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First
Annual Meeting
April 14, 2003
Hubbs
Sea World Conference Room
San Diego CA
Abstracts
Emerging
Issues in San Francisco Estuary Tidal Wetlands Restoration
Authors:
Brown, L.R., U.S. Geological Survey, Placer Hall, 6000 J Street,
Sacramento, CA 95819-6129, 96-278-3098, lrbrown@usgs.gov
Abstract:
Tidal wetland restoration is a key component of the Ecosystem Restoration
Program (ERP) of the CALFED Bay-Delta Program (CALFED). One of the ERP’s
many goals is to restore from 12,000 to 20,000 hectares of freshwater
tidal marsh habitat in the Sacramento-San Joaquin Delta (Delta). This
area represents approximately 30 to 50 percent of the freshwater tidal
wetlands lost from the Delta since 1900. The purpose of this and other
habitat restoration efforts is to benefit populations of plants and animals,
with an emphasis on native species. The ERP assumes that the restoration
of tidal marsh habitat will re-establish ecosystem processes that will
support increased populations of native species and commercially valuable
introduced species. Literature reviews and results from recent and ongoing
research indicate that the expected benefits of habitat restoration may
not be achieved in all cases because of emerging issues ranging from the
effects of invasive species to conflicts with other CALFED program areas,
such as water quality. The purpose of this presentation is to review some
of these emerging issues and identify areas of uncertainty that can be
addressed through scientific research.
Value
of coastal wetland habitats to fish feeding and growth: a bioenergetics
evaluation.
Authors:
Madon, S. P. Pacific Estuarine Research Laboratory, San Diego State University,
San Diego, CA 92182-1870. smadon@perl.sdsu.edu
PH: 619 594 5809
Abstract: Bioenergetics
models explicitly link fish energetic processes to abiotic and biotic
environmental factors, and are thus valuable for assessing the effects
of estuarine processes and disturbances on fish growth. I developed and
used bioenergetics models in conjunction with field and lab studies to:
(1) quantify the value of vegetated salt marsh habitats to feeding and
growth of the California killifish, Fundulus parvipinnis, and to
(2) assess growth dynamics of the California halibut, Paralichthys
californicus, in wetlands impacted by mouth closures. Killifish:
Field estimates of food consumption show that killifish can approximately
double their daily food intake by adding marsh surface foods to their
diet. The model predicts that killifish grow from 20-100% faster if they
add intertidal marsh surfaces to their subtidal feeding areas. Killifish
that hatch early (April-May) experience thermal regimes and periods of
marsh access through ontogeny that vary from those hatched late (August-September).
These differences in thermal and marsh access experiences between early-
and late-hatched fish lead to large differences in growth achieved by
the next spawning season. Early-hatched killifish are 35-50% larger than
late-hatched individuals at 1 yr. age. Halibut: California halibut
use coastal wetlands as juveniles but show ontogenetic differences in
their tolerance for varying abiotic conditions within these systems. Lab
experiments reveal that small juveniles (< 200 mm TL) are largely tolerant
of variable estuarine conditions and can grow over wide ranges of water
temperatures and salinities. Large juvenile halibut (> 200 mm TL) have
reduced tolerances for these abiotic conditions and increased requirements
for larger prey, and thus have to emigrate to open-coast environments
to maintain growth and fitness. Estuarine mouth closure, a common phenomenon
in many coastal wetlands of southern California, likely poses the greatest
risk to large juveniles. Bioenergetic model simulations that incorporate
both abiotic (temperature, salinity) and biotic (prey type, prey size
and prey density) influences reveal that systems such as Tijuana Estuary
which have continuously remained open to tidal flushing since the 1980s,
are better for supporting juvenile halibut growth, than those such as
Los Penasquitos Lagoon where mouth closures occur frequently.
Stable isotope ratios as tracers
of estuarine migration and habitat utilization in larval and juvenile
fishes
Authors: Sharon
Z. Herzka, Department of Ecology, Center for Scientific Investigation
and Higher Education of Ensenada, Baja California, Mexico, PO Box 434844,
San Diego, CA 92143. 011-52-646-175-0500 (W), 011-52-646-175-0545 (F),
sherzka@cicese.mx
Abstract: Many
fish species recruit from coastal areas to estuaries during early life.
Within estuarine systems, the use of specific habitats can be stage-specific.
