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John L. David

Publications and source records attributed to John L. David.

2 recordsLinked to original sources

Modification of rod surface elevation tables for monitoring extreme elevation shifts in wetlands

Rod surface elevation tables (RSETs) are effective tools for measuring changes in ground surface height, but these are not designed to withstand large changes in height (e.g., ±50 cm). After extreme changes in elevation due to erosion or accretion, RSET sites may be deemed unusable; however, this equipment usually can function indefinitely with in-situ modifications. Here, we provide a methodological description for in-situ modifications to RSETs that can be invaluable for long-term monitoring. In a sampling site with a high rate of surface elevation loss, longer pins can be inserted into the RSET arm to continue measurements. In a site with a high rate of accretion, RSETs buried in sediment can be raised by adding rod extensions, which is a particularly effective approach if the surface elevation can be measured before and after the attachment. Any modification to an RSET requires a reconceptualization of the original equations used to estimate change in the surface elevation, and these revised equations are described in this paper. We tested the measurement variability of the RSET before and after modification in West Dongting Lake, China. Results indicated that modification did not compromise data quality or precision and stability of RSET measurements. The reconceptualized equations incorporate offset adjustments that maintain datum consistency, enabling continuous data collection across pre- and postmodification phases with millimeter-scale precision. These RSET modifications can be used to extend the life of long-term RSET monitoring sites if the surface elevation has changed beyond the measurement capacity of the original RSET.

Ecosystem Health and Sustainability

Trends in vegetation and height of the topographic surface in a tidal freshwater swamp experiencing rooting zone saltwater intrusion

A decrease in the ground surface height of coastal wetlands is of worldwide concern because of its relationship to peat loss, coastal carbon, and biodiversity in freshwater wetlands. We asked if it is possible to determine indicators of impending transitions of freshwater swamps to other coastal types by examining long-term changes in the environment and vegetation. In a tidal Taxodium distichum swamp in Hickory Point State Forest, Maryland, the topographic surface height (ground surface height) decreased by as much as 25.6 ± 2.2 to 50.8 ± 3.8 cm at two Surface Elevation Tables from 2015 to 2021 following salinity intrusion events related to hurricanes and offshore storms (e.g., Hurricane Melissa). In 2019, rooting zone salinity exceeded 5 ppt for >24.9 % of the time, with a maximum salinity level of 12.5 ppt. Tree growth of T. distichum trees declined and 60 % of these trees died along a 4 m wide × 125 m transect in 2014–2016. Root biomass and ground surface height decreased roughly in conjunction with a salinity pulse in the rooting zone during Hurricane Melissa in 2019. Saplings survived but T. distichum seedlings were uncommon and did not survive in the study area. Typha × glauca increased in cover (0.2 to 5.6 % cover plot −1 ) from 2014 to 2016 so a vegetation shift toward T. × glauca was apparent by 2021. This work captures a multi-year trend of decreasing ground surface height, tree growth and health, and freshwater status in the rooting zone that may be an indicator of impending vegetation transition.

Maryland