The continental shelf is characterized by gently dipping seafloor and forms a relatively flat surface (hence the name, "shelf") compared to the steeper and deeper continental slope. It extends nearly 50 kilometers (35 miles) in the gulf region - wider than in areas to the north and south of the sanctuary - and provides an especially large, relatively shallow habitat for foraging coastal and oceanic seabirds, marine mammals and fishes.
The shelf seafloor in the sanctuary consists mostly of sediment (sand, silt and minor amounts of broken shell material) along with areas of rock outcrops and coarse gravel. The most notable seafloor features are the large underwater sand dunes between the Farallon Islands and Point Reyes and the approximately 18-kilometer-long rocky ridge that includes Hurst Shoal, Farallon Islands, Fanny Shoals, Rittenberg Bank and Noonday Rock.
Benthic faunal communities differ according to these various habitat types.
Species that live in sediment-dominated areas of the continental shelf have adapted to the continuous shifting of sediments by ocean currents. For example, clams live permanently buried in the sand, extending their siphons to the surface to filter water in order to feed.
Dense fields of sea pens (Order Pennatulacea) are also found on the silty shelf. Each sea pen is a colony of polyps (small anemone-like individuals) that is anchored to the soft-sediment bottom and visually resembles old-fashioned quill pens.
Dungeness crabs, Cancer magister, one of the most economically important fisheries in the area, are concentrated on sandy and silty seafloor areas. They are opportunistic feeders, consuming clams, fishes, isopods and amphipods.
Areas of variable relief and rocky substrate on the shelf are often associated with high species diversity. The complex physical structure created by rocky, hard-bottom areas within the outer continental shelf region provides habitats for a very different suite of organisms than those found in soft-bottom areas: rockfishes, deep-water corals, sponges, anemones and others. This abundance of benthic life associated with hard substrates attracts pelagic predators, including seabirds and marine mammals, which hunt for fish and invertebrate prey along the bottom and in the waters above the seafloor.
Conservation and management issues affecting sanctuary resources on the shelf include seabed disturbance (e.g., trawl disturbance and dumping of dredge spoils), marine debris, the presence of radioactive waste containers from the mid 1900s and accumulation of contaminants in the sediment and food web. In order to make decisions about these and other potential issues, scientists need more information, such as characterization of the sanctuary ecosystem, data on baseline conditions of the benthic community for future damage assessment, and knowledge of cultural resources and potential sunken polluters.
MonitoringThe following list includes some of the projects underway in the sanctuary. Please click on the Projects tab at the top of this page for more information.
Seafloor Mapping in Monterey Bay, Cordell Bank and Gulf of the Farallones National Marine Sanctuaries
In April 2004, scientists from the National Oceanic and Atmospheric Administration (NOAA) and the U.S. Geological Survey conducted a 21-day research cruise aboard the NOAA Ship McArthur II. This study was one of the most extensive efforts to date to document the seafloor of the continental shelf in the three central California national marine sanctuaries.
Researchers mapped approximately 480 kilometers of the seafloor with side scan sonar and collected underwater video over approximately 200 kilometers to characterize the habitat types and diversity and the benthic assemblages of sea life on the continental shelf; including a first look at many areas. Results from this seafloor mapping study provide valuable characterization of sanctuary biology and geology that is useful as a foundation for management of the national marine sanctuaries.