Short communication: Reply to Comment by Domínguez-Villar on “Land surface temperature changes in Northern Iberia since 4000 yr BP, based in δ13C of speleothems” (Martín-Chivelet et al., 2011)

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dc.contributor.authorMartín Chivelet, Javier
dc.contributor.authorMuñoz García, Belén
dc.contributor.authorEdwards, R. Lawrence
dc.contributor.authorTurrero Jiménez, María Jesús
dc.contributor.authorOrtega Martínez, Ana Isabel
dc.date.accessioned2023-06-19T13:37:31Z
dc.date.available2023-06-19T13:37:31Z
dc.date.issued2013
dc.description.abstractWe have considered the additional data that Domínguez-Villar (this issue) has provided, as well as his criticisms of the interpretations of Martín-Chivelet et al. (2011). We argue that with or without the additional data, our original interpretations are the most likely interpretations, on the basis of Ockham's Razor. Those of Domínguez-Villar violate Ockham's Razor, and in the final analysis do not offer an alternative explanation for the Martín-Chivelet et al. (2011) and Domínguez-Villar (this issue) data. In particular, all of the 230Th ages (reported by both Martín-Chivelet et al. (2011) and Domínguez-Villar (this issue)) are in stratigraphic order, within quoted errors, so that our original chronology is robust, with no reason to invoke diagenetic processes. Given this chronology, the empirical relationship between δ13C and temperature also hold. Finally, our original mechanism for the cause of this relationship (prior calcite precipitation) has been invoked in a number of other studies to explain carbon isotopic variations and remains a perfectly plausible explanation for the observations at the studied caves.
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/58048
dc.identifier.doi10.1016/j.gloplacha.2012.12.005
dc.identifier.issn0921-8181
dc.identifier.officialurlhttps://www.journals.elsevier.com/global-and-planetary-change/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/34150
dc.journal.titleGlobal and planetary change
dc.language.isoeng
dc.page.final130
dc.page.initial129
dc.publisherElsevier
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.cdu551.7
dc.subject.keywordClimate change
dc.subject.keywordPaleoclimate
dc.subject.keywordSpeleothem
dc.subject.keywordStable isotopes
dc.subject.keywordHolocene
dc.subject.keywordIberia
dc.subject.ucmGeología estratigráfica
dc.subject.unesco2506.19 Estratigrafía
dc.titleShort communication: Reply to Comment by Domínguez-Villar on “Land surface temperature changes in Northern Iberia since 4000 yr BP, based in δ13C of speleothems” (Martín-Chivelet et al., 2011)
dc.typejournal article
dc.volume.number101
dspace.entity.typePublication
relation.isAuthorOfPublicationec6fc8e5-d413-47bf-9ada-4ff280f9e849
relation.isAuthorOfPublication.latestForDiscoveryec6fc8e5-d413-47bf-9ada-4ff280f9e849
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