Coral reefs are important for supporting biodiversity, fisheries, tourism, and coastal protection, but are in decline worldwide, primarily due to extreme heat waves and subsequent coral bleaching, in addition to other stressors.
Coral Reef Ecosystem Studies (CREST)
Florida Keys Calcification Monitoring Network
Measuring coral growth to help restore reefs
First Ecosystem-Wide Study of Seafloor Erosion
Divergence of seafloor elevation and sea level rise in coral reef ecosystems
Corals as Geochemical Archives
Reconstructing paleo-environmental conditions on the reef
Holocene Coral-Reef Development
To gain insights into the future, researchers are studying the past
Coral Reef Seafloor Erosion and Coastal Hazards
Regional-scale erosion measurements indicate that seafloor erosion is increasing water depths along the coastline
The specific objectives of this project are to identify and describe the processes that are important in determining rates of coral-reef construction. How quickly the skeletons of calcifying organisms accumulate to form massive barrier-reef structure is determined by processes of both construction (how fast organisms grow and reproduce) and destruction (how fast reefs break down by mechanical, chemical, and biological means).
Overview and Objectives
By combining our research activities involving mapping, monitoring, and retrospectively investigating reef processes such as calcification, reef metabolism, and microbial cycling, we will reveal linkages among them and establish connections to ecosystem services or outputs including reef edification, seawater chemistry, sand production, and habitat construction. Our work addresses several key issues related to the current status and potential declining health and resilience of shallow-water reef communities in the U.S. Caribbean, Gulf of Mexico, and Florida Keys. Improved understanding and information resulting from our work will help guide policies and best management practices to preserve and restore U.S. coral reef resources.
The specific objectives of this project are to identify and describe the processes that are important in determining rates of coral-reef construction. How quickly the skeletons of calcifying organisms accumulate to form massive barrier-reef structure is determined by processes of both construction (how fast organisms grow and reproduce) and destruction (how fast reefs break down by mechanical, chemical, and biological means). The components of our project represent multiple disciplines working together to answer one fundamental question: 'what are the drivers determining calcification rates and reef construction, and will reefs cease to accrete (grow) in the near future in the context of ocean warming, ocean acidification, and/or compromised water quality?' We will also explore the seasonal, spatial (vertical and horizontal), and retrospective (historical and geological) heterogeneity in the reef processes we are investigating. A greater knowledge of the natural variability in these processes will afford us a much better chance of detecting and understanding potential impacts of global climate change or altered water quality on reef building.
Measuring Coral Growth to Help Restore Reefs
It is critical to start measuring calcification rates in a systematic way now, particularly at subtropical latitudes where conditions fluctuate seasonally, so that we can understand how dynamic ocean conditions affect calcifying organisms today and predict possible changes in the future. We established a calcification monitoring network in the Florida Keys and have been measuring calcification rates since 2009.
Coral Reef Seafloor Erosion and Coastal Hazards
Synchronized field work focused on geochemistry, geology, and metabolic processes overlaid on a habitat map of an entire reef to produce a synoptic overview of reef processes that contribute to carbonate precipitation and dissolution.
Reef History and Climate Change
Ecosystem-wide study of seafloor erosion, changing coastal water depths, and effects on coastal storm and wave impacts along the Florida Keys Coral Reef Tract in South Florida.
Holocene Coral-Reef Development
With the continuing threat of climate change and other anthropogenic disturbances, the future of Florida's coral reefs is uncertain. One way to gain insights into the future trajectories of Florida's coral reefs is to investigate how they responded to environmental disturbances in the past.
Microbial Processes on Reefs
The microbial community on coral reefs is generally underappreciated given the ubiquity, abundance, complexity, and formative role these prokaryotes serve in the metabolic and chemical processes on reefs. We use microbiological and metagenomic techniques to decipher the roles the microbial community are playing in processes such as coral disease, submarine groundwater discharge, calcification, and dissolution.
Previous Research
Community Calcification & Metabolism
Changing ocean chemistry resulting from climate change and ocean acidification also affects coral reefs at the community level. The severity of impacts to coral reefs depends, in part, on the ability of reefs to continue growing enough to keep up with rising sea level.
Benthic Habitat Mapping & Monitoring
Benthic community composition, percent cover, areal extent, and temporal stability are critical factors that contribute to the value of a given marine habitat. Knowledge of these benthic cover components provides a baseline for National Park Service resource managers, as well as a tool for planning research activities for other CREST scientists.
