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Holocene formation and evolution of coastal dunes ridges, Brittany (France)

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Standard

Holocene formation and evolution of coastal dunes ridges, Brittany (France). / Van Vliet-Lanoë, Brigitte; Goslin, Jérôme; Hénaff, Alain; Hallégouët, Bernard; Delacourt, Christophe; Le Cornec, Erwan; Meurisse-Fort, Murielle.

I: Comptes Rendus - Geoscience, Bind 348, Nr. 6, 2016, s. 462-470.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Van Vliet-Lanoë, B, Goslin, J, Hénaff, A, Hallégouët, B, Delacourt, C, Le Cornec, E & Meurisse-Fort, M 2016, 'Holocene formation and evolution of coastal dunes ridges, Brittany (France)', Comptes Rendus - Geoscience, bind 348, nr. 6, s. 462-470. https://doi.org/10.1016/j.crte.2015.01.001

APA

Van Vliet-Lanoë, B., Goslin, J., Hénaff, A., Hallégouët, B., Delacourt, C., Le Cornec, E., & Meurisse-Fort, M. (2016). Holocene formation and evolution of coastal dunes ridges, Brittany (France). Comptes Rendus - Geoscience, 348(6), 462-470. https://doi.org/10.1016/j.crte.2015.01.001

Vancouver

Van Vliet-Lanoë B, Goslin J, Hénaff A, Hallégouët B, Delacourt C, Le Cornec E o.a. Holocene formation and evolution of coastal dunes ridges, Brittany (France). Comptes Rendus - Geoscience. 2016;348(6):462-470. https://doi.org/10.1016/j.crte.2015.01.001

Author

Van Vliet-Lanoë, Brigitte ; Goslin, Jérôme ; Hénaff, Alain ; Hallégouët, Bernard ; Delacourt, Christophe ; Le Cornec, Erwan ; Meurisse-Fort, Murielle. / Holocene formation and evolution of coastal dunes ridges, Brittany (France). I: Comptes Rendus - Geoscience. 2016 ; Bind 348, Nr. 6. s. 462-470.

Bibtex

@article{c95c71a1a7cd49e98aad36bf2cdec06b,
title = "Holocene formation and evolution of coastal dunes ridges, Brittany (France)",
abstract = "Holocene coastal dune formation under a continuously rising sea level (SL) is an abnormal response to increasing storm frequency. The aim of this work is to understand the coastal sedimentary budget and the present-day sand starvation, controlled by climate and man. Dating in Brittany shows that Aeolian deposition initiated from ca. 4000 cal BP, with the slowing down of the SL rise. Pre-historical dunes appeared here from ca. 3000 cal BP, without SL regression. After, further building phases recycled the same stock of sands. Historical dunes I developed from ca. 350 AD. Major storms between 900 and 1200 AD resulted in the construction of washover coastal ridges, the Historical dunes II. A part of the sand was evacuated offshore. From ca. 1350 AD, the pre-existing ridges are reworked forming the Historical dunes III, leading to rapid coastal erosion and inland drift. Holocene dunes with a rising SL constitute a temporary anomaly, mostly forced by man, soon erased by storms in Brittany.",
keywords = "Anthropic perturbation, Climate, Dunes, Holocene, Sand starvation",
author = "{Van Vliet-Lano{\"e}}, Brigitte and J{\'e}r{\^o}me Goslin and Alain H{\'e}naff and Bernard Hall{\'e}gou{\"e}t and Christophe Delacourt and {Le Cornec}, Erwan and Murielle Meurisse-Fort",
year = "2016",
doi = "10.1016/j.crte.2015.01.001",
language = "English",
volume = "348",
pages = "462--470",
journal = "Comptes Rendus Geoscience",
issn = "1631-0713",
publisher = "Elsevier",
number = "6",

}

RIS

TY - JOUR

T1 - Holocene formation and evolution of coastal dunes ridges, Brittany (France)

AU - Van Vliet-Lanoë, Brigitte

AU - Goslin, Jérôme

AU - Hénaff, Alain

AU - Hallégouët, Bernard

AU - Delacourt, Christophe

AU - Le Cornec, Erwan

AU - Meurisse-Fort, Murielle

PY - 2016

Y1 - 2016

N2 - Holocene coastal dune formation under a continuously rising sea level (SL) is an abnormal response to increasing storm frequency. The aim of this work is to understand the coastal sedimentary budget and the present-day sand starvation, controlled by climate and man. Dating in Brittany shows that Aeolian deposition initiated from ca. 4000 cal BP, with the slowing down of the SL rise. Pre-historical dunes appeared here from ca. 3000 cal BP, without SL regression. After, further building phases recycled the same stock of sands. Historical dunes I developed from ca. 350 AD. Major storms between 900 and 1200 AD resulted in the construction of washover coastal ridges, the Historical dunes II. A part of the sand was evacuated offshore. From ca. 1350 AD, the pre-existing ridges are reworked forming the Historical dunes III, leading to rapid coastal erosion and inland drift. Holocene dunes with a rising SL constitute a temporary anomaly, mostly forced by man, soon erased by storms in Brittany.

AB - Holocene coastal dune formation under a continuously rising sea level (SL) is an abnormal response to increasing storm frequency. The aim of this work is to understand the coastal sedimentary budget and the present-day sand starvation, controlled by climate and man. Dating in Brittany shows that Aeolian deposition initiated from ca. 4000 cal BP, with the slowing down of the SL rise. Pre-historical dunes appeared here from ca. 3000 cal BP, without SL regression. After, further building phases recycled the same stock of sands. Historical dunes I developed from ca. 350 AD. Major storms between 900 and 1200 AD resulted in the construction of washover coastal ridges, the Historical dunes II. A part of the sand was evacuated offshore. From ca. 1350 AD, the pre-existing ridges are reworked forming the Historical dunes III, leading to rapid coastal erosion and inland drift. Holocene dunes with a rising SL constitute a temporary anomaly, mostly forced by man, soon erased by storms in Brittany.

KW - Anthropic perturbation

KW - Climate

KW - Dunes

KW - Holocene

KW - Sand starvation

U2 - 10.1016/j.crte.2015.01.001

DO - 10.1016/j.crte.2015.01.001

M3 - Journal article

AN - SCOPUS:84924401981

VL - 348

SP - 462

EP - 470

JO - Comptes Rendus Geoscience

JF - Comptes Rendus Geoscience

SN - 1631-0713

IS - 6

ER -

ID: 199962408