Monterey Bay National Marine Sanctuary

 


INTERTIDAL SYSTEMS

 

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Surfgrass Beds Recover, Slowly

For over two decades, researchers from the University of California Santa Cruz (UCSC) have sampled an abandoned intertidal sewage outfall to document the ecological recovery there once the discharge was terminated. The most recent survey, completed in June 1998, indicates that the surfgrass beds have finally recovered. The recovery was slow and erratic over the years.

Twenty-five years ago domestic sewage was discharged onto the rocky intertidal on two sides of Monterey Bay. The Pacific Grove outfall at Point Pinos and the Santa Cruz County "Eastcliff" outfall at Soquel (Pleasure) Point both had been in operation for over twenty years. By the early 1970s they discharged daily 1.5 to 3 million gallons of primary treated sewage, respectively, over the wave-swept rocks. These sewage-impacted areas were characterized by classes taught at Stanford University's Hopkins Marine Station (the Point Pinos site) and UCSC (the Soquel site). The effect was similar at both: fishes, crustaceans, limpets, snails, sponges, ascidians, foliose red algae, and surfgrasses were conspicuously absent. In their place was a near-complete cover of diatoms and low-growing coralline algae, interspersed with clumps of sea lettuce, the red alga Prionitis lanceolata, deformed individuals of oar kelp, and large, solitary sea anemones.

Survey Shows Storm Damage Along Sanctuary

In the months of October 1997 and April 1998 scanning airborne laser (LIDAR) surveys were conducted jointly by the USGS, NASA, and NOAA along 1,200 km of the West Coast. The shoreline of the Sanctuary was a focus for one of the survey segments which collects high-resolution topographic information. The primary purpose of the investigation was to document beach and coastal bluff changes as a result of severe El Niño-induced winter storms. Highlights of the LIDAR investigations include documentation of: erosion of the dune/cliff system in southern Monterey Bay of up to 20 m, active bluff retreat along many segments of the Sanctuary shoreline, and dramatic changes in beach width and morphology during the course of the winter. Products from the study will include high-resolution maps depicting coastal topography in October 1997 and April 1998, along with a map showing change between the two survey dates. Further information can be viewed at the web site:

http://aol.wff.nasa.gov/aoltm/projects/beachmap/98results/

Bruce M. Richmond
USGS Coastal and Marine Geology Program

Both outfalls were terminated in the mid-1970s when the sewage was redirected to longer outfalls discharging subtidally. Changes following termination were similar. Ephemeral green algae, especially sea lettuce, were conspicuous within months, to be replaced over the succeeding few years by a variety of foliose red algae and kelps, along with numerous invertebrates previously missing. Other species, such as sponges and ascidians, took much longer to become re-established. Particularly slow in becoming re-established were the visual dominants in these low intertidal areas, surfgrasses (Phyllospadix scouleri and P. torreyi); their come-back was accompanied by the slow decimation of the low-growing coralline algae, the visual dominant of the sewage-impacted areas. From a distance, the areas slowly changed from pink (coralline algae) to green (surfgrasses) as they recovered.

Changes following the termination of the discharge at Soquel Point were documented by teams from UCSC, following sampling done the previous three years. Each spring the teams quantitatively sampled the Soquel Point site. A comparative site 1 km to the northeast at Opal Cliffs that showed little sign of impact from the discharge was also sampled. Quarter-meter-square quadrats were placed randomly within permanent plots at each site and the abundance of species recorded. Abundance of surfgrass was estimated by counting the number of 10x10cm squares in the quarter-meter-square quadrats that contained attached plants (total number of squares in a quadrat=25).

The abundance of surfgrass at Opal Cliffs remained high throughout the twenty-five years of sampling, with over half of the squares containing plants on most sampling dates. Considering the number and length of the surfgrass leaves (most over 30 cm long), this abundance means that there was nearly complete and uniform cover of surfgrass. In contrast, there was no surfgrass at all at the Soquel Point site when the sewage was being discharged. (See figure 1 below.) The first plants were noted in a few quadrats in 1980, four years after the discharge was stopped, but their abundance increased very slowly, mainly as the seedlings spread by clonal growth. The two sites were finally statistically indistinguishable with respect to surfgrass cover in 1997, twenty-one years after the outfall was abandoned, and a similar high abundance was found again in 1998.

Periodic examination of the abandoned outfall site at Point Pinos also revealed a slow recovery of the surfgrass beds, and they now appear nearly as fully recovered as at the Soquel Point site. The re-establishment of surfgrass was probably inhibited at both sites by the dense cover of low-growing coralline algae. At Soquel Point, where quantitative data are available, the abundance of coralline algae has slowly decreased from being present in all the 10 x 10 cm squares in 1976 and before to being present in slightly more than half in 1998, compared to fewer than 10 percent at the Opal Cliffs site. The two species apparently compete for space, and when well established, the coralline algae probably inhibit seedlings from getting established (the seedling may attach to the algal fronds, which then break off, carrying the seedlings with them). However, once securely attached on the underlying rock, the surfgrass rhizomes slowly grow outward, replacing the coralline algae and trapping sand, which further changes the habitat.

Surfgrass beds are rich, productive, and diverse systems. The twisted rhizomes and long leaves provide shelter and habitat for many animals, as does the thick layer of sand trapped by the rhizomes. Storm-detached leaves become litter that is scattered across the ocean floor and down into deeper water, providing resources for numerous detritivores and their predators far beyond the intertidal. It is reassuring that these surfgrass beds, decimated by sewage discharge, have now - after several decades - essentially recovered to their former health.

John Pearse, Eric Danner, Lani Watson, and Chela Zabin
Institute of Marine Sciences,
University of California Santa Cruz

Visitor Impacts at Fitzgerald Marine Reserve

Although the number of persons collecting invertebrates from the intertidal zone at Fitzgerald Marine Reserve has declined 94 percent from 1972 to 1996, annual visitor attendance has more than doubled - to 135,000 - during the same period. (Attendance for 1998 was lower - around 110,000 - because the Reserve's sign was destroyed in a traffic accident.)

Most visitation at the Reserve is concentrated in a 500-m length of rocky intertidal reef. Human impact has changed markedly during the 1972-1996 period, from the gathering of intertidal organisms for food and curios to trampling, rock rolling, and displacement.

To determine the extent of recovery from present-day visitor impact along a 350-m length of reef, two sites were selected at random in the mid-tide zones. One section of each site was cordoned off from public use and posted with signs in April 1994; to control for human impact, the second section at each site was given no special treatment. Five quadrats (one square meter each) in each of the four sections have been monitored on a monthly basis since April 1994.

Observations are made on faunal abundances and floral frequencies and dominances. Populations of some attached vertebrates such as the aggregated sea anemone (Anthopleura elegantissima) appear to be increasing in areas where visitors are excluded and decreasing in heavily-traveled areas. (Further data are in the process of being analyzed.)

Bob Breen
Fitzgerald Marine Reserve



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Last modified on: June 1, 1999