Coral Disease
Coral diseases have been reported worldwide and with increasing frequency. Disease is now recognized as one of the major causes of reef degradation and coral mortality.
Below are other science projects associated with this project.
Microbial Processes on Reefs
Fine-scale Benthic Habitat Mapping
Reef History and Climate Change
Holocene Coral-Reef Development
Coral Reef Seafloor Erosion and Coastal Hazards
Measuring Coral Growth to Help Restore Reefs
Coral Reef Community Calcification and Metabolism
Below are data or web applications associated with this project.
Experimental Coral-Physiology Data for Acropora palmata in Florida, USA
Experimental Coral-Growth Data and Time-Series Imagery for Acropora palmata and Pseudodiploria strigosa in St. Croix, U.S. Virgin Islands
Underwater temperature on off-shore coral reefs of the Florida Keys, U.S.A.
Experimental Data on Construction and Erosion of Orbicella Coral Reefs in the Florida Keys, U.S.A.
Descriptive Core Logs, Core Photographs, Radiocarbon Ages, and Accretion Data from Holocene Reef Cores Collected Throughout the Florida Keys Reef Tract
Microbial and environmental dataset from Crocker Reef, Florida Keys, 2014-2015
Below are multimedia items associated with this project.
Coral reefs are important for supporting biodiversity, fisheries, tourism, and coastal protection, but are in decline worldwide, primarily due to extreme heat waves and subsequent coral bleaching, in addition to other stressors.
The complex, three-dimensional reefs built by corals over hundreds to thousands of years provide invaluable ecosystem services to society—contributing billions of dollars per year to the global economy through shoreline protection, tourism, and habitat for biodiversity and fisheries.
The complex, three-dimensional reefs built by corals over hundreds to thousands of years provide invaluable ecosystem services to society—contributing billions of dollars per year to the global economy through shoreline protection, tourism, and habitat for biodiversity and fisheries.
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.
A diver uses an underwater drill to take a core sample from a massive brain coral (Diploria strigosa) in Dry Tortugas National Park.
A diver uses an underwater drill to take a core sample from a massive brain coral (Diploria strigosa) in Dry Tortugas National Park.
These Elkhorn corals (Acropora palmata) near Buck Island, U.S. Virgin Islands have died and collapsed into rubble. As coral reef structure degrades, valuable habitat for marine life is lost and nearby coastlines become more susceptible to storms, waves and erosion.
These Elkhorn corals (Acropora palmata) near Buck Island, U.S. Virgin Islands have died and collapsed into rubble. As coral reef structure degrades, valuable habitat for marine life is lost and nearby coastlines become more susceptible to storms, waves and erosion.
Healthy Elkhorn coral (Acropora palmata) near unpopulated 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) near unpopulated 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.
Taken at Palmyra National Wildlife Refuge
Taken at Palmyra National Wildlife Refuge
Don Hickey tightens a bolt on a coral calcification monitoring station. Corals are being monitored for growth and sampled for climate proxy indicators (isotopes, elemental ratios).
Don Hickey tightens a bolt on a coral calcification monitoring station. Corals are being monitored for growth and sampled for climate proxy indicators (isotopes, elemental ratios).
Shallow coral reefs in the U.S. Virgin Islands are in jeopardy due to climate warming and ocean acidification.
Shallow coral reefs in the U.S. Virgin Islands are in jeopardy due to climate warming and ocean acidification.
Below are publications associated with this project.
Discovery of a rare pillar coral (Dendrogyra cylindrus) death assemblage off southeast Florida reveals multi-century persistence during the late Holocene
The potential for coral reef restoration to mitigate coastal flooding as sea levels rise
Upwelling, climate change, and the shifting geography of coral reef development
Assigning causality to events in the Holocene record of coral reefs
Scale dependence of coral reef oases and their environmental correlates
Reestablishing a stepping-stone population of the threatened elkhorn coral Acropora palmata to aid regional recovery
Disturbances drive changes in coral community assemblages and coral calcification capacity
Heat accumulation on coral reefs mitigated by internal waves
Considerations for maximizing the adaptive potential of restored coral populations in the western Atlantic
The unprecedented loss of Florida's reef-building corals and the emergence of a novel coral-reef assemblage
Improving estimates of coral reef construction and erosion with in-situ measurements
Quantifying uncertainty in Sr/Ca-based estimates of SST from the coral Orbicella faveolata
Below are news stories associated with this project.
Below are FAQ associated with this project.
Why are coral reefs in peril and what is being done to protect them?
