A sediment core extracted from a salt marsh along the Herring River at the National Park Service’s Cape Cod National Seashore in Massachusetts. USGS scientists and partners are applying the mineral olivine to the marsh to study its role in capturing carbon dioxide in tidal wetlands. Credit: Kevin Kroeger, USGS.
Kevin D Kroeger, PhD
Kevin Kroeger has studied coastal ecosystems since 1990, with focus on a range of topics including fluxes and biogeochemistry of nitrogen in groundwater discharge to estuaries and wetlands, estuarine water quality, and carbon and greenhouse gas cycling and fluxes in coastal wetlands.
Kroeger is lead of the Biogeochemical Processes group at Woods Hole Coastal and Marine Science Center, and lead of a new project titled: Biogeochemical Drivers of Wetland Persistence and Feedbacks on Coastal Hazards The objectives of this Project are to provide guidance to federal (National Park Service, Fish & Wildlife Service, Army Corp of Engineers), state, local and private land owners and managers regarding stability and persistence of coastal wetlands under a range of hydrological management conditions and changing environmental conditions. Tidal wetlands provide critical services to society, including protection of infrastructure from coastal hazards, and habitat provision for economically important species. A large fraction of U.S. tidal wetlands, however, has been lost or degraded during recent centuries due to human actions, largely related to development and utilization of coastal lands. Feedbacks and interactions among natural and anthropogenic drivers have altered the stability and persistence of coastal wetlands. Decisions regarding hydrological management can alter the balance of organic matter production, retention and preservation, and thus management actions can either promote wetland persistence and resilience, or cause catastrophic loss of elevation, putting coastal infrastructure at increased risk of flooding or storm damage. This project impacts wetland management decisions. The contiguous U.S. has close to 2 million hectares of estuarine and marine wetlands. Nearly all of that area is under some level of management, with the federal government being the largest single manager. Land managers at FWS and NPS, and flood managers at ACOE, must make decisions regarding whether to spend substantial funds to maintain, repair and enhance water control structures under increasing rates of sea level change, or alternatively whether to reduce or remove hydrological management, to restore managed wetlands to more natural hydrology and enhance the capability of wetlands to build elevation over time, and to migrate landward. Society needs guidance and predictions regarding the result of those decisions for continued elevation gain, migration, and ongoing persistence of the wetlands.
Professional Experience
Present: Research Chemist, USGS Coastal and Marine Geology Program, Woods Hole Science Center, Woods Hole, MA
2004-2006: Mendenhall Fellow, US Geological Survey Geologic Division, St Petersburg, FL
2003-2004: Postdoctoral Scholar, Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA
1997-2003: Research Fellow and Teaching Fellow, Bos
Education and Certifications
PhD Boston University Marine Program (Biogeochemistry)
M.S. University of Connecticut (Marine Science)
B.A. University of Tennessee (Ecology)
Affiliations and Memberships*
Contributing Author: 2nd State of the Carbon Cycle Report (SOCCR-2), Chapter 15 Tidal Wetlands and Estuaries
Lead, USGS Woods Hole Coastal Biogeochemical Processes Project
Participant, 2017 EPA AFOL
Science and Products
Quantifying Restoration Impacts of Wetland Ecosystem Health and Carbon Export
Sea level Rise and Carbon Cycle Processes in Managed Coastal Wetlands
Wetland Carbon Working Group: Improving Methodologies and Estimates of Carbon and Greenhouse Gas Flux in Wetlands
Submarine Groundwater Discharge
Global Science and Data Network for Coastal Blue Carbon (SBC)
NASA-USGS National Blue Carbon Monitoring System
Environmental Geochemistry
Advancing understanding of ecosystem responses to climate change with warming experiments: what we have learned and what is unknown?
