The importance of non-tidal water-level variability for reconstructing Holocene relative sea level
Salt-marsh sediment is an important geological archive for reconstructing Holocene relative sea level. The vertical uncertainty of these reconstructions is usually quantified as proportional to tidal range, resulting in a presumed primacy of microtidal regions for generating precise records. We anal...
| Auteurs principaux: | , , |
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| Autres auteurs: | |
| Format: | Journal Article |
| Langue: | English |
| Publié: |
2024
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| Sujets: | |
| Accès en ligne: | https://hdl.handle.net/10356/174625 |