Tracking the temporal and spatial migration patterns in nursery areas
is important for both management and conservation purposes. The stable
isotope ratios of fish tissues integrate the isotopic composition of their
food sources, which in turn reflect isotopic signatures that can be related
to specific habitat types. Stable isotope ratios can thus be used to infer
patterns of recent habitat utilization. Moreover, a change in habitat
may result in feeding on an isotopically distinct food web, in which case
the isotopic composition of the tissues will gradually shift to reflect
the new foods. Stable isotopes can thus serve as natural tracers to identify
individual fish that have recently undergone a change in habitat. A stable-isotope
based empirical model was developed to estimate the size and time elapsed
following a change in habitat preference for individual fish. Its applicability
to studies of migration among habitats during the early life of estuarine-dependent
marine fishes will be discussed.
Insights gained from top-down food
web investigations in the Sacramento-San Joaquin Delta: Implications for
Restoration
Authors: Lenny
Grimaldo, Environmental Scientist/Fishery Biologist, Department of Water
Resources, 3251 S Street, Sacramento, CA 95816. (916)227-9178 lgrimald@water.ca.gov
Abstract: Our
ability to design restoration projects aimed at improving ecosystem conditions
for native fishes in the Sacramento-San Joaquin Delta has remained limited
by a lack of basic ecology information. We present results from two food
web studies that shed light on the trophic dynamics of native and introduced
fishes residing in flooded islands of the Delta. We analysed the stable
carbon and nitrogen isotope ratios of over 1,300 juvenile fishes and other
food web components. Our results showed that, 1) carbon sources assimilated
by juvenile fishes differed between species occupying inshore and offshore
habitats, and 2) trophic hierarchy among fishes was best described by
functional feeding groups. Diet content analyses corroborated the isotope
data, showing that juvenile fish prey items were largely comprised of
invertebrates found in respective habitats whereas sub-adult fish diets
were more diverse, yet still reflective of local prey resources. We conclude
that restoration should proceed using our increasing understanding about
the relationships between habitats, trophic pathways and fish abundances
as criteria for selecting and prioritizing potential sites. We now recognize
that not all shallow habitat is equal in form or function, and therefore,
expect for fish to vary accordingly based on inherent feeding and rearing
strategies.
Juvenile Steelhead and Coho Salmon
Use of the Albion and Navarro River Estuaries
Authors: Steve
Cannata, Associate Fisheries Biologist, California Department of Fish
and Game, 1487 Sandy Prairie Court, Fortuna, CA 95540. scannata@dfg.ca.gov
Abstract: Studies
of the Navarro and Albion River estuaries were conducted to help determine
their roles as juvenile steelhead (Oncorhynchus mykiss) and coho
salmon (O. kisutch) habitat. These two estuaries are located
less than five miles apart, on the coast of Mendocino County. The study
period for the Navarro River estuary was May 20, 1996 to December 3, 1997.
The study period for the Albion River estuary was May 22 to December 24,
1997. We used a beach seine (100 X 8 ft. with an 8 X 8 ft. bag, mesh sizes
were ½ inch in seine and 3/8 inch in the bag) to sample fish populations
at 9-10 sites in each estuary. Samples were collected from one to four
times per month at each site. Vertical profiles of water temperature,
salinity, conductivity, and dissolved oxygen also were collected at each
site.
We found that juvenile steelhead estuarine utilization patterns vary
dramatically between the Albion and Navarro River estuaries. Steelhead
catches totaled 1,510 from 194 beach seine (catch per unit effort CPUE
= 7.8) samples taken from the Navarro estuary and only five were captured
from 250 beach seine samples (CPUE = 0.02) collected from the Albion estuary.
Juvenile steelhead population estimate for the lower two miles of the
Navarro estuary was made using the adjusted Petersen estimator for recapture
with replacement. The population estimate and 95% confidence interval
(CI) for steelhead < 150 mm FL was 2,921 ± 635. The population
estimate and 95% CI for steelhead ³ 150 mm FL was 5913 ± 2361.
The number of juvenile coho salmon captured from each estuary was similar
49 (CPUE = 0.20) and 47 (CPUE = 0.24) for the Albion and Navarro estuaries
respectively. Coho from the Albion ranged in size from approximately 60
to 109 mm FL, and 91 to 150 mm FL from the Navarro. Several other fish
species contribute to the estuarine ecosystems. Thirty fish species were
observed from the Albion River estuary and 34 fish species were observed
from the Navarro.
A key difference between the two estuaries is that the Albion stays open
to tidal exchange year round while the Navarro estuary typically converts
to a lagoon during the summer. Under lagoon conditions, the Navarro River
estuary exhibits seasonal meromixes, forming strong vertical, temperature
and salinity stratification. Bottom saline water reached 30oC
and was as much as 11oC higher than fresh surface water. Other
factors that differ between the two estuaries include basin size, water
quality parameters, the substrate composition, aquatic vegetation type,
channel morphology, harbor development, and upstream water diversions.
