Laboratoire des Sciences du Climat et de l'Environnement,
LSCE/IPSL,CEA-CNRS-UVSQ-Université Paris Saclay, 91198 Gif sur Yvette,
France
Karline Soetaert
Royal Netherlands Institute of Sea Research (NIOZ), Department of
Estuarine and Delta Systems, Korringaweg 7, P.O. Box 140, 4401 NT Yerseke,
the Netherlands
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2,208
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Cumulative views and downloads
(calculated since 06 Apr 2022)
Total article views: 1,835 (including HTML, PDF, and XML)
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1,345
409
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HTML: 1,345
PDF: 409
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Total: 1,835
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BibTeX: 94
EndNote: 170
Views and downloads (calculated since 04 Oct 2022)
Cumulative views and downloads
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Total article views: 1,158 (including HTML, PDF, and XML)
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863
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Total: 1,158
Supplement: 94
BibTeX: 6
EndNote: 5
Views and downloads (calculated since 06 Apr 2022)
Cumulative views and downloads
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Viewed (geographical distribution)
Total article views: 2,993 (including HTML, PDF, and XML)
Thereof 2,880 with geography defined
and 113 with unknown origin.
Total article views: 1,835 (including HTML, PDF, and XML)
Thereof 1,798 with geography defined
and 37 with unknown origin.
Total article views: 1,158 (including HTML, PDF, and XML)
Thereof 1,082 with geography defined
and 76 with unknown origin.
The coastal marine environment serves as a transition zone in the land–ocean continuum and is susceptible to episodic phenomena such as flash floods, which cause massive organic matter deposition. Here, we present a model of sediment early diagenesis that explicitly describes this type of deposition while also incorporating unique flood deposit characteristics. This model can be used to investigate the temporal evolution of marine sediments following abrupt changes in environmental conditions.
The coastal marine environment serves as a transition zone in the land–ocean continuum and is...