Journal cover Journal topic
Climate of the Past An interactive open-access journal of the European Geosciences Union
Clim. Past, 13, 533-544, 2017
https://doi.org/10.5194/cp-13-533-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
24 May 2017
A 21 000-year record of fluorescent organic matter markers in the WAIS Divide ice core
Juliana D'Andrilli et al.
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Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
 
RC1: 'Referee report', Anonymous Referee #1, 03 Jan 2017 Printer-friendly Version 
SC2: 'Reply to RC1', Juliana D'Andrilli, 24 Jan 2017 Printer-friendly Version 
AC1: 'Author Comment: Reply to RC1', Juliana D'Andrilli, 09 Feb 2017 Printer-friendly Version 
 
RC2: 'Review of “A 21,000 year record of organic matter quality in the WAIS Divide ice core”', Anonymous Referee #2, 04 Jan 2017 Printer-friendly Version 
SC3: 'Reply to RC2', Juliana D'Andrilli, 24 Jan 2017 Printer-friendly Version 
AC2: 'Author Comment: Reply to RC2', Juliana D'Andrilli, 09 Feb 2017 Printer-friendly Version 
 
RC3: 'Referee Report', Anonymous Referee #3, 08 Jan 2017 Printer-friendly Version Supplement 
SC4: 'Reply to RC3', Juliana D'Andrilli, 24 Jan 2017 Printer-friendly Version 
AC3: 'Author Comment: Reply to RC3', Juliana D'Andrilli, 09 Feb 2017 Printer-friendly Version 
 
SC1: 'Comments on PARAFAC and fluorescence from Andy Baker, UNSW Sydney', Andy Baker, 20 Jan 2017 Printer-friendly Version 
SC5: 'Reply to SC1', Juliana D'Andrilli, 24 Jan 2017 Printer-friendly Version 
AC4: 'Author Comment: Reply to SC1', Juliana D'Andrilli, 09 Feb 2017 Printer-friendly Version 
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (13 Feb 2017) by Carlo Barbante  
AR by Juliana D'Andrilli on behalf of the Authors (26 Mar 2017)  Author's response  Manuscript
ED: Publish as is (19 Apr 2017) by Carlo Barbante  
CC BY 4.0
Publications Copernicus
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Short summary
Climate-driven trends in fluorescent organic matter (OM) markers from Antarctic ice cores revealed fluctuations over 21.0 kyr, reflecting environmental shifts as a result of global ecosystem response in a warming climate. Precursors of lignin-like fluorescent chemical species were detected as OM markers from the Last Glacial Maximum to the mid-Holocene. Holocene ice contained the most complex lignin-like fluorescent OM markers. Thus, ice cores contain paleoecological OM markers of Earth’s past.
Climate-driven trends in fluorescent organic matter (OM) markers from Antarctic ice cores...
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