Scientists from the Florence Bascom Geoscience Center first sampled four islands in Florida Bay, Everglades National Park, in April 2014 to collect cores to study sea level rise and storm history in the region. In September 2017, Hurricane Irma (a category 4 storm at landfall in the Florida Keys) passed just to the west of our field sites. The western-mo
G. Lynn Wingard, Ph.D.
Lynn Wingard’s research focus is on the application of paleoecologic techniques to the interpretation of Holocene marine and estuarine ecosystems. Current emphasis is on deriving baseline environmental data for Greater Everglades Ecosystem Restoration resource managers and on examining the interaction of climate and sea level on south Florida’s coastline in the Holocene.
Professional Experience
1991-Present Research Geologist, U.S. Geological Survey
Lynn Wingard has been a Research Geologist with the USGS since 1991. She has conducted biostratigraphic and paleoecologic research on Mesozoic and Cenozoic Atlantic and Gulf Coastal Plain sediments throughout her career. Her early research focused on molluscan taxonomy and evolution across the Cretaceous Tertiary boundary and she examined the role of taxonomic assignments in calculations of extinction at the boundary. Investigations into the subsurface geology and paleoenvironments in Florida led to a reclassification of the subsurface Oligocene units and she assisted the Florida State Geologic Survey in their state map efforts.
Beginning in 1994, Lynn has served as Principal Investigator on projects related to the Greater Everglades Ecosystem Restoration as part of the USGS Priority Ecosystem Science Program and she has served in a number of advisory roles related to this research. Her work has helped define salinity targets for Florida’s southern estuaries and has contributed to estimating historic freshwater flow through the wetlands. Her collaboration with Everglades resource managers has demonstrated the importance of paleoecology and the emerging field of conservation paleobiology in providing valuable scientific information to guide restoration efforts. Recent work has focused on sea level rise and storm history and how these driving factors have shaped the south Florida coastline over the last 5,000 years and what this tells us in terms of future projections of coastal change.
Science Leadership and Advisory Roles
- 1993: helped draft Program Implementation Plan for USGS South Florida Ecosystem Initiative
- 2001-Present: member of 6 CERP - Comprehensive Everglades Restoration Plan - Teams; currently serving on Southern Coastal Systems Sub-Team and Biscayne Bay Southeast Everglades Ecosystem Restoration Eco-subteam
- 2002: helped draft DOI and USGS Science Plans in Support of Greater Everglades Ecosystem Restoration
Education and Certifications
1979 BS (Geology / Biology) The College of William & Mary, Williamsburg VA
1983 MS (Geology) George Washington University, Washington DC
1990 PhD (Geology) George Washington University, Washington DC
Science and Products
Determining Target Salinity Values for Restoration of the Estuaries of the Greater Everglades
Sea Level Rise and Climate: Impacts on the Greater Everglades Ecosystem and Restoration
Scientists from the Florence Bascom Geoscience Center first sampled four islands in Florida Bay, Everglades National Park, in April 2014 to collect cores to study sea level rise and storm history in the region. In September 2017, Hurricane Irma (a category 4 storm at landfall in the Florida Keys) passed just to the west of our field sites. The western-mo
In Photo: Berm of Jim Foot Key about 1.5 years after Hurricane Irma. The red circle indicates the same position as shown in the April 2014 photo. The mature mangrove trees have not recovered from the storm.
In Photo: Berm of Jim Foot Key about 1.5 years after Hurricane Irma. The red circle indicates the same position as shown in the April 2014 photo. The mature mangrove trees have not recovered from the storm.
In Photo: Eastern berm of Jim Foot Key, April 2019. This photo taken from Florida Bay, looking in toward the center of the island (now covered in water). The arrow points toward a breach in the berm, first noted in 2014, but the cut has deepened significantly after Hurricane Irma, and the island interior
In Photo: Eastern berm of Jim Foot Key, April 2019. This photo taken from Florida Bay, looking in toward the center of the island (now covered in water). The arrow points toward a breach in the berm, first noted in 2014, but the cut has deepened significantly after Hurricane Irma, and the island interior
A USGS researcher conducts fieldwork on Buttonwood Key, an island in Florida Bay, to determine the impacts of Hurricane Irma. The storm left thick deposits of mud on the island, which are being measured, sampled and photographed. Many of the islands in Florida Bay have open mudflats in the center, surrounded by mangroves on the perimeter.
A USGS researcher conducts fieldwork on Buttonwood Key, an island in Florida Bay, to determine the impacts of Hurricane Irma. The storm left thick deposits of mud on the island, which are being measured, sampled and photographed. Many of the islands in Florida Bay have open mudflats in the center, surrounded by mangroves on the perimeter.