Gualala River Estuary and Lower River Assessment
Authors:
Thomas P. Keegan, Senior Fisheries Scientist, ECORP Consulting,
Inc., 2260 Douglas Blvd., Suite 160, Roseville, CA 95661. TKeegan@ecorpconsulting.com
Abstract:
The Sotoyome Resource Conservation District, in partnership with the Gualala
River Watershed Council, has been awarded a grant by the California Coastal
Conservancy (CCC) to perform a Gualala Estuary and Lower River Study (Study)
and enhancement plan. The Study is intended to determine the carrying
capacity and health of the estuarine ecosystem for salmonids, as well
as to confirm its importance in terms of over-all Gualala River ecosystem
function. This two-year study effort includes monitoring the fish community,
benthic community, and water quality parameters from May 2002 through
October 2003. In addition, a bathymetric survey of the estuary, vegetation
mapping and wetland surveys adjacent to the estuary, hydrological characterization
of the freshwater inflow, sediment input, as well as marine inter-relationships
will also be investigated.
Nine 2-day aquatic
sampling events were conducted in the Gualala River Estuary (Mendocino-Sonoma
County line) at regular intervals (about 3 weeks between sampling events)
between June 16 and November 27 2002. The work effort focused on collecting
juvenile steelhead from three major sections of the Gualala Estuary: Upper
Estuary (confluence of North Fork Gualala River to Highway 1 bridge),
Middle Estuary (Highway 1 bridge to mid-channel island), and Lower
Estuary (mid-channel island to mouth of estuary), and calculating
juvenile steelhead population estimates at the time of each sampling event.
Sampling was conducted using an inflatable boat-deployed bagged beach
seine (100 ft. length, 1/8" mesh). The entire catch was processed,
which included identification, length (nearest millimeter), and weight
measurements (salmonids only to the nearest 0.1 gram) of all fish and
invertebrate species. In addition, all salmonids over 70 mm in length
were freeze-branded with a unique character for each sampling event. All
subsequently recaptured fish were denoted and tabulated by the sampling
event from which they were marked (as indicated by the identifying freeze-brand
mark). Efficacy of the freeze branding technique was also evaluated.
Water temperature,
salinity and dissolved oxygen profiles were conducted at 1-ft intervals
at the deepest location within each of the three major sections of the
estuary. In addition, continuous-recording water temperature units were
deployed to collect surface and bottom temperatures within each of the
three major sections of the estuary. Suitability of rearing habitat within
each major estuarine section was evaluated and suitable habitat quantified
for each sampling event, using published suitability criteria.
Multiple year
classes (age 0+, age 1+, and age 2+ and older) were present during each
sampling event. Age-specific timing of presence and distribution within
the estuary was identified. The suitability of several population estimators
was evaluated. Schnabel and Schumacher population estimates for juvenile
steelhead in the Gualala Estuary over 70 mm in length, based upon multiple
mark and recapture events, ranged between 9,134 and 11,731 fish between
the third and eighth sampling events. The final estimate prior to the
initial estuary breach of the season (sampled on October 24) was 9,200
fish. Post-breach sampling documented the presence of few juvenile steelhead
remaining in the estuary.
Fish
populations of small coastal lagoons in southern California.
Authors:
Camm C. Swift, Presenter. Emeritus, Section of Fishes, Natural
History Museum of Los Angeles County. Mailing address: 346 West Leroy
Avenue, Arcadia, CA 91007-6909, 626-447-5846, camswift@pacbell.net
Abstract:
Coastal lagoons north of Pt. Conception on Vandenberg Air Force Base and
southward on Marine Corps Base Camp Pendleton differ in their fish faunas.
In both areas barrier sand bars close the lagoons for most of the dry
season. Salinities are usually less than 5 ppt. Water temperatures fluctuate
minimally paralleling moderated coastal air temperatures. Lagoon temperatures
in the north are warmer than the ocean whereas in the south water temperatures
are warmer than the ocean in winter and cooler than the ocean in summer.
The numerically dominant fish both north and south is the brackish water
tidewater goby. In the north lagoons and tributary streams are also nurseries
for cool water species, prickly sculpin and starry flounder, and in the
south for warm water species, topsmelt, diamond turbot, and striped mullet.
Young and juvenile staghorn sculpin recruit to lagoons both north and
south. Other common local estuarine species (California killifish, barred
pipefish, shiner surfperch, California halibut, arrow goby, mudsucker,
cheekspot goby, shadow goby, and the non-native yellowfin goby) are rarely
encountered in these non-tidal systems. The El Nino of 1998 provided enough
water for several of these rare species to invade these small systems
for one or a few years.
