As part of the USGS Coral Reef Project, we are developing new and unique oceanographic and environmental archives from coral skeleton records to better understand the compounding effects of land-use and environmental change on coral reef health.
The Problem
In addition to overfishing, physical damage, and coastal development, declining water quality is one of the most serious and sustained threats to coral reefs and is thought to be a primary cause of the global decline in shallow coral reefs. Isolating the effects of water quality stressors is difficult without determining the physical and biological controls on reef health. However, to evaluate recent trends and establish links to environmental and land-use change, there is a need to put these changes into a temporal and spatial context in order to identify thresholds and ranges of variability in the environment.
Our Approach
By measuring both physical changes (such as bioerosion, calcification, and growth rate) and chemical variations, records of climate change and land-use histories can be developed to supplement disperse observational networks and offer an accessible source of hydrologic, environmental, and land-use information in locations where instrumental records are not available. We are conducting innovative research to develop new and unique oceanographic and environmental archives from coral skeleton records to better understand the compounding effects of land-use and environmental change on coral reef health.
Specifically, we are conducting applied research to strategically address scientific knowledge gaps that impede informed management decisions related to planning and implementing activities in priority coral reef ecosystems and associated watersheds, such as identifying the causes and sources of pollution or estimating load reductions expected from implementation of specific management measures. We apply recently developed nutrient proxies to provide pre-instrumental records of nutrient loading to coral reefs in impacted sites. When these results are coupled to records of reef growth, we can develop a matrix of susceptibility in the context of nutrient loading and changes to carbonate chemistry. We aim to introduce coral-derived time-series information into monitoring and future management decisions to reduce and prevent land-based sources of pollution, including forecasting future impacts and response to load reductions expected from implementation of specific management tactics.
Caption for large image at top of page: Photograph of Asan-1 core (1.17 m in length) taken for image analysis using a Geotek Multi-Sensor Logger (MSL) system. Age dates were assigned based on year of collection, tissue layer, and band counting using annual density growth patterns captured in CT imagery. Image from Prouty et al., 2014
Please also see the associated efforts on the Coral Reef Ecosystem Studies (CREST) Project website:
Learn more about our related studies.
Coral Reef Ecosystem Studies (CREST)
Reef History and Climate Change
Holocene Coral-Reef Development
Below are data releases associated with this project.
Geochemistry time series and growth parameters from Tutuila, American Samoa coral record (ver. 2.0, June 2021)
Coral geochemistry time series from Kahekili, west Maui
Water-column environmental variables and accompanying discrete CTD measurements collected offshore the U.S. Mid- and South Atlantic
Radiocarbon dating of deep-sea black corals collected off the southeastern United States
Olowalu chronology and geochemistry time-series, West Maui
Below are publications associated with this project.
Rebounds, regresses, and recovery: A 15-year study of the coral reef community at Pila‘a, Kaua‘i after decades of natural and anthropogenic stress events
Bomb-produced radiocarbon across the South Pacific Gyre — A new record from American Samoa with utility for fisheries science
New geochemical tools for investigating resource and energy functions at deep-sea cold seeps using amino-acid δ15N in chemosymbiotic mussels (Bathymodiolus childressi)
Pulse sediment event does not impact the metabolism of a mixed coral reef community
Coral skeleton δ15N as a tracer of historic nutrient loading to a coral reef in Maui, Hawaii
A 50-year Sr/Ca time series from an enclosed, shallow-water Guam coral: In situ monitoring and extraction of a temperature trend, annual cycle, and ENSO and PDO signals
Carbonate system parameters of an algal-dominated reef along west Maui
Vulnerability of coral reefs to bioerosion from land-based sources of pollution
The use of passive membrane samplers to assess organic contaminant inputs at five coastal sites in west Maui, Hawaii
Reconstructing surface ocean circulation with 129I time series records from corals
Rare earth element behavior during groundwater – seawater mixing along the Kona Coast of Hawaii
Observations of nearshore groundwater discharge: Kahekili Beach Park submarine springs, Maui, Hawaii
- Overview
As part of the USGS Coral Reef Project, we are developing new and unique oceanographic and environmental archives from coral skeleton records to better understand the compounding effects of land-use and environmental change on coral reef health.
The Problem
In addition to overfishing, physical damage, and coastal development, declining water quality is one of the most serious and sustained threats to coral reefs and is thought to be a primary cause of the global decline in shallow coral reefs. Isolating the effects of water quality stressors is difficult without determining the physical and biological controls on reef health. However, to evaluate recent trends and establish links to environmental and land-use change, there is a need to put these changes into a temporal and spatial context in order to identify thresholds and ranges of variability in the environment.