In Photo: The red circle indicates the same position as shown in the April 2014 photo. The mangroves have lost all their leaves and the berm is significantly thinner following the storm.
In Photo: The red circle indicates the same position as shown in the April 2014 photo. The mangroves have lost all their leaves and the berm is significantly thinner following the storm.
In Photo: View south/southeast along eastern shoreline in April 2014 shows a dense berm of mangrove trees. The bay is not visible.
In Photo: View south/southeast along eastern shoreline in April 2014 shows a dense berm of mangrove trees. The bay is not visible.
Tangled web of prop roots from red mangrove trees, intermixed with black mangroves and white mangroves farther back in the forest. Mangrove forests cover much of the southwestern coastal region of Everglades National Park. The red mangroves are the most salinity tolerant and grow with their prop roots in the water or within the range of high tide.
Tangled web of prop roots from red mangrove trees, intermixed with black mangroves and white mangroves farther back in the forest. Mangrove forests cover much of the southwestern coastal region of Everglades National Park. The red mangroves are the most salinity tolerant and grow with their prop roots in the water or within the range of high tide.
Alligators are very abundant in the freshwater wetlands of Everglades National Park and can usually be seen along the Anhinga trail in the park, especially when water levels are low. This ~5-foot gator is resting on exposed limestone bedrock alongside the trail.
Alligators are very abundant in the freshwater wetlands of Everglades National Park and can usually be seen along the Anhinga trail in the park, especially when water levels are low. This ~5-foot gator is resting on exposed limestone bedrock alongside the trail.
An American Alligator in Everglades National Park. The species was once listed as Endangered, but was removed in 1987 after a successful recovery.
An American Alligator in Everglades National Park. The species was once listed as Endangered, but was removed in 1987 after a successful recovery.
American crocodiles are restricted in their range within the USA to southern Florida. Decisions on restoration of the Everglades must incorporate protection for this threatened species.
American crocodiles are restricted in their range within the USA to southern Florida. Decisions on restoration of the Everglades must incorporate protection for this threatened species.
Anhingas are considered primitive birds because they do not produce oils like ducks and other water fowl. They must dry their feathers periodically in order to fly or even remain buoyant, so they remain perched for significant periods of time with wings outstretched.
Anhingas are considered primitive birds because they do not produce oils like ducks and other water fowl. They must dry their feathers periodically in order to fly or even remain buoyant, so they remain perched for significant periods of time with wings outstretched.
Water levels are critical to the life cycle of alligators. Part of the Everglades restoration plan is to determine what historical water levels and flow rates supported healthy alligator populations.
Water levels are critical to the life cycle of alligators. Part of the Everglades restoration plan is to determine what historical water levels and flow rates supported healthy alligator populations.
Great Blue Herons are found throughout much of North America, but are always associated with water. Because they fish by sight, they need relatively shallow water. Release of too much water through the canals north of the Everglades can interfere with their ability to find food.
Great Blue Herons are found throughout much of North America, but are always associated with water. Because they fish by sight, they need relatively shallow water. Release of too much water through the canals north of the Everglades can interfere with their ability to find food.
Using mollusks as indicators of restoration in nearshore zones of south Florida's estuaries
Review of ESA SYMP 7: A dynamic perspective on ecosystem restoration–establishing temporal connectivity at the intersection between paleoecology and restoration ecology
Postcards from the field
Climate, sea level, and people - Changing South Florida's mangrove coast
Estimating late 19th century hydrology in the Greater Everglades Ecosystem: An integration of paleoecologic data and models
Impacts of Hurricane Irma on Florida Bay Islands, Everglades National Park, U.S.A.
