Please use this identifier to cite or link to this item: https://doi.org/10.1007/s11273-011-9238-y
Title: Surface elevation change in natural and re-created intertidal habitats, eastern England, UK, with particular reference to Freiston Shore
Authors: Spencer, T.
Friess, D.A. 
Möller, I.
Brown, S.L.
Garbutt, R.A.
French, J.R.
Keywords: Accretion plate
Managed realignment
Sea-level rise
Shallow subsidence
Surface elevation table
Tidal wetland creation
Issue Date: Feb-2012
Citation: Spencer, T., Friess, D.A., Möller, I., Brown, S.L., Garbutt, R.A., French, J.R. (2012-02). Surface elevation change in natural and re-created intertidal habitats, eastern England, UK, with particular reference to Freiston Shore. Wetlands Ecology and Management 20 (1) : 9-33. ScholarBank@NUS Repository. https://doi.org/10.1007/s11273-011-9238-y
Abstract: Quantification of processes contributing to overall surface elevation change is critical to the accurate assessment of saltmarsh sedimentary status, particularly when predicting system stability in relation to accelerated sea level rise. Rates of short-term (up to 5.5 years) surface elevation change and accretion on a temperate saltmarsh were measured at an open coast managed realignment (habitat creation) trial, and the surrounding intertidal zone using surface elevation table-marker horizon (accretion plate) methodologies. Mean surface elevation changes on vegetated saltmarsh control sites, at some distance from the hydrodynamic disturbance of breaches in a former sea defence line, showed rates of change compatible with marsh surface dynamics seen elsewhere in the region, exceeding rates of regional relative sea-level rise. Within the managed realignment, sites close to the breaches showed exceptionally high rates of both accretion and surface elevation change, most likely as a result of high localized sediment supply from breach and channel enlargement and the presence of surfaces left unnaturally low in the tidal frame. Positive surface elevation change on the landward side of the breaches reached >30.4 mm a -1, up to one hundred times greater than rates of surface elevation change at locations 1 km from the breach entrances. Shallow sub-surface processes, or 'surface subsidence', was an important process on natural marshes outside the managed realignment but not seen within the site, due to the consolidated nature of the underlying substrate. The Freiston Shore managed realignment site shows remarkably similar time variation in mean elevation to that of the longer record from the Tollesbury managed realignment site, Blackwater estuary, Essex coast, UK. It is not clear how long it will take for re-created intertidal habitats at both Freiston Shore and Tollesbury to approach an 'equilibrium' elevation within the tidal frame but modelling suggests that in natural wetlands on the coast of eastern England this process takes at least 150 years. © 2011 Springer Science+Business Media B.V.
Source Title: Wetlands Ecology and Management
URI: http://scholarbank.nus.edu.sg/handle/10635/114173
ISSN: 09234861
DOI: 10.1007/s11273-011-9238-y
Appears in Collections:Staff Publications

Show full item record
Files in This Item:
There are no files associated with this item.

SCOPUSTM   
Citations

8
checked on May 20, 2018

WEB OF SCIENCETM
Citations

9
checked on Apr 23, 2018

Page view(s)

33
checked on Mar 12, 2018

Google ScholarTM

Check

Altmetric


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.