Our Approach
Shimmering and bubbles indicate active freshwater discharging from the submarine groundwater vents along shallow reefs in west Maui. Corals are degraded and there is very little evidence of live coral cover. By measuring both physical changes (such as bioerosion, calcification, and growth rate) and chemical variations, records of climate change and land-use histories can be developed to supplement disperse observational networks and offer an accessible source of hydrologic, environmental, and land-use information in locations where instrumental records are not available. We are conducting innovative research to develop new and unique oceanographic and environmental archives from coral skeleton records to better understand the compounding effects of land-use and environmental change on coral reef health.
Specifically, we are conducting applied research to strategically address scientific knowledge gaps that impede informed management decisions related to planning and implementing activities in priority coral reef ecosystems and associated watersheds, such as identifying the causes and sources of pollution or estimating load reductions expected from implementation of specific management measures. We apply recently developed nutrient proxies to provide pre-instrumental records of nutrient loading to coral reefs in impacted sites. When these results are coupled to records of reef growth, we can develop a matrix of susceptibility in the context of nutrient loading and changes to carbonate chemistry. We aim to introduce coral-derived time-series information into monitoring and future management decisions to reduce and prevent land-based sources of pollution, including forecasting future impacts and response to load reductions expected from implementation of specific management tactics.
Caption for large image at top of page: Photograph of Asan-1 core (1.17 m in length) taken for image analysis using a Geotek Multi-Sensor Logger (MSL) system. Age dates were assigned based on year of collection, tissue layer, and band counting using annual density growth patterns captured in CT imagery. Image from Prouty et al., 2014
Please also see the associated efforts on the Coral Reef Ecosystem Studies (CREST) Project website:
Coral core section (left panel) from Guam, showing annual growth bands and the corresponding annual density values (right panel) for the upper 24 years. In the core section, a high- and low-density couplet constitutes an annual growth band. - Science
Learn more about our related studies.
Coral Reef Ecosystem Studies (CREST)
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...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. - Data
Below are data releases associated with this project.
Geochemistry time series and growth parameters from Tutuila, American Samoa coral record (ver. 2.0, June 2021)
Geochemical analysis (including radiocarbon, stable carbon isotope, and elemental composition) and growth parameters (including calcification rate, density, and extension information) were measured from a coral core collected from a reef off the southern side of Tutuila, American Samoa. The core was collected near Matautuloa Point on 8 April 2012 in collaboration with the Ecosystem Sciences DivisiCoral geochemistry time series from Kahekili, west Maui
Geochemical analysis (including stable boron, boron:calcium ratio, and carbon and oxygen isotopes) were measured from coral cores collected in July 2013 from the shallow reef at Kahekili in Kaanapali, west Maui, Hawaii from scleractinian Porites lobata.Water-column environmental variables and accompanying discrete CTD measurements collected offshore the U.S. Mid- and South Atlantic
Various water column variables, including salinity, dissolved inorganic nutrients, dissolved inorganic carbon, and radio-carbon isotopes were measured in samples collected using a Niskin-bottle rosette at selected depths from deepwater sites offshore the US Mid- and South Atlantic from September 2017 to April 2019. CTD (Conductivity Temperature Depth) data were also collected at each depth that aRadiocarbon dating of deep-sea black corals collected off the southeastern United States
Results of radiocarbon dating of deep-sea (500 m to 700 m) black corals are presented. These corals were collected off the southeastern United States as part of the Southeastern United States Deep-Sea Corals (SEADESC) Initiative.Olowalu chronology and geochemistry time-series, West Maui
Chronology and time-series geochemistry data of a coral core collected from Olowalu, West Maui, Hawaii. The chronology is based on density banding, radiocarbon bomb-curve, and uranium thorium dating techniques. The geochemistry time-series data contains major and minor elements over the length of the coral life span, as measured from laser ablation inductively coupled mass spectrometry (LA-ICP-MS) - Publications
Below are publications associated with this project.
