Holocene sea-level variability from Chesapeake Bay Tidal Marshes, USA (Record no. 12874)
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| 000 -LEADER | |
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| fixed length control field | 02393nab a2200277 4500 |
| 005 - DATE & TIME | |
| control field | 20220822201818.0 |
| 008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION | |
| fixed length control field | 220822b |||||||| |||| 00| 0 eng d |
| 100 ## - MAIN ENTRY--PERSONAL NAME | |
| Personal name | Cronin, Thomas M |
| 245 ## - TITLE STATEMENT | |
| Title | Holocene sea-level variability from Chesapeake Bay Tidal Marshes, USA |
| 260 ## - PUBLICATION, DISTRIBUTION, ETC. (IMPRINT) | |
| Name of publisher, distributor, etc | sage |
| Date of publication, distribution, etc | 2019 |
| 300 ## - PHYSICAL DESCRIPTION | |
| Pages | Vol 29, Issue 11, 2019 : (1679-1693 p.). |
| 520 ## - SUMMARY, ETC. | |
| Summary, etc | We reconstructed the last 10,000 years of Holocene relative sea-level rise (RSLR) from sediment core records near Chesapeake Bay, eastern United States, including new marsh records from the Potomac and Rappahannock Rivers, Virginia. Results show mean RSLR rates of 2.6 mm yr−1 from 10 to 8 kilo-annum (ka) due to combined final ice-sheet melting during deglaciation and glacio-isostatic adjustment (GIA subsidence). Mean RSLR rates from ~6 ka to present were 1.4 mm yr−1 due mainly to GIA, consistent with other East Coast marsh records and geophysical models. However, a progressively slower mean rate (<1.0 mm yr−1) characterized the last 1000 years when a multi-century-long period of tidal marsh development occurred during the ‘Medieval Climate Anomaly’ (MCA) and ‘Little Ice Age’ (LIA) in the Chesapeake Bay region and other East Coast marshes. This decrease was most likely due to climatic and glaciological processes and, correcting for GIA, represents a fall in global mean sea level (GMSL) near the end of Holocene Neoglacial cooling. These pre-historical climate- and GIA-driven Chesapeake Bay sea-level changes contrast sharply with those based on Chesapeake Bay tide-gauge rates (3.1–4.5 mm yr−1) (back to 1903). After subtracting the GIA subsidence component, these rates can be attributed to long-term (millennial) global factors of accelerated ocean thermal expansion (~1.0 mm yr−1) and mass loss from alpine glaciers and Greenland and Antarctic Ice Sheets (1.5–2.0 mm yr−1). |
| 650 ## - Subject | |
| Subject | Chesapeake Bay, |
| 650 ## - Subject | |
| Subject | foraminifera, |
| 650 ## - Subject | |
| Subject | Holocene, |
| 650 ## - Subject | |
| Subject | sea level, |
| 650 ## - Subject | |
| Subject | tidal marsh, |
| 650 ## - Subject | |
| Subject | US East Coast |
| 700 ## - Added Entry Personal Name | |
| Added Entry Personal Name | Clevenger, Megan K |
| 700 ## - Added Entry Personal Name | |
| Added Entry Personal Name | Tibert, Neil E |
| 773 0# - HOST ITEM ENTRY | |
| Host Biblionumber | 12756 |
| Host Itemnumber | 16504 |
| Place, publisher, and date of publication | London: Sage Publication Ltd, 2019. |
| Title | Holocene/ |
| International Standard Serial Number | 09596836 |
| 856 ## - ELECTRONIC LOCATION AND ACCESS | |
| Uniform Resource Identifier | https://doi.org/10.1177/0959683619862028 |
| 942 ## - ADDED ENTRY ELEMENTS (KOHA) | |
| Koha item type | Articles |
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| 650 ## - Subject | |
| -- | 52305 |
| 650 ## - Subject | |
| -- | 52306 |
| 700 ## - Added Entry Personal Name | |
| -- | 52307 |
| 700 ## - Added Entry Personal Name | |
| -- | 52308 |
| 942 ## - ADDED ENTRY ELEMENTS (KOHA) | |
| -- | ddc |
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