Articles | Volume 14, issue 6
https://doi.org/10.5194/cp-14-871-2018
https://doi.org/10.5194/cp-14-871-2018
Research article
 | 
21 Jun 2018
Research article |  | 21 Jun 2018

High-latitude Southern Hemisphere fire history during the mid- to late Holocene (6000–750 BP)

Dario Battistel, Natalie M. Kehrwald, Piero Zennaro, Giuseppe Pellegrino, Elena Barbaro, Roberta Zangrando, Xanthi X. Pedeli, Cristiano Varin, Andrea Spolaor, Paul T. Vallelonga, Andrea Gambaro, and Carlo Barbante

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (29 Mar 2018) by Eric Wolff
AR by Dario Battistel on behalf of the Authors (13 Apr 2018)  Manuscript 
ED: Referee Nomination & Report Request started (27 Apr 2018) by Eric Wolff
RR by Anonymous Referee #1 (07 May 2018)
RR by Anonymous Referee #2 (18 May 2018)
ED: Reconsider after major revisions (31 May 2018) by Eric Wolff
AR by Dario Battistel on behalf of the Authors (11 Jun 2018)
ED: Publish as is (14 Jun 2018) by Eric Wolff
AR by Dario Battistel on behalf of the Authors (14 Jun 2018)
Download
Short summary
From the analysis of an Antarctic ice core we showed that during the mid- to late Holocene (6000–750 BP) the long-term fire activity increased with higher rates starting at ~ 4000 BP and, more surprisingly, peaked between 2500 and 1500 BP. The anomalous increase in biomass burning centered at about 2000 BP is due to a complex interaction between changes in atmospheric circulation and biomass availability, with the main contribution coming from southern South America.