Geochemical Data Supporting Analysis of Fate and Transport of Nitrogen in the Nearshore Groundwater and Subterranean Estuary near East Falmouth, Massachusetts, 2015-2016
Inventory of Managed Coastal Wetlands in Delaware Bay and Delaware's Inland Bays
Restoration and Conservation Opportunity Maps for the conterminous U.S. (CONUS)
Nearshore groundwater seepage and geochemical data measured in 2015 at Guinea Creek, Rehoboth Bay, Delaware
Carbon dioxide and methane fluxes with supporting environmental data from coastal wetlands across Cape Cod, Massachusetts (ver 2.0, June 2022)
Saline tidal wetlands are important sites of carbon sequestration and produce negligible methane (CH4) emissions due to regular inundation with sulfate-rich seawater. Yet, widespread management of coastal hydrology has restricted vast areas of coastal wetlands to tidal exchange. These ecosystems often undergo impoundment and freshening, which in turn cause vegetation shifts like invasion by Phragm
Continuous Water Level, Salinity, and Temperature Data from Coastal Wetland Monitoring Wells, Cape Cod, Massachusetts (ver. 2.0, August 2022)
Static chamber gas fluxes and carbon and nitrogen isotope content of age-dated sediment cores from a Phragmites wetland in Sage Lot Pond, Massachusetts, 2013-2015
Geochemical data supporting analysis of fate and transport of nitrogen in the near shore groundwater and subterranean estuary near East Falmouth, Massachusetts, 2015
Collection, analysis, and age-dating of sediment cores from Herring River wetlands and other nearby wetlands in Wellfleet, Massachusetts, 2015-17
Collection, Analysis, and Age-Dating of Sediment Cores from Salt Marshes, Rhode Island, 2016
Collection, analysis, and age-dating of sediment cores from natural and restored salt marshes on Cape Cod, Massachusetts, 2015-16
Collection, analysis, and age-dating of sediment cores from mangrove and salt marsh ecosystems in Tampa Bay, Florida, 2015
A sediment core extracted from a salt marsh along the Herring River at the National Park Service’s Cape Cod National Seashore in Massachusetts. USGS scientists and partners are applying the mineral olivine to the marsh to study its role in capturing carbon dioxide in tidal wetlands. Credit: Kevin Kroeger, USGS.
A salt marsh along the Herring River at the National Park Service’s Cape Cod National Seashore in Massachusetts. USGS scientists and partners are applying the mineral olivine to the marsh to study its role in capturing carbon dioxide in tidal wetlands.
A salt marsh along the Herring River at the National Park Service’s Cape Cod National Seashore in Massachusetts. USGS scientists and partners are applying the mineral olivine to the marsh to study its role in capturing carbon dioxide in tidal wetlands.
A salt marsh along the Herring River at the National Park Service’s Cape Cod National Seashore in Massachusetts. USGS scientists and partners are applying the mineral olivine to the marsh to study its role in capturing carbon dioxide in tidal wetlands. Credit: Kevin Kroeger, USGS.
A salt marsh along the Herring River at the National Park Service’s Cape Cod National Seashore in Massachusetts. USGS scientists and partners are applying the mineral olivine to the marsh to study its role in capturing carbon dioxide in tidal wetlands. Credit: Kevin Kroeger, USGS.
Evidence of nitrate attenuation in intertidal and subtidal groundwater in a subterranean estuary at a Cape Cod embayment, East Falmouth, Massachusetts, 2015–16
Tracking mangrove condition changes using dense Landsat time series
U.S. Geological Survey climate science plan—Future research directions
The Coastal Carbon Library and Atlas: Open source soil data and tools supporting blue carbon research and policy
Carbonate chemistry and carbon sequestration driven by inorganic carbon outwelling from mangroves and saltmarshes
Practical guide to measuring wetland carbon pools and fluxes
Wetlands cover a small portion of the world, but have disproportionate influence on global carbon (C) sequestration, carbon dioxide and methane emissions, and aquatic C fluxes. However, the underlying biogeochemical processes that affect wetland C pools and fluxes are complex and dynamic, making measurements of wetland C challenging. Over decades of research, many observational, experimental, and
Geologic carbon management options for the North Atlantic-Appalachian Region
High-frequency variability of carbon dioxide fluxes in tidal water over a temperate salt marsh
Mapping methane reduction potential of tidal wetland restoration in the United States
Forecasting sea level rise-driven inundation in diked and tidally restricted coastal lowlands
Higher temperature sensitivity of ecosystem respiration in low marsh compared to high elevation marsh ecosystems
Mechanisms and magnitude of dissolved silica release from a New England salt marsh
Science and Products
Quantifying Restoration Impacts of Wetland Ecosystem Health and Carbon Export
Sea level Rise and Carbon Cycle Processes in Managed Coastal Wetlands
Wetland Carbon Working Group: Improving Methodologies and Estimates of Carbon and Greenhouse Gas Flux in Wetlands
Submarine Groundwater Discharge
Global Science and Data Network for Coastal Blue Carbon (SBC)
NASA-USGS National Blue Carbon Monitoring System
Environmental Geochemistry
Advancing understanding of ecosystem responses to climate change with warming experiments: what we have learned and what is unknown?
