Staff Publications

Staff Publications

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    'Staff publications' is the digital repository of Wageningen University & Research

    'Staff publications' contains references to publications authored by Wageningen University staff from 1976 onward.

    Publications authored by the staff of the Research Institutes are available from 1995 onwards.

    Full text documents are added when available. The database is updated daily and currently holds about 240,000 items, of which 72,000 in open access.

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Record number 562032
Title Mississippi Delta subsidence primarily caused by compaction of Holocene strata
Author(s) Törnqvist, Torbjörn E.; Wallace, Davin J.; Storms, Joep E.A.; Wallinga, Jakob; Dam, Remke L. Van; Blaauw, Martijn; Derksen, Mayke S.; Klerks, Cornelis J.W.; Meijneken, Camiel; Snijders, Els M.A.
Source Nature Geoscience 1 (2008)3. - ISSN 1752-0894 - p. 173 - 176.
DOI https://doi.org/10.1038/ngeo129
Publication type Refereed Article in a scientific journal
Publication year 2008
Abstract

Coastal subsidence causes sea-level rise, shoreline erosion and wetland loss, which poses a threat to coastal populations. This is especially evident in the Mississippi Delta in the southern United States, which was devastated by Hurricane Katrina in 2005. The loss of protective wetlands is considered a critical factor in the extensive flood damage. The causes of subsidence in coastal Louisiana, attributed to factors as diverse as shallow compaction and deep crustal processes, remain controversial. Current estimates of subsidence rates vary by several orders of magnitude. Here, we use a series of radiocarbon-dated sediment cores from the Mississippi Delta to analyse late Holocene deposits and assess compaction rates. We find that millennial-scale compaction rates primarily associated with peat can reach 5mm per year, values that exceed recent model predictions. Locally and on timescales of decades to centuries, rates are likely to be 10 mm or more per year. We conclude that compaction of Holocene strata contributes significantly to the exceptionally high rates of relative sea-level rise and coastal wetland loss in the Mississippi Delta, and is likely to cause subsidence in other organic-rich and often densely populated coastal plains.

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