research Institute, PO Box 628, Moss Landing, California 95039, USA 4Monterey Bay Dolphin Project, 84 Fishermans Wharf, Monterey, California 93940, USA
*Corresponding author. Email: croll@biology.ucsc.edu

ABSTRACT: Blue whales Balaenoptera musculus meet the highest prey demands of any predator that has ever existed by feeding exclusively upon dense but patchy schools of pelagic euphausiids. We examined the role that seasonally high primary
production supported by coastal upwelling combined with topographic breaks off California play in creating, collecting, and maintaining euphausiids at densities sufficient to allow exploitation by whales. We used concurrent ship- and mooring-based
oceanographic, hydroacoustic, and net sampling, whale-sighting records, visual surveys, and timedepth recorder deployment to examine temporal and spatial linkages between (1) intensity of upwelling, (2) primary production, (3) development, density
and distribution of euphausiids, and (4) the distribution, abundance, and foraging behavior of blue whales in Monterey Bay, California between 1992 and 1996. Blue whales fed exclusively upon adult euphausiids Thysanoessa spinifera and Euphausia
pacifica that were larger than those generally available in the Bay. Foraging whales dove repeatedly to dense euphausiid aggregations between 150 and 200 m on the edge of the Monterey Bay Submarine Canyon. Euphausiid aggregations where whales were
foraging averaged 153 g m3, approximately 2 orders of magnitude greater than mean euphausiid densities in the Bay (1.3 g m3). High euphausiid densities are supported by high primary production between April and August
(249 mgC m3 d1) and a submarine canyon that provides deep water down-current from an upwelling region. Peak euphausiid densities occur in late summer/early fall, lagging the seasonal increase in primary production by 3 to
4 mo. This lag results from the temporal development of euphausiids spawned around the spring increase in primary production and the shoreward collapse of productivity due to decreased upwelling in late summer. The migratory movements of the California
blue whale probably reflect seasonal patterns in productivity in other foraging areas similar to those we describe for Monterey Bay.
KEY WORDS: Pelagic · Foraging ecology · Predation · Blue whale · Upwelling
Full text in pdf format

Published in MEPS Vol.
289
(2005) on March 30
Print ISSN: 0171-8630; Online ISSN: 1616-1599.
Copyright © Inter-Research, Oldendorf/Luhe, 2005
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