What
do long-term datasets reveal about the ecology of longfin smelt (Spirinchus
thaleichthys) in the San Francisco Bay estuary?
Authors:
Jonathan A. Rosenfield; Univ. California Davis, Center for Integrated
Watershed Science and Management. jarosenfield@ucdavis.edu.
Randall D. Baxter; California Department of Fish and Game, Central Valley
Bay Delta Branch
Abstract:
Longfin smelt (Spirinchus thaleichthys) are native to the San Francisco
Bay estuary, where they are a species of special management concern. Preliminary
analyses of several long-term (>20 year) data sets indicate that these
fish have seasonal migration patterns that are influenced by annual outflow
conditions. These migrations, and their interaction with annual meteorological
conditions, complicate estimation of population size and management for
preferred conditions. When these intra-estuary migrations are taken into
account, several lines of data reveal a long-term decline in this population.
The long-term data sets also suggest important aspects of longfin smelt
behavior and ecology which may improve the efficacy of future sampling
and management of this important population.
The
prevalence of nonindigenous species in southern California bays and harbors
and their effects on benthic macroinvertebrate communities
Authors:
J.A. Ranasinghe, Presenter, SCCWRP, 7171 Fenwick Lane, Westminster,
CA, 92683, 714-372-9218, anandar@sccwrp.org;
R.G. Velarde, City of San Diego, 4918 N. Harbor Dr., San Diego, CA, 92106,
619-758-2331, rvelarde@sandiego.gov;
D.B. Cadien, CSDLAC, P.O. Box 4998, Whittier, CA, 90745, 310-830-2400,
dcadien@lacsd.org; T.K. Mikel,
ABC Labs, Inc., 29 North Olive St., Ventura, CA, 93001, 805-644-8686,
tkmikel@pacbell.net; H. Lee II,
U.S. EPA, Western Ecology Division, Newport, OR, 97365, 541-867-5001,
lee.henry@epa.gov
Abstract:
We assessed the prevalence of nonindigenous species (NIS) in the benthic
macrofauna of southern California embayments from 123 samples collected
in 1998. NIS were prevalent, occurring in 121 samples. They accounted
for only 4.3% of the species but contributed 27.5% of the abundance. In
another 1999 West Coast study that excluded San Francisco Bay, NIS were
more prevalent in southern California embayments than other areas. NIS
occurred at 100%, 33%, 71% and 68% of sampling sites in southern California,
northern California, Oregon and Washington, respectively. On average,
they contributed 11.9%, 2.8%, 15.1% and 10.8% of the species and 22.7%,
2.6%, 14.1%, and 6.0% of the abundance in each sample. In the southern
California study, there were no apparent differences in NIS abundance,
proportional abundance or composition among ports servicing ocean-going
vessels, small boat marinas, or areas where boats were not moored. NIS
abundance in southern California embayments was positively correlated
with the abundance and richness of other species; there was no negative
impact at this gross level. However, negative effects on specific native
taxa cannot be ruled out without further study. The positive correlations
are likely related to biogenic structures built by the two most abundant
NIS.
Circulation
Impacts of the Cabrillo Shallow Water Habitat, Port of Los Angeles, CA
Authors:
Robert McAdory* and David Mark, Estuarine Engineering Branch,
Coastal and Hydraulics Laboratory, US Army Engineer Research and Development
Center, Vicksburg, MS, and Jane Grandon, US Army Engineer District, Los
Angeles, CA.
*Member of CAERS
Abstract:
Cabrillo Beach is a small, popular beach in the southwest corner of the
Port of Los Angeles in the San Pedro neighborhood, co-located with the
Cabrillo Marine Aquarium. http://www.scc.ca.gov/Wheel/lapage/6_so_la/harbor/cab.html
The beach has
water quality problems, particularly e-coli, due in part to the beach's
isolated location and the resulting poor circulation of water into and
out of its vicinity. The Port constructed the ~ 17 ft deep Cabrillo Shallow
Water Habitat (CSWH) along the breakwater between Cabrillo Beach and Angel's
Gate to provide habitat and feeding area for fish and marine birds. Determining
of the impact of this habitat on water quality at Cabrillo Beach included
use of a numerical model for hydrodynamics in the Los Angeles Harbor.
Model calculations were performed with and with out the CSWH and with
and without a proposed expansion of the CSWH. Results of the calculations
showed that very little change in the circulation of the water in the
vicinity of Cabrillo Beach. The modeling will be discussed and short videos
of the circulation as calculated will be presented.
