This dataset contains observations of species occurrences from seafloor imagery collected by the autonomous underwater vehicle (AUV) during the 2012 Expedition to Cobb Seamount. The National Oceanographic and Atmospheric Administration-operated SeaBED-class AUV which collected photographic images from 4 transects ranging from 436 m to 1154 m in depth.

This data set contains oceanographic data (CTD logs, GIS data), biological tracking logs, and color underwater screen-grab images obtained from fixed system video cameras. The objective was to collect samples of corals and invertebrates, and to examine distributions and coral-invertebrate associations. Underwater images are in .jpg, .bmp, and .tif formats.

This data set contains oceanographic data (CTD Data, Fathometer, Knudsen echo sounder, Mocness plankton tow net, Oxygen, and Salinity). The researchers used a submersible, a remotely operated vehicle, and other technology to assess and record conditions in the water column and on the seafloor to gather baseline data along Florida's shelf edge.

This dataset contains observations of species occurrences from seafloor imagery collected by the remotely operated underwater vehicle (ROV) during the 2012 Expedition to Cobb Seamount. The ROV operated by Fisheries and Oceans Canada was a customized Deep Ocean Engineering Phantom HD2+2 which collected photographic images from 12 transects ranging from 35 m to 211 m in depth.

This data set contains oceanographic data (ADCP, ship sensor, navigation), specimen logs, and color underwater screen-grab images taken with a 24-megapixel digital photo camera. The objective was to explore various regions to search for new habitats, species and communities of organisms, search for bioluminescence on the deep seafloor, explore the relationship between vision and bioluminescence in benthic animals, and explore for further examples of unusual benthic/pelagic coupling involving bioluminescence.

Pulley Ridge is a series of drowned barrier islands that extends almost 200 km in 60-100 m water depths. This drowned ridge is located on the Florida Platform in the southeastern Gulf of Mexico about 250 km west of Cape Sable, Florida. This barrier island chain formed during the initial stage of the Holocene marine transgression. These islands were then submerged and left abandoned near the outer edge of the Florida Platform. The southern portion of Pulley Ridge hosts zooxanthellate scleractinian corals, green, red and brown macro algae, and a mix of deep and typically shallow-water tropical fishes. This reef community is in unusually deep water, and its extent and the controls on its distribution were unknown. To address these questions scientists from the U.S. Geological Survey Coastal and Marine Geology Program in cooperation with scientists from the University of South Florida Department of Marine Sciences have completed a detailed mapping of the southernmost 35 km of Pulley Ridge. The area was mapped using multibeam bathymetry, sidescan-sonar imagery, and high-resolution seismic-reflection profiling to define the geologic framework on which the reef is established. Submersible dives, remotely operated vehicle (ROV) transects, and transects of bottom photographs and video were collected to identify the corals and to map their distribution. This extensive suite of data has been compiled and preliminary analysis of the data suggests that the reefs are not tied to the ridge system, but instead are more broadly distributed. Whether reef distribution is controlled by oceanographic conditions or by subtle differences in the substrate that overlies the barrier island system is unclear, and are topics of continued research.

Pulley Ridge is a series of drowned barrier islands that extends almost 200 km in 60-100 m water depths. This drowned ridge is located on the Florida Platform in the southeastern Gulf of Mexico about 250 km west of Cape Sable, Florida. This barrier island chain formed during the initial stage of the Holocene marine transgression. These islands were then submerged and left abandoned near the outer edge of the Florida Platform. The southern portion of Pulley Ridge hosts zooxanthellate scleractinian corals, green, red and brown macro algae, and a mix of deep and typically shallow-water tropical fishes. This reef community is in unusually deep water, and its extent and the controls on its distribution were unknown. To address these questions scientists from the U.S. Geological Survey Coastal and Marine Geology Program in cooperation with scientists from the University of South Florida Department of Marine Sciences have completed a detailed mapping of the southernmost 35 km of Pulley Ridge. The area was mapped using multibeam bathymetry, sidescan-sonar imagery, and high-resolution seismic-reflection profiling to define the geologic framework on which the reef is established. Submersible dives, remotely operated vehicle (ROV) transects, and transects of bottom photographs and video were collected to identify the corals and to map their distribution. This extensive suite of data has been compiled and preliminary analysis of the data suggests that the reefs are not tied to the ridge system, but instead are more broadly distributed. Whether reef distribution is controlled by oceanographic conditions or by subtle differences in the substrate that overlies the barrier island system is unclear, and are topics of continued research.

This dataset contains oceanographic images and videos obtained with Diver Propulsion Vehicles (DPVs) equipped with multiple Canon DSLR cameras. Project archaeologists and biologists also conducted SCUBA diving visual and photographic surveys of target locations to ascertain the characteristics of the located targets. The main goals of this expedition were to document located archaeological sites with digital underwater imaging techniques for archaeological and biological assessment, and to provide opportunities for University of Miami underwater archaeology students to participate in a remote sensing field project and gain experience in data processing and interpretation.

The Ocean Data Platform (ODP) is placed on the sea floor to measure water current profiles, waves, temperature and conductivity. The ODP consists of an upward looking acoustic doppler current profiler (ADP) (SonTek/YSI ADP, www.ysi.com) and a temperature/conductivity recorder (Model SBE37-SM, Sea-Bird Electronics, Inc., www.seabird.com). This metadata record refers to the SonTek ADP dataset. ADP sensors include three acoustic transducers, internal temperature sensor (temperature data automatically compensate for changes in sound speed), compass/tilt sensor (magnetic heading and 2-axis tilt) and a pressure sensor. When an ODP is recovered, another one is typically deployed in the same place. Time series data combining multiple deployments from a given site may also be available. Please contact CRED with any questions. For program information see the web site https://www.fisheries.noaa.gov/pacific-islands/ecosystems/coral-reefs-pacific

This cruise used the remotely operated vehicle (ROV) Jason II to: explore 4-6 new sites for the occurrence of deep water coral reefs; made collections of Lophelia and other corals for genetic and physiological studies, made collections of communities associated with Lophelia and other corals for ecological studies; collected quantitative digital imagery for characterization of sites and coral communities; collect spatially explicit physical near bottom oceanographic data; deploy cameras and microbial arrays; reposition larval traps and current meters; collected push cores; and conducted a series of linked archaeological/ biological investigations on deep water shipwrecks.