Predicting marsh vulnerability to sea-level rise using Holocene relative sea-level data

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作者
Benjamin P. Horton
Ian Shennan
Sarah L. Bradley
Niamh Cahill
Matthew Kirwan
Robert E. Kopp
Timothy A. Shaw
机构
[1] Nanyang Technological University,Asian School of the Environment
[2] Nanyang Technological University,Earth Observatory of Singapore
[3] Durham University,Department of Geography
[4] Delft University of Technology,Department of Geoscience and Remote Sensing
[5] University College Dublin,School of Mathematics and Statistics
[6] College of William and Mary,Virginia Institute of Marine Science
[7] Rutgers University,Institute of Earth, Ocean, and Atmospheric Sciences
[8] Rutgers University,Department of Earth and Planetary Sciences
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Tidal marshes rank among Earth’s vulnerable ecosystems, which will retreat if future rates of relative sea-level rise (RSLR) exceed marshes’ ability to accrete vertically. Here, we assess the limits to marsh vulnerability by analyzing >780 Holocene reconstructions of tidal marsh evolution in Great Britain. These reconstructions include both transgressive (tidal marsh retreat) and regressive (tidal marsh expansion) contacts. The probability of a marsh retreat was conditional upon Holocene rates of RSLR, which varied between −7.7 and 15.2 mm/yr. Holocene records indicate that marshes are nine times more likely to retreat than expand when RSLR rates are ≥7.1 mm/yr. Coupling estimated probabilities of marsh retreat with projections of future RSLR suggests a major risk of tidal marsh loss in the twenty-first century. All of Great Britain has a >80% probability of a marsh retreat under Representative Concentration Pathway (RCP) 8.5 by 2100, with areas of southern and eastern England achieving this probability by 2040.
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