Articles | Volume 14, issue 6
https://doi.org/10.5194/cp-14-871-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-14-871-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
21 Jun 2018
Research article |
| 21 Jun 2018
| 21 Jun 2018
High-latitude Southern Hemisphere fire history during the mid- to late Holocene (6000–750 BP)
Department of Environmental Science, Informatics and Statistics, University Ca' Foscari of Venice,
Via Torino 155, 30170 Mestre Venezia, Venice, Italy
Institute for the Dynamics of Environmental
Processes – IDPA-CNR, Via Torino 155,
30170 Mestre Venezia, Venice, Italy
Natalie M. Kehrwald
US Geological Survey,
Geosciences and Environmental Change Science Center, Denver, CO 80225, USA
Piero Zennaro
Department of Environmental Science, Informatics and Statistics, University Ca' Foscari of Venice,
Via Torino 155, 30170 Mestre Venezia, Venice, Italy
Giuseppe Pellegrino
Department of Environmental Science, Informatics and Statistics, University Ca' Foscari of Venice,
Via Torino 155, 30170 Mestre Venezia, Venice, Italy
Elena Barbaro
Department of Environmental Science, Informatics and Statistics, University Ca' Foscari of Venice,
Via Torino 155, 30170 Mestre Venezia, Venice, Italy
Institute for the Dynamics of Environmental
Processes – IDPA-CNR, Via Torino 155,
30170 Mestre Venezia, Venice, Italy
Roberta Zangrando
Institute for the Dynamics of Environmental
Processes – IDPA-CNR, Via Torino 155,
30170 Mestre Venezia, Venice, Italy
Xanthi X. Pedeli
Department of Environmental Science, Informatics and Statistics, University Ca' Foscari of Venice,
Via Torino 155, 30170 Mestre Venezia, Venice, Italy
Cristiano Varin
Department of Environmental Science, Informatics and Statistics, University Ca' Foscari of Venice,
Via Torino 155, 30170 Mestre Venezia, Venice, Italy
Andrea Spolaor
Institute for the Dynamics of Environmental
Processes – IDPA-CNR, Via Torino 155,
30170 Mestre Venezia, Venice, Italy
Paul T. Vallelonga
Centre for Ice and Climate, Niels Bohr Institute, University of
Copenhagen, Juliane Maries Vej 30, 2100 Copenhagen, Denmark
Andrea Gambaro
Department of Environmental Science, Informatics and Statistics, University Ca' Foscari of Venice,
Via Torino 155, 30170 Mestre Venezia, Venice, Italy
Institute for the Dynamics of Environmental
Processes – IDPA-CNR, Via Torino 155,
30170 Mestre Venezia, Venice, Italy
Carlo Barbante
Department of Environmental Science, Informatics and Statistics, University Ca' Foscari of Venice,
Via Torino 155, 30170 Mestre Venezia, Venice, Italy
Institute for the Dynamics of Environmental
Processes – IDPA-CNR, Via Torino 155,
30170 Mestre Venezia, Venice, Italy
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Cited
13 citations as recorded by crossref.
- Improved estimates of preindustrial biomass burning reduce the magnitude of aerosol climate forcing in the Southern Hemisphere P. Liu et al. 10.1126/sciadv.abc1379
- Organic tracers from biomass burning in snow from the coast to the ice sheet summit of East Antarctica G. Shi et al. 10.1016/j.atmosenv.2018.12.058
- Holocene changes in biomass burning in the boreal Northern Hemisphere, reconstructed from anhydrosugar fluxes in an Arctic sediment profile A. Chen et al. 10.1016/j.scitotenv.2023.161460
- Connections of climate change and variability to large and extreme forest fires in southeast Australia N. Abram et al. 10.1038/s43247-020-00065-8
- Biomarker proxies for reconstructing Quaternary climate and environmental change E. McClymont et al. 10.1002/jqs.3559
- Analysis of levoglucosan and its isomers in atmospheric samples by ion chromatography with electrospray lithium cationisation - Triple quadrupole tandem mass spectrometry E. Sanz Rodriguez et al. 10.1016/j.chroma.2019.460557
- Fast Liquid Chromatography Coupled with Tandem Mass Spectrometry for the Analysis of Vanillic and Syringic Acids in Ice Cores E. Barbaro et al. 10.1021/acs.analchem.1c05412
- Environmental significance of levoglucosan records in a central Tibetan ice core C. You et al. 10.1016/j.scib.2018.12.016
- Five thousand years of fire history in the high North Atlantic region: natural variability and ancient human forcing D. Segato et al. 10.5194/cp-17-1533-2021
- Fire records in glacier ice C. You & T. Yao 10.1093/nsr/nwy159
- A Review of Speleothems as Archives for Paleofire Proxies, With Australian Case Studies M. Campbell et al. 10.1029/2022RG000790
- Anhydrosugars as tracers in the Earth system L. Suciu et al. 10.1007/s10533-019-00622-0
- Southern hemisphere fire history since the late glacial, reconstructed from an Antarctic sediment core A. Chen et al. 10.1016/j.quascirev.2021.107300
13 citations as recorded by crossref.
- Improved estimates of preindustrial biomass burning reduce the magnitude of aerosol climate forcing in the Southern Hemisphere P. Liu et al. 10.1126/sciadv.abc1379
- Organic tracers from biomass burning in snow from the coast to the ice sheet summit of East Antarctica G. Shi et al. 10.1016/j.atmosenv.2018.12.058
- Holocene changes in biomass burning in the boreal Northern Hemisphere, reconstructed from anhydrosugar fluxes in an Arctic sediment profile A. Chen et al. 10.1016/j.scitotenv.2023.161460
- Connections of climate change and variability to large and extreme forest fires in southeast Australia N. Abram et al. 10.1038/s43247-020-00065-8
- Biomarker proxies for reconstructing Quaternary climate and environmental change E. McClymont et al. 10.1002/jqs.3559
- Analysis of levoglucosan and its isomers in atmospheric samples by ion chromatography with electrospray lithium cationisation - Triple quadrupole tandem mass spectrometry E. Sanz Rodriguez et al. 10.1016/j.chroma.2019.460557
- Fast Liquid Chromatography Coupled with Tandem Mass Spectrometry for the Analysis of Vanillic and Syringic Acids in Ice Cores E. Barbaro et al. 10.1021/acs.analchem.1c05412
- Environmental significance of levoglucosan records in a central Tibetan ice core C. You et al. 10.1016/j.scib.2018.12.016
- Five thousand years of fire history in the high North Atlantic region: natural variability and ancient human forcing D. Segato et al. 10.5194/cp-17-1533-2021
- Fire records in glacier ice C. You & T. Yao 10.1093/nsr/nwy159
- A Review of Speleothems as Archives for Paleofire Proxies, With Australian Case Studies M. Campbell et al. 10.1029/2022RG000790
- Anhydrosugars as tracers in the Earth system L. Suciu et al. 10.1007/s10533-019-00622-0
- Southern hemisphere fire history since the late glacial, reconstructed from an Antarctic sediment core A. Chen et al. 10.1016/j.quascirev.2021.107300
Latest update: 18 Apr 2024
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.
From the analysis of an Antarctic ice core we showed that during the mