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The Ecology of Deep Water Octocorals off the Northeast Coast of the United States  (Year 2 of 3)
Project Number: NAGL-02-06B
Principle Investigators: Watling, L. E., P. J. Auster, and K. J. Eckelbarger
Region(s): Gulf of Maine

Representative Images
Representative Images
Representative Images
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To most people, the concept of a deep water coral is an oxymoron. In fact, until the wide publicity about recent legislation banning trawling in deep coral beds off the coast of Norway, the existence of these species was known only to a handful of scientists and a large number of fishermen. In North America there is little knowledge of their existence in the minds of the general public as well as the broader scientific community. Along the American east coast deep water corals have been known since at least 1862 when scientific surveys noted the presence of Primnoa species on Georges Bank. Several other deep water coral species from depths greater than 200 fathoms off the coasts of New England and Nova Scotia were also documented during the latter part of the 19th century. Aging studies of corals such as Primnoa (and others from the octocoral group) have shown that colonies can be centuries old. As recently as the late 1960s, long-lived corals were described as common components of the gravel fauna of the Gulf of Maine. Submersible dives over the last fifteen years in many of the areas previously described as coral habitats has demonstrated their rarity. Given that the existence of these remarkable, and often beautiful, species has been known for more than a century, it is striking that we know almost nothing about their biology and the role they may play as habitat for vagile deep water fauna, including those species targeted in recent exploratory fisheries. This proposal has as its major objective the characterization of deep-water octocoral communities in the Gulf of Maine and the outer continental shelf of the northeastern United States. These coral areas have been known to generations of fishermen, principally as a result of gear damage or by-catch, first with long-liners and gill netters, and then with draggers. Because of the difficulty associated with studying these animals, scientists have only recently begun to understand their potential importance to benthic ecosystems, their rarity in the underwater landscape, and their sensitivity to human caused disturbances. For this project, an ROV will be used to determine if the gorgonian species of the nearshore Gulf of Maine are con-specific with the gorgonians from the outer continental shelf off Georges Bank, if gorgonian diversity is the same nearshore and offshore, if inshore gorgonians represent pseudopopulations of the offshore gorgonian populations, if size class distributions of inshore and offshore gorgonian populations are similar, and if gorgonian associates in both inshore and offshore areas are representative of the regional benthic fauna. The results of this work will form the basis for future protection of rare and potentially valuable corals that serve as habitat for a variety of other taxa and are seriously threatened by human activities (e.g., fishing gear, hydrocarbon extraction). Further, the collapse of demersal fish populations has focused attention on deep coral communities as critical habitat for some economically important species such as those of the genus Sebastes, as well as taxa that are of interest in deepwater exploratory fisheries (e.g., slimeheads - known as orange roughy from the species targeted off New Zealand and Australia). The results of this research will qualify, and begin to quantify the services that deep octocoral assemblages may provide to various life stages of economically (and potentially) important species of fish and invertebrates. Further, this study will characterize the habitats in which corals occur on the northeast continental shelf and slope. Such knowledge, combined with studies from other areas, will allow us to develop a plan to assess coral distribution and abundance on the outer continental shelf and upper slope within the U.S. EEZ.

An offshoot of this project was implemented during 2001 as a joint project with NOAA’s Ocean Exploration Office (DeepEast Project). The field component utilized the DSV ALVIN and focused on the deep regions of 3 canyons and two seamounts. However, due to Hurricane Emily, only two canyons were visited with ALVIN but a multibeam map of the summit of Bear Seamount was produced. The original scope of the NURC project was not implemented until 2002.

In 2002, the cruise was focused on the northern Gulf of Maine. Due to technical problems with the ROV, caused by fouling in fishing gear, only 2 days of diving were completed. Unused operational funds from this cruise were carried over for use in 2003 (that will result in 3 actual operations days). A proposal was submitted to the National Geographic Society’s Committee for Research and Exploration for additional funding in order to conduct 8 operations days at this site. The planned 2003 cruise to Georges Bank submarine canyons will be conducted as well during this period.
 

The purpose of this year’s work was to find and survey sites of deep water coral populations. We knew of two sites from 2002, and had a list of other prospective sites, based on bathymetry, that needed to be investigated. There is only old NOAA bathymetric data available for the section of Jordan Basin that was most likely to have corals, so the choice of dive sites was made with quite rudimentary information. Nevertheless, we dove on several likely sites, which are listed in the table below.

Dive #, Site; Date; Lat (N); Long (W); Depth (m)
1, NE Monhegan Island; 08-05-2003; 43 47.7362; 069 18.1591; 89
2, 114 Bump, north; 08-06-2003; 43 21.8807; 067 48.7473; 241
3, 96 Bump; 08-07-2003; 43 16.2601; 067 56.6006; 220
4, 118 Bump; 08-07-2003; 43 33.8353; 067 50.5785; 220
5, 79 Bump; 08-08-2003; 43 04.0712; 067 46.9739; 187
6, 114 Bump; 08-08-2003; 43 21.9039; 067 48.7745; 215
7, 79N Bump; 08-10-2003; 43 58.2161; 067 27.2061; 181-156
8, Mt. Desert Rock, S canyon, north wall; 08-11-2003; 43 56.8753; 068 11.6600; 199-114
9, Mt. Desert Rock, S canyon, south wall; 08-11-2003; 43 56.1912; 068 12.1657; 173-113

Besides 114 Bump and Mt. Desert Rock, only two other sites produced coral colonies – 96 Bump and 118 Bump. Three species of octocoral are now known from these sites: Paragorgia arborea, both pink and white forms from 114 Bump; Primnoa resedaeformis from 114 Bump and Mt. Desert Rock South Canyon, south wall; and an unknown (?new) species of Paramuricea, both golden and purple forms, from 114 Bump, 96 Bump, and 118 Bump. The latter species was mis-identified as a species of Acanthogorgia while we were at sea.

Tissue samples were taken from 14 coral specimens for reproductive morphology and genetic studies. Of the 14 specimens, 11 are Paramuricea sp. (two color morphs), 2 are Pr. resedaeformis, and one is P. arborea. One or two samples of tissue were preserved in alcohol for genetic studies and sent to Dr. Scott France at the College of Charleston. He has sequenced the DNA of three mitochondrial genes from all specimens but those sequences have not yet been analyzed.

A total of 347 tissue samples were taken for reproductive morphology. They have all been embedded in plastic for sectioning and examination by electron microscopy. The sectioning work on these tissue blocks has just begun.

Invertebrate associates were collected from all 14 coral specimens. The P. arborea had a rarely collected amphipod species, as yet undetermined but apparently in the genus Mesopleutes, on it. The Paramuricea were nearly bare of associates, except for the occasional copepod. Most likely any copepods strongly associated with the coral would have escaped or were left in the bio-box on the ROV. The Primnoa specimens were devoid of attached associates.

{Fish counts –Peter.}

Video transects were conducted seven sites for censusing fishes. Sites were characterized based on cover attributes provided by sedimentary and epifaunal structures. Acadian redfish, Sebastes fasciatus, was the most abundant taxa in areas of dense coral cover as well as at sites with dense sponges. Subsequent analyses based on density and fish species richness demonstrated that areas of dense epifaunal cover serve as habitats functionally equivalent to deepwater corals.

Leg 1    Begin Date: 8/5/2003   End Date: 8/11/2003
  Support Vessel/Platform: R/V Connecticut
System Ops Days Dives Dive Time (hrs) Depth (m)
KRAKEN (MAXrover MKI) 7 9 16.44 262.2
 
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