Articles | Volume 10, issue 4
https://doi.org/10.5194/cp-10-1421-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.Warming, euxinia and sea level rise during the Paleocene–Eocene Thermal Maximum on the Gulf Coastal Plain: implications for ocean oxygenation and nutrient cycling
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- Final revised paper (published on 25 Jul 2014)
- Supplement to the final revised paper
- Preprint (discussion started on 03 Dec 2013)
- Supplement to the preprint
Interactive discussion
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
- Printer-friendly version
- Supplement
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SC C2797: 'Comments', Ellen Thomas, 04 Dec 2013
- AC C3354: 'Reply to comments Ellen Thomas', Appy Sluijs, 05 Feb 2014
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SC C2972: 'Some general and specific questions and comments', Matthew Huber, 23 Dec 2013
- AC C3443: 'Reply to comments Matthew Huber', Appy Sluijs, 11 Feb 2014
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RC C3164: 'Comments on Sluijs et al.', M. F. Schaller, 20 Jan 2014
- AC C3505: 'Reply to comments Schaller', Appy Sluijs, 25 Feb 2014
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RC C3257: 'Comments on “Extreme warming..." by Sluijs et al.', Armelle Riboulleau, 27 Jan 2014
- AC C3523: 'Reply to comments Riboulleau', Appy Sluijs, 25 Feb 2014
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SC C3424: 'Correlation of the Tuscahoma Formation with the Paleocene-Eocene GSSP', Richard Fluegeman, 10 Feb 2014
- AC C3651: 'Reply to comments Fluegeman', Appy Sluijs, 17 Mar 2014
- EC C3698: 'Revised submission', Yves Godderis, 26 Apr 2014