Articles | Volume 5, issue 4
https://doi.org/10.5194/esurf-5-689-2017
https://doi.org/10.5194/esurf-5-689-2017
Research article
 | 
02 Nov 2017
Research article |  | 02 Nov 2017

Late Holocene evolution of a coupled, mud-dominated delta plain–chenier plain system, coastal Louisiana, USA

Marc P. Hijma, Zhixiong Shen, Torbjörn E. Törnqvist, and Barbara Mauz

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AR by M. P. Hijma on behalf of the Authors (12 Sep 2017)  Author's response   Manuscript 
ED: Publish as is (25 Sep 2017) by Richard Gloaguen
ED: Publish as is (25 Sep 2017) by Tom Coulthard (Editor)
AR by M. P. Hijma on behalf of the Authors (25 Sep 2017)
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Short summary
We show that in the last 3 kyr the evolution of the Chenier Plain, >200 km west of the Mississippi Delta, was influenced by changes in the position of the main river mouth, local sediment sources and sea-level rise. This information can be used to constrain future generations of numerical models to obtain more robust predictions of the effects of improved sediment management and accelerated rates of relative sea-level rise on the evolution of mud-dominated coastal environments worldwide.