Rapid inundation of the southern Florida coastline despite low relative sea-level rise rates during the late-Holocene
A North American Hydroclimate Synthesis (NAHS) of the Common Era
Application of paleoecology to ecosystem restoration: A case study from south Florida’s estuaries
The role of paleoecology in restoration and resource management—The past as a guide to future decision-making: Review and example from the Greater Everglades Ecosystem, U.S.A
Application of molluscan analyses to the reconstruction of past environmental conditions in estuaries
Biological indicators of changes in water quality and habitats of the coastal and estuarine areas of the Greater Everglades Ecosystem; Chapter 11
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
- Science
Determining Target Salinity Values for Restoration of the Estuaries of the Greater Everglades
The Greater Everglades Ecosystem, which includes Everglades National Park and Biscayne National Park, experienced significant alterations in the 20th century with the construction of canals to divert water, water management practices, growth of agriculture, and the rapidly expanding urban population of Miami and south Florida. In the 1990s a federal, state, and local effort to restore the Greater...Sea Level Rise and Climate: Impacts on the Greater Everglades Ecosystem and Restoration
The Greater Everglades Ecosystem covers much of south Florida, and the highest areas are only a few meters above sea level. Predictions of sea level rise and changes in storm intensity for the 21st century are particularly concerning to the urban population of Miami and the east coast, but also represent a challenge to Everglades National Park and Biscayne National Park resource managers. The... - Multimedia
Impacts to island in Florida Bay following Hurricane Irma, 2017Impacts to island in Florida Bay following Hurricane Irma, 2017
Scientists from the Florence Bascom Geoscience Center first sampled four islands in Florida Bay, Everglades National Park, in April 2014 to collect cores to study sea level rise and storm history in the region. In September 2017, Hurricane Irma (a category 4 storm at landfall in the Florida Keys) passed just to the west of our field sites. The western-mo
Scientists from the Florence Bascom Geoscience Center first sampled four islands in Florida Bay, Everglades National Park, in April 2014 to collect cores to study sea level rise and storm history in the region. In September 2017, Hurricane Irma (a category 4 storm at landfall in the Florida Keys) passed just to the west of our field sites. The western-mo
Berm at Jim Foot Key, Florida (2019)In Photo: Berm of Jim Foot Key about 1.5 years after Hurricane Irma. The red circle indicates the same position as shown in the April 2014 photo. The mature mangrove trees have not recovered from the storm.
In Photo: Berm of Jim Foot Key about 1.5 years after Hurricane Irma. The red circle indicates the same position as shown in the April 2014 photo. The mature mangrove trees have not recovered from the storm.
Breach in Eastern Berm of Jim Foot Key, FloridaIn Photo: Eastern berm of Jim Foot Key, April 2019. This photo taken from Florida Bay, looking in toward the center of the island (now covered in water). The arrow points toward a breach in the berm, first noted in 2014, but the cut has deepened significantly after Hurricane Irma, and the island interior
In Photo: Eastern berm of Jim Foot Key, April 2019. This photo taken from Florida Bay, looking in toward the center of the island (now covered in water). The arrow points toward a breach in the berm, first noted in 2014, but the cut has deepened significantly after Hurricane Irma, and the island interior
Fieldwork on Florida Bay IslandsA USGS researcher conducts fieldwork on Buttonwood Key, an island in Florida Bay, to determine the impacts of Hurricane Irma. The storm left thick deposits of mud on the island, which are being measured, sampled and photographed. Many of the islands in Florida Bay have open mudflats in the center, surrounded by mangroves on the perimeter.
A USGS researcher conducts fieldwork on Buttonwood Key, an island in Florida Bay, to determine the impacts of Hurricane Irma. The storm left thick deposits of mud on the island, which are being measured, sampled and photographed. Many of the islands in Florida Bay have open mudflats in the center, surrounded by mangroves on the perimeter.
Berm at Jim Foot Key, Florida (2018)In Photo: The red circle indicates the same position as shown in the April 2014 photo. The mangroves have lost all their leaves and the berm is significantly thinner following the storm.
In Photo: The red circle indicates the same position as shown in the April 2014 photo. The mangroves have lost all their leaves and the berm is significantly thinner following the storm.
Berm at Jim Foot Key, Florida (2014)In Photo: View south/southeast along eastern shoreline in April 2014 shows a dense berm of mangrove trees. The bay is not visible.
In Photo: View south/southeast along eastern shoreline in April 2014 shows a dense berm of mangrove trees. The bay is not visible.
Mangrove forest, Shark River Slough, Everglades National ParkMangrove forest, Shark River Slough, Everglades National ParkTangled web of prop roots from red mangrove trees, intermixed with black mangroves and white mangroves farther back in the forest. Mangrove forests cover much of the southwestern coastal region of Everglades National Park. The red mangroves are the most salinity tolerant and grow with their prop roots in the water or within the range of high tide.
Tangled web of prop roots from red mangrove trees, intermixed with black mangroves and white mangroves farther back in the forest. Mangrove forests cover much of the southwestern coastal region of Everglades National Park. The red mangroves are the most salinity tolerant and grow with their prop roots in the water or within the range of high tide.
Alligator Resting in Afternoon SunAlligators are very abundant in the freshwater wetlands of Everglades National Park and can usually be seen along the Anhinga trail in the park, especially when water levels are low. This ~5-foot gator is resting on exposed limestone bedrock alongside the trail.
