Michael Johannes Osland, Ph.D.
Michael Osland is a Research Ecologist at the USGS Wetland and Aquatic Research Center in Lafayette, Louisiana.
In broad terms, his research examines the effects of global change on ecosystems and the implications for ecological conservation and restoration. Much of his research focuses on wetland ecosystems at the dynamic interface between land and ocean (mangrove forests, salt marshes).
RESEARCH AREAS: ecology, global change, climate change, plant ecology, wetlands, restoration ecology, ecosystem ecology, biogeography, mangrove forests, salt marshes, sea-level rise
EDUCATION
Ph.D., Ecology, Duke University, 2009
B.A., Biology, Willamette University, 2000
PROFESSIONAL POSITIONS
2011-Present Research Ecologist, U.S. Geological Survey, Wetland and Aquatic Research Center, Louisiana, USA
2009-2011 Postdoctoral Research Scientist, U.S. Environmental Protection Agency, Gulf Ecology Division, Florida, USA
2006-2007 Fulbright Fellow; via the Organization for Tropical Studies, Costa Rica
2003-2009 Graduate Student, Duke University, North Carolina, USA
2000-2003 U.S. Peace Corps Volunteer, Agroforestry, El Salvador
Science and Products
Advancing mangrove macroecology
Linear and nonlinear effects of temperature and precipitation on ecosystem properties in tidal saline wetlands
Assessing coastal wetland vulnerability to sea-level rise along the northern Gulf of Mexico coast: Gaps and opportunities for developing a coordinated regional sampling network
Barrier island habitat map and vegetation survey—Dauphin Island, Alabama, 2015
Mangrove species' responses to winter air temperature extremes in China
Created mangrove wetlands store belowground carbon and surface elevation change enables them to adjust to sea-level rise
Macroclimatic change expected to transform coastal wetland ecosystems this century
Climatic controls on the global distribution, abundance, and species richness of mangrove forests
Mangrove expansion and contraction at a poleward range limit: Climate extremes and land-ocean temperature gradients
Barriers to and opportunities for landward migration of coastal wetlands with sea-level rise
Salt marsh-mangrove ecotones: using structural gradients to investigate the effects of woody plant encroachment on plant-soil interactions and ecosystem carbon pools
The physiology of mangrove trees with changing climate
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.
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Advancing mangrove macroecology
Mangrove forests provide a wide range of ecosystem services to society, yet they are among the most anthropogenically impacted coastal ecosystems in the world. In this chapter, we discuss and provide examples for how macroecology can advance our understanding of mangrove ecosystems. Macroecology is broadly defined as a discipline that uses statistical analyses to investigate large-scale, universalAuthorsVictor H. Rivera-Monroy, Michael J. Osland, John W. Day, Santanu Ray, Andre S. Rovai, Richard H. Day, Joyita MukherjeeLinear and nonlinear effects of temperature and precipitation on ecosystem properties in tidal saline wetlands
Climate greatly influences the structure and functioning of tidal saline wetland ecosystems. However, there is a need to better quantify the effects of climatic drivers on ecosystem properties, particularly near climate-sensitive ecological transition zones. Here, we used climate- and literature-derived ecological data from tidal saline wetlands to test hypotheses regarding the influence of climatAuthorsLaura C. Feher, Michael J. Osland, Kereen T. Griffith, James B. Grace, Rebecca J. Howard, Camille L. Stagg, Nicholas M. Enwright, Ken W. Krauss, Christopher A. Gabler, Richard H. Day, Kerrylee RogersAssessing coastal wetland vulnerability to sea-level rise along the northern Gulf of Mexico coast: Gaps and opportunities for developing a coordinated regional sampling network
