Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/73090
Title: El Holoceno en Canarias
Authors: Lomoschitz Mora-Figueroa, Alejandro 
Rodríguez Santana, Ángel 
González Ramos, Antonio Juan 
Betancort, Juan-Francisco
Coca Saenz De Albéniz, Josep 
Meco Cabrera, Joaquín Francisco 
UNESCO Clasification: 2416 Paleontología
Keywords: Canary Islands
Issue Date: 2019
Publisher: Universidad del País Vasco
Aranzadi (Thomson Reuters)
Conference: XV reunión nacional de Cuaternario 
Abstract: Fuerteventura (Canary Islands) hosts the most representative emergent Holocene marine deposits in the middle latitudes of the eastern Atlantic Ocean. The deposits consist of berms and beachrocks suggesting a cyclical cause as the orbital movement of the Earth. Radiocarbon ages place a group at around 4.2 kyr BP and another group at around 1.4 kyr BP. They have been recorded at 4 m and 3.5 m apmsl respectively. The present-day tidal amplitude is around 3 m. Assuming a similar value for the Holocene, the corresponding relative sea level rises were around 2.5 m and 2 m apmsl respectively. During these two periods, the sea surface temperatures at the southern tip of the Canary Current were colder than the present-day SST. Intercalated terrestrial deposits indicate a lowering of the sea-level at ca. 3 kyr BP.
URI: http://hdl.handle.net/10553/73090
ISBN: 978-84-17713-16-4
Source: XV Reunión Nacional de Cuaternario: Libro de resúmenes, p. 67-70
URL: http://dialnet.unirioja.es/servlet/articulo?codigo=7398296
Appears in Collections:Actas de congresos
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