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<shortName>GCE LTER Sedimentation-Erosion Table (SET) Monitoring</shortName>
<title>GCE LTER Sedimentation-Erosion Table (SET) Monitoring</title>
<creator>
<individualName>
<salutation>Dr.</salutation>
<givenName>Christopher</givenName>
<givenName>B.</givenName>
<surName>Craft</surName>
</individualName>
<organizationName>Indiana University at Bloomington</organizationName>
<address>
<deliveryPoint>Indiana University - School of Public and Environmental Affairs</deliveryPoint>
<deliveryPoint>Room 408. MSB II.</deliveryPoint>
<deliveryPoint>702 N. Walnut Grove Ave.</deliveryPoint>
<city>Bloomington</city>
<administrativeArea>Indiana</administrativeArea>
<postalCode>47405</postalCode>
<country>USA</country>
</address>
<electronicMailAddress>ccraft@indiana.edu</electronicMailAddress>
<userId directory="https://orcid.org">https://orcid.org/0000-0002-6225-786X</userId>
</creator>
<metadataProvider><organizationName>Georgia Coastal Ecosystems LTER Project</organizationName>
<address>
<deliveryPoint>Dept. of Marine Sciences</deliveryPoint>
<deliveryPoint>University of Georgia</deliveryPoint>
<city>Athens</city>
<administrativeArea>Georgia</administrativeArea>
<postalCode>30602-3636</postalCode>
<country>USA</country>
</address>
<electronicMailAddress>gcelter@uga.edu</electronicMailAddress>
<onlineUrl>https://gce-lter.marsci.uga.edu/</onlineUrl>
</metadataProvider>
<associatedParty>
<individualName>
<salutation>Dr.</salutation>
<givenName>Christopher</givenName>
<givenName>B.</givenName>
<surName>Craft</surName>
</individualName>
<organizationName>Indiana University at Bloomington</organizationName>
<address>
<deliveryPoint>Indiana University - School of Public and Environmental Affairs</deliveryPoint>
<deliveryPoint>Room 408. MSB II.</deliveryPoint>
<deliveryPoint>702 N. Walnut Grove Ave.</deliveryPoint>
<city>Bloomington</city>
<administrativeArea>Indiana</administrativeArea>
<postalCode>47405</postalCode>
<country>USA</country>
</address>
<electronicMailAddress>ccraft@indiana.edu</electronicMailAddress>
<userId directory="https://orcid.org">https://orcid.org/0000-0002-6225-786X</userId>
<role>Principal investigator</role>
</associatedParty>
<associatedParty>
<individualName>
<salutation>Dr.</salutation>
<givenName>Ellen</givenName>
<surName>Herbert</surName>
</individualName>
<organizationName>Ducks Unlimited</organizationName>
<address>
<deliveryPoint>Ducks Unlimited</deliveryPoint>
<city>Memphis</city>
<administrativeArea>Tennessee</administrativeArea>
<country>USA</country>
</address>
<electronicMailAddress>eherbert@ducks.org</electronicMailAddress>
<role>Co-investigator</role>
</associatedParty>
<associatedParty>
<individualName>
<givenName>Sasha</givenName>
<surName>Greenspan</surName>
</individualName>
<organizationName>University of Georgia Marine Institute</organizationName>
<address>
<deliveryPoint>University of Georgia Marine Institute</deliveryPoint>
<city>Sapelo Island</city>
<administrativeArea>Georgia</administrativeArea>
<postalCode>31327</postalCode>
<country>USA</country>
</address>
<electronicMailAddress>sgreensp@uga.edu</electronicMailAddress>
<role>Co-investigator</role>
</associatedParty>
<pubDate>2026</pubDate>
<abstract>
<section>
<title>Project Goals</title>
<para>We monitor marsh surface elevation at all ten GCE LTER sites to measure changes in the marsh surface in response to sea level rise. We use a permanent sedimentation-erosion table (SET) benchmark installed at each site and a portable measuring device to measure millimeter-scale changes in marsh surface elevation from 36 fixed locations (4 angles times 9 points per angles) at each site.  We also measure sedimentation in three 0.25 m by 0.25 m plots at each site using feldspar marker layers.</para>
</section>
<section>