Coastal wetland responses to sea-level rise are greatly influenced by biogeomorphic processes that affect wetland surface elevation. Small changes in elevation relative to sea level can lead to comparatively large changes in ecosystem structure, function, and stability. The surface elevation table-marker horizon (SET-MH) approach is being used globally to quantify the relative contributions of proAuthorsMichael J. Osland, Kereen T. Griffith, Jack C. Larriviere, Laura C. Feher, Donald R. Cahoon, Nicholas M. Enwright, David A. Oster, John M. Tirpak, Mark S. Woodrey, Renee C. Collini, Joseph J. Baustian, Joshua L. Breithaupt, Julia A Cherry, Jeremy R. Conrad, Nicole Cormier, Carlos A. Coronado-Molina, Joseph F. Donoghue, Sean A. Graham, Jennifer W. Harper, Mark W. Hester, Rebecca J. Howard, Ken W. Krauss, Daniel Kroes, Robert R. Lane, Karen L. McKee, Irving A. Mendelssohn, Beth A. Middleton, Jena A. Moon, Sarai Piazza, Nicole M. Rankin, Fred H. Sklar, Gregory D. Steyer, Kathleen M. Swanson, Christopher M. Swarzenski, William Vervaeke, Jonathan M Willis, K. Van WilsonBarrier island habitat map and vegetation survey—Dauphin Island, Alabama, 2015
Barrier islands are dynamic environments due to their position at the land-sea interface. Storms, waves, tides, currents, and relative sea-level rise are powerful forces that shape barrier island geomorphology and habitats (for example, beach, dune, marsh, and forest). Hurricane Katrina in 2005 and the Deep Water Horizon oil spill in 2010 are two major events that have affected habitats and naturaAuthorsNicholas M. Enwright, Sinéad M. Borchert, Richard H. Day, Laura C. Feher, Michael J. Osland, Lei Wang, Hongqing WangMangrove species' responses to winter air temperature extremes in China
The global distribution and diversity of mangrove forests is greatly influenced by the frequency and intensity of winter air temperature extremes. However, our understanding of how different mangrove species respond to winter temperature extremes has been lacking because extreme freezing and chilling events are, by definition, relatively uncommon and also difficult to replicate experimentally. InAuthorsLuzhen Chen, Wenqing Wang, Qingshun Q. Li, Yihui Zhang, Shengchang Yang, Michael J. Osland, Jinliang Huang, Congjiao PengCreated mangrove wetlands store belowground carbon and surface elevation change enables them to adjust to sea-level rise
Mangrove wetlands provide ecosystem services for millions of people, most prominently by providing storm protection, food and fodder. Mangrove wetlands are also valuable ecosystems for promoting carbon (C) sequestration and storage. However, loss of mangrove wetlands and these ecosystem services are a global concern, prompting the restoration and creation of mangrove wetlands as a potential solutiAuthorsKen W. Krauss, Nicole Cormier, Michael J. Osland, Matthew L. Kirwan, Camille L. Stagg, Janet A. Nestlerode, Marc J. Russell, Andrew From, Amanda C. Spivak, Darrin D. Dantin, James E. Harvey, Alejandro E. AlmarioMacroclimatic change expected to transform coastal wetland ecosystems this century
Coastal wetlands, existing at the interface between land and sea, are highly vulnerable to climate change. Macroclimate (for example, temperature and precipitation regimes) greatly influences coastal wetland ecosystem structure and function. However, research on climate change impacts in coastal wetlands has concentrated primarily on sea-level rise and largely ignored macroclimatic drivers, despitAuthorsChristopher A. Gabler, Michael J. Osland, James B. Grace, Camille L. Stagg, Richard H. Day, Stephen B. Hartley, Nicholas M. Enwright, Andrew From, Meagan L. McCoy, Jennie L. McLeodClimatic controls on the global distribution, abundance, and species richness of mangrove forests