Alligators are very abundant in the freshwater wetlands of Everglades National Park and can usually be seen along the Anhinga trail in the park, especially when water levels are low. This ~5-foot gator is resting on exposed limestone bedrock alongside the trail.
American Alligator Close UpAn American Alligator in Everglades National Park. The species was once listed as Endangered, but was removed in 1987 after a successful recovery.
An American Alligator in Everglades National Park. The species was once listed as Endangered, but was removed in 1987 after a successful recovery.
American CrocodileAmerican crocodiles are restricted in their range within the USA to southern Florida. Decisions on restoration of the Everglades must incorporate protection for this threatened species.
American crocodiles are restricted in their range within the USA to southern Florida. Decisions on restoration of the Everglades must incorporate protection for this threatened species.
Anhinga Drying Its FeathersAnhingas are considered primitive birds because they do not produce oils like ducks and other water fowl. They must dry their feathers periodically in order to fly or even remain buoyant, so they remain perched for significant periods of time with wings outstretched.
Anhingas are considered primitive birds because they do not produce oils like ducks and other water fowl. They must dry their feathers periodically in order to fly or even remain buoyant, so they remain perched for significant periods of time with wings outstretched.
Alligator Resting on Limestone Bedrock in Taylor SloughAlligator Resting on Limestone Bedrock in Taylor SloughWater levels are critical to the life cycle of alligators. Part of the Everglades restoration plan is to determine what historical water levels and flow rates supported healthy alligator populations.
Water levels are critical to the life cycle of alligators. Part of the Everglades restoration plan is to determine what historical water levels and flow rates supported healthy alligator populations.
Great Blue HeronGreat Blue Herons are found throughout much of North America, but are always associated with water. Because they fish by sight, they need relatively shallow water. Release of too much water through the canals north of the Everglades can interfere with their ability to find food.
Great Blue Herons are found throughout much of North America, but are always associated with water. Because they fish by sight, they need relatively shallow water. Release of too much water through the canals north of the Everglades can interfere with their ability to find food.
- Publications
Filter Total Items: 36
Using mollusks as indicators of restoration in nearshore zones of south Florida's estuaries
Current south Florida ecosystem restoration efforts are focused on restoring more natural freshwater flow through the wetlands and into the estuaries to reestablish natural salinity gradients, particularly in the nearshore zones. Indicator taxa are used to monitor and assess restoration progress and the current suite of biota used for the estuaries in south Florida (Biscayne Bay, Florida Bay, andAuthorsG. Lynn Wingard, Bethany Stackhouse, Andre DanielsReview of ESA SYMP 7: A dynamic perspective on ecosystem restoration–establishing temporal connectivity at the intersection between paleoecology and restoration ecology
Landscape connectivity is vital not only spatially, but also temporally; as ecosystems change, it is important to be aware of past, present, and future variables that may impact ecosystem function and biodiversity. As climate and environments continue to change, choosing appropriate restoration targets is becoming more challenging. By considering the paleoecological and paleoenvironmental record fAuthorsRachel Reid, Jenny McGuire, Jens-Christiane Svenning, G. Lynn Wingard, David Moreno-MateosPostcards from the field
My research focuses on pre-20th century conditions in the Greater Everglades Ecosystem of south Florida to provide the context for resource managers to set targets for restoration. A primary goal of Everglades restoration is to re-establish more natural delivery of freshwater to the wetlands and estuaries in the region. By analyzing biotic assemblages from sediment cores collected from Florida BAuthorsG. Lynn WingardClimate, sea level, and people - Changing South Florida's mangrove coast
South Florida’s coast is a land of contrasts that appeals to almost everyone, whether they seek out quiet natural environments along the mangrove waterways and in the wilderness of the Everglades or vibrant international culture in Miami. Yet this paradise is threatened by a number of forces – changing climate, rising sea level, and too many people, to name a few. Florida’s past is filled with stoAuthorsG. Lynn WingardEstimating late 19th century hydrology in the Greater Everglades Ecosystem: An integration of paleoecologic data and models
Determining hydrologic conditions prior to instrumental records is a challenge for restoration of freshwater ecosystems worldwide. Paleoecologic data provide this information on past conditions and when these data are used to adjust hydrologic models, allow conditions to be hindcast that may not be directly estimated from the paleo-data alone. In this context, the paleo-data provide real-world esAuthorsFrank E. Marshall, Christopher E. Bernhardt, G. Lynn WingardImpacts of Hurricane Irma on Florida Bay Islands, Everglades National Park, U.S.A.
