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Mississippi Delta subsidence primarily caused by compaction of Holocene strata


Coastal subsidence causes sea-level rise, shoreline erosion and wetland loss, which poses a threat to coastal populations1. 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 controversial2,3,4,5,6,7,8,9,10,11. Current estimates of subsidence rates vary by several orders of magnitude3,6. 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 5 mm per year, values that exceed recent model predictions5,9. 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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Figure 1: Map of the study area.
Figure 2: Cross-section perpendicular to Bayou Lafourche near Paincourtville, Louisiana.
Figure 3: Relationship between overburden thickness and compaction rate.
Figure 4: Comparison of compaction-prone and compaction-free 14C samples.


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This analysis is based mainly on field data collected from 1993 to 1995, supported by grant 770-07-238 from the Netherlands Organisation for Scientific Research (NWO). Further funding was provided by NOAA and USGS to the Long-term Estuary Assessment Group through the Center for Bioenvironmental Research at Tulane and Xavier Universities, and by the Koninklijke/Shell Exploratie en Produktie Laboratorium. We benefited greatly from comments by T. Meckel. This paper is dedicated to the late Henk Berendsen, whose deep understanding of alluvial stratigraphy has had a profound impact on the work presented here.

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Correspondence to Torbjörn E. Törnqvist, Davin J. Wallace, Joep E. A. Storms, Jakob Wallinga, Remke L. van Dam, Martijn Blaauw, Mayke S. Derksen, Cornelis J. W. Klerks, Camiel Meijneken or Els M. A. Snijders.

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Törnqvist, T., Wallace, D., Storms, J. et al. Mississippi Delta subsidence primarily caused by compaction of Holocene strata. Nature Geosci 1, 173–176 (2008).

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