<title>Associated GCE LTER research questions</title>
<para>Area 2: Patterns within the Domain (<ulink url="http://gce-lter.marsci.uga.edu/public/research/gce3_area2.asp">more information</ulink>)</para>
<para>Question 2: How do the spatial and temporal patterns of biogeochemical processes, primary production, community dynamics, decomposition, and disturbance vary across the estuarine landscape, and how do they relate to environmental gradients? (<ulink url="http://gce-lter.marsci.uga.edu/public/research/gce2_q2.asp">more information</ulink>)</para>
</section>
</abstract>
<keywordSet name="habitat">
<keyword>marsh</keyword>
</keywordSet>
<keywordSet name="measurement">
<keyword>sedimentology</keyword>
</keywordSet>
<keywordSet name="organization">
<keyword>LTER</keyword>
<keyword>NSF</keyword>
</keywordSet>
<keywordSet name="site">
<keyword>GCE</keyword>
</keywordSet>
<keywordSet name="taxonomic">
<keyword>Iva</keyword>
<keyword>plants</keyword>
<keyword>Spartina</keyword>
<keyword>Zizaniopsis</keyword>
</keywordSet>
<keywordSet name="theme">
<keyword>geology</keyword>
</keywordSet>
<coverage>
<geographicCoverage>
<geographicDescription>Overall geographic extent of the research project</geographicDescription>
<boundingCoordinates>
<westBoundingCoordinate>-81.493498</westBoundingCoordinate>
<eastBoundingCoordinate>-81.195661</eastBoundingCoordinate>
<northBoundingCoordinate>31.552554</northBoundingCoordinate>
<southBoundingCoordinate>31.304063</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<temporalCoverage>
<ongoing>
<beginDate>
<calendarDate>2001-07-01</calendarDate>
</beginDate>
</ongoing>
</temporalCoverage>
</coverage>
<funding>
<section>
<para>Core monitorn activity of GCE LTER, $4,920,000</para>
</section>
</funding>
<studyAreaDescription>
<descriptor name="hydrology" citableClassificationSystem="false">
<descriptorValue>estuary marsh complex</descriptorValue>
</descriptor>
<coverage>
<geographicCoverage>
<geographicDescription>Eulonia - Transitional salt marsh/upland forest site at the upper reach of the Sapelo River near Eulonia, Georgia. The main marsh area is to the north of the channel where the upland is controlled by DNR. Several small creeks lie within the study area.  Residential development is increasing on the upland areas south of the channel. A hydrographic sonde is deployed within this site attached to a private dock to the south of the main channel near the HW-17 bridge. The sonde is accessed from a dock on a private residence off of highway 17. As of late 2017 the property is owned by Linda Hornby. She asks that we notify her by text about an hour before arriving to service the sondes. There is no reason to go to this property other than for sonde work.</geographicDescription>
<boundingCoordinates>
<westBoundingCoordinate>-81.428481</westBoundingCoordinate>
<eastBoundingCoordinate>-81.410732</eastBoundingCoordinate>
<northBoundingCoordinate>31.546750</northBoundingCoordinate>
<southBoundingCoordinate>31.533963</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<geographicCoverage>
<geographicDescription>Hunt Camp - Barrier island/marsh site on western Sapelo Island.  This site is located at the upper reaches of the Duplin River, and is within the Sapelo Island National Estuarine Research Reserve. Existing well fields border small marsh area to northwest, some wells have been installed to south end of hammock where marsh is more extensive and permanent plots are located. Two existing hydrographic sondes and weather stations within this site are operated by SINERR (Hunt Camp dock) and UGAMI (flume dock).</geographicDescription>
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<westBoundingCoordinate>-81.295506</westBoundingCoordinate>
<eastBoundingCoordinate>-81.258908</eastBoundingCoordinate>
<northBoundingCoordinate>31.497026</northBoundingCoordinate>
