Static chamber gas fluxes and carbon and nitrogen isotope content of age-dated sediment cores from a Phragmites wetland in Sage Lot Pond, Massachusetts, 2013-2015
Dates
Publication Date
2022-05-26
Time Period
2013-07-19
Time Period
2013-08-15
Time Period
2013-09-20
Time Period
2014
Time Period
2015-05-21
Citation
O'Keefe Suttles, J.A., Eagle, M.J., Martin, R.M., Moseman-Valtierra, S., and Kroeger, K.D., 2022, Static chamber gas fluxes and carbon and nitrogen isotope content of age-dated sediment cores from a Phragmites wetland in Sage Lot Pond, Massachusetts, 2013-2015: U.S. Geological Survey data release, https://doi.org/10.5066/P9JM751N.
Summary
Coastal wetlands are major global carbon sinks, however, they are heterogeneous and dynamic ecosystems. To characterize spatial and temporal variability in a New England salt marsh, static chamber measurements of greenhouse gas (GHG) fluxes were compared among major plant-defined zones (high marsh dominated by Distichlis spicata and a zone of invasive Phragmites australis) during 2013 and 2014 growing seasons. Two sediment cores were collected in 2015 from the Phragmites zone to support previously reported core collections from the high marsh sites (Gonneea and others 2018). Collected cores were up to 70 cm in length with dry bulk density ranges from 0.04 to 0.33 grams per cubic centimeter and carbon content 22.4% to 46.6%. Gamma counting [...]
Summary
Coastal wetlands are major global carbon sinks, however, they are heterogeneous and dynamic ecosystems. To characterize spatial and temporal variability in a New England salt marsh, static chamber measurements of greenhouse gas (GHG) fluxes were compared among major plant-defined zones (high marsh dominated by Distichlis spicata and a zone of invasive Phragmites australis) during 2013 and 2014 growing seasons. Two sediment cores were collected in 2015 from the Phragmites zone to support previously reported core collections from the high marsh sites (Gonneea and others 2018). Collected cores were up to 70 cm in length with dry bulk density ranges from 0.04 to 0.33 grams per cubic centimeter and carbon content 22.4% to 46.6%. Gamma counting results for excess lead-210 were used to construct Constant Rate of Supply (CRS) age models to age-date individual depth intervals in the cores. Additionally, gamma counting results for other radionuclides, particularly cesium-137 gave further insight to evaluate how vertical accretion and carbon burial rates have changed during the past century.
Cited Reference: Gonneea, M.E., O'Keefe Suttles, J.A., and Kroeger, K.D., 2018, Collection, analysis, and age-dating of sediment cores from salt marshes on the south shore of Cape Cod, Massachusetts, from 2013 through 2014: U.S. Geological Survey data release, https://doi.org/10.5066/F7H41QPP.
The purpose of this study was to measure greenhouse gas fluxes across a seasonal time-scale and to determine sediment carbon content and sediment accumulation rates across contrasting plant-defined zones in order to model controls on GHG fluxes in a New England salt marsh. These data support research focused on understanding controls and scaling of carbon exchange in order to inform possible Blue Carbon management interventions in these vulnerable ecosystems.
Preview Image
Split sediment core collected from a Phragmites site at Sage Lot Pond in 2015.