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Tidal Marshes across a Chesapeake Bay Subestuary Are Not Keeping up with Sea-Level Rise
Sea-level rise is a major factor in wetland loss worldwide, and in much of Chesapeake Bay (USA) the rate of sea-level rise is higher than the current global rate of 3.2 mm yr(-1) due to regional subsidence. Marshes along estuarine salinity gradients differ in vegetation composition, productivity, de...
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| Gepubliceerd in: | PLoS One |
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| Hoofdauteurs: | , , |
| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
Public Library of Science
2016
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| Onderwerpen: | |
| Online toegang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4965100/ https://ncbi.nlm.nih.gov/pubmed/27467784 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1371/journal.pone.0159753 |
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