Link to USGS home page Link to USGS home page
Coastal and Marine Geology Program
Coastal & Marine Geology Program > St. Petersburg Coastal and Marine Science Center > Pulley Ridge

Pulley Ridge

Pulley Ridge
Photo Galleries:
Research Methods
Stony Corals
Octocorals
Coralline Algae
Algae
Fish
Project Contact:
Robert B. Halley

Introduction

Pulley Ridge is a 100+ km-long series of N-S trending, drowned, barrier islands on the southwest Florida Shelf approximately 250 km west of Cape Sable, Florida (Fig. 1). The ridge has been mapped using multibeam bathymetry, submarines and remotely operated vehicles, and a variety of geophysical tools. The ridge is a subtle feature about 5 km across with less than 10 m of relief. The shallowest parts of the ridge are about 60 m deep (Fig. 2). Surprisingly at this depth, the southern portion of the ridge hosts an unusual variety of zooxanthellate scleractinian corals, green, red and brown macro algae, and typically shallow-water tropical fishes.

Index map showing Pulley Ridge.
Figure 1. Index map showing location of Pulley Ridge. [larger version]

Index map showing Pulley Ridge. Figure 2. Pulley Ridge was mapped with the USF Kongsberg Simrad EM 3000 high-resolution multibeam sonar, which produces both bathymetry and backscatter. The multibeam mapping efforts were led by David Naar and Brian Donahue of USF, in coordination with Bob Halley and David Twichell of the USGS and by Bret Jarrett, Al Hine, and Stan Locker of USF. Kate Ciembronowicz of both USF and USGS completed the post-processing of several multibeam bathymetry data sets spanning 1999 to 2004. The raw data was processed in Caris and gridded to a 5 m resolution seen here. Black line indicates area believed to contain hermatipic coral cover.[larger version]

The corals Agaricia sp. and Leptoceris cucullata are most abundant, and are deeply pigmented in shades of tan-brown and blue-purple, respectively. These corals form plates up to 50 cm in diameter and account for up to 60% live coral cover at some localities. Less common species include Montastrea cavernosa, Madracis formosa, M. decactis, Porities divaricata, and Oculina tellena. Sponges, calcareous and fleshy algae, octocorals, and sediment occupy surfaces between the corals. Coralline algae appear to be producing as much or more sediment than corals, and coralline algal nodule and cobble zones surround much of the ridge in deeper water (greater than 80 m).

In addition to coralline algae other abundant macro algae include Halimeda tuna, Lobophora variegata, Ventricaria ventricosa, Verdigellas peltata, Dictyota sp., Kallymenia sp., and particularly striking fields of Andaymonene menzeii. The latter algae covers many hectares at densities of tens of individuals per square meter, constructing regions that appear like lettuce fields growing in the dusk at this depth on the sea floor.

The fishes of Pulley ridge comprise a mixture of shallow water and deep species sharing this unusual habitat. More than 60 species have been identified. Commercial species include Epinephelus morio (red grouper) and Mycteroperca phenax (scamp). Typical shallow-water tropical species include Thalassoma bifasciatum (bluehead), Stegastes partitus (bicolor damselfish), Cephalopholis fulva (coney), Lachnolaimus maximus (hogfish), Pomacanthus paru (French angelfish), and Holacanthus tricolor (rock beauty). The deepwater fauna is represented by Chaetodon aya (bank butterflyfish), Sargocentron bullisi (deepwater squirrelfish), Bodianus pulchellus (spotfin hogfish), Pronotogrammus martinicensis (roughtongue bass), and Liopropoma eukrines (wrasse bass). Malacanthus plumieri (sand tilefish) and several other species construct large burrows and mounds that serve as refuge for multiple species. Mounds and pits larger than 1m2 are apparent on side-scan sonar images and have been counted in excess of 200/km2 for parts of the ridge.

The extent of algal cover and abundance of herbivores suggest benthic productivity is moderate to high on parts of the ridge. Such productivity is unusual, if not unique at this depth in the Gulf of Mexico and Caribbean. Several factors help to account for the existence of this community. First, the underlying drowned barrier islands provided both elevated topography and lithified substrate for the hard bottom community that now occupies the southern ridge. Second, the region is dominated by the western edge of the Loop Current that brings relatively clear and warm water to the southern ridge. Third, the ridge is within the thermocline, a water mass that is known to provide nutrients during upwelling to shallow reefs in Florida.

Notwithstanding the positive factors for reef growth listed above, this largely photosynthetic community appears to be thriving on 1-2% (5-30 microEinsteins/1m2/sec) of the available surface light (PAR) and about 5% of the light typically available to shallow-water reefs (500 – 1000 microEinsteins/1m2/sec). The corals generally appear to be healthy, with no obvious evidence of coral bleaching or disease. Although the community is clearly one adapted to low light conditions, the variety and extent of photosynthetic organisms between 60 and 70 meters depth is impressive.

Is southern Pulley Ridge the United State's deepest coral reef? That depends, of course, on one's preferred definition of a coral reef. There are deeper, ahermatypic coral buildups both in the Gulf of Mexico and Atlantic off Florida coasts. Classically, a coral reef is a wave resistant structure built by hermatypic corals and hazardous to shipping. From a geologist's point of view, Pulley Ridge corals appear to have built a biostrome, an accumulation at least a few meters thick, although corals may not account for the bulk of the topography. From that of a biologist, the most abundant corals in the ridge are hermatypic corals but they are lying, mostly unattached, on the surface. Clearly a ship's captain could not run his vessel aground on this reef, so mariners would not consider this a reef. Nevertheless, from the scientific perspective of a structure built from hermatypic corals, southern Pulley Ridge may well be the deepest coral reef in the United States.

Project Contacts:
Robert B. Halley
U.S. Geological Survey
600 Fourth Street South
St. Petersburg, Florida 33701
(727) 803-8747 x 3020
rhalley@usgs.gov
Albert C. Hine
University of South Florida
140 Seventh Avenue South
St. Petersburg, Florida 33701
(727) 553-1161
hine@seas.marine.usf.edu
Bret Jarret
University of South Florida
140 Seventh Avenue South
St. Petersburg, Florida 33701
(727) 553-1183
bjarrett@seas.marine.usf.edu
David C. Twichell
USGS, Woods Hole Field Center
384 Woods Hole Road
Quissett Campus
Woods Hole, MA 02543-1598
(508) 457-2260
dtwichell@usgs.gov


printer icon printable poster:
USGS Open File Report 02-308
Pulley Ridge: The US's Deepest Hermatypic Coral Reef?

Related Research Projects:

Coral Reefs
USGS

Related Links:

USGS Scientist Addresses the Gulf of Mexico Fishery Management Council
USGS

USGS Scientists Use the SeaBOSS to Explore What Could Be the Deepest Coral Reef in the Continental United States
USGS

USGS Scientists Team Up with National Geographic's Sustainable Seas Expedition to Explore Deep Reefs at Pulley Ridge
USGS


Coastal & Marine Geology Program > St. Petersburg Coastal and Marine Science Center > Pulley Ridge


FirstGov.gov U. S. Department of the Interior | U.S. Geological Survey
Center for Coastal & Regional Marine Studies

email Feedback | USGS privacy statement | Disclaimer | Accessibility

This page is http://coastal.er.usgs.gov/pulley-ridge/index.html
Updated May 06, 2013 @ 09:24 AM (JSS)