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St. Petersburg Coastal and Marine Science Center images.

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Coupled Plasma-Optical Emission Spectrometer
Coupled Plasma-Optical Emission Spectrometer
Coupled Plasma-Optical Emission Spectrometer
Coupled Plasma-Optical Emission Spectrometer

We use a Inductively Coupled Plasma-Optical Emission Spectrometer (ICP-OES) to determine the Sr/Ca in coral aragonite samples in the laboratory at the USGS St. Petersburg Coastal and Marine Science Center.

We use a Inductively Coupled Plasma-Optical Emission Spectrometer (ICP-OES) to determine the Sr/Ca in coral aragonite samples in the laboratory at the USGS St. Petersburg Coastal and Marine Science Center.

A cinderblock with monitoring devices on it sits in shallow water on a reef with corals growing on it and off in the distance.
Elkhorn coral in Biscayne National Park
Elkhorn coral in Biscayne National Park
Elkhorn coral in Biscayne National Park

The CMHRP is testing the calcification rates of different genetic strains of threatened Elkhorn coral (Acropora palmata) to advise local and Federal agencies engaged in coral reef restoration.

The CMHRP is testing the calcification rates of different genetic strains of threatened Elkhorn coral (Acropora palmata) to advise local and Federal agencies engaged in coral reef restoration.

“Variance” images derived from videos of Madeira Beach (left) and Cowells Beach (right)
“Variance” images derived from videos of beaches studied
“Variance” images derived from videos of beaches studied
“Variance” images derived from videos of beaches studied

“Variance” images derived from the same videos used in the studies. Left, Madeira Beach; right, Cowells Beach. In a variance image, the more variation in light intensity at a given pixel, the brighter the value assigned to that pixel. Bright areas indicate many changes in light intensity, caused by a lot of movement.

“Variance” images derived from the same videos used in the studies. Left, Madeira Beach; right, Cowells Beach. In a variance image, the more variation in light intensity at a given pixel, the brighter the value assigned to that pixel. Bright areas indicate many changes in light intensity, caused by a lot of movement.

Left: shades of blue show water depth. Right: changes in colors show accretion or erosion of the seafloor
Examples of sediment dynamics offshore of barrier islands
Examples of sediment dynamics offshore of barrier islands
Examples of sediment dynamics offshore of barrier islands

Examples of sediment dynamics offshore of barrier islands include the development and erosion of shoals, tidal deltas, and sand ridges.

Using the computer-driven triaxial micro-milling machine to subsample a coral slab. 
Computer-driven triaxial micro-milling machine
Computer-driven triaxial micro-milling machine
Computer-driven triaxial micro-milling machine

Using the computer-driven triaxial micro-milling machine to subsample a coral slab. 

Globigerinoides ruber
SEM image of a Globigerinoides ruber
SEM image of a Globigerinoides ruber
SEM image of a Globigerinoides ruber

SEM image of a Globigerinoides ruber specimen from the Gulf of Mexico.

Underwater photo of a vast area of dead corals on the seafloor at Buck Island, U.S. Virgin Islands
Some elkhorn corals in the U.S. Virgin Islands have died
Some elkhorn corals in the U.S. Virgin Islands have died
Some elkhorn corals in the U.S. Virgin Islands have died

Elkhorn corals (Acropora palmata) on the seafloor along the northeastern coast of Buck Island, U.S. Virgin Islands, have died and collapsed into rubble. As coral reef structure degrades, habitat for marine life is lost and nearby coastlines become more susceptible to storms, waves, and erosion.

Elkhorn corals (Acropora palmata) on the seafloor along the northeastern coast of Buck Island, U.S. Virgin Islands, have died and collapsed into rubble. As coral reef structure degrades, habitat for marine life is lost and nearby coastlines become more susceptible to storms, waves, and erosion.

A view of healthy elkhorn corals on the seafloor in the U.S. Virgin Islands
Healthy elkhorn coral on the seafloor in the U.S. Virgin Islands
Healthy elkhorn coral on the seafloor in the U.S. Virgin Islands
Healthy elkhorn coral on the seafloor in the U.S. Virgin Islands

Healthy elkhorn coral (Acropora palmata) on the seafloor along the southeastern coast of Buck Island, U.S. Virgin Islands. Elkhorn coral is one of many important reef-building species that create 3D structure on the seafloor. Coral reef structure provides habitat for marine life and helps break up waves as they approach the coastline.

