Coastal Rivers
The coastal plain is one of the least well studied ecoregions in North America and the running waters found on this part of the landscape are no exception. Coastal Rivers are historically understudied by both lotic and estuarine ecologists. The Coastal Estuarine Ecosystems Lab has ongoing research on these important and understudied systems in both Texas and the Chesapeake Bay watershed.
Texas Research ProjectsArid land streams are nearly as poorly studied as coastal plain streams. The Texas coastline is largely alluvial coastal plain and ranges from desert toward the Mexico-USA border, to semi-arid around Corpus Christi, to mesic as you approach Louisiana. The region is sub-tropical and serves as a mixing zone between tropical and temperate species. For all of these reasons the stream ecology of coastal Texas is both fascinating, potentially unique, and can serve as a model system for addressing questions about how streams will respond to climate change. Recent work funded by NSF in partnership with the Reese Lab at Dauphin Island Sea Lab and the Hogan Lab at TAMUCC that is wrapping up has focused on understanding how climate shapes ecosystem resistance and resilience. We found that, contrary to expectations, arid systems are more sensitive to perturbations than mesic systems. Currently, we’re using stable isotope analysis and measurements of ecosystem metabolism and secondary production to understand how climate shapes the relative importance of top down and bottom up forcing on ecosystem functioning and community structure. This work is in partnership with the Ulseth Lab at Sam Houston State University and the Vander Zanden Lab and Whiles Lab at the University of Florida. This project is funded by the National Academy of Science Engineering and Medicine, and the National Science Foundation. |
Chesapeake Bay ResearchThe Chesapeake Bay TMDL has led to the implementation of a large number of regenerative storm water conveyance (RSC) system style restorations in the Chesapeake Bay watershed. RSC restorations reconnect streams with their flood plain by building a series of rock weir dams and filling incised channels with new substrate. |