2.1 Study area
The San Francisco Bay (SF Bay) is the largest estuary on the west coast
of North America. It is designated as a Western Hemisphere Shorebird
Reserve Network site of hemispheric importance because it is visited by
over half a million wintering and migratory shorebirds each year
(Morrison, 1981; Myers et al., 1987; Page, Stenzel, & Kjelmyr, 1999).
Western sandpipers are one of the most abundant shorebird species in SF
Bay, foraging on tidal mudflats throughout the non-breeding season (Page
et al., 1999). Western sandpipers exhibit strong foraging site fidelity
and have similar home range sizes in winter and spring in this region
(Warnock & Takekawa, 1996). In addition to serving as an important
wintering area for western sandpipers, SF Bay is a heavily utilized
migratory stopover for sandpipers wintering at more southern latitudes
(Bishop, Warnock, & Takekawa, 2006; Butler, Delgado, De La Cueva,
Pulido, & Sandercock, 1996; Iverson, Warnock, Butler, Bishop, &
Warnock, 1996). The influx of migratory western sandpipers in April
leads to increased population densities and rapid depletion of
invertebrate prey that could increase competition (Rowan, 2012). Our
study was conducted on the Dumbarton shoal, an intertidal mudflat on the
southwestern side of SF Bay. This mudflat supports a high biomass of
benthic invertebrates and biofilm consumed by western sandpipers, but
it’s invertebrate carrying capacity is exceeded in April (Rowan, 2012).