<southBoundingCoordinate>31.462320</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<geographicCoverage>
<geographicDescription>Four Mile Island - Low salt marsh/estuary site encompassing the southwestern end of Four Mile Island and the Sapelo River near Sapelo Sound. The large island is totally marsh, with no upland, and no development. Nearby areas, like "Sutherland Bluff", are developing with golf courses. A hydrographic sonde is deployed within this site attached to channel marker 4 (under U.S. Coast Guard permit). Salinity regime is similar to seawater.</geographicDescription>
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<westBoundingCoordinate>-81.318961</westBoundingCoordinate>
<eastBoundingCoordinate>-81.292844</eastBoundingCoordinate>
<northBoundingCoordinate>31.552554</northBoundingCoordinate>
<southBoundingCoordinate>31.533604</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<geographicCoverage>
<geographicDescription>North Sapelo - High salinity marsh/Sapelo Sound site.  Few or no small creeks, but one large creek is easily accessed. Further upstream upland drainage is affected by culvert at Reynolds' duck pond. Upland is heavily forested. Hydrographic sonde is deployed adjacent to this site attached to a channel marker (under U.S. Coast Guard permit). A huge mud flat is present at the northern tip of Sapelo Island.</geographicDescription>
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<westBoundingCoordinate>-81.233249</westBoundingCoordinate>
<eastBoundingCoordinate>-81.195661</eastBoundingCoordinate>
<northBoundingCoordinate>31.546868</northBoundingCoordinate>
<southBoundingCoordinate>31.515188</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<geographicCoverage>
<geographicDescription>Meridian - Inland marsh and tidal creek site near Meridian, Georgia. The primary marsh site is to the south of the dock in front of the Sapelo Island Visitor Center. Some small creeks and one large creek (Hudson Creek) are present. Upland is heavily forested. Marsh to the north of the dock can be used for additional studies if larger areas are required. Upland to the North is being developed for residential use, so future access is uncertain. The USGS super station site (weather station plus multiple-sensor sonde) is deployed off the ferry dock. Salinity is similar to seawater because there is little freshwater input from the upland.</geographicDescription>
<boundingCoordinates>
<westBoundingCoordinate>-81.370752</westBoundingCoordinate>
<eastBoundingCoordinate>-81.357256</eastBoundingCoordinate>
<northBoundingCoordinate>31.463533</northBoundingCoordinate>
<southBoundingCoordinate>31.448419</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<geographicCoverage>
<geographicDescription>Folly River - Salt marsh/tidal creek site at the Folly River near Doboy Sound.  No upland areas present. The north side of Doboy Sound immediately opposite is similar, but creeks are not as nice. No existing markers are close enough for sonde deployment, so we will initially use the existing sonde at Marsh Landing operated by UGAMI for surrogate hydrographic data.</geographicDescription>
<boundingCoordinates>
<westBoundingCoordinate>-81.354413</westBoundingCoordinate>
<eastBoundingCoordinate>-81.327201</eastBoundingCoordinate>
<northBoundingCoordinate>31.442538</northBoundingCoordinate>
<southBoundingCoordinate>31.417640</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<geographicCoverage>
