Figure 1. Submarine canyons within the Monterey Bay National Marine Sanctuary. [View Larger]
Monterey Canyon, in the center of Monterey Bay, is the largest submarine canyon along the coast of North America. Similar in size to the Grand Canyon in Arizona, it is 470 kilometers (292 miles) long and approximately 12 kilometers at its widest point, with a maximum rim to floor relief of 1,700 meters (5,577 feet). The Monterey Canyon system includes two additional canyon heads, Soquel Canyon and Carmel Canyon, which flank Monterey Canyon to the north and south, respectively.
Numerous smaller canyons, including Pioneer, Ascension, Año Nuevo, Cabrillo, Sur, Partington, Lucia, Villa and La Cruz, cut into the continental shelf and slope of the sanctuary. The walls and floors of submarine canyons cover approximately 2,175 square kilometers, or 16 percent, of the sanctuary seafloor. The great majority of canyon habitat is soft-bottom; a much smaller portion is hard-bottom.
Much of the sediment carried by longshore currents ends up in the axes of active submarine canyons. It is estimated that approximately 500,000 cubic meters (17,657,333 cubic feet) of sand as well as large volumes of finer-grained material descend into Monterey Canyon each year.
Lucia Canyon, the major submarine canyon in the southern portion of the sanctuary, and its many heads act as funnels for the rapid transport of detritus eroded from the Santa Lucia Mountains to the deep abyssal plain. Submarine landslides from canyon walls also deposit sediments on the canyon floor. The organic material associated with sediments provides nutrients to deep-sea organisms.
Submarine canyon sediment transport events are thought to be episodic. Potential triggering events include storms, earthquakes, moderate sea and surf conditions, tidal fluctuation, and flooding rivers. The frequency of these events is not well known. Current monitoring efforts, including repeat bathymetric mapping and installation of instruments in the canyons, enable scientists to determine locations where deposition and erosion take place and to quantify the frequency and intensity of sediment transport events.
Most organisms observed in canyons are not unique to canyon systems but are also found at similar depths outsides canyons. However, because submarine canyons extend from shallow waters of the continental shelf to the deep sea and contain a wide range of habitats, they contain an incredible diversity of organisms.
Mobile fishes and invertebrates, such as prickly sharks and krill, have been found to aggregate in canyon heads and along canyon walls. Rocky outcrops along canyon walls are colonized by invertebrates - including feather stars, corals and tunicates - and provide shelter for a variety of rockfishes. Clams and worms burrow into canyon walls. The soft sediments on the canyon floor support a diverse community of invertebrates (e.g., sea pens, sea cucumbers, brittle stars, sea stars) and fishes (e.g., flatfishes, ratfishes, whiptails, grenadiers, sablefish, hake, thornyheads).
Submarine canyons are vulnerable to a variety of human activities because they extend across a range of depths. A comparison of contaminant loads in surface and deep-sea fishes in Monterey Bay found elevated concentrations of persistent organic pollutants, such as PCBs and DDT, in fishes collected from the Monterey Submarine Canyon.
Blackgill rockfish (Sebastes melanostomus) . This photo was taken at a depth of -381.5 meters in Sur Canyon as a part of a deep-sea coral expedition conducted by NMFS aboard the R/V Shimida in December, 2010.
<em>Icichthys lockingtoni</em> (Medusafish; Centrolophidae) collected during mesopelagic fishes survey aboard NOAA SHIP Bell M. Shimada, at shelf off Davenport/Cabrillo Canyon (SESA 5), 0-293 meters, May 2015. Identified by Robert N. Lea (CAS) and Erica J. Burton (MBNMS). Scale: Centimeter ruler.
One important sanctuary management issue relating to submarine canyons revolves around whether to allow installation of communication cables - and if so, where to place them. If routed across submarine canyons, the cables may break as sediments rush down these geologic features. In addition, loops from slack cables are potential entanglement hazards for mobile species, such as marine mammals.
MonitoringThe proximity of canyons to the shore in the sanctuary provides scientists with a unique opportunity to study canyon habitats. Recent monitoring efforts have focused on sediment movement events, mapping of benthic habitats, and determining the abundance and distribution of fishes and invertebrates. These programs tend to use in-situ instrumentation to study sediment movements and manned or remotely operated submersibles to study the distribution and abundance of habitats and organisms.
Gravity Flow Event in Monterey Canyon
Instruments deployed to monitor sediment deposition and movement rates in the Monterey Submarine Canyon detected a large sediment gravity flow event on December 20, 2001. Using information on the deployment and recovery locations of the instruments, Monterey Bay Aquarium Research Institute (MBARI) scientists determined that the event likely started in less than 290 meters of water.
After the event, a sediment core collected from the axis of the canyon at a depth of 1,297 meters contained fresh, greenish chlorophyll-rich organic material - suggesting that the event extended to at least this depth in the canyon. The only trigger identified for this mass movement event appeared to be moderate sea and surf conditions.
In-Situ Measurements of Turbidity Currents in the Monterey Submarine Canyon
In a 2002-2003 study by the United States Geological Survey and the Naval Postgraduate School, the first-ever in-situ measurements of velocity profiles of four turbidity currents were recorded. Maximum along-canyon velocity reached 190 centimeters per second, which is equivalent to 4.25 miles per hour. The turbidity events all occurred in winter. Two of these turbidity currents appeared to be related to storms and another was likely human-induced.
Deep-Water Demersal Fishes and Habitats
Benthic groundfishes (primarily rockfishes in the genus Sebastes) and associated habitats in deep water were assessed in Soquel Submarine Canyon. At least 52 species were identified from 83 transects in 1992-1993 and from 26 transects in 2002-2003. The most abundant taxa observed during this study included poachers, Pacific hagfish, Pacific hake, Dover sole, lingcod, shortspine thornyhead and rockfishes. Distinct habitat guilds of fishes were identified.
Small species were associated with mud and cobble substrates of low relief, whereas larger species of rockfishes were on high-relief structures such as vertical rock walls, ridges and boulder fields. The cover and protection offered by submarine canyons appear to allow pockets of rockfish populations to flourish, in contrast to more exposed areas, where the populations are more easily fished.
Demersal Fishes in Ascension and Partington Canyons
Researchers created habitat maps of the headward parts of Ascension and Partington Canyons using MBARI multibeam bathymetric and backscatter data, processed to five-meter grid resolution, and newly collected side scan sonar data. Seafloor features depicted on the habitat maps were ground truthed, and fish assemblages were surveyed using the Delta submersible along 50-meter depth contours between 200 and 350 meters in Ascension Canyon and at 75, 150, 250 and 350 meters in Partington Canyon.
In Partington Canyon, 3,389 fishes representing 48 species, including 27 rockfish species, were documented from 16 transects conducted in 2003. Rockfishes were dominant at all depths, but species distribution varied with depth. Species diversity was greatest at 250 meters in this region. Habitat associations of dominant fishes were determined in each location.