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Responses of dune plant communities to continental uplift from a major earthquake: Sudden releases from coastal squeeze
Indexado
WoS WOS:000354049700040
Scopus SCOPUS_ID:84929073581
DOI 10.1371/JOURNAL.PONE.0124334
Año 2015
Tipo artículo de investigación

Citas Totales

Autores Afiliación Chile

Instituciones Chile

% Participación
Internacional

Autores
Afiliación Extranjera

Instituciones
Extranjeras


Abstract



Vegetated dunes are recognized as important natural barriers that shelter inland ecosystems and coastlines suffering daily erosive impacts of the sea and extreme events, such as tsunamis. However, societal responses to erosion and shoreline retreat often result in man-made coastal defence structures that cover part of the intertidal and upper shore zones causing coastal squeeze and habitat loss, especially for upper shore biota, such as dune plants. Coseismic uplift of up to 2.0 m on the Peninsula de Arauco (South central Chile, ca. 37.5 degrees S) caused by the 2010 Maule earthquake drastically modified the coastal landscape, including major increases in the width of uplifted beaches and the immediate conversion of mid to low sandy intertidal habitat to supralittoral sandy habitat above the reach of average tides and waves. To investigate the early stage responses in species richness, cover and across-shore distribution of the hitherto absent dune plants, we surveyed two formerly intertidal armoured sites and a nearby intertidal unarmoured site on a sandy beach located on the uplifted coast of Llico (Peninsula de Arauco) over two years. Almost 2 years after the 2010 earthquake, dune plants began to recruit, then rapidly grew and produced dune hummocks in the new upper beach habitats created by uplift at the three sites. Initial vegetation responses were very similar among sites. However, over the course of the study, the emerging vegetated dunes of the armoured sites suffered a slowdown in the development of the spatial distribution process, and remained impoverished in species richness and cover compared to the unarmoured site. Our results suggest that when released from the effects of coastal squeeze, vegetated dunes can recover without restoration actions. However, subsequent human activities and management of newly created beach and dune habitats can significantly alter the trajectory of vegetated dune development. Management that integrates the effects of natural and human induced disturbances, and promotes the development of dune vegetation as natural barriers can provide societal and conservation benefits in coastal ecosystems.

Revista



Revista ISSN
P Lo S One 1932-6203

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Disciplinas de Investigación



WOS
Biology
Multidisciplinary Sciences
Scopus
Sin Disciplinas
SciELO
Sin Disciplinas

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Publicaciones WoS (Ediciones: ISSHP, ISTP, AHCI, SSCI, SCI), Scopus, SciELO Chile.

Colaboración Institucional



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Autores - Afiliación



Ord. Autor Género Institución - País
1 Rodil, Ivan F. Hombre Univ Porto - Portugal
University of Porto, Interdisciplinary Centre of Marine and Environmental Research - Portugal
CIIMAR - Interdisciplinary Centre of Marine and Environmental Research - Portugal
2 JARAMILLO-LOPETEGUI, EDUARDO JUVENAL Hombre Universidad Austral de Chile - Chile
3 Hubbard, David M. Hombre UNIV CALIF SANTA BARBARA - Estados Unidos
University of California, Santa Barbara - Estados Unidos
4 Dugan, Jenifer Mujer UNIV CALIF SANTA BARBARA - Estados Unidos
University of California, Santa Barbara - Estados Unidos
5 Melnick, Daniel Hombre Univ Potsdam - Alemania
Universität Potsdam - Alemania
6 VELASQUEZ-GALLARDO, CARLOS Hombre Universidad Austral de Chile - Chile

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Origen de Citas Identificadas



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Citas identificadas: Las citas provienen de documentos incluidos en la base de datos de DATACIENCIA

Citas Identificadas: 15.38 %
Citas No-identificadas: 84.62 %

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Citas identificadas: Las citas provienen de documentos incluidos en la base de datos de DATACIENCIA

Citas Identificadas: 15.38 %
Citas No-identificadas: 84.62 %

Financiamiento



Fuente
National Science Foundation
Comisión Nacional de Investigación Científica y Tecnológica
CONICYT Chile (National Commission for Science) through Proyectos Fondecyt
Santa Barbara Coastal LTER
Directorate for Geosciences

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Agradecimientos



Agradecimiento
This study was supported by CONICYT Chile (National Commission for Science, Chile; www.conicyt.cl) through Proyectos Fondecyt 1090650 and 1121043 granted to EJ. Support for JED was provided by The Santa Barbara Coastal LTER funded by the National Science Foundation (award no. OCE-0620276). IFR is a postdoctoral fellow from the Portuguese Foundation for Science and Technology-FCT (SFRH/BPD/87042/2012). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.

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