Northeastern Section (45th Annual) and Southeastern Section (59th Annual) Joint Meeting (13-16 March 2010)
Paper No. 54-10
Presentation Time: 1:30 PM-5:35 PM

CARBON SEQUESTRATION RATES OF DIFFERENT MARSH ZONES IN THE SCHOODIC MARSH OF ACADIA NATIONAL PARK, MAINE

SORRELL, Lee Matthew, Department of Geosciences and Natural Resources, Western Carolina University, Cullowhee, NC 28723, lmsorrell1@catamount.wcu.edu and TANNER, Benjamin R., Geosciences and Natural Resources Management, Western Carolina University, 335 Stillwell Building, Cullowhee, NC 28723

Salt marshes are potential carbon sinks but marsh zones can transgress if relative sea level rise exceeds critical thresholds. This research was undertaken in the Schoodic Section of Acadia National Park, Maine, in order to determine which marsh zones have the highest carbon sequestration potential. Nine 60cm cores were taken from the Schoodic Marsh, three each from high, low, and freshwater marsh areas, to use for calculation of carbon sequestration rates. Percent organic carbon was determined using an elemental analyzer. Soil bulk density was also determined and sedimentation rates were calculated based on bulk radiocarbon dates of basal core sediments. Five out of the nine cores have been processed thus far (2 freshwater marsh, 2 high marsh, and one low marsh). The low marsh core had the lowest percentage of organic carbon but the sequestration rate was highest (87.4 g C m-2 yr-1) due to a high sedimentation rate. Only a minimum carbon sequestration rate could be calculated for this core due to the radiocarbon date being modern. We used the maximum calibrated 2σ age of 278 years BP, which allowed for the calculation of a minimum sedimentation rate. The two high marsh cores had the lowest carbon sequestration rates (39.0 +/- 6.4 g C m-2 yr-1 and 55.1 +/- 6.0 g C m-2 yr-1). The two freshwater marsh cores showed intermediate carbon sequestration rates (54.4 +/- 5.6 g C m-2 yr-1 and 61.6 +/- 9.0 g C m-2 yr-1). The data for this marsh show that carbon storage potential is higher when low marsh overtakes high marsh, but could decrease if high marsh overtakes freshwater marsh. Release of methane in freshwater marsh zones could offset the additional carbon storage potential. The analysis of the remaining four cores will test current findings.

Northeastern Section (45th Annual) and Southeastern Section (59th Annual) Joint Meeting (13-16 March 2010)
General Information for this Meeting
Session No. 54--Booth# 56
Coastal and Nearshore Processes Affecting Our National Parks (Posters)
Sheraton Baltimore City Center: International ABCDF
1:30 PM-5:35 PM, Monday, 15 March 2010

Geological Society of America Abstracts with Programs, Vol. 42, No. 1, p. 141

© Copyright 2010 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.