<geographicDescription>Dean Creek - Doboy Sound/salt marsh site at the southern end of Sapelo Island near Dean Creek and the Sapelo lighthouse.  A few small creeks are present, but a large creek (Dean Creek) is easily accessed. Upland is composed of small hammocks and some constructed causeways, with sand dune complexes east of Dean Creek and extending to the beach. Upper end of the watershed is affected by a culvert at Beach Road and heavy student use of marsh immediately adjacent to culvert. A hydrographic sonde is deployed in Doboy Sound near Commodore Island approximately 1.5km from this site. GCE6 is also the focus of Sapelo Island Microbial Observatory research on microbial diversity  and  genomics (http://simo.marsci.uga.edu)</geographicDescription>
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<westBoundingCoordinate>-81.299522</westBoundingCoordinate>
<eastBoundingCoordinate>-81.264378</eastBoundingCoordinate>
<northBoundingCoordinate>31.394072</northBoundingCoordinate>
<southBoundingCoordinate>31.371003</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<geographicCoverage>
<geographicDescription>Carrs Island - Freshwater marsh site along the northern bank of Hammersmith Creek at the south end of Carrs Island. Upland area is heavily forested. Northern 3/4 of the island was diked for rice agriculture, but the southern 1/4 is undisturbed. A hydrographic sonde is deployed in the Altamaha River near Hammersmith Creek, adjacent to this site.</geographicDescription>
<boundingCoordinates>
<westBoundingCoordinate>-81.493498</westBoundingCoordinate>
<eastBoundingCoordinate>-81.475900</eastBoundingCoordinate>
<northBoundingCoordinate>31.348774</northBoundingCoordinate>
<southBoundingCoordinate>31.334364</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<geographicCoverage>
<geographicDescription>Alligator Creek - Mid-estuary/salt marsh site on the west side of Friday Cap Creek along the Altamaha River. This is a brackish marsh with salinities around 14 PSU during drought, less than 5 PSU normally. A hydrographic sonde is deployed adjacent to this site in the Altamaha River near Alligator Creek, attached to the US Coast Guard Daymarker 2 pilings.</geographicDescription>
<boundingCoordinates>
<westBoundingCoordinate>-81.426272</westBoundingCoordinate>
<eastBoundingCoordinate>-81.410634</eastBoundingCoordinate>
<northBoundingCoordinate>31.317808</northBoundingCoordinate>
<southBoundingCoordinate>31.304063</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<geographicCoverage>
<geographicDescription>Rockdedundy Island - Lower estuary tidal creek and marsh site at Rockdedundy Island west of Wolf Island. A hydrographic sonde is deployed approximately 2km from this site in the Altamaha River near Rockdedundy Island, attached to the US Coast Guard Daymarker 201 pilings.</geographicDescription>
<boundingCoordinates>
<westBoundingCoordinate>-81.346730</westBoundingCoordinate>
<eastBoundingCoordinate>-81.326495</eastBoundingCoordinate>
<northBoundingCoordinate>31.358142</northBoundingCoordinate>
<southBoundingCoordinate>31.339173</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
</coverage>
<associatedMaterial category="data">
<distribution>
<online>
<onlineDescription>GIS file (ArcGIS shapefile)</onlineDescription>
<url>https://gce-lter.marsci.uga.edu/private/registration/files/gis/GCE-7-2011_GIS_GCE_7_2011_GIS_gce_set_locations_shapefile.zip</url>
</online>
</distribution>
</associatedMaterial>
<associatedMaterial category="data">
<distribution>
<online>
<onlineDescription>GIS file (ArcGIS shapefile)</onlineDescription>
<url>https://gce-lter.marsci.uga.edu/private/registration/files/GIS/GCE-7-2011_GIS_GCE_SET_locations_1thru11.zip</url>
</online>
</distribution>
</associatedMaterial>
<associatedMaterial category="data">
<distribution>
<online>
<onlineDescription>Map (Google Earth KML/KMZ or map image)</onlineDescription>
<url>https://gce-lter.marsci.uga.edu/private/registration/files/maps/GCE-7-2011_Maps_gce_set_locations.kml</url>
</online>
</distribution>
</associatedMaterial>
<associatedMaterial category="data">
<distribution>
<online>