Breach
II: Understanding variability in tidal marsh restoration processes and
patterns in the San Francisco Bay-Delta
Authors:
Charles Simenstad, School of Aquatic and Fishery Sciences, University
of Washington; Denise Reed, Department of Geology and Geophysics, University
of New Orleans; Philip Williams, Michele Orr, Philip Williams & Associates,
Inc., Stephen Bollens, Romberg Tiburon Center for Environmental
Studies, San Francisco State University; Nadav Nur, Pt. Reyes Bird Observatory
Abstract:
BREACH II research builds on and expands our initial (BREACH I) CALFED
Category III-supported research in the Sacramento-San Joaquin Delta to
address the considerable uncertainty in predicting the outcome and ecological
benefit of restoring shallow-water tidal habitat in three different regions
of the Bay--Delta: the Delta, Suisun Bay, and San Pablo/North Bay. BREACH
II studies address both the feasibility of restoration of shallow water
habitat, and differences inherent to different regions of the Bay-Delta
continuum, as well as evaluate the contribution of that endpoint to the
long-term recovery of fisheries and ecological integrity of the Bay-Delta.
Goals of the BREACH II investigations are to: (1) systematically address
the present status, rates, and patterns of tidal ecosystem restoration
in recognizably different Bay-Delta ecosystems; (2) evaluate factors that
promote rapid restoration of shallow-water habitat versus factors
that have potentially inhibited natural rates and patterns of functional
development; (3) evaluate the contribution of shallow water habitats to
food webs supporting Bay-Delta ecosystems; and (4) assess the overall
outcome of breached-levee restoration in the different Bay-Delta regions
and recommend optimum strategies and spatial distribution of future restoration
initiatives. The focus of our sampling design and synthesis is a BREACH
conceptual model that we have developed for restoration patterns, rates
and processes in the Delta. We are expanding from the initial BREACH studies
in the Delta to Suisun Bay-San Pablo/North Bay our approach of using the
"natural experiment" of the diverse age distribution of selected
breached-levee sites in a 'space-for-time substitution' to predict the
patterns and rates (trajectories) of restoration that would be expected
from levee breaching. As in our initial CALFED studies in the Delta, we
are systematically evaluating the rates and patterns of restoration, and
determining sources of variability, in both naturally and artificially
restored diked wetland sites of a broad spectrum of ages as compared to
the reference sites. Our objectives include: (1) Assess hydrological,
geomorphological, biogeochemical and ecological indicators at diverse,
differently-aged sites of formerly diked wetlands that have reverted to
tidal inundation; (2) compare indices of fish and wildlife habitat quality
of these naturally breached-dike sites to existing mitigation and restoration
sites that were purposefully constructed by dike breaching or comparable
restoration actions; and, (3) using the same indicators, compare the status
of these restored wetlands to wetland function at natural reference marsh
sites. This approach is integrated into a developing conceptual model
that relates transitional phases in the development of shallow water habitat
to the support of fish and wildlife. Our products are intended to provide
critical information necessary to predict whether breached-dike restoration
strategies proposed under CALFED would provide natural wetland functions
to support tidal (shallow-water) aquatic habitat for other aquatic and
terrestrial species of concern and rehabilitate a robust Bay-Delta food
web.
Successes
and shortcomings in habitat restoration: a case study of Cerithidea
californica (Gastropoda) colonization and fitness in a created tidal
mudflat
Authors:
Anna R. Armitage, Peggy Fong, UCLA Dept. of Organismic Biology,
Ecology and Evolution, 621 Charles E. Young Dr. S., Los Angeles, CA 90095-1606.
armitag9@ucla.edu
Abstract:
Salt marsh restoration often involves re-establishing tidal flow and vascular
plant transplantation, and faunal colonization is expected to follow.
A four-year study of the colonization and fitness of a common gastropod,
Cerithidea californica, in a created southern California tidal
mudflat revealed some successes and shortcomings in the development of
the created site. Snail densities in the created site were lower than
in an adjacent natural site throughout the study period, although the
differences between sites decreased in magnitude by the end of the study,
suggesting a recovery trajectory. Snails were not evenly distributed throughout
the created site due to habitat quality and limited snail dispersal ability.
Principal components analysis suggested that environmental factors explained
some of the initial variability in adult (48%) density but little of the
variability in juvenile density. After four years, up to 79% of the variation
in adult snail density was explained by distance from the natural/created
site transition zone. Juvenile snails were not related to distance from
the transition zone, possibly due to their greater dispersal ability.
Snails that did colonize the created site displayed similar fitness as
snails in the natural site, as growth rates, mortality rates, and reproductive
output were similar between sites. Thus, although C. californica
fitness was similar between sites, environmental factors and dispersal
limitations restricted snail colonization and suggest that the habitat
value of the created site is not yet equivalent to that of the natural
site.
