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Ecosystems Land Change Science Program

The Land Change Science Program in the USGS Ecosystems Mission Area strives to advance the understanding of the physical, chemical, and biological components of the Earth system, the causes and consequences of ecosystem and land use change, and the vulnerability and resilience of the Earth system to such changes.

News

The Slime Trail: How USGS eDNA Efforts Are Revealing What Lives in the Deep Gulf

The Slime Trail: How USGS eDNA Efforts Are Revealing What Lives in the Deep Gulf

FORT Updates: From Plains to Peaks - Vol. 4 | Issue 3

FORT Updates: From Plains to Peaks - Vol. 4 | Issue 3

A Pristine Headwaters Ecosystem as an Outdoor Laboratory for Foundational Science

A Pristine Headwaters Ecosystem as an Outdoor Laboratory for Foundational Science

Publications

On the fidelity of oxygen isotope-based sea level reconstructions: A case study of Marine Isotope Stage 3 On the fidelity of oxygen isotope-based sea level reconstructions: A case study of Marine Isotope Stage 3

Although foraminiferal oxygen isotope records (δ18OF) have long been used to develop time-continuous estimates of past global ice volume, growing evidence indicates that the ice volume and temperature contributions to δ18OF diverge considerably over the last glacial cycle. Across Marine Isotope Stage 3 (MIS 3; 57 to 29 ka), estimates of peak global sea level based on δ18OF are ∼30 m...
Authors
Tamara Pico, Jesse R. Farmer, Sarah Shackleton, Robert K. Poirier, Bradley R. Markle, Lorraine E. Lisiecki

Probabilistic forecasting of coastal wetland elevation and soil carbon response to sea-level rise Probabilistic forecasting of coastal wetland elevation and soil carbon response to sea-level rise

Tidal wetlands build soil as a dynamic response to inundation, resulting in carbon sequestration and resilience to sea-level rise. Process models can be used to make site-specific forecasts, anticipate future changes, and plan management responses. But to be actionable, forecasts from these models need to be accompanied by descriptions of their confidence. In this study, we demonstrate...
Authors
James R. Holmquist, E. Fay Belshe, Brandon M. Boyd, Lauren N. Brown, Samantha K. Chapman, Ron Corstanje, Meagan J. Eagle, Christopher N. Janousek, Minjee Jung, David H. Klinges, Michael Lonneman, James T. Morris, Gregory B. Noe, André Rovai, Jonathan Sanderman, Amanda C. Spivak, Katherine Todd-Brown, Megan Vahsen, Nicholas Ward, Lisamarie Windham-Myers, J. Patrick Megonigal

Microfocus X-ray computed tomography to evaluate ostracode shell density and other metrics for monitoring ocean acidification in the Arctic Ocean Microfocus X-ray computed tomography to evaluate ostracode shell density and other metrics for monitoring ocean acidification in the Arctic Ocean

Ocean acidification (OA) poses a significant threat to the ability of marine calcifying organisms—such as mollusks, corals, crustaceans, and plankton—to form and maintain their calcium carbonate-based shells. While some species show greater sensitivity to OA than others, the impacts on benthic marine calcifiers remain inadequately understood. This study investigates the shell density...
Authors
Laura Gemery, Katsunori Kimoto, David J. Horne, Michiyo Yamamoto-Kawai, Siyi Yin, Ryan J. McAleer, Lee W. Cooper, Jacqueline M. Grebmeier, Aaron M. Jubb, Masanobu Yamamoto

Science

Wolverine Glacier

Wolverine Glacier is located in Alaska’s Kenai Mountains, along the western flank of Prince William Sound. Glacier observations began in 1966 and continue through present as the western most USGS Benchmark Glacier.
Wolverine Glacier

Wolverine Glacier

Wolverine Glacier is located in Alaska’s Kenai Mountains, along the western flank of Prince William Sound. Glacier observations began in 1966 and continue through present as the western most USGS Benchmark Glacier.
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Lemon Creek Glacier

Lemon Creek Glacier is located in southeast Alaska, at the southernmost tip of the Juneau Icefield. Glacier observations began at this site in 1953 and continue through present, serving as a central site between glaciers in the contiguous USA and those in mainland Alaska.
Lemon Creek Glacier

Lemon Creek Glacier

Lemon Creek Glacier is located in southeast Alaska, at the southernmost tip of the Juneau Icefield. Glacier observations began at this site in 1953 and continue through present, serving as a central site between glaciers in the contiguous USA and those in mainland Alaska.
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Gulkana Glacier

Gulkana Glacier is located in the high-latitude continental climate regime of Alaska’s Delta Mountains. Glacier observations began at this site in 1966 and continue through present as the northern most USGS Benchmark Glacier.
Gulkana Glacier

Gulkana Glacier

Gulkana Glacier is located in the high-latitude continental climate regime of Alaska’s Delta Mountains. Glacier observations began at this site in 1966 and continue through present as the northern most USGS Benchmark Glacier.
Learn More
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