Mangrove forests are highly productive tidal saline wetland ecosystems found along sheltered tropical and subtropical coasts. Ecologists have long assumed that climatic drivers (i.e., temperature and rainfall regimes) govern the global distribution, structure, and function of mangrove forests. However, data constraints have hindered the quantification of direct climate-mangrove linkages in many paAuthorsMichael J. Osland, Laura C. Feher, Kereen Griffith, Kyle C. Cavanaugh, Nicholas M. Enwright, Richard H. Day, Camille L. Stagg, Ken W. Krauss, Rebecca J. Howard, James B. Grace, Kerrylee RogersMangrove expansion and contraction at a poleward range limit: Climate extremes and land-ocean temperature gradients
Within the context of climate change, there is a pressing need to better understand the ecological implications of changes in the frequency and intensity of climate extremes. Along subtropical coasts, less frequent and warmer freeze events are expected to permit freeze-sensitive mangrove forests to expand poleward and displace freeze-tolerant salt marshes. Here, our aim was to better understand thAuthorsMichael J. Osland, Richard H. Day, Courtney T. Hall, Marisa D Brumfield, Jason Dugas, William R. JonesBarriers to and opportunities for landward migration of coastal wetlands with sea-level rise
In the 21st century, accelerated sea-level rise and continued coastal development are expected to greatly alter coastal landscapes across the globe. Historically, many coastal ecosystems have responded to sea-level fluctuations via horizontal and vertical movement on the landscape. However, anthropogenic activities, including urbanization and the construction of flood-prevention infrastructure, caAuthorsNicholas M. Enwright, Kereen T. Griffith, Michael J. OslandSalt marsh-mangrove ecotones: using structural gradients to investigate the effects of woody plant encroachment on plant-soil interactions and ecosystem carbon pools
Changing winter climate extremes are expected to result in the poleward migration of mangrove forests at the expense of salt marshes. Although mangroves and marshes are both highly valued ecosystems, the ecological implications of mangrove expansion have not been fully investigated. Here, we examined the effects of mangrove expansion on below-ground properties related to peat development and carbAuthorsErik S. Yando, Michael J. Osland, Jonathan M Willis, Richard H. Day, Ken W. Krauss, Mark W. HesterThe physiology of mangrove trees with changing climate
Mangrove forests grow on saline, periodically flooded soils of the tropical and subtropical coasts. The tree species that comprise the mangrove are halophytes that have suites of traits that confer differing levels of tolerance of salinity, aridity, inundation and extremes of temperature. Here we review how climate change and elevated levels of atmospheric CO2 will influence mangrove forests. ToleAuthorsCatherine E. Lovelock, Ken W. Krauss, Michael J. Osland, Ruth Reef, Marilyn C. BallNon-USGS Publications**
Russell M, Teague A, Alvarez F, Dantin D, Osland M, Harvey J, Nestlerode J, Rogers J, Jackson L, Pilant D, Genthner F, Lewis M, Spivak A, Harwell M, Neale A. 2013. Neighborhood scale quantification of ecosystem goods and services. pp 50, U.S. Environmental Protection Agency, Office of Research and Development, Gulf Ecology Division, Gulf Breeze, Florida, EPA/600/R-13/295, November 2013.Osland MJ, González E, Richardson CJ. 2011. Restoring diversity after cattail expansion: disturbance, resilience, and seasonality in a tropical dry wetland. Ecological Applications, 21, 715-728.Osland MJ, González E, Richardson CJ. 2011. Coastal freshwater wetland plant community response to seasonal drought and flooding in northwestern Costa Rica Wetlands, 31, 641-652. DOI:10.1007/s13157-011-0180-9Osland MJ, Pahl JW, Richardson CJ. 2009. Native bamboo (Arundinaria gigantea (Walter) Muhl., Poaceae) establishment and growth after the removal of an invasive non-native shrub (Ligustrum sinense Lour., Oleaceae): implications for restoration. Castanea, 74, 247-258.Osland MJ (2009). Managing invasive plants during wetland restoration: the role of disturbance, plant strategies, and environmental filters. Ph.D. Dissertation. Duke University, Durham, NC.**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.
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