The two estuarine systems composing San Francisco Bay have distinct zooplankton communities and seasonal population dynamics. In the South Bay, a shallow lagoon-type estuary, the copepods
Acartia spp. and
Oithona davisae dominate. As in estuaries along the northeast coast of the U.S., there is a seasonal succession involving the replacement of a cold-season
Acartia species (
A. clausi s.l.) by a warm-season species (
A. californiensis), presumably resulting from the differential production and hatching of dormant eggs.
Oithona davisae is most abundant during the fall. Copepods of northern San Francisco Bay, a partially-mixed estuary of the Sacramento-San Joaquin Rivers, organize into discrete populations according to salinity distribution:
Sinocalanus doerrii (a recently introduced species) at the riverine boundary, Eurytemora affinis in the oligohaline mixing zone,
Acartia spp. in polyhaline waters (18–30\%), and neritic species (e.g.,
Paracalanus parvus) at the seaward boundary.
Sinocalanus doerrii and
E. affinis are present year-round.
Acartia clausi s.l. is present almost year-round in the northern reach, and
A. californiensis occurs only briefly there in summer-fall. The difference in succession of
Acartia species between the two regions of San Francisco Bay may reflect differences in the seasonal temperature cycle (the South Bay warms earlier), and the perennial transport of
A. clausi s.l. into the northern reach from the seaward boundary by nontidal advection.
Large numbers (>10
6 m
–3) of net microzooplankton (>64 µm), in cluding the rotifer
Synchaeta sp. and three species of tintinnid ciliates, occur in the South Bay and in the seaward northern reach where salinity exceeds about 5–10

Maximum densities of these microzooplankton are associated with high concentrations of chlorophyll. Meroplankton (of gastropods, bivalves, barnacles, and polychaetes) constitute a large fraction of zooplankton biomass in the South Bay during winter-spring and in the northern reach during summer-fall.
Seasonal cycles of zooplankton abundance appear to be constant among years (1978–1981) and are similar in the deep (>10 m) channels and lateral shoals (<3 m).="" the="" seasonal="" zooplankton="" community="" dynamics="" are="" discussed="" in="" relation="" to:="" (1)="" river="" discharge="" which="" alters="" salinity="" distribution="" and="" residence="" time="" of="" plankton;="" (2)="" temperature="" which="" induces="" production="" and="" hatching="" of="" dormant="" copepod="" eggs;="" (3)="" coastal="" hydrography="" which="" brings="" neritic="" copepods="" of="" different="" zoogeographic="" affinities="" into="" the="" bay;="" and="" (4)="" seasonal="" cycles="" of="">3>
Keywords San Francisco Bay - zooplankton densities - seasonal cycles - estuarine circulation - spatial distribution - estuarine ecology