Opportunity Information: Apply for G14AS00057
Apply for G14AS00057
- The Geological Survey in the science and technology and other research and development sector is offering a public funding opportunity titled "Cooperative Ecosystem Studies Unit, Chesapeake Watershed CESU" and is now available to receive applicants.
- Interested and eligible applicants and submit their applications by referencing the CFDA number(s): 15.808 U.S. Geological Survey Research and Data Collection.
- This funding opportunity was created on Apr 14, 2014 and posted on Apr 14, 2014.
- Applicants must submit their applications by Apr 25, 2014. (Agency may still review applications by suitable applicants for the remaining/unused allocated funding in 2026.)
- The funding agency has allocated a total of $180,000.00 to eligible and selected applicants.
- The number of recipients for this funding is limited to 1 candidate(s).
- Eligible applicants include: Others (see text field entitled Additional Information on Eligibility for clarification).
- This financial assistance opportunity is being issued under a Cooperative Ecosystem Studies Unit (CESU) Program. CESUs are partnerships that provide research, technical assistance, and education. Eligible recipients must be a participating partner of the Chesapeake Watershed Cooperative Ecosystem Studies Unit (CESU) Program.
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Opportunity Summary:
The Cooperative Ecosystem Studies Unit, Chesapeake Watershed CESU grant opportunity (Funding Opportunity Number G14AS00057) is a US Geological Survey (USGS) discretionary funding announcement focused on applied research about how coastal marshes can persist as sea levels rise. It is offered as a cooperative agreement under the CESU framework, meaning the work is intended to be carried out collaboratively with USGS involvement rather than as a simple, hands-off grant. The core scientific question is the concept of a "threshold rate" of sea level rise: many modern marsh models suggest marshes can keep up with rising seas only up to a certain rate, after which they begin to drown or convert to open water unless they can migrate inland.
The opportunity centers on marsh resilience mechanisms. Coastal wetlands generally respond to sea level rise in two ways: they can move landward (often called transgression or migration) if there is space and suitable topography, or they can build elevation vertically through sediment deposition and organic matter accumulation (accretion). Historically, many marshes have survived changing sea levels by vertical building, but accelerating sea level rise, changing sediment supplies, and human-altered shorelines raise the risk that vertical accretion may not keep pace. Over roughly the last decade leading up to this announcement, researchers developed numerical models that combine biological processes (plant growth, organic matter production, vegetation effects on sediment trapping) with physical processes (tidal inundation, sediment delivery, erosion) to predict marsh evolution and long-term persistence. A major, still not fully tested outcome of these models is the idea that marsh survival is not a gradual decline but can hinge on a threshold, where conditions are stable up to a point and then fail beyond it.
A key takeaway driving the proposed research is that the threshold rate for marsh survival may be controlled by two relatively straightforward characteristics: tidal range and sediment availability. Tidal range matters because it helps define the vertical "growth window" for marsh plants, shaping where vegetation can thrive and how often the marsh platform is flooded, which in turn influences how much sediment can be deposited and retained. Sediment availability matters because suspended sediments in the water column are a primary source of mineral material that can be deposited on the marsh surface during flooding, contributing to elevation gain. If sediment concentrations are too low, even healthy vegetation may not be able to trap enough mineral matter to build elevation at the pace required by sea level rise.
To ground these model-based ideas in real measurements, USGS describes field and historical-data approaches aimed at quantifying marsh accretion and sediment supply. The work includes estimating accretion rates using marsh geochronologies, specifically lead-210 (Pb-210) and cesium-137 (Cs-137) radionuclide dating methods commonly used to reconstruct sediment accumulation over decadal timescales. The project also involves analyzing historical photographs to assess landscape change over time, which can provide evidence of marsh stability, conversion to open water, or landward movement. In parallel, USGS is measuring suspended sediment concentrations in the water column across seasonal timescales, which helps characterize how much sediment is actually available to the marsh during different conditions throughout the year. Together, these measurements support a more rigorous test of whether simple predictors like tidal range and sediment supply can explain observed marsh resilience limits and help validate or improve existing biophysical models.
Administratively, the award is managed by the USGS under CFDA number 15.808 (U.S. Geological Survey Research and Data Collection). The announcement anticipated a single award (Expected Awards: 1) with an estimated total funding amount of $180,000. No cost sharing or matching requirement is indicated. The funding instrument is a cooperative agreement, and the activity category is Science and Technology and other Research and Development. The posting date and creation date were both April 14, 2014, with an original and current closing date of April 25, 2014, and the archive date listed as July 14, 2014. Although the award ceiling and floor are listed as 0 in the source data (often a formatting artifact in older grants listings), the total estimated funding provides the practical scale of the opportunity.
Eligibility is restricted to partners in the Chesapeake Watershed Cooperative Ecosystem Studies Unit (CESU) Program. CESUs are partnership networks designed to streamline collaboration among federal agencies, universities, and other research organizations to deliver research, technical assistance, and education. In this case, only participating Chesapeake Watershed CESU partners could apply, which typically includes institutions already part of that designated CESU consortium.
For further details, the announcement directs applicants to Grants.gov and provides a point of contact for access issues: Faith Graves at 703-648-7356 and fgraves@usgs.gov.