Estuarine
macroalgae take up nutrients from sediments leading to increased growth
and tissue nutrient content
Authors:
K. Kamer1, R. L. Kennison2, P. Fong2,
and K. Schiff1, kristak@sccwrp.org,
1Southern California Coastal Water Research Project, Westminster,
CA, 92683, 2Department
of Organismic Biology, Ecology and Evolution, University of California,
Los Angeles, Los Angeles, CA, 90095
Abstract:
Bloom-forming macroalgae such as Enteromorpha intestinalis take
up nutrients from the water column as well as those fluxing from sediments.
We hypothesized that the importance of these sources to E. intestinalis
varies along a nutrient resource gradient within an estuary. We tested
this by constructing experimental units using water and sediments collected
from 3 sites in Upper Newport Bay estuary, California, US, that varied
greatly in water column nutrient concentrations. For each site there were
three treatments: sediments + water; sediments + water + algae (E.
intestinalis); inert sand + water + algae. Water in units was exchanged
weekly simulating low turnover characteristic of poorly flushed estuaries.
The importance of the water column versus sediments as sources of nutrients
to E. intestinalis varied with the magnitude of the different sources.
When initial water column DIN and SRP levels were low, estuarine sediments
increased E. intestinalis growth and tissue nutrient content. In
units from sites where initial water column DIN was high, there was no
effect of estuarine sediments on algal growth or tissue N content. However,
salinity was low in these units and may have inhibited algal growth. Water
column DIN was depleted each week of the experiment. Thus, the water column
was a primary source of nutrients to the algae when water column nutrient
supply was high, and the sediments supplemented nutrient supply to the
algae when water column nutrient sources were low. Depletion of water
column DIN in sediment + water units indicated that the sediments acted
as a nutrient sink in the absence of algae in this experiment. Previous
studies have demonstrated the potential importance of sediments as a source
of nutrients to primary producers; our data provide direct experimental
evidence that macroalgae utilize and ecologically benefit from nutrients
stored in estuarine sediments.
Using
macroalgae as an indicator of terrestrial influences in southern California
estuaries.
Authors:
Risa A. Cohen and Peggy Fong, University of California, Los Angeles
Abstract:
The relative importance of terrestrial and marine sources of nutrients
to estuaries has long been debated. In northern California it has been
shown that ocean sources may dominate, but in southern California the
majority of studies have focused on nutrient inputs from watersheds. Our
objective was to use Enteromorpha spp., opportunistic macroalgae
that respond rapidly to changes in salinity and nutrient availability,
to obtain integrated measures of freshwater input, nutrient supply and
nutrient source in estuarine areas. We outplanted cultured algae in the
field along salinity gradients in three southern California estuaries,
Newport Bay, Mugu Lagoon and Carpinteria Salt Marsh for 24 hours. Algal
tissue was then analyzed for potassium content (K+) to measure
osmoregulatory changes, nitrogen content (total N, NO3-
and NH4+) to examine changes in nutrient supply
and d 15N
to assess nutrient sources. A total of ten stations along the salinity
gradient at each estuary were sampled and replication was 5-fold at each
station. Experimental cages were anchored in the same locations for assays
performed during both wet and dry seasons. Physical measurements of environmental
parameters (salinity, water nutrient concentration) were also taken at
each station. Although salinity correlated well with tissue K+
content for site, season, and estuary, there was little agreement between
water N concentration and both tissue N and d 15N.
These findings from the bioassay suggest that the rivers may not be the
main sources of nutrients to these estuaries, even during the wet season.
Therefore, the amount of nutrients from groundwater and other unidentified
sources must also be determined to ensure successful management plans.
