Wednesday, Oct 01, 2014

Jerry Smith Reports >>

Pescadero Marsh Natural Preserve Salinity,
Tidewater Goby and Red-legged Frog Monitoring 1995-1996

Jerry J. Smith
Dawn K. Reis

Department of Biological Sciences
San Jose State University
San Jose, CA 95192
June 25, 1997

A Report Prepared for the California Department of Parks and Recreation 3790-301-722(7)

INTRODUCTION

The Pescadero Marsh, a 320 acre coastal wetland, includes an estuary/seasonal lagoon at the
confluence of Pescadero and Butano creeks, fresh and brackish water marshes, brackish water
ponds, and riparian areas along the streams. Modifications to the marsh complex due to past
human land uses include restricted water flow, due to a levee system throughout the marsh, and
reduced tidal prism, due to both the levees and sedimentation from land uses in the upper
watershed. Although it no longer functions as it did 150 years ago, Pescadero Marsh supports a high
diversity of animal and plant life, and is a refuge for a number of sensitive species (Smith 1990;
Jennings and Hayes 1990). Federally endangered tidewater gobies (Eucyclogobius newberryi)
use the lagoon and marsh habitats. Federally threatened California red-legged frogs (Rana
aurora draytonii) and federally endangered San Francisco garter snakes (Ihamnophis sirtalis
tetrataenia) use the fresher portions of the complex. Low salinity habitat (less than 4 parts per
thousand (PPT)) is required for California red-legged frog egg survival (Jennings and Hayes
1990), and relatively low salinity habitat (less than 7.5 PPT) is required for larval survival
(Jennings, pers. comm.). Tidewater gobies tolerate fresh or saltwater habitats, but avoid
strongly tidal areas when the sandbar is open (Smith 1990). North Marsh and Butano Marsh,
partially leveed wetlands in the northern and southern portions of the lagoon/marsh complex
(Figure 1), provide extensive habitat for both California red-legged frog and for tidewater goby,
but the quality of that habitat depends upon the timing of sandbar formation, water surface
elevations, the amount of flooded marshland and upon water salinity.

Portions of the Pescadero Marsh Restoration Project were implemented in the summer and fall
of 1993. One modification involved removal of portions of the levees separating North, Middle
and East Butano marshes (near water quality stations D3 and D6, Figure 1); previously an
opening had been made in the levee separating the eastern end of East Butano Marsh from
Butano Creek. These modifications allow Butano Creek flood waters to flow through the Butano
Marshes. They also allow tidal water, or water impounded by a closed sandbar, to move much
more easily throughout the Butano Marsh complex.

The second major restoration effort involved modifying the northern portion of the marsh
complex. A small culvert through the levee separating North Marsh and North Pond from
Pescadero Creek was replaced with 6 large culverts and two small culverts (water sampling
station B). In addition, a:levee that formerly separated North Pond was removed (north of water
sampling site C2).

Finally, a low levee (designed for + 5.5 feet) was added to separate North
Marsh from the channel leading to North Pond. Two large, normally-closed, culverts were
installed in the low levee (between water sampling sites C3 and Fl and between Cl and El).
One result of these modifications was to restore tidal action to North Pond, and the channel
leading to it, when the 6 large culverts are open; the culverts were to be left open except for
brief periods immediately following sandbar closure. The second intended result to was to
isolate North Marsh as a fresh-water to mildly brackish-water habitat for red-legged frogs and
San Francisco garter snakes. North Marsh would also serve as a potential refuge for tidewater
goby in case yellowfin goby (Acanthogobius flavimanus) became established in the saltier
portions of the marsh complex. The only open connection between North Marsh and the
remainder of the lagoon/marsh complex was to be a permanently open 12 inch culvert at +4.5
feet extending through the levee between water sampling sites Band El.

This report describes the results of water level and salinity sampling in 1994, 1995 and 1996 and
sampling for adult and larval frogs and tidewater gobies in 1995 and 1996. The monitoring was
designed to evaluate the functioning of the estuary/marsh complex in response to the restoration
actions and to propose additional management actions to maintain water levels, salinities and
other habitat conditions suitable for red-legged frogs, San Francisco garter snakes and tidewater
gobies.

Check out Part 1 of this report here in pdf format.

Check out Part 2 of this report here in pdf format.