Coral reefs can be damaged by natural processes, such as storms, but they are increasingly at risk from human activities. Oil spills and pollutants can threaten entire reefs. Excessive nutrients from land sources, such as sewage and agricultural fertilizers, promote the growth of algae that can smother corals. Other organisms harmful to corals, such as crown-of-thorns starfish, multiply when the...
The specific objectives of this project are to identify and describe the processes that are important in determining rates of coral-reef construction. How quickly the skeletons of calcifying organisms accumulate to form massive barrier-reef structure is determined by processes of both construction (how fast organisms grow and reproduce) and destruction (how fast reefs break down by mechanical, chemical, and biological means).
Overview and Objectives
By combining our research activities involving mapping, monitoring, and retrospectively investigating reef processes such as calcification, reef metabolism, and microbial cycling, we will reveal linkages among them and establish connections to ecosystem services or outputs including reef edification, seawater chemistry, sand production, and habitat construction. Our work addresses several key issues related to the current status and potential declining health and resilience of shallow-water reef communities in the U.S. Caribbean, Gulf of Mexico, and Florida Keys. Improved understanding and information resulting from our work will help guide policies and best management practices to preserve and restore U.S. coral reef resources.
The specific objectives of this project are to identify and describe the processes that are important in determining rates of coral-reef construction. How quickly the skeletons of calcifying organisms accumulate to form massive barrier-reef structure is determined by processes of both construction (how fast organisms grow and reproduce) and destruction (how fast reefs break down by mechanical, chemical, and biological means). The components of our project represent multiple disciplines working together to answer one fundamental question: 'what are the drivers determining calcification rates and reef construction, and will reefs cease to accrete (grow) in the near future in the context of ocean warming, ocean acidification, and/or compromised water quality?' We will also explore the seasonal, spatial (vertical and horizontal), and retrospective (historical and geological) heterogeneity in the reef processes we are investigating. A greater knowledge of the natural variability in these processes will afford us a much better chance of detecting and understanding potential impacts of global climate change or altered water quality on reef building.
Measuring Coral Growth to Help Restore Reefs
It is critical to start measuring calcification rates in a systematic way now, particularly at subtropical latitudes where conditions fluctuate seasonally, so that we can understand how dynamic ocean conditions affect calcifying organisms today and predict possible changes in the future. We established a calcification monitoring network in the Florida Keys and have been measuring calcification rates since 2009.
Coral Reef Seafloor Erosion and Coastal Hazards
Synchronized field work focused on geochemistry, geology, and metabolic processes overlaid on a habitat map of an entire reef to produce a synoptic overview of reef processes that contribute to carbonate precipitation and dissolution.
Reef History and Climate Change
Ecosystem-wide study of seafloor erosion, changing coastal water depths, and effects on coastal storm and wave impacts along the Florida Keys Coral Reef Tract in South Florida.
Holocene Coral-Reef Development
With the continuing threat of climate change and other anthropogenic disturbances, the future of Florida's coral reefs is uncertain. One way to gain insights into the future trajectories of Florida's coral reefs is to investigate how they responded to environmental disturbances in the past.
Microbial Processes on Reefs
The microbial community on coral reefs is generally underappreciated given the ubiquity, abundance, complexity, and formative role these prokaryotes serve in the metabolic and chemical processes on reefs. We use microbiological and metagenomic techniques to decipher the roles the microbial community are playing in processes such as coral disease, submarine groundwater discharge, calcification, and dissolution.
Previous Research
Community Calcification & Metabolism
Changing ocean chemistry resulting from climate change and ocean acidification also affects coral reefs at the community level. The severity of impacts to coral reefs depends, in part, on the ability of reefs to continue growing enough to keep up with rising sea level.
Benthic Habitat Mapping & Monitoring
Benthic community composition, percent cover, areal extent, and temporal stability are critical factors that contribute to the value of a given marine habitat. Knowledge of these benthic cover components provides a baseline for National Park Service resource managers, as well as a tool for planning research activities for other CREST scientists.
Coral Disease
Coral diseases have been reported worldwide and with increasing frequency. Disease is now recognized as one of the major causes of reef degradation and coral mortality.
Below are other science projects associated with this project.
Microbial Processes on Reefs
Fine-scale Benthic Habitat Mapping
Reef History and Climate Change
Holocene Coral-Reef Development
Coral Reef Seafloor Erosion and Coastal Hazards
Measuring Coral Growth to Help Restore Reefs
Coral Reef Community Calcification and Metabolism
Below are data or web applications associated with this project.