<onlineDescription>Map (Google Earth KML/KMZ or map image)</onlineDescription>
<url>https://gce-lter.marsci.uga.edu/private/registration/files/Maps/GCE-7-2011_Maps_GCE_SET_locations_1thru11.kml</url>
</online>
</distribution>
</associatedMaterial>
</studyAreaDescription>
<designDescription>
<description>
<section>
<title>Project Location</title>
<para>GCE LTER monitoring sites, mid-marsh locations</para>
</section>
<section>
<title>Equipment</title>
<para>Two 12 foot boardwalks, in parallel, are deployed about 10-12 feet from each other.  Between the two boardwalks, a 4 inch piece of aluminum irrigation pipe is installed to a depth of approximately 20 feet.  The top of the pipe is cut level and filled with concrete. This serves as a benchmark on which the portable SET measuring device is placed.  Three 0.25 m by 0.25 m feldspar plots are established just outside of the parallel boardwalks.  The plots are demarcated by two pieces of 1 inch diameter white pvc pipe, each about 2 feet tall.  A thick layer of white feldspar powder is placed atop of each plot once a year to provide a marker horizon above which sediment carried in by tidal inundation is deposited. An example plot from GCE 6 (Dean Creek) is attached.</para>
</section>
</description>
</designDescription>
<associatedMaterial category="publication" id="gce.1037" date="2017">
<distribution>
<offline>
<mediumName>Stahl, M., Widney, S. and Craft, C.B. 2017. Presentation: Tidal freshwater forests: a sentinel for climate change. SPEA Ph.D. Students' 17th Annual Conference, February 24, 2017, Bloomington, IN.</mediumName>
</offline>
</distribution>
</associatedMaterial>
<associatedMaterial category="publication" id="gce.1038" date="2017">
<distribution>
<offline>
<mediumName>Craft, C.B., Stahl, M. and Widney, S. 2017. Presentation: Tidal freshwater forests: sentinels for climate change. 10th International Workshop on Nutrient Cycling and Retention in Natural and Constructed Wetlands, September 21-24, Trebon, Czech Republic.</mediumName>
</offline>
</distribution>
</associatedMaterial>
<associatedMaterial category="publication" id="gce.1039" date="2017">
<distribution>
<offline>
<mediumName>Widney, S., Stahl, M. and Craft, C.B. 2017. Presentation: Tidal forests: sentinels for climate change. Society of Wetland Scientists Annual Meeting, June 8, 2017, San Juan, Puerto Rico.</mediumName>
</offline>
</distribution>
</associatedMaterial>
<associatedMaterial category="data" id="knb-lter-gce.276" date="2020-12-08">
<distribution>
<online>
<onlineDescription>GEL-GCEM-0508b - Sediment elevation measurements for 10 GCE-LTER sampling sites from December 2001 to December 2020</onlineDescription>
<url>https://gce-lter.marsci.uga.edu/public/app/dataset_details.asp?id=276</url>
</online>
</distribution>
</associatedMaterial>
<associatedMaterial category="data" id="knb-lter-gce.278" date="2011-05-17">
<distribution>
<online>
<onlineDescription>GEL-GCEM-0508c - Soil accretion at 10 GCE marsh sampling sites from December 2001 to May 2011</onlineDescription>
<url>https://gce-lter.marsci.uga.edu/public/app/dataset_details.asp?id=278</url>
</online>
</distribution>
</associatedMaterial>
<associatedMaterial category="data" id="knb-lter-gce.692" date="2011-05-17">
<distribution>
<online>
<onlineDescription>GEL-GCEM-1908 - Soil accretion at 10 GCE marsh sampling sites from December 2011 to December 2016</onlineDescription>
<url>https://gce-lter.marsci.uga.edu/public/app/dataset_details.asp?id=692</url>
</online>
</distribution>
</associatedMaterial>
<associatedMaterial category="document">
<distribution>
<online>
<onlineDescription>Project description or documentation</onlineDescription>
<url>https://gce-lter.marsci.uga.edu/private/registration/files/documents/GCE-7-2011_Documents_deancreek#6.doc</url>
</online>
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