Figure 1. Zones of soft-bottom habitat within the Monterey Bay National Marine Sanctuary. [View Larger]
Waves and currents interact with the sandy seafloor in this relatively shallow zone, creating sand waves and ripples and organizing sediment particles into different group sizes.
The composition of the benthic invertebrate communities living in these sediments has been studied extensively in Monterey Bay. Two communities are organized along a gradient of wave-induced substrate motion:
- The crustacean zone: this shallower zone, characterized by strong water motion and sandy sediments, is occupied by small, mobile, deposit-feeding crustaceans. Few animals live in permanent tubes or burrows here.
- The polychaete zone: characterized by more stable, fine sand with a significant amount of mud, this deeper zone is dominated by polychaete worms living in relatively permanent tubes and burrows. Many other relatively sessile and suspension-feeding groups (e.g., brittle stars, clams, tube anemones, sea pens) are common here.
Benthic fishes are less abundant in the crustacean zone than the polychaete zone. Fish diversity on the sandy seafloor is relatively low compared to adjacent reefs, but some of the most abundant species are important forage for large predatory fishes, seabirds and marine mammals. In the sanctuary, representative species in this habitat are juvenile lingcod, white croaker, plainfin midshipman, staghorn sculpin, sand sole, English sole, speckled sand dab and curlfin sole.
The most common natural disturbance in the sandy seafloor habitat is from wave action. Other disturbances are biotic - such as from the digging activities of feeding southern sea otters, Enhydra lutris.
A bed of Eel grass (Zostera marina) near the commercial wharf and pier in Monterey. It is a perennial flowering plant that is closely related to terrestrial grasses and is commonly found on mud or sand bottoms in protected waters of bays and estuaries in low intertidal and subtidal zones, only rarely being exposed at low tide.
A C-O sole (Pleuronichthys coenosus) crusing around the bottom of Monterey Harbor. This flatfish is "right-sided," and gets its name from the markings on its caudal fin: a crescent shape and a ring, which resemble a letter C and a letter O.
Mapping the seafloor is an ongoing research priority for the sanctuary. In 2004, scientists from the National Oceanic and Atmospheric Administration (NOAA) and the United States Geological Survey (USGS) used side scan sonar and underwater video technology to map the seafloor in previously unexplored areas and to ground truth existing habitat maps. In addition, researchers were able to characterize benthic macroinvertebrates and fish assemblages associated with different habitat types on the continental shelf. For example, sand-wave habitats were often occupied by sand dabs and often contained schools of juvenile rockfishes, while sediment-ripple habitats were commonly occupied by white brittle stars buried within the sediment.
Ecological Effects of the Moss Landing Thermal Discharge
Researchers from Moss Landing Marine Laboratories evaluated the ecosystem impacts of the Moss Landing Power Plant's thermal discharge into the sanctuary. The benthic community inhabiting subtidal sand bottom at one, four and six meters was sampled at the plume and at adjacent control sites. No impact on the shallow sandy seafloor of the thermal plume was detected. This study was the first to complete a baseline characterization of sandy seafloor community structure at this shallow depth in central California.
Distribution and Behavior of Sea Otters Relative to the Moss Landing Thermal Discharge Plume
Southern sea otters, Enhydra lutris nereis, have been observed in the thermal plume generated by the Moss Landing Power Plant. The plume is located over the shallow sandy bottom seaward of the entrance to Moss Landing Harbor. This study, completed by a researcher with UC Santa Cruz, found that sea otters are using the area within and immediately surrounding the thermal plume in a non-random fashion; however, the cause of this pattern could not be determined.
Sea otter behavior, and in particular feeding behavior, was generally similar between plume and non-plume areas. Plume foragers had a slightly higher frequency of occurrence of prey types associated with hard substrates, such as mussels and Cancer crab species, while non-plume foragers fed more commonly on soft-bottom species, including clams and fat innkeeper worms.
Identification of Critical Inshore Spawning Grounds for Market Squid
The market squid, Loligo opalescens, supports the largest commercial marine fishery in California, both in terms of quantity landed and dollars paid ex-vessel. This monitoring project, completed by researchers with the Marine Biological Laboratory and Woods Hole Oceanographic Institution, used acoustic sampling technology to find and measure the areas of greatest concentration of the market squid's benthic egg masses. This method, after further refinement, may allow quantification of the squid's annual reproductive output in Monterey Bay and identification of critical spawning habitat for this species.
The City and County of San Francisco own and operate a pollution control plant that discharges treated municipal wastewater and storm water into the Pacific Ocean about six kilometers (3.75 miles) offshore of Ocean Beach. Approximately 50 stations are sampled annually for sediment quality and benthic infaunal community analysis. Ten of these sampling stations fall in the sanctuary.
No change in sediment grain size has been detected at the outfall. Benthic infaunal community composition represents an assortment of native species common in central California. Sediment grain size appears to be the most important factor structuring infaunal communities. The relative abundance of crustaceans on the shallow sand bars is consistent with the pattern of wave disturbance zonation described in prior studies in Monterey Bay. Wave action along the nearshore (20 meters) route of the cable caused cable strumming and consequent incision of rocky siltstone outcrops. In addition, frayed cable at the 43-meter station probably resulted from seafloor abrasion during high-energy events. Intense trawling activity in the area is another possible cause of damage to the cable.