Healthy elkhorn coral (Acropora palmata) on the seafloor along the southeastern coast of Buck Island, U.S. Virgin Islands. Elkhorn coral is one of many important reef-building species that create 3D structure on the seafloor. Coral reef structure provides habitat for marine life and helps break up waves as they approach the coastline.

Calcareous planispiral estuarine foraminifera Cribroelphidium poeyanum from Grand Bay
Calcareous estuarine foraminifera Cribroelphidium poeyanum
Calcareous estuarine foraminifera Cribroelphidium poeyanum
Calcareous estuarine foraminifera Cribroelphidium poeyanum

Scanning electron microscope (SEM) image of calcareous planispiral estuarine foraminifera Cribroelphidium poeyanum collected from Grand Bay estuary.

Images of Matanzas, Florida, from before and after Hurricane Matthew, and DEM showing the associated change
Orthomosaic and DEM images of Matanzas, Florida
Orthomosaic and DEM images of Matanzas, Florida
Orthomosaic and DEM images of Matanzas, Florida

Orthomosaic images of Matanzas, Florida, from (a) before and (b) after Hurricane Matthew, and (c) a digital elevation model (DEM) showing the associated topographic change. Note, these results were produced by applying Structure-from-Motion (SfM) to NOAA oblique photographs, but similar results can be obtained using UAS aerial imagery.

Orthomosaic images of Matanzas, Florida, from (a) before and (b) after Hurricane Matthew, and (c) a digital elevation model (DEM) showing the associated topographic change. Note, these results were produced by applying Structure-from-Motion (SfM) to NOAA oblique photographs, but similar results can be obtained using UAS aerial imagery.

Calcareous trochospiral estuarine foraminifera Ammonia tepida from Grand Bay
Calcareous estuarine foraminifera Ammonia tepida from Grand Bay
Calcareous estuarine foraminifera Ammonia tepida from Grand Bay
Calcareous estuarine foraminifera Ammonia tepida from Grand Bay

Scanning electron microscope (SEM) image of calcareous trochospiral estuarine foraminifera Ammonia tepida collected from Grand Bay estuary

Calcification monitoring station with a colony of the massive starlet coral, Siderastrea siderea, fastened in place.
Calcification monitoring station
Calcification monitoring station
Calcification monitoring station

Calcification monitoring station with a colony of the massive starlet coral, Siderastrea siderea, fastened in place.

Calcification monitoring station with a colony of the massive starlet coral, Siderastrea siderea, fastened in place.

multicores
Multicores
Multicores
Multicores

Multicores collected from the northern Gulf of Mexico. These cores contain roughly 1 meter of sediment from the seafloor, and represent the past ~2000 years of deposition.

Multicores collected from the northern Gulf of Mexico. These cores contain roughly 1 meter of sediment from the seafloor, and represent the past ~2000 years of deposition.

Low dunes near Cape Canaveral launch pads 39A and 39B often overwash during storm events
Low dunes near Cape Canaveral launch pads often overwash during storms
Low dunes near Cape Canaveral launch pads often overwash during storms
Low dunes near Cape Canaveral launch pads often overwash during storms

Low dunes near Cape Canaveral launch pads 39A and 39B often overwash during storm events, transporting sand landward. Critical infrastructure may be buried or flooded. In addition, significant landward transport of sand may lead to extensive shoreline erosion.

Low dunes near Cape Canaveral launch pads 39A and 39B often overwash during storm events, transporting sand landward. Critical infrastructure may be buried or flooded. In addition, significant landward transport of sand may lead to extensive shoreline erosion.

Images of Madeira Beach, Florida, from video taken June 20, 2017
Images of Madeira Beach, Florida, from video taken June 20, 2017
Images of Madeira Beach, Florida, from video taken June 20, 2017
Images of Madeira Beach, Florida, from video taken June 20, 2017

Views of Madeira Beach, Florida, produced from a 17-minute video shot on June 20, 2017. Left: Snapshot, or first frame of video. Right: Time-averaged image, sometimes called a “timex,” created by averaging the intensity of light recorded at each spot, or “pixel,” during the 17-minute video.

Views of Madeira Beach, Florida, produced from a 17-minute video shot on June 20, 2017. Left: Snapshot, or first frame of video. Right: Time-averaged image, sometimes called a “timex,” created by averaging the intensity of light recorded at each spot, or “pixel,” during the 17-minute video.

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