Geochemical Data Supporting Analysis of Fate and Transport of Nitrogen in the Nearshore Groundwater and Subterranean Estuary near East Falmouth, Massachusetts, 2015-2016
Inventory of Managed Coastal Wetlands in Delaware Bay and Delaware's Inland Bays
Restoration and Conservation Opportunity Maps for the conterminous U.S. (CONUS)
Nearshore groundwater seepage and geochemical data measured in 2015 at Guinea Creek, Rehoboth Bay, Delaware
Carbon dioxide and methane fluxes with supporting environmental data from coastal wetlands across Cape Cod, Massachusetts (ver 2.0, June 2022)
Saline tidal wetlands are important sites of carbon sequestration and produce negligible methane (CH4) emissions due to regular inundation with sulfate-rich seawater. Yet, widespread management of coastal hydrology has restricted vast areas of coastal wetlands to tidal exchange. These ecosystems often undergo impoundment and freshening, which in turn cause vegetation shifts like invasion by Phragm
Continuous Water Level, Salinity, and Temperature Data from Coastal Wetland Monitoring Wells, Cape Cod, Massachusetts (ver. 2.0, August 2022)
Static chamber gas fluxes and carbon and nitrogen isotope content of age-dated sediment cores from a Phragmites wetland in Sage Lot Pond, Massachusetts, 2013-2015
Geochemical data supporting analysis of fate and transport of nitrogen in the near shore groundwater and subterranean estuary near East Falmouth, Massachusetts, 2015
Collection, analysis, and age-dating of sediment cores from Herring River wetlands and other nearby wetlands in Wellfleet, Massachusetts, 2015-17
Collection, Analysis, and Age-Dating of Sediment Cores from Salt Marshes, Rhode Island, 2016
Collection, analysis, and age-dating of sediment cores from natural and restored salt marshes on Cape Cod, Massachusetts, 2015-16
Collection, analysis, and age-dating of sediment cores from mangrove and salt marsh ecosystems in Tampa Bay, Florida, 2015
A sediment core extracted from a salt marsh along the Herring River at the National Park Service’s Cape Cod National Seashore in Massachusetts. USGS scientists and partners are applying the mineral olivine to the marsh to study its role in capturing carbon dioxide in tidal wetlands. Credit: Kevin Kroeger, USGS.
A sediment core extracted from a salt marsh along the Herring River at the National Park Service’s Cape Cod National Seashore in Massachusetts. USGS scientists and partners are applying the mineral olivine to the marsh to study its role in capturing carbon dioxide in tidal wetlands. Credit: Kevin Kroeger, USGS.
A salt marsh along the Herring River at the National Park Service’s Cape Cod National Seashore in Massachusetts. USGS scientists and partners are applying the mineral olivine to the marsh to study its role in capturing carbon dioxide in tidal wetlands.
A salt marsh along the Herring River at the National Park Service’s Cape Cod National Seashore in Massachusetts. USGS scientists and partners are applying the mineral olivine to the marsh to study its role in capturing carbon dioxide in tidal wetlands.
A salt marsh along the Herring River at the National Park Service’s Cape Cod National Seashore in Massachusetts. USGS scientists and partners are applying the mineral olivine to the marsh to study its role in capturing carbon dioxide in tidal wetlands. Credit: Kevin Kroeger, USGS.
A salt marsh along the Herring River at the National Park Service’s Cape Cod National Seashore in Massachusetts. USGS scientists and partners are applying the mineral olivine to the marsh to study its role in capturing carbon dioxide in tidal wetlands. Credit: Kevin Kroeger, USGS.
Evidence of nitrate attenuation in intertidal and subtidal groundwater in a subterranean estuary at a Cape Cod embayment, East Falmouth, Massachusetts, 2015–16
Tracking mangrove condition changes using dense Landsat time series
U.S. Geological Survey climate science plan—Future research directions
The Coastal Carbon Library and Atlas: Open source soil data and tools supporting blue carbon research and policy
Carbonate chemistry and carbon sequestration driven by inorganic carbon outwelling from mangroves and saltmarshes
Practical guide to measuring wetland carbon pools and fluxes
Wetlands cover a small portion of the world, but have disproportionate influence on global carbon (C) sequestration, carbon dioxide and methane emissions, and aquatic C fluxes. However, the underlying biogeochemical processes that affect wetland C pools and fluxes are complex and dynamic, making measurements of wetland C challenging. Over decades of research, many observational, experimental, and
Geologic carbon management options for the North Atlantic-Appalachian Region
High-frequency variability of carbon dioxide fluxes in tidal water over a temperate salt marsh
Mapping methane reduction potential of tidal wetland restoration in the United States
Forecasting sea level rise-driven inundation in diked and tidally restricted coastal lowlands
Higher temperature sensitivity of ecosystem respiration in low marsh compared to high elevation marsh ecosystems
Mechanisms and magnitude of dissolved silica release from a New England salt marsh
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government