Reply to the comment by Boulila and Hinnov towards "Chronology of the Early Toarcian environmental crisis in the Lorraine Sub-Basin (NE Paris Basin)" by W. Ruebsam, P. Münzberger, and L. Schwark [Earth and Planetary Science Letters 404 (2014) 273-282]
Reply to the comment by Boulila and Hinnov towards "Chronology of the Early Toarcian environmental crisis in the Lorraine Sub-Basin (NE Paris Basin)" by W. Ruebsam, P. Münzberger, and L. Schwark [Earth and Planetary Science Letters 404 (2014) 273-282]
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回复 Boulila 和 Hinnov 对 W Ruebsam、P Münzberger 和 L Schwark 撰写的“洛林次盆地(巴黎盆地东北部)早期托阿尔纪环境危机年代学”的评论 [地球与行星科学快报 404 (2014) 273 -282]
DOI:
10.1016/j.epsl.2015.02.022
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发表时间:
2015
影响因子:
5.3
通讯作者:
P. Schwark
中科院分区:
文献类型:
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作者:
Rübsam;Münzberger;P. Schwark
Recently Boulila and Hinnov provided an alternative interpretation for the cyclostratigraphy of the Early Toarcian in the Lorraine Basin proposed by Ruebsam et al.(2014). Floating chronologies based on cyclostratigraphy, in particular when discrete time lines (eg tephra layers, intrusions, etc.) are missing, are subject to contrasting interpretation and discussion as exemplified for the Early Toarcian by previous contributions (eg Kemp et al., 2011, Boulila et al., 2014, Huang and Hesselbo, 2014). In the following we address the discussion raised by Boulila and Hinnov with specific focus on differential sedimentation rates in sub-basins on the NW-Tethyan Shelf during the Early Toarcian and how this may have affected i) the duration of individual ammonite (sub) zones and the Toarcian carbon isotopic excursion, ii) the expression of a 405 ka cycle and iii) the obliquity-forcing on paleoclimate.
DOI:
--
发表时间:
2006
期刊:
影响因子:
--
作者:
M. Clémence;E. Huret;A. Bartolini;B. Galbrun;S. Gardin;L. Hinnov;V. Beaumont
通讯作者:
V. Beaumont
影响因子:
6.1
作者:
Huang, Chunju;Hesselbo, Stephen P.
通讯作者:
Hesselbo, Stephen P.