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      Vulnerability of Louisiana's coastal wetlands to present-day rates of relative sea-level rise

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          Abstract

          Coastal Louisiana has lost about 5,000 km 2 of wetlands over the past century and concern exists whether remaining wetlands will persist while facing some of the world's highest rates of relative sea-level rise (RSLR). Here we analyse an unprecedented data set derived from 274 rod surface-elevation table-marker horizon stations, to determine present-day surface-elevation change, vertical accretion and shallow subsidence rates. Comparison of vertical accretion rates with RSLR rates at the land surface (present-day RSLR rates are 12±8 mm per year) shows that 65% of wetlands in the Mississippi Delta (SE Louisiana) may keep pace with RSLR, whereas 58% of the sites in the Chenier Plain (SW Louisiana) do not, rendering much of this area highly vulnerable to RLSR. At least 60% of the total subsidence rate occurs within the uppermost 5–10 m, which may account for the higher vulnerability of coastal Louisiana wetlands compared to their counterparts elsewhere.

          Abstract

          Coastal Louisiana wetlands face some of the world's highest rates of relative sea-level rise and loss. Here, the authors show that there is a strong regional component to coastal Louisiana wetland vulnerability to relative sea-level rise as well as contributing to the understanding of subsidence in the region.

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          Limits on the adaptability of coastal marshes to rising sea level

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            The vulnerability of Indo-Pacific mangrove forests to sea-level rise.

            Sea-level rise can threaten the long-term sustainability of coastal communities and valuable ecosystems such as coral reefs, salt marshes and mangroves. Mangrove forests have the capacity to keep pace with sea-level rise and to avoid inundation through vertical accretion of sediments, which allows them to maintain wetland soil elevations suitable for plant growth. The Indo-Pacific region holds most of the world's mangrove forests, but sediment delivery in this region is declining, owing to anthropogenic activities such as damming of rivers. This decline is of particular concern because the Indo-Pacific region is expected to have variable, but high, rates of future sea-level rise. Here we analyse recent trends in mangrove surface elevation changes across the Indo-Pacific region using data from a network of surface elevation table instruments. We find that sediment availability can enable mangrove forests to maintain rates of soil-surface elevation gain that match or exceed that of sea-level rise, but for 69 per cent of our study sites the current rate of sea-level rise exceeded the soil surface elevation gain. We also present a model based on our field data, which suggests that mangrove forests at sites with low tidal range and low sediment supply could be submerged as early as 2070.
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              Numerical models of salt marsh evolution: Ecological, geomorphic, and climatic factors

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                Author and article information

                Journal
                Nat Commun
                Nat Commun
                Nature Communications
                Nature Publishing Group
                2041-1723
                14 March 2017
                2017
                : 8
                : 14792
                Affiliations
                [1 ]Department of Earth and Environmental Sciences, Tulane University , 6823 St. Charles Avenue, New Orleans, Louisiana 70118-5698, USA
                Author notes
                [*]

                Present address: The Center for Integrative Geosciences, The University of Connecticut at Storrs, 354 Mansfield Road, Beach Hall, Storrs, Connecticut 06269, USA

                Author information
                http://orcid.org/0000-0003-2485-3449
                Article
                ncomms14792
                10.1038/ncomms14792
                5355890
                28290444
                a905b8b8-ecc7-42c1-9f06-b51adbc3653d
                Copyright © 2017, The Author(s)

                This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article's Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

                History
                : 26 April 2016
                : 31 January 2017
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