late holocene evolution of a coupled, mud-dominated delta plain–chenier plain system, coastal louisiana, usa
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2017
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Abstract
Major deltas and their adjacent coastal plains are commonly
linked by means of coast-parallel fluxes of water, sediment, and nutrients.
Observations of the evolution of these interlinked systems over centennial to
millennial timescales are essential to understand the interaction between
point sources of sediment discharge (i.e. deltaic distributaries) and
adjacent coastal plains across large spatial (i.e. hundreds of kilometres)
scales. This information is needed to constrain future generations of
numerical models to predict coastal evolution in relation to climate change
and other human activities. Here we examine the coastal plain (Chenier Plain,
CP) adjacent to the Mississippi River delta, one of the world's largest
deltas. We use a refined chronology based on 22 new optically stimulated
luminescence and 22 new radiocarbon ages to test the hypothesis that cyclic
Mississippi subdelta shifting has influenced the evolution of the adjacent
CP. We show that over the past 3 kyr, accumulation rates in the CP were
generally 0–1 Mt yr−1. However, between 1.2 and 0.5 ka, when the
Mississippi River shifted to a position more proximal to the CP, these rates
increased to 2.9 ±1.1 Mt yr−1 or 0.5–1.5 % of the total
sediment load of the Mississippi River. We conclude that CP evolution during
the past 3 kyr was partly a direct consequence of shifting subdeltas, in
addition to changing regional sediment sources and modest rates of relative
sea-level (RSL) rise. The RSL history of the CP during this time period was
constrained by new limiting data points from the base of overwash deposits
associated with the cheniers.
These findings have implications for Mississippi River sediment diversions that are currently being planned to restore portions of this vulnerable coast. Only if such diversions are located in the western portion of the Mississippi Delta plain could they potentially contribute to sustaining the CP shoreline. Our findings highlight the importance of a better understanding of mud-dominated shorelines that are often associated with major deltas, in light of the enormous investments in coastal management and restoration that will likely be made around the globe, now and especially later during this century.
These findings have implications for Mississippi River sediment diversions that are currently being planned to restore portions of this vulnerable coast. Only if such diversions are located in the western portion of the Mississippi Delta plain could they potentially contribute to sustaining the CP shoreline. Our findings highlight the importance of a better understanding of mud-dominated shorelines that are often associated with major deltas, in light of the enormous investments in coastal management and restoration that will likely be made around the globe, now and especially later during this century.
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hijma2017earthlate
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| Authors | ;M. P. Hijma;M. P. Hijma;Z. Shen;Z. Shen;T. E. Törnqvist;B. Mauz |
| Journal | experimental gerontology |
| Year | 2017 |
| DOI |
10.5194/esurf-5-689-2017
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