2024-03-28T09:36:05Zhttp://digital.csic.es/dspace-oai/requestoai:digital.csic.es:10261/1743962019-01-22T01:57:39Zcom_10261_82com_10261_8col_10261_335
Formation and evolution of back‐barrier perched lakes in rocky coasts: An example of a Holocene system in north‐west Spain
Sáez, Alberto
Carballeira, R.
Pueyo Mur, Juan José
Vázquez-Loureiro, D.
Leira, Manel
Hernández, Armand
Valero-Garcés, Blas L.
Bao, Roberto
Ministerio de Economía y Competitividad (España)
Fundação para a Ciência e a Tecnologia (Portugal)
Hernández, Armand [0000-0001-7245-9863]
Valero-Garcés, Blas L. [0000-0003-2214-7057]
Bedrock topography
sequence stratigraphy
Coastal lakes
Galicia
high‐resolution chronology
Holocene
sea‐level changes
Coastal back‐barrier perched lakes are freshwater bodies that are elevated over sea‐level and are not directly subjected to the inflow of seawater. This study provides a detailed reconstruction of the Doniños back‐barrier perched lake that developed at the end of a small river valley in the rocky coast of the north‐west Iberian Peninsula during the Holocene transgression. Its sequence stratigraphy was reconstructed based on a core transect across the system, the analyses of its lithofacies and microfossil assemblages, and a high‐resolution radiocarbon‐based chronology. The Doniños perched lake was formed ca 4·5 ka bp. The setting of the perched lake was favoured by Late Holocene sea‐level stabilization and the formation of a barrier and back‐barrier basin, which was contemporaneous with the high systems tract period. This basin developed over marine and lagoonal sediments deposited between 10·2 ka bp and 8·0 ka bp, during rapidly rising sea‐level characteristic of the transgressive systems track period. At 1·1 ka bp, the barrier was breached and the perched lake was partially emptied, causing the erosion of the back‐barrier basin sediments and a significant sedimentary hiatus. Both enhanced storminess and human intervention were likely to be responsible for this event. After 1 ka bp, the barrier reclosed and the present‐day lake was reformed, with the water level reaching as high as 5 m above mean sea‐level. The depositional evolution of the Doniños system serves as a model of coastal back‐barrier perched lakes in coastal clastic systems that have developed over gently seaward‐dipping rugged substrates at small distances from the shoreline and under conditions of rising sea‐level and high sediment supply. A review of estuaries, back‐barrier lagoons, pocket beaches and back‐barrier perched lakes in the rocky coast of north‐west Spain shows that the elevation of the bedrock is the main factor controlling the origin and evolution of these systems.
2019-01-21T08:56:38Z
2019-01-21T08:56:38Z
2018-01
artículo
Sedimentology; 65(6): 1891-1917 (2018)
0037-0746
http://hdl.handle.net/10261/174396
10.1111/sed.12451
1365-3091
http://dx.doi.org/10.13039/501100003329
http://dx.doi.org/10.13039/501100001871
eng
https://doi.org/10.1111/sed.12451
Sí
closedAccess
John Wiley & Sons