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Micropaleontology of the Noja sand dunes (Cantabria, N. Spain)

dc.contributor.authorPascual, Ana
dc.contributor.authorCarriedo, J.
dc.contributor.authorMartín Rubio, Maite
dc.contributor.authorMartínez García, Blanca
dc.contributor.authorFlor, G.
dc.contributor.authorRodríguez Lázaro, Julio
dc.date.accessioned2014-07-08T09:52:55Z
dc.date.available2014-07-08T09:52:55Z
dc.date.issued2006
dc.identifier.urihttp://hdl.handle.net/10272/8454
dc.description.abstractA total of 45 species of benthic foraminifers and 8 of ostracods have been studied from the sandy sediment of dunes from Noja (Cantabria, Spain). Dominant assemblages are formed by the species Lobatula lobatula and Cibicides refulgens, accompanied by Quinqueloculina seminula, Rosalina globularis and Textularia sagittula (foraminifers) and by Loxoconcha elliptica and Caudites calceolatus (ostracods). Since those species are present in the Noja beaches or are occurring as thanatocoenotic specimens transported from the marine shelf, we can propose that the sediment of the dunes is originated in the beaches, and accumulated by dominant winds from the NW. In the dunes of the Trengandin beaches the further occurrence of individuals of euryhaline species, such as Ammonia tepida at the base of the dunes, suggests the existence of sources of water coming from the karstic urgonian limestones of the outcrops in the areaen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherBenthic foraminifersen_US
dc.subject.otherOstracodsen_US
dc.subject.otherSand dunesen_US
dc.subject.otherNoja- Cantabriaen_US
dc.subject.otherBay of Biscayen_US
dc.titleContenido micropaleontológico de las arenas dunares de Noja (Cantabria)en_US
dc.titleMicropaleontology of the Noja sand dunes (Cantabria, N. Spain)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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