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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Reply to the comment on 'Sea-level control on facies architecture in the Cenomanian-Coniacian Apulian margin (Western Tethys): A record of glacio-eustatic fluctuations during the Cretaceous greenhouse?' by S. Galeotti, G. Rusciadelli, M. Sprovieri, L. Lanci, A. Gaudio and S. Pekar [Palaeogeography, Palaeoclimatology, Palaeoecology 276 (2009) 196-205]
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Reply to the comment on 'Sea-level control on facies architecture in the Cenomanian-Coniacian Apulian margin (Western Tethys): A record of glacio-eustatic fluctuations during the Cretaceous greenhouse?' by S. Galeotti, G. Rusciadelli, M. Sprovieri, L. Lanci, A. Gaudio and S. Pekar [Palaeogeography, Palaeoclimatology, Palaeoecology 276 (2009) 196-205]

机译：回复关于“海平面控制西诺曼尼亚-科尼亚人普利亚边缘（西特提斯）的相结构的海平面控制：白垩纪温室内冰川垂向波动的记录？”作者：S。Galeotti，G。Rusciadelli，M.Sprovieri，L.Lanci，A。Gaudio和S. Pekar [古地理，古气候，古生态276（2009）196-205]

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Parente et al. (2010) (hereafter Petal10) (Comment on "Sea-level control on facies architecture in the Cenomanian-Coniacian Apulian margin (Western Tethys): A record of glacio-eustatic fluctuations during the Cretaceous greenhouse?" by S. Galeotti, G. Rusciadelli, M. Sprovieri, L. Lanci, A. Gaudio and S. Pekar [Palaeogeography, Palaeoclimatology, Palaeoecology 276 (2009) 196-205], Palaeogeogr. Palaeoclimatol. Palaeoecol, 2010-this issue) discuss our contribution to the correlation of eustatic sea-level changes observed in the Cenomanian-Coniacian Apulian margin (Western Tethys) to reference records of sea-level fluctuation and the methods implied in constructing such correlation. Their conclusions stem from a fundamental misinterpretation of the method used in our study, particularly as far as the approach used to put the observed sequences, which are interpreted to reflect global sea-level changes, into context. In their comment, Petal10 extensively discuss the pitfalls implied in calibrating records and events in carbonate platform settings to a standard chronostratigraphy on the basis of biostratigraphy. This approach would be an obvious element of concern, but does not form the basis of the calibration in our study, which is based on the following procedure: 1. Biostratigraphy and event stratigraphy-based correlation - not calibration - of the events observed in the carbonate platform to the adjacent base-of-slope Monte Turno record; 2. Calibration of the Monte Turno bio- and chemostratigraphic record to reference (glacio)eustatic and chemostratigraphic records.
机译：Parente等。 （2010年，以下简称为Petal10）（S。Galeotti，G.发表的评论：“海平面控制西诺曼尼亚-科尼亚人普利亚缘（西特提斯）的相结构的记录：白垩纪温室期间的冰川-欧拉波动记录？”。 Rusciadelli，M.Sprovieri，L.Lanci，A.Gaudio和S.Pekar [古地理，古气候学，古生态学276（2009）196-205]，古地理Greoeoclimatol。Palaeoecol，2010-本期）讨论了我们对相关性的贡献在Cenomanian-Coniacian Apulian边缘（西特提斯）观测到的海平面变化，以参考海平面波动的记录以及建立这种相关关系的方法。他们的结论源于我们研究中所用方法的根本误解，尤其是将观测到的序列（其被解释为反映全球海平面变化的方法）用于背景的方法方面。在他们的评论中，Petal10广泛讨论了根据生物地​​层学将碳酸盐岩平台环境中的记录和事件校准为标准年代地层所隐含的陷阱。这种方法显然是一个值得关注的因素，但它并不构成我们研究中校准的基础，该校准基于以下步骤：1.生物地层学和基于事件地层的相关性-而非校准-碳酸盐岩台地到相邻的坡底Monte Turno记录; 2.校准Monte Turno生物和化学书记的记录，以参考（冰川）止血和化学书记的记录。

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