Frequently Asked Questions (FAQs)
What is the name and number of this funding opportunity?
This opportunity is the Cooperative Ecosystem Studies Unit, Chesapeake Watershed CESU grant opportunity, Funding Opportunity Number G14AS00057.
Which federal agency is offering the award?
The award is offered by the U.S. Geological Survey (USGS).
What type of funding instrument is being used?
The funding instrument is a cooperative agreement under the CESU framework, meaning the work is intended to be carried out collaboratively with USGS involvement rather than as a hands-off grant.
What is the main scientific focus of the project?
The focus is applied research on how coastal marshes can persist as sea levels rise, with particular emphasis on the idea that marsh survival may depend on a "threshold rate" of sea level rise.
What does "threshold rate" of sea level rise mean in this context?
It refers to the concept suggested by many modern marsh models that marshes may be able to keep pace with rising seas only up to a certain rate; beyond that point, marshes may begin to drown or convert to open water unless they can migrate inland.
What marsh resilience mechanisms are highlighted in the announcement?
The announcement highlights two general responses of coastal wetlands to sea level rise: (1) moving landward (often called transgression or migration) when space and suitable topography exist, and (2) building elevation vertically through sediment deposition and organic matter accumulation (accretion).
Why is vertical accretion a concern under accelerating sea level rise?
Historically, many marshes have survived changing sea levels by building vertically, but accelerating sea level rise, changing sediment supplies, and human-altered shorelines raise the risk that vertical accretion may not keep pace.
What kinds of models are motivating the proposed research?
Over roughly the decade leading up to the announcement, researchers developed numerical models that combine biological processes (such as plant growth and vegetation effects on sediment trapping) with physical processes (such as tidal inundation, sediment delivery, and erosion) to predict marsh evolution and long-term persistence.
What major model-based outcome is described as not fully tested?
A key outcome is the idea that marsh survival may hinge on a threshold (stable up to a point, then failing beyond it) rather than declining gradually as sea level rise accelerates.
What two characteristics are suggested as simple predictors of marsh survival thresholds?
The announcement suggests the threshold rate for marsh survival may be controlled by tidal range and sediment availability.
Why does tidal range matter for marsh resilience?
Tidal range helps define the vertical "growth window" for marsh plants and shapes inundation frequency, influencing how much sediment can be deposited and retained on the marsh platform.
Why does sediment availability matter for marsh resilience?
Suspended sediments in the water column are a primary source of mineral material deposited during flooding, contributing to elevation gain. If sediment concentrations are too low, vegetation may not be able to trap enough mineral matter to build elevation at the pace required by sea level rise.
What field and historical-data approaches are included to test the model ideas?
The announcement describes quantifying marsh accretion and sediment supply using (1) marsh geochronologies (Pb-210 and Cs-137 radionuclide dating) to reconstruct decadal sediment accumulation, (2) historical photographs to assess landscape change over time, and (3) seasonal measurements of suspended sediment concentrations in the water column.
Which radionuclide dating methods are specifically mentioned?
Lead-210 (Pb-210) and cesium-137 (Cs-137) methods are specifically mentioned for estimating accretion rates over decadal timescales.
What is the purpose of analyzing historical photographs in this project?
Historical photographs are used to assess landscape change over time, which can provide evidence of marsh stability, conversion to open water, or landward movement.
Why measure suspended sediment concentrations seasonally?
Seasonal measurements help characterize how much sediment is available to the marsh under different conditions throughout the year, supporting a more rigorous test of whether sediment supply (along with tidal range) explains observed marsh resilience limits.
How does this work relate to marsh evolution and long-term persistence modeling?
The measurements are intended to test whether simple predictors like tidal range and sediment supply can explain observed resilience limits and help validate or improve existing biophysical marsh models.
What is the CFDA number associated with this opportunity?
The award is managed under CFDA 15.808 (U.S. Geological Survey Research and Data Collection).
What is the activity category listed for the opportunity?
The activity category is Science and Technology and other Research and Development.
How many awards were anticipated?
The announcement anticipated a single award (Expected Awards: 1).
What is the estimated total funding amount?
The estimated total funding amount is $180,000.
Is cost sharing or matching required?
No cost sharing or matching requirement is indicated in the provided information.
Are there stated award ceiling and floor amounts?
The award ceiling and floor are listed as 0 in the source data, which is noted as often being a formatting artifact in older grants listings. The practical scale is indicated by the estimated total funding amount of $180,000.
Who is eligible to apply?
Eligibility is restricted to partners in the Chesapeake Watershed Cooperative Ecosystem Studies Unit (CESU) Program.
What does CESU eligibility imply for applicants?
It means only participating Chesapeake Watershed CESU partners (typically institutions already included in that designated CESU consortium) could apply.
When was the opportunity posted?
The posting date (and creation date) listed is April 14, 2014.
What was the application closing date?
The original and current closing date listed is April 25, 2014.
When was the opportunity archived?
The archive date listed is July 14, 2014.
Where are applicants directed to find additional application details?
Applicants are directed to Grants.gov for further details.
Who should be contacted for Grants.gov access issues?
The point of contact for access issues is Faith Graves at 703-648-7356 or fgraves@usgs.gov.
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