Nutrient
and Macroalgal Dynamics in 5 Southern California Estuaries
Authors:
Rachel L. Kennision1, Krista Kamer2, and
Peggy Fong1 rlk@ucla.edu,
1Department of Organismic Biology, Ecology and Evolution, University
of California, Los Angeles, Los Angeles, CA, 90095, 2Southern
California Coastal Water Research Project, Westminster, CA, 92683
Abstract:
We investigated seasonal nutrient dynamics and macroalgal community responses
in 5 estuaries in southern California that have a wide range of distinct
characteristics. Tijuana River National Estuarine Research Reserve, Los
Penasquitos Lagoon, Newport Backbay State Ecological Reserve, Mugu Lagoon
and Carpinteria Salt Marsh Reserve have been sampled seasonally since
December 2001. Three transects were permanently established in each estuary:
at the mouth, at the primary freshwater input, and midway between the
two. Along each transect we sampled water column salinity, organic and
inorganic N and P and dissolved oxygen concentrations; sediment grain
size, N and P concentrations, organic content and redox potential; algal
species percent cover, biomass, and tissue N and P content. By gathering
data along freshwater gradients within estuaries, we can make within-estuary
comparisons of nutrient availability and algal biomass as well as between-estuary
comparisons. Preliminary results show seasonal patterns for algal biomass
with blooms in December and June. For all estuaries combined, water column
NO3 was higher in December than in June, and there was no significant
relationship between water column NO3 and total algal biomass,
suggesting that water column NO3 is not an accurate estimation
of available nutrients in the system. These data will be used to determine
relationships between nutrient inputs, nutrient availability, macroalgal
abundance and dissolved oxygen availability; one of the overall goals
of this project is to provide data that will assist in development of
nutrient criteria for estuaries by local and regional water quality agencies.
The
North versus The South: are nutrient dynamics fundamentally different?
Authors:
Peggy Fong, Katharyn E. Boyer, and Anna R. Armitage
Abstract:
In general, estuaries in southern CA are smaller, receive less freshwater
during a shorter wet season, are less tidally influenced, and have much
more developed watersheds than their counterparts to the north. As sources,
sinks, and processing of nutrients are all influenced by these factors,
it is likely that estuaries in these two regions have fundamentally different
nutrient dynamics. Two lines of evidence support this hypothesis. First,
15N content of algae collected in summer (2000) from estuaries
spanning the coast from Tijuana Estuary to Bodega Bay suggests that nutrient
sources in northern CA are dominated by upwelled water that advects into
the estuary. Within northern estuaries, tissue N content of algae decreases
from the ocean to the river as the tidal water is stripped of nutrients.
In contrast, in southern CA both 15N and tissue N content in
algae was highest where the river enters the estuary, decreasing as nutrients
are removed while water moves down-estuary. Very high 15N suggests
that recycled and groundwater nutrient sources dominate. The second line
of evidence, from nutrient limitation experiments, suggests that in summer,
both N and P limit algae from estuaries in southern CA while neither nutrient
limits algal growth in northern CA. Thus, in summer, recycling and groundwater
supplies are not sufficient to meet the nutrient demands of algae in southern
CA while upwelling and advection are sufficient in northern CA. This may
be related to many factors, including differences in the rates of supply
from these sources as well as differences in algal growth and biomass
accumulation between these regions.
Historical
Changes In Mission Bay And Observed Changes In Benthos
Authors: Jeffrey
A. Crooks, Tijuana River National Estuarine Research Reserve, Imperial
Beach, CA, Deborah M. Dexter Dept. of Biology, San Diego State University,
San Diego, CA.
Abstract:
Mission Bay has undergone dramatic changes over the last 150 years. Originally
described as a relatively deep water lagoon fringed by extensive marshlands,
the bay underwent its first major anthropogenic transformation with the
diversion of the San Diego River into the eastern end of the bay in the
mid-1800's. This caused much of the Mission Bay to fill with sediments.
In the mid-1900's, the river was again diverted, this time bypassing Mission
Bay and discharging into the Pacific Ocean via a flood control channel.
The bay itself was also dramatically modified, with extensive dredging
and filling leaving little natural habitat remaining. This massive habitat
alteration, coupled with organic enrichment from urban runoff, overharvesting,
and exotic species invasions, have greatly altered biotic assemblages
in the bay. The cumulative effects of these stresses can be tracked by
examining shifts in bivalve communities over time, although it is difficult
to assess the relative magnitude of each. Experimental manipulations,
however, can provide some insight into factors causing alterations in
benthic community structure. These suggest that the invasion of an exotic
mussel, Musculista senhousia, has been important as an agent of change
in the bay.
Water
Circulation And Transport In Mission Bay
Authors:
J. L. Largier, Scripps Institution of Oceanography, University of California
San Diego, La Jolla, CA 92093-0209; jlargier@ucsd.edu, M. L. Carter, Scripps
Institution of Oceanography, UCSD, D. Sutton, San Diego Supercomputer
Center, UCSD, M. Roughan, Scripps Institution of Oceanography, UCSD, J.
Helly, San Diego Supercomputer Center, UCSD, P. Atjai, Marine and Environmental
Studies Program, University of San Diego, L. Clarke, Scripps Institution
of Oceanography, UCSD
Abstract: Mission
Bay is characterized by long dry summers with low or zero inflow of freshwater.