Filter Total Items: 20Rebounds, regresses, and recovery: A 15-year study of the coral reef community at Pila‘a, Kaua‘i after decades of natural and anthropogenic stress events
Pila‘a reef on the north shore of Kaua‘i, Hawai‘i was subjected to a major flood event in 2001 that deposited extensive sediment on the reef flat, resulting in high coral mortality. To document potential recovery, this study replicated benthic and sediment surveys conducted immediately following the event and 15 years later. Coral cores were analyzed to determine coral growth rates and density. OuBomb-produced radiocarbon across the South Pacific Gyre — A new record from American Samoa with utility for fisheries science
Coral skeletal structures can provide a robust record of nuclear bomb produced 14C with valuable insight into air-sea exchange processes and water movement with applications to fisheries science. To expand these records in the South Pacific, a coral core from Tutuila Island, American Samoa was dated with density band counting covering a 59-yr period (1953–2012). Seasonal signals in elemental ratioNew geochemical tools for investigating resource and energy functions at deep-sea cold seeps using amino-acid δ15N in chemosymbiotic mussels (Bathymodiolus childressi)
In order to reconstruct the ecosystem structure of chemosynthetic environments in the fossil record, geochemical proxies must be developed. Here, we present a suite of novel compound-specific isotope parameters for tracing chemosynthetic production with a focus on understanding nitrogen dynamics in deep-sea cold seep environments. We examined the chemosymbiotic bivalve Bathymodiolus childressi froPulse sediment event does not impact the metabolism of a mixed coral reef community
Sedimentation can bury corals, cause physical abrasion, and alter both spectral intensity and quality; however, few studies have quantified the effects of sedimentation on coral reef metabolism in the context of episodic sedimentation events. Here, we present the first study to measure coral community metabolism - calcification and photosynthesis - in a manipulative mesocosm experiment simulatingCoral skeleton δ15N as a tracer of historic nutrient loading to a coral reef in Maui, Hawaii
Excess nutrient loading to nearshore environments has been linked to declining water quality and ecosystem health. Macro-algal blooms, eutrophication, and reduction in coral cover have been observed in West Maui, Hawaii, and linked to nutrient inputs from coastal submarine groundwater seeps. Here, we present a forty-year record of nitrogen isotopes (δ15N) of intra-crystalline coral skeletal organiA 50-year Sr/Ca time series from an enclosed, shallow-water Guam coral: In situ monitoring and extraction of a temperature trend, annual cycle, and ENSO and PDO signals
Located on the northern edge of the West Pacific Warm Pool and having a developed economy and modern infrastructure, Guam is well positioned and equipped for obtaining natural records of the west Pacific maritime paleoclimate. This study was a proof of concept to explore whether useful climate proxy records might be obtained from coral at readily accessible, even if geochemically nonoptimal, coastCarbonate system parameters of an algal-dominated reef along west Maui
Constraining coral reef metabolism and carbon chemistry dynamics are fundamental for understanding and predicting reef vulnerability to rising coastal CO2 concentrations and decreasing seawater pH. However, few studies exist along reefs occupying densely inhabited shorelines with known input from land-based sources of pollution. The shallow coral reefs off Kahekili, West Maui, are exposed to nutriVulnerability of coral reefs to bioerosion from land-based sources of pollution
Ocean acidification (OA), the gradual decline in ocean pH and [ ] caused by rising levels of atmospheric CO2, poses a significant threat to coral reef ecosystems, depressing rates of calcium carbonate (CaCO3) production, and enhancing rates of bioerosion and dissolution. As ocean pH and [ ] decline globally, there is increasing emphasis on managing local stressors that can exacerbate the vulnerabiThe use of passive membrane samplers to assess organic contaminant inputs at five coastal sites in west Maui, Hawaii
Five passive membrane samplers were deployed for 28 continuous days at select sites along and near the west Maui coastline to assess organic compounds and contaminant inputs to diverse, shallow coral reef ecosystems. Daily and weekly fluctuations in such inputs were captured on the membranes using integrative sampling. The distribution of organic compounds observed at these five coastal sites showReconstructing surface ocean circulation with 129I time series records from corals
The long-lived radionuclide 129I (half-life: 15.7 × 106 yr) is well-known as a useful environmental tracer. At present, the global 129I in surface water is about 1–2 orders of magnitude higher than pre-1960 levels. Since the 1990s, anthropogenic 129I produced from industrial nuclear fuels reprocessing plants has been the primary source of 129I in marine surface waters of the Atlantic and around thRare earth element behavior during groundwater – seawater mixing along the Kona Coast of Hawaii
Groundwater and seawater samples were collected from nearshore wells and offshore along the Kona Coast of the Big Island of Hawaii to investigate rare earth element (REE) behavior in local subterranean estuaries. Previous investigations showed that submarine groundwater discharge (SGD) is the predominant flux of terrestrial waters to the coastal ocean along the arid Kona Coast of Hawaii. GroundwatObservations of nearshore groundwater discharge: Kahekili Beach Park submarine springs, Maui, Hawaii
Study regionThe study region encompasses the nearshore, coastal waters off west Maui, Hawaii. Here abundant groundwater—that carries with it a strong land-based fingerprint—discharges into the coastal waters and over a coral reef.Study focusCoastal groundwater discharge is a ubiquitous hydrologic feature that has been shown to impact nearshore ecosystems and material budgets. A unique combined geo