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Productive wetlands restored for carbon sequestration quickly become net CO(2) sinks with site-level factors driving uptake variability
Inundated wetlands can potentially sequester substantial amounts of soil carbon (C) over the long-term because of slow decomposition and high primary productivity, particularly in climates with long growing seasons. Restoring such wetlands may provide one of several effective negative emission techn...
Autores principales: | , , , , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Public Library of Science
2021
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7993764/ https://www.ncbi.nlm.nih.gov/pubmed/33765085 http://dx.doi.org/10.1371/journal.pone.0248398 |
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author | Valach, Alex C. Kasak, Kuno Hemes, Kyle S. Anthony, Tyler L. Dronova, Iryna Taddeo, Sophie Silver, Whendee L. Szutu, Daphne Verfaillie, Joseph Baldocchi, Dennis D. |
author_facet | Valach, Alex C. Kasak, Kuno Hemes, Kyle S. Anthony, Tyler L. Dronova, Iryna Taddeo, Sophie Silver, Whendee L. Szutu, Daphne Verfaillie, Joseph Baldocchi, Dennis D. |
author_sort | Valach, Alex C. |
collection | PubMed |
description | Inundated wetlands can potentially sequester substantial amounts of soil carbon (C) over the long-term because of slow decomposition and high primary productivity, particularly in climates with long growing seasons. Restoring such wetlands may provide one of several effective negative emission technologies to remove atmospheric CO(2) and mitigate climate change. However, there remains considerable uncertainty whether these heterogeneous ecotones are consistent net C sinks and to what degree restoration and management methods affect C sequestration. Since wetland C dynamics are largely driven by climate, it is difficult to draw comparisons across regions. With many restored wetlands having different functional outcomes, we need to better understand the importance of site-specific conditions and how they change over time. We report on 21 site-years of C fluxes using eddy covariance measurements from five restored fresh to brackish wetlands in a Mediterranean climate. The wetlands ranged from 3 to 23 years after restoration and showed that several factors related to restoration methods and site conditions altered the magnitude of C sequestration by affecting vegetation cover and structure. Vegetation established within two years of re-flooding but followed different trajectories depending on design aspects, such as bathymetry-determined water levels, planting methods, and soil nutrients. A minimum of 55% vegetation cover was needed to become a net C sink, which most wetlands achieved once vegetation was established. Established wetlands had a high C sequestration efficiency (i.e. the ratio of net to gross ecosystem productivity) comparable to upland ecosystems but varied between years undergoing boom-bust growth cycles and C uptake strength was susceptible to disturbance events. We highlight the large C sequestration potential of productive inundated marshes, aided by restoration design and management targeted to maximise vegetation extent and minimise disturbance. These findings have important implications for wetland restoration, policy, and management practitioners. |
format | Online Article Text |
id | pubmed-7993764 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2021 |
publisher | Public Library of Science |
record_format | MEDLINE/PubMed |
spelling | pubmed-79937642021-04-05 Productive wetlands restored for carbon sequestration quickly become net CO(2) sinks with site-level factors driving uptake variability Valach, Alex C. Kasak, Kuno Hemes, Kyle S. Anthony, Tyler L. Dronova, Iryna Taddeo, Sophie Silver, Whendee L. Szutu, Daphne Verfaillie, Joseph Baldocchi, Dennis D. PLoS One Research Article Inundated wetlands can potentially sequester substantial amounts of soil carbon (C) over the long-term because of slow decomposition and high primary productivity, particularly in climates with long growing seasons. Restoring such wetlands may provide one of several effective negative emission technologies to remove atmospheric CO(2) and mitigate climate change. However, there remains considerable uncertainty whether these heterogeneous ecotones are consistent net C sinks and to what degree restoration and management methods affect C sequestration. Since wetland C dynamics are largely driven by climate, it is difficult to draw comparisons across regions. With many restored wetlands having different functional outcomes, we need to better understand the importance of site-specific conditions and how they change over time. We report on 21 site-years of C fluxes using eddy covariance measurements from five restored fresh to brackish wetlands in a Mediterranean climate. The wetlands ranged from 3 to 23 years after restoration and showed that several factors related to restoration methods and site conditions altered the magnitude of C sequestration by affecting vegetation cover and structure. Vegetation established within two years of re-flooding but followed different trajectories depending on design aspects, such as bathymetry-determined water levels, planting methods, and soil nutrients. A minimum of 55% vegetation cover was needed to become a net C sink, which most wetlands achieved once vegetation was established. Established wetlands had a high C sequestration efficiency (i.e. the ratio of net to gross ecosystem productivity) comparable to upland ecosystems but varied between years undergoing boom-bust growth cycles and C uptake strength was susceptible to disturbance events. We highlight the large C sequestration potential of productive inundated marshes, aided by restoration design and management targeted to maximise vegetation extent and minimise disturbance. These findings have important implications for wetland restoration, policy, and management practitioners. Public Library of Science 2021-03-25 /pmc/articles/PMC7993764/ /pubmed/33765085 http://dx.doi.org/10.1371/journal.pone.0248398 Text en © 2021 Valach et al http://creativecommons.org/licenses/by/4.0/ This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/) , which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. |
spellingShingle | Research Article Valach, Alex C. Kasak, Kuno Hemes, Kyle S. Anthony, Tyler L. Dronova, Iryna Taddeo, Sophie Silver, Whendee L. Szutu, Daphne Verfaillie, Joseph Baldocchi, Dennis D. Productive wetlands restored for carbon sequestration quickly become net CO(2) sinks with site-level factors driving uptake variability |
title | Productive wetlands restored for carbon sequestration quickly become net CO(2) sinks with site-level factors driving uptake variability |
title_full | Productive wetlands restored for carbon sequestration quickly become net CO(2) sinks with site-level factors driving uptake variability |
title_fullStr | Productive wetlands restored for carbon sequestration quickly become net CO(2) sinks with site-level factors driving uptake variability |
title_full_unstemmed | Productive wetlands restored for carbon sequestration quickly become net CO(2) sinks with site-level factors driving uptake variability |
title_short | Productive wetlands restored for carbon sequestration quickly become net CO(2) sinks with site-level factors driving uptake variability |
title_sort | productive wetlands restored for carbon sequestration quickly become net co(2) sinks with site-level factors driving uptake variability |
topic | Research Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7993764/ https://www.ncbi.nlm.nih.gov/pubmed/33765085 http://dx.doi.org/10.1371/journal.pone.0248398 |
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