The importance of non-tidal water-level variability for reconstructing Holocene relative sea level

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...

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Bibliographic Details
Main Authors: Kemp, Andrew C., Shaw, Timothy Adam, Piecuch, Christopher G.
Other Authors: Asian School of the Environment
Format: Article
Language:English
Published: 2024
Subjects:
Earth and Environmental Sciences
Salt marsh
Microtidal
Chesapeake bay
Highest occurrence of foraminifera
Online Access:https://hdl.handle.net/10356/174625
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Institution: Nanyang Technological University
Language: English

Internet

https://hdl.handle.net/10356/174625

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