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.
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
Below are publications associated with this project.
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
Considerations for maximizing the adaptive potential of restored coral populations in the western Atlantic
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
A 3,000‐year lag between the geological and ecological shutdown of Florida's coral reefs
A framework for identifying and characterising coral reef “oases” against a backdrop of degradation
Sea-level rise could overwhelm coral reefs
Plasticity in skeletal characteristics of nursery-raised staghorn coral, Acropora cervicornis
Fidelity of the Sr/Ca proxy in recording ocean temperature in the western Atlantic coral Siderastrea siderea
Collection methods and descriptions of coral cores extracted from massive corals in Dry Tortugas National Park, Florida, U.S.A.
Multi-species coral Sr/Ca-based sea-surface temperature reconstruction using Orbicella faveolata and Siderastrea siderea from the Florida Straits
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...
- Overview
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).
Calcification monitoring station with a colony of the massive starlet coral, Siderastrea siderea, fastened in place. (Public domain.) 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.
The U.S. Geological Survey is conducting research to guide the recovery of the threatened Elkhorn coral, Acropora palmata, in Dry Tortugas National Park and throughout the western Atlantic. A small Elkhorn colony, raised from a fragment collected after a storm, is shown here in the foreground after it was cemented to the reef to establish a new coral population. Elkhorn coral is a foundational species that creates large underwater ramparts that protect coastal communities from the onslaught of waves. 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.
- Science
Below are other science projects associated with this project.
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...Fine-scale Benthic Habitat Mapping
Both ATRIS configurations were deployed in Dry Tortugas National Park (DRTO) to fill information gaps in the spatial coverage of existing habitat maps.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.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.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...Coral Reef Community Calcification and Metabolism
This task focuses on forecasting and hind-casting the future and past response of coral reef calcification and growth to changes in seawater carbonate chemistry from pre-industrial time to the year 2100. - Data
Below are data or web applications associated with this project.
Underwater temperature on off-shore coral reefs of the Florida Keys, U.S.A.
The USGS Coral Reef Ecosystems Studies project provides science that helps resource managers tasked with the stewardship of coral reef resources. Coral reef organisms are very sensitive to high and low water-temperature extremes. It is critical to precisely know water temperatures experienced by corals and associated plants and animals that live in the dynamic, nearshore environment to document thExperimental Data on Construction and Erosion of Orbicella Coral Reefs in the Florida Keys, U.S.A.
The USGS Coral Reef Ecosystems Studies project provides science that helps resource managers tasked with the stewardship of coral reef resources. This data release contains data on coral-growth rates for Orbicella sp. coral colonies grown at five sites on the Florida Keys reef tract from 2013 to 2015, survey data for census-based carbonate budgeting at Hen and Chickens Reef (Islamorada, Florida),Descriptive Core Logs, Core Photographs, Radiocarbon Ages, and Accretion Data from Holocene Reef Cores Collected Throughout the Florida Keys Reef Tract
The USGS core archive (Reich and others, 2009; USGS Core Archive) houses an extensive collection of coral-reef cores that USGS researchers have collected from throughout the Florida Keys reef tract (FKRT; fig. 1). USGS scientists have compiled all available data on the 71 core records that recovered Holocene reef framework, including radiometric ages (radiocarbon and U-series), data on reef develo - Multimedia
- Publications
Below are publications associated with this project.
Filter Total Items: 67Reestablishing a stepping-stone population of the threatened elkhorn coral Acropora palmata to aid regional recovery
Recovery of the elkhorn coral Acropora palmata is critical to reversing coral reef ecosystem collapse in the western Atlantic, but the species is severely threatened. To gauge potential for the species’ restoration in Florida, USA, we conducted an assisted migration experiment where 50 coral fragments of 5 nursery-raised genetic strains (genets) from the upper Florida Keys were moved to 5 sites acAuthorsIlsa B. Kuffner, Anastasios Stathakopoulos, Lauren Toth, Lucy BartlettDisturbances drive changes in coral community assemblages and coral calcification capacity
Anthropogenic environmental change has increased coral reef disturbance regimes in recent decades, altering the structure and function of many coral reefs globally. In this study, we used coral community survey data collected from 1996 to 2015 to evaluate coral calcification capacity (CCC) dynamics with respect to recorded pulse disturbances for 121 reef sites in the Main Hawaiian Islands and Mo'oAuthorsTravis A. Courtney, Brian B. Barnes, Iliana Chollett, Robin Elahi, Kevin Gross, James R. Guest, Ilsa B. Kuffner, Elizabeth A. Lenz, Hanna R Nelson, Caroline Rogers, Lauren Toth, Andreas J AnderssonConsiderations for maximizing the adaptive potential of restored coral populations in the western Atlantic
