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Florence Bascom Geoscience Center

The primary mission of the Florence Bascom Geoscience Center (FBGC) is to provide detailed scientific data and assessments to support natural resource management, public safety, and national security. The FBGC specializes in:

Geologic mapping and hazards

Paleontology, stratigraphy, and environmental geology

Special geologic studies at the intersection of national security and mineral resources

Publications

Capitalization of positional (Lower/Middle/Upper) and temporal (Early/Middle/Late) adjectives in the names of formal chronostratigraphic and geochronologic units of the Phanerozoic Capitalization of positional (Lower/Middle/Upper) and temporal (Early/Middle/Late) adjectives in the names of formal chronostratigraphic and geochronologic units of the Phanerozoic

Many authors are understandably confused about the capitalization of the words “lower,” “middle,” “upper,” “early,” and “late.” Where these words are used simply as descriptive adjectives, they should be in lowercase; where they form the first word of a formal chronostratigraphic or geochronologic unit name, they should be in uppercase.
Authors
Lucy E. Edwards, Randall C. Orndorff

Root biomass and productivity in coastal swamp forests of Louisiana (USA) Root biomass and productivity in coastal swamp forests of Louisiana (USA)

Coastal swamp forests (CSF) occupy approximately 225,000 ha in Southeastern Louisiana (USA), and across a large percentage of this area, CSF are subjected to sediment starvation, salinity intrusion, and chronic submergence. We assessed root biomass and productivity in nine CSF in Louisiana, and found that root biomass ranged from 420.8 g m−2 to 1712.2 g m−2 to a soil depth of 30 cm. Root...
Authors
Ken W. Krauss, Jorge A. Villa, Blair A. Miller, Eric J. Ward, Andrew S. From, Gregory B. Noe

Science

Chesapeake Stream Team

Connecting Conservation Practices to Local Stream Health in the Chesapeake Bay Watershed
Chesapeake Stream Team

Chesapeake Stream Team

Connecting Conservation Practices to Local Stream Health in the Chesapeake Bay Watershed
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Evaluating the Effects of Stream-Restoration Practices in an Impaired Agricultural System

Stream-restoration practices are widely used throughout the Chesapeake Bay watershed to improve stream health and function, but research into their effectiveness is limited in agricultural settings. A study in Turtle Creek, Pennsylvania, suggests that stream-restoration practices can significantly reduce streambank erosion and enhance floodplain deposition, changes that can reduce in-stream...
Evaluating the Effects of Stream-Restoration Practices in an Impaired Agricultural System

Evaluating the Effects of Stream-Restoration Practices in an Impaired Agricultural System

Stream-restoration practices are widely used throughout the Chesapeake Bay watershed to improve stream health and function, but research into their effectiveness is limited in agricultural settings. A study in Turtle Creek, Pennsylvania, suggests that stream-restoration practices can significantly reduce streambank erosion and enhance floodplain deposition, changes that can reduce in-stream...
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The “sediment shadow” in Chesapeake Bay’s tidal freshwater rivers has important implications for restoration

Chesapeake Bay restoration efforts are focused on reducing nitrogen, phosphorus, and sediment loads to the estuary. A new synthesis of existing long-term records of suspended-sediment concentrations suggests that only a limited amount of watershed sediment is currently transported by rivers past the tidal freshwater zone and into saltier waters of the Chesapeake Bay.
The “sediment shadow” in Chesapeake Bay’s tidal freshwater rivers has important implications for restoration

The “sediment shadow” in Chesapeake Bay’s tidal freshwater rivers has important implications for restoration

Chesapeake Bay restoration efforts are focused on reducing nitrogen, phosphorus, and sediment loads to the estuary. A new synthesis of existing long-term records of suspended-sediment concentrations suggests that only a limited amount of watershed sediment is currently transported by rivers past the tidal freshwater zone and into saltier waters of the Chesapeake Bay.
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