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Comment on “Formation of chenier plain of the Doñana marshland (SW Spain): Observations and geomorphic model” by A. Rodríguez-Ramírez and C.M. Yáñez-Camacho [Marine Geology 254 (2008) 187–196]

dc.contributor.authorLario Gómez, Javier
dc.contributor.authorDabrio González, Cristino José
dc.contributor.authorZazo Cardeña , Caridad
dc.contributor.authorGoy Goy, José Luis
dc.contributor.authorBorja, Francisco
dc.contributor.authorCabero del Río, Ana
dc.contributor.authorBardají Azcárate, Teresa
dc.contributor.authorSilva Barroso, Pablo Gabriel
dc.date.accessioned2023-06-20T00:13:04Z
dc.date.available2023-06-20T00:13:04Z
dc.date.issued2010
dc.description.abstractRodríguez-Ramírez and Yáñez-Camacho (2008), Rodríguez-Vidal et al. (2009) and Rodríguez-Ramírez et al. (2009) have kept an ongoing discussion about the validity of radiocarbon ages in reconstructing Holocene palaeogeographical models in the Gulf of Cadiz. The discussion considered the validity and correctness of the ΔR value to beused in the area to calibrate radiocarbon ages ofmarine samples. These papers suggest that theΔR value proposed by Lario (1996) and Dabrio et al. (1999, 2000) is erroneous, and consequently, that all the evolutionary models based on radiocarbon ages from marine samples that have been proposed in this area since 1996 must be revised.However, the papers commentedhere use erroneously the R, regional R andΔR values.After reviewing the published data, it is apparent that the most reliable values of ΔR in the Gulf of Cadiz for middle-late Holocene samples range between ΔR=35±85 yr and ΔR=95±15 yr. This means that the values used in Lario (1996) and Dabrio et al. (1999, 2000) fall in this range, and also that the calibrated ages used by several authors adopting these values are fully reliable. Calibrations using ΔR values inside this range do not yield significant differences in terms of geological age owing to the magnitude of errors resulting from the methods employed.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/15749
dc.identifier.doi10.1016/j.margeo.2010.02.023
dc.identifier.issn0025-3227
dc.identifier.officialurlhttp://www.elsevier.com/locate/margeo
dc.identifier.urihttps://hdl.handle.net/20.500.14352/42216
dc.journal.titleMarine Geology
dc.language.isoeng
dc.page.final286
dc.page.initial283
dc.publisherElsevier
dc.rights.accessRightsopen access
dc.subject.cdu551.79(460.355)
dc.subject.keywordRadiocarbon
dc.subject.keywordCalibration
dc.subject.keywordReservoir effect
dc.subject.keywordHolocene
dc.subject.keywordGulf of Cadiz
dc.subject.ucmGeología estratigráfica
dc.subject.unesco2506.19 Estratigrafía
dc.titleComment on “Formation of chenier plain of the Doñana marshland (SW Spain): Observations and geomorphic model” by A. Rodríguez-Ramírez and C.M. Yáñez-Camacho [Marine Geology 254 (2008) 187–196]
dc.typejournal article
dc.volume.number275
dspace.entity.typePublication
relation.isAuthorOfPublication55faa814-a938-4b9e-9840-d51419e44f20
relation.isAuthorOfPublication1556fc8c-dd30-40b0-a180-d00679f99678
relation.isAuthorOfPublication.latestForDiscovery1556fc8c-dd30-40b0-a180-d00679f99678

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