Comment on “Carbonate deposition and diagenesis in evaporitic environments: The evaporative and sulphur-bearing limestones during the settlement of the Messinian Salinity Crisis in Sicily and Calabria” by Caruso et al., 2015. Palaeo3, 429, 136-162
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- 作者：Vinicio Manzia ; b ; vinicio.manzi@unipr.it" class="auth_mail" title="E-mail the corresponding author ; Rocco Gennaria ; b ; Stefano Luglic ; Nicola Minellia ; Matteo Reghizzia ; Marco Roveria ; b ; B. Charlotte Schreiberd
- 关键词：Messinian Salinity Crisis ; Calcare di Base ; Evaporites ; Sicily ; Stratigraphy
- 刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
- 出版年：2016
- 出版时间：1 October 2016
- 年：2016
- 卷：459
- 期：Complete
- 页码：585-596
- 全文大小：4084 K
文摘
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In this study we challenge the conclusions of the paper by Caruso et al. (2015).
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We rule out the elements supporting a diachronous MSC onset.
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The base of the Calcare di Base of Sicily is a regional scale unconformity.
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Basinward this unconformity passes to its correlative conformity.
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We clarify the stratigraphic relationships among the different MSC units of Sicily.