The Effects of Sandbar Formation and Inflows on
Aquatic Habitat and Fish utilization in Pescadero,
San Gregorio, Waddell and Pomponio Creek.
Estuary/Lagoon Systems, 1985-1989

Jerry J. Smith

Department of Biological sciences
San Jose state University
San Jose, CA 95192
21 December 1990

Report Prepared Under Inter-agency Agreement 84-04-324
Between Trustees for California State University and the California Department of Parks and Recreation.

Abstract

The fish habitat quality of the small lagoon/estuaries at
Pescadero, San Gregorio and Waddell creeks was generally good,
but limited in extent, when the stream mouths were open to full
tidal mixing in winter and early spring. In late spring, summer
and fall, habitat quality depended primarily upon the timing of
sandbar formation and breaching and upon the quantity and quality
of freshwater inflows to the lagoons after sandbar formation.
Adequate inflows to these shallow lagoons after bar formation
resulted in rapid conversion of the lagoons to unstratified fresh
water, relatively cool water temperatures, high dissolved oxygen
levels and high invertebrate abundance. Low inflows to the
lagoons, due to late sandbar formation, drought or upstream
diversions, resulted in delay or failure of salinity
destratification. Saline, stratified lagoons acted as solar
collectors and had higher water temperatures, especially within
the more saline bottom waters. Stratified lagoons also often’ had
low bottom dissolved oxygen levels and reduced invertebrates.
Summer or early fall natural or artificial sandbar breaching
was usually rapidly followed by sandbar re-formation; resulting
in stratified, saline, warm and unproductive lagoons: However,
in the summer of 1989 the sandbar at Pescadero Lagoon
remained open for several months after artificial sandbar
breaching. Although the upstream portions of the estuary were
shallow, stratified and warm, the well-mixed main embayment was
cool and well-oxygenated. Fish populations utilizing the lagoons consisted;
of freshwater, estuarine and saltwater species. The number of
species increased with lagoon size. The highest diversity
occurred at Pescadero Lagoon in early summer of 1986, when many
juvenile saltwater fishes were present in the open lagoon. After
lagoon conversion towards freshwater conditions, following
sandbar closure, many saltwater species declined or disappeared.
Many species also declined or disappeared in the warm, saline,
unproductive lagoons associated with the drought years.
Juvenile steelhead survival and growth was excellent when the
lagoons were open to full tidal mixing and when the closed
lagoons were converted to fresh water. Growth was poor during
long, stratified transition periods between sandbar closure and
conversion of the lagoons to fresh water. Survival was poor
during periods of prolonged warm, stratified conditions. The
high numbers and/or large sizes of steelhead reared in the
lagoons during years of freshwater conversion demonstrate that
these lagoons can potentially contribute the majority of
steelhead smolts produced in these small coastal watersheds.

Managing these lagoons for production of juvenile steelhead requires:

1) prevention of artificial summer sandbar breaching; and
2) insuring sufficient inflows after sandbar formation to rapidly
convert stratified, saline lagoons to fresh water.

Introduction

The annual summer drought in California results in sharp
declines in stream flows in coastal streams. For smaller streams,
declining stream flow and summer beach development result in
development of a sandbar which dams the stream mouth to produce
a lagoon. These lagoons may provide warm, deep-water areas for
swimming and boating and habitat for fish and wildlife. The
raised water levels behind the sandbar can also flood adjacent
lands, producing valuable wetlands and/or threatening
agricultural or urban developments. Despite recent interest in
wetlands and estuaries, relatively few studies have been done on
California central coast lagoons, although they were long ago
shown to be important for steelhead (Oncoryhnchus rnykiss) and
salmon (0. kisutgb) (Shapovalov and Taft 1954). Lagoons and
their associated wetlands have been actively managed by diversion
of inflow waters for agricultural and municipal uses, diking of.
surrounding land, and artificial breaching of the sandbar for
flood, odor, and insect control. This report summarizes the
results of studies undertaken for the California Department of
Parks and Recreation to determine habitat dynamics and fish
utilization ‘in four small coastal lagoons. The goals of the
studies were: A) to provide information to guide the restoration
and management of wetlands and the estuary/lagoon at Pescadero
Marsh Natural Preserve (NP) r and B) to provide information on
sandbar management and lagoon inflows necessary to maintain
aquatic habitat in the face of upstream diversions and drought
conditions.

Check out Part 1 of the full report in pdf format here.

Check out Part 2 of the full report in pdf format here.

 

Help to Restore the Marsh!




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*ESTIMATES: STEEHEAD REARING*
*click to view

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Heron and other predatory birds were seen feeding on the shorelines.

November 25, 2010

January 3, 2008

KGO news report 2010

KGO news report 2003