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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...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Public Library of Science
2016
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4965100/ https://www.ncbi.nlm.nih.gov/pubmed/27467784 http://dx.doi.org/10.1371/journal.pone.0159753 |