Hurricane Irma made landfall in south Florida, USA, on September 10, 2017 as a category 4 storm. In January 2018, fieldwork was conducted on four previously (2014) sampled islands in Florida Bay, Everglades National Park to examine changes between 2014 and 2018. The objectives were to determine if the net impact of the storm was gain or loss of island landmass and/or elevation; observe and quantifAuthorsG. Lynn Wingard, Sarah E. Bergstresser, Bethany Stackhouse, Miriam Jones, Marci E. Marot, Kristen Hoefke, Andre Daniels, Katherine KellerRapid inundation of the southern Florida coastline despite low relative sea-level rise rates during the late-Holocene
Sediment cores from Florida Bay, Everglades National Park were examined to determine ecosystem response to relative sea-level rise (RSLR) over the Holocene. High-resolution multiproxy analysis from four sites show freshwater wetlands transitioned to mangrove environments 4–3.6 ka, followed by estuarine environments 3.4–2.8 ka, during a period of enhanced climate variability. We calculate a RSLR raAuthorsMiriam Jones, G. Lynn Wingard, Bethany Stackhouse, Katherine Keller, Debra A. Willard, Marci E. Marot, Bryan D. Landacre, Christopher E. BernhardtA North American Hydroclimate Synthesis (NAHS) of the Common Era
This study presents a synthesis of century-scale hydroclimate variations in North America for the Common Era (last 2000 years) using new age models of previously published multiple proxy-based paleoclimate data. This North American Hydroclimate Synthesis (NAHS) examines regional hydroclimate patterns and related environmental indicators, including vegetation, lake water elevation, stream flow andAuthorsJessica R. Rodysill, Lesleigh Anderson, Thomas M. Cronin, Miriam C. Jones, Robert S. Thompson, David B. Wahl, Debra A. Willard, Jason A. Addison, Jay R. Alder, Katherine H. Anderson, Lysanna Anderson, John A. Barron, Christopher E. Bernhardt, Steven W. Hostetler, Natalie M. Kehrwald, Nicole Khan, Julie N. Richey, Scott W. Starratt, Laura E. Strickland, Michael Toomey, Claire C. Treat, G. Lynn WingardByWater Resources Mission Area, Climate Research and Development Program, Energy Resources Program, Groundwater and Streamflow Information Program, Mineral Resources Program, National Laboratories Program, Science and Decisions Center, Florence Bascom Geoscience Center, Geology, Minerals, Energy, and Geophysics Science Center, Geosciences and Environmental Change Science Center, St. Petersburg Coastal and Marine Science CenterApplication of paleoecology to ecosystem restoration: A case study from south Florida’s estuaries
Paleoecological analyses of biotic assemblages from cores collected throughout south Florida’s estuaries indicate gradually increasing salinities over approximately the last 2000 years, consistent with rising sea level. Around the beginning of the twentieth century these gradual patterns of change began to shift, corresponding to the beginning of human alteration of the environment via canal constAuthorsG. Lynn WingardThe role of paleoecology in restoration and resource management—The past as a guide to future decision-making: Review and example from the Greater Everglades Ecosystem, U.S.A
Resource managers around the world are challenged to develop feasible plans for sustainable conservation and/or restoration of the lands, waters, and wildlife they administer—a challenge made greater by anticipated climate change and associated effects over the next century. Increasingly, paleoecologic and geologic archives are being used to extend the period of record of observed data and provideAuthorsG. Lynn Wingard, Christopher E. Bernhardt, Anna WachnickaApplication of molluscan analyses to the reconstruction of past environmental conditions in estuaries
Molluscs possess a number of attributes that make them an excellent source of past environmental conditions in estuaries: they are common in estuarine environments; they typically have hard shells and are usually well preserved in sediments; they are relatively easy to detect in the environment; they have limited mobility as adults; they grow by incremental addition of layers to their shells; andAuthorsG. Lynn Wingard, Donna SurgeBiological indicators of changes in water quality and habitats of the coastal and estuarine areas of the Greater Everglades Ecosystem; Chapter 11
This chapter summarizes the application of various biological indicators to studying the anthropogenic and natural changes in water quality and habitats that have occurred in the coastal and estuarine areas of the Greater Everglades ecosystem.AuthorsAnna Wachnicka, G. Lynn WingardNon-USGS Publications**
Marshall, F.E., Bernhardt, C.B., and Wingard, G.L. 2020. Estimating late 19th century hydrology in the Greater Everglades Ecosystem: An integration of paleoecologic data and models. Frontiers in Environmental Science: Freshwater Science. DOI: 10.3389/fenvs.2020.00003**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.