Identificador persistente para citar o vincular este elemento: http://hdl.handle.net/10553/42153
Campo DC Valoridioma
dc.contributor.authorMeco, Joaquínen_US
dc.contributor.authorLomoschitz, Alejandroen_US
dc.contributor.authorRodríguez Santana, Ángelen_US
dc.contributor.authorRamos, Antonio J.G.en_US
dc.contributor.authorBetancort, Juan F.en_US
dc.contributor.authorCoca, Josepen_US
dc.contributor.otherCoca Saez de Albeniz, Josep-
dc.contributor.otherRodriguez Santana, Angel-
dc.date.accessioned2018-10-17T08:03:13Z-
dc.date.available2018-10-17T08:03:13Z-
dc.date.issued2018en_US
dc.identifier.issn0031-0182en_US
dc.identifier.urihttp://hdl.handle.net/10553/42153-
dc.description.abstractThe eastern coast of Fuerteventura (Canary Islands, Spain) hosts the most complete and representative emergent Holocene marine deposits in the middle latitudes (27 degrees N to 30 degrees N) of the eastern Atlantic Ocean. The deposits consist of berms of gravel and foreshore sands which form beach rocks comprising > 62 bed sets, with each bed set containing dozens of individual laminations suggesting a cyclical cause as, for example, the orbital movement of the Earth. Calibrated radiocarbon ages place a group of older Holocene highstands of Fuerteventura at around the Mid-Late Holocene boundary (around 4.2 kyr B.P.), and another group of more recent highstands in the Dark Age Period (around 1.4 kyr B.P.) of the Northern Hemisphere. 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. Moreover, terrestrial deposits intercalated between the marine deposits indicate a lowering of the sea level at ca. 3 kyr B.P. When the sea levels reached their highstands during these two periods, the sea surface temperatures (SST) at the southern tip of the cold Canary Current were, respectively, 0.5 and 1.5 degrees C colder than the present-day SST (21.23 degrees C). The fossil fauna content confirms that these highstands occurred in cold conditions. In contrast, the present SST reaches the range of temperatures of the Holocene Optimum in the area.en_US
dc.languageengen_US
dc.relation.ispartofPalaeogeography, Palaeoclimatology, Palaeoecologyen_US
dc.sourcePalaeogeography, Palaeoclimatology, Palaeoecology [ISSN 0031-0182], v. 507, p. 214-225, (Octubre 2018)en_US
dc.subject2416 Paleontologíaen_US
dc.subject.otherMarine terracesen_US
dc.subject.otherHolocene climateen_US
dc.subject.otherSea-level highstandsen_US
dc.subject.otherOrbital forcingen_US
dc.subject.otherGIA effectsen_US
dc.subject.otherNE Atlantic Oceanen_US
dc.titleMid and Late Holocene sea level variations in the Canary Islandsen_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.palaeo.2018.07.020en_US
dc.identifier.scopus85050281910-
dc.identifier.isi000442055900017-
dcterms.isPartOfPalaeogeography Palaeoclimatology Palaeoecology-
dcterms.sourcePalaeogeography Palaeoclimatology Palaeoecology[ISSN 0031-0182],v. 507, p. 214-225-
dc.contributor.authorscopusid6602093969-
dc.contributor.authorscopusid6507150380-
dc.contributor.authorscopusid57189466695-
dc.contributor.authorscopusid56505656800-
dc.contributor.authorscopusid6602503518-
dc.contributor.authorscopusid7006741572-
dc.description.lastpage225en_US
dc.description.firstpage214en_US
dc.relation.volume507en_US
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.identifier.wosWOS:000442055900017-
dc.contributor.daisngid1788859-
dc.contributor.daisngid2025802-
dc.contributor.daisngid1821092-
dc.contributor.daisngid71632-
dc.contributor.daisngid30350490-
dc.contributor.daisngid3925610-
dc.contributor.daisngid1955355-
dc.identifier.investigatorRIDH-7067-2015-
dc.identifier.investigatorRIDH-8596-2015-
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Meco, J-
dc.contributor.wosstandardWOS:Lomoschitz, A-
dc.contributor.wosstandardWOS:Rodriguez Santana, Ángel-
dc.contributor.wosstandardWOS:Ramos, AJG-
dc.contributor.wosstandardWOS:Betancort, JF-
dc.contributor.wosstandardWOS:Coca, J-
dc.date.coverdateOctubre 2018en_US
dc.identifier.ulpgcen_US
dc.description.sjr1,322
dc.description.jcr2,616
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
item.grantfulltextnone-
item.fulltextSin texto completo-
crisitem.author.deptGIR IOCAG:Geología Aplicada y Regional-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Ingeniería Civil-
crisitem.author.deptGIR ECOAQUA: Oceanografía Física y Geofísica Aplicada-
crisitem.author.deptIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.deptDepartamento de Física-
crisitem.author.deptGIR ECOAQUA: Biodiversidad y Conservación-
crisitem.author.deptIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.deptDepartamento de Biología-
crisitem.author.deptGIR ECOAQUA: Biodiversidad y Conservación-
crisitem.author.deptIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.orcid0000-0001-7658-9956-
crisitem.author.orcid0000-0002-8812-0351-
crisitem.author.orcid0000-0003-1960-6777-
crisitem.author.orcid0000-0003-1374-5805-
crisitem.author.orcid0000-0003-0625-8240-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.parentorgIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.parentorgIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.parentorgIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.fullNameMeco Cabrera, Joaquín Francisco-
crisitem.author.fullNameLomoschitz Mora-Figueroa, Alejandro-
crisitem.author.fullNameRodríguez Santana, Ángel-
crisitem.author.fullNameGonzález Ramos, Antonio Juan-
crisitem.author.fullNameSaenz De Albeniz,Josep Coca-
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