DOI: 10.1016/j.gloplacha.2012.12.005
论文题名: Reply to Comment by Domínguez-Villar on "Land surface temperature changes in Northern Iberia since 4000yr BP, based in δ13C of speleothems" (Martín-Chivelet et al., 2011)
作者: Martín-Chivelet J. ; Muñoz-García M.B. ; Edwards R.L. ; Turrero M.J. ; Ortega A.I.
刊名: Global and Planetary Change
ISSN: 0921-8335
出版年: 2013
卷: 101 起始页码: 129
结束页码: 130
语种: 英语
英文关键词: Climate change
; Holocene
; Iberia
; Paleoclimate
; Speleothem
; Stable isotopes
Scopus关键词: Holocenes
; Iberia
; Paleoclimates
; Speleothem
; Stable isotopes
; Climate change
; Isotopes
; Stratigraphy
; Atmospheric temperature
; biostratigraphy
; carbon isotope
; chronology
; climate change
; data set
; Holocene
; land surface
; observational method
; paleoclimate
; precipitation (climatology)
; stable isotope
; surface temperature
; Iberian Peninsula
英文摘要: We 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. © 2013 Elsevier B.V. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84873113513&doi=10.1016%2fj.gloplacha.2012.12.005&partnerID=40&md5=c11b8a1ba384eded292672d40d9e1836
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/11241
Appears in Collections: 全球变化的国际研究计划
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作者单位: Universidad Complutense de Madrid, Dpt. Estratigrafía, Facultad de Ciencias Geológicas and Instituto de Geociencias IGEO (CSIC, UCM), 28040 Madrid, Spain
Recommended Citation:
Martín-Chivelet J.,Muñoz-García M.B.,Edwards R.L.,et al. Reply to Comment by Domínguez-Villar on "Land surface temperature changes in Northern Iberia since 4000yr BP, based in δ13C of speleothems" (Martín-Chivelet et al., 2011)[J]. Global and Planetary Change,2013-01-01,101.