As in many estuaries in California and other mediterranean-climate regions,
the primary exchange of waters between parts of the bay and with the ocean
is due to tidal circulation. Model estimates of residence time match well
with observed temperature gradients in the outer bay and hypersalinity
in the inner bay – ocean water that remains in the shallow bay will
become warmer and also increasingly salty due to an evaporative loss of
freshwater. This tidal mixing of back-bay waters was quantified through
dye release experiments and direct measurements of current velocities
over time. In the outer bay, tidal exchange is active and water types
are similar to that in the open ocean. In winter, significant freshwater
inflow to the inner bay occurs briefly during and immediately following
rain events. This results in high turbidity and low salinity in the bay.
The resultant stratification leads to enhanced flushing so that low-salinity
water exhibits short residence times. However, when the volume of inflow
is small the freshwater may mix into the back-bay waters and remain resident
for weeks or more.
Plankton
Dynamics In Relation To The Physical And Chemical Environment In Mission
Bay
Authors:
Ronald S. Kaufmann, Marine and Environmental Studies Program, University
of San Diego, 5998 Alcala Park, San Diego, CA 92110, kaufmann@sandiego.edu,
Ryan B. Griggs, Marine and Environmental Studies Program, University of
San Diego, John N. Kittinger, Marine and Environmental Studies Program,
University of San Diego, Brandon L. Swope, Marine and Environmental Studies
Program, University of San Diego, B. Chris Stransky, Amec Earth and Environmental,
San Diego, CA, Hiram A. Sarabia, San Diego BayKeeper, San Diego, CA
Abstract:
Mission Bay is a shallow estuary flushed primarily by tidal circulation
and surrounded on three sides by the City of San Diego. Three freshwater
creeks and over 100 storm drains empty into the bay, carrying chemicals
that have the potential to impact plankton communities both positively
and negatively. A time series study was initiated in July 2001 to examine
temporal and spatial variation in the concentrations of nutrients (nitrate,
phosphate, silica) and the dynamics of plankton communities within Mission
Bay. Nutrient concentrations in the bay have been relatively low, with
considerable seasonal and spatial variation. During the summer, regions
near the mouth of the bay have displayed consistently lower temperature,
salinity, and concentrations of nutrients compared to more poorly flushed
sites in the eastern portion of the bay. Seasonal variation in phytoplankton
populations has followed a classical paradigm, with greater abundances
of diatoms in the spring and dinoflagellates in the summer. Independent
of
abundance, phytoplankton diversity has been correlated inversely with
concentrations of nutrients, particularly phosphate. The data collected
thus far suggest that variation in plankton communities within Mission
Bay may be
influenced by spatial variation in nutrient availability and hydrographic
conditions, both of which are related to water circulation.
A
Fourteen-Year Assessment Of Fishes In Mission Bay Surveyed With Experimental
Gillnets.
Authors: M.A.
Shane, Presenter, Hubbs-Sea World Research Institute, 2595 Ingraham Street,
San Diego, CA, 92109, 619-226-3946 (W), 619-226-3944 (F), mshane@hswri.org;
M.A. Drawbridge, Hubbs-Sea World Research Institute, 2595 Ingraham Street,
San Diego, CA, 92109, 619-226-3870 (W), 619-226-3944 (F), mdrawbr@hswri.org.
Abstract: Since
1988 the fish populations in Mission Bay San Diego, California have been
sampled with multiple-mesh gillnets. During this 14-year sampling period
data was analyzed from 550 hours of effort (324 overnight sets) in Mission
Bay. Trends in CPUE were examined for 4 fish categories (sport fishery,
elasmobranches, embiotocids, and sciaenids). The CPUE for most species
remained somewhat constant during this time period. However, CPUE for
leopard shark, gray smoothound, and yellowfin croaker have consistently
increased throughout the 14-year period.
Wetland
Research In Mission Bay.
Authors:
Drew M. Talley, Department of Evolution and Ecology, University of California
Davis, Lisa A. Levin, Scripps Institution of Oceanography, University
of California San Diego
Abstract:
The wetlands located in the back of Mission Bay include salt marsh, tidal
flat and sea-grass beds. Much of this is a remnant of a once-extensive
wetland – but there are also 7 acres of recently restored salt marsh
habitat. These areas form a reserve jointly owned by UC San Diego and
the City of San Diego and this has been the site of much research during
the past 3 decades. Investigations have focused on marsh plants, algae,
invertebrates, fishes and how they interact with sediments and each other.
Research themes have included effects of invasive species, recovery of
restored marsh ecosystems, trophic interactions, diversity, habitat linkages,
and larval dispersal. This presentation will highlight the important role
played by Mission Bay in developing understanding of wetland ecology along
the Pacific coast.
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