Active coral restoration typically involves two interventions: crossing gametes to facilitate sexual larval propagation; and fragmenting, growing, and outplanting adult colonies to enhance asexual propagation. From an evolutionary perspective, the goal of these efforts is to establish self‐sustaining, sexually reproducing coral populations that have sufficient genetic and phenotypic variation to aAuthorsIliana B. Baums, Andrew C Baker, Sarah W Davies, Andrea G Grottoli, Carly D Kenkel, Sheila A Kitchen, Ilsa B. Kuffner, Todd C LaJeunesse, Mikhail V Matz, Margaret W Miller, John E Parkinson, Andrew A ShantzImproving estimates of coral reef construction and erosion with in-situ measurements
The decline in living coral since the 1970s has conspicuously slowed reef construction on a global scale, but the related process of reef erosion is less visible and not often quantified. Here we present new data on the constructional and deconstructional side of the carbonate-budget equation in the Florida Keys, U.S.A. We documented Orbicella spp. calcification rates at four offshore reefs and quAuthorsIlsa B. Kuffner, Lauren Toth, J. Harold Hudson, William B. Goodwin, Anastasios Stathakopoulos, Lucy Bartlett, Elizabeth M. WhitcherQuantifying uncertainty in Sr/Ca-based estimates of SST from the coral Orbicella faveolata
The strontium to calcium ratio (Sr/Ca) in aragonitic skeletons of massive corals provides a proxy for sea surface temperature (SST) that can be used to reconstruct paleoclimates across decades, centuries, and, potentially, millennia. Determining the reproducibility of Sr/Ca records among contemporaneous coral colonies from the same region is critical to quantifying uncertainties associated with thAuthorsJennifer A. Flannery, Julie N. Richey, Lauren Toth, Ilsa B. Kuffner, Richard Z. PooreA 3,000‐year lag between the geological and ecological shutdown of Florida's coral reefs
The global‐scale degradation of coral reefs has reached a critical threshold wherein further declines threaten both ecological functionality and the persistence of reef structure. Geological records can provide valuable insights into the long‐term controls on reef development that may be key to solving the modern coral‐reef crisis. Our analyses of new and existing coral‐reef cores from throughoutAuthorsLauren Toth, Ilsa B. Kuffner, Anastasios Stathakopoulos, Eugene A. ShinnA framework for identifying and characterising coral reef “oases” against a backdrop of degradation
Human activities have led to widespread ecological decline; however, the severity of degradation is spatially heterogeneous due to some locations resisting, escaping, or rebounding from disturbances.We developed a framework for identifying oases within coral reef regions using long‐term monitoring data. We calculated standardised estimates of coral cover (z‐scores) to distinguish sites that deviatAuthorsJames R. Guest, Peter J. Edmunds, Ruth D. Gates, Ilsa B. Kuffner, Andreas J Andersson, Brian B. Barnes, Iliana Chollett, Travis A. Courtney, Robin Elahi, Kevin Gross, Elizabeth A. Lenz, Satoshi Mitarai, Peter J. Mumby, Hannah R. Nelson, Britt A. Parker, Hollie M. Putnam, Caroline S. Rogers, Lauren TothSea-level rise could overwhelm coral reefs
An assessment of the capacity of coral reefs to grow fast enough to keep up with projected rises in sea level finds that most reefs will fall behind if nothing is done to restore them.AuthorsIlsa B. KuffnerPlasticity in skeletal characteristics of nursery-raised staghorn coral, Acropora cervicornis
Staghorn coral, Acropora cervicornis, is a threatened species and the primary focus of western Atlantic reef restoration efforts to date. We compared linear extension, calcification rate, and skeletal density of nursery-raised A. cervicornis branches reared for 6 months either on blocks attached to substratum or hanging from PVC trees in the water column. We demonstrate that branches grown on theAuthorsIlsa B. Kuffner, Erich Bartels, Anastasios Stathakopoulos, Ian C. Enochs, Graham Kolodziej, Lauren Toth, Derek P. ManzelloFidelity of the Sr/Ca proxy in recording ocean temperature in the western Atlantic coral Siderastrea siderea
Massive corals provide a useful archive of environmental variability, but careful testing of geochemical proxies in corals is necessary to validate the relationship between each proxy and environmental parameter throughout the full range of conditions experienced by the recording organisms. Here we use samples from a coral-growth study to test the hypothesis that Sr/Ca in the coral Siderastrea sidAuthorsIlsa B. Kuffner, Kelsey E. Roberts, Jennifer A. Flannery, Jennifer M. Morrison, Julie N. RicheyCollection methods and descriptions of coral cores extracted from massive corals in Dry Tortugas National Park, Florida, U.S.A.
Cores from living coral colonies were collected from Dry Tortugas National Park, Florida, U.S.A., to obtain skeletal records of past coral growth and allow geochemical reconstruction of environmental variables during the corals’ centuries-long lifespans. The samples were collected as part of the U.S. Geological Survey Coral Reef Ecosystems Studies project (http:/coastal.er.usgs.gov/crest) that proAuthorsMichael S. Weinzierl, Christopher D. Reich, T. Donald Hickey, Lucy A. Bartlett, Ilsa B. KuffnerMulti-species coral Sr/Ca-based sea-surface temperature reconstruction using Orbicella faveolata and Siderastrea siderea from the Florida Straits
We present new, monthly-resolved Sr/Ca-based sea-surface temperature (SST) records from two species of massive coral, Orbicella faveolata and Siderastrea siderea, from the Dry Tortugas National Park, FL, USA (DTNP). We combine these new records with published data from three additional S. siderea coral colonies to generate a 278-year long multi-species stacked Sr/Ca-SST record from DTNP. The compoAuthorsJennifer A. Flannery, Julie N. Richey, Kaustubh Thirumalai, Richard Z. Poore, Kristine L. DeLong - News
Below are news stories associated with this project.
Filter Total Items: 32 - FAQ
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...