Experimental Coral-Physiology Data for Acropora palmata in Florida, USA
Experimental Coral-Growth Data and Time-Series Imagery for Acropora palmata and Pseudodiploria strigosa in St. Croix, U.S. Virgin Islands
Underwater temperature on off-shore coral reefs of the Florida Keys, U.S.A.
Experimental Data on Construction and Erosion of Orbicella Coral Reefs in the Florida Keys, U.S.A.
Descriptive Core Logs, Core Photographs, Radiocarbon Ages, and Accretion Data from Holocene Reef Cores Collected Throughout the Florida Keys Reef Tract
Microbial and environmental dataset from Crocker Reef, Florida Keys, 2014-2015
Below are multimedia items associated with this project.
Coral reefs are important for supporting biodiversity, fisheries, tourism, and coastal protection, but are in decline worldwide, primarily due to extreme heat waves and subsequent coral bleaching, in addition to other stressors.
Coral reefs are important for supporting biodiversity, fisheries, tourism, and coastal protection, but are in decline worldwide, primarily due to extreme heat waves and subsequent coral bleaching, in addition to other stressors.
The complex, three-dimensional reefs built by corals over hundreds to thousands of years provide invaluable ecosystem services to society—contributing billions of dollars per year to the global economy through shoreline protection, tourism, and habitat for biodiversity and fisheries.
The complex, three-dimensional reefs built by corals over hundreds to thousands of years provide invaluable ecosystem services to society—contributing billions of dollars per year to the global economy through shoreline protection, tourism, and habitat for biodiversity and fisheries.
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.
A diver uses an underwater drill to take a core sample from a massive brain coral (Diploria strigosa) in Dry Tortugas National Park.
A diver uses an underwater drill to take a core sample from a massive brain coral (Diploria strigosa) in Dry Tortugas National Park.
These Elkhorn corals (Acropora palmata) near Buck Island, U.S. Virgin Islands have died and collapsed into rubble. As coral reef structure degrades, valuable habitat for marine life is lost and nearby coastlines become more susceptible to storms, waves and erosion.
These Elkhorn corals (Acropora palmata) near Buck Island, U.S. Virgin Islands have died and collapsed into rubble. As coral reef structure degrades, valuable habitat for marine life is lost and nearby coastlines become more susceptible to storms, waves and erosion.
Healthy Elkhorn coral (Acropora palmata) near unpopulated 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) near unpopulated 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.
Taken at Palmyra National Wildlife Refuge
Taken at Palmyra National Wildlife Refuge
Don Hickey tightens a bolt on a coral calcification monitoring station. Corals are being monitored for growth and sampled for climate proxy indicators (isotopes, elemental ratios).
Don Hickey tightens a bolt on a coral calcification monitoring station. Corals are being monitored for growth and sampled for climate proxy indicators (isotopes, elemental ratios).
Shallow coral reefs in the U.S. Virgin Islands are in jeopardy due to climate warming and ocean acidification.
Shallow coral reefs in the U.S. Virgin Islands are in jeopardy due to climate warming and ocean acidification.
Below are publications associated with this project.
Discovery of a rare pillar coral (Dendrogyra cylindrus) death assemblage off southeast Florida reveals multi-century persistence during the late Holocene
The potential for coral reef restoration to mitigate coastal flooding as sea levels rise
Upwelling, climate change, and the shifting geography of coral reef development
Assigning causality to events in the Holocene record of coral reefs
Scale dependence of coral reef oases and their environmental correlates
Reestablishing a stepping-stone population of the threatened elkhorn coral Acropora palmata to aid regional recovery
Disturbances drive changes in coral community assemblages and coral calcification capacity
Heat accumulation on coral reefs mitigated by internal waves
Considerations for maximizing the adaptive potential of restored coral populations in the western Atlantic
The unprecedented loss of Florida's reef-building corals and the emergence of a novel coral-reef assemblage
Improving estimates of coral reef construction and erosion with in-situ measurements
Quantifying uncertainty in Sr/Ca-based estimates of SST from the coral Orbicella faveolata
Below are news stories associated with this project.
Below are FAQ associated with this project.
Why are coral reefs in peril and what is being done to protect them?
Coral reefs can be damaged by natural processes, such as storms, but they are increasingly at risk from human activities. Oil spills and pollutants can threaten entire reefs. Excessive nutrients from land sources, such as sewage and agricultural fertilizers, promote the growth of algae that can smother corals. Other organisms harmful to corals, such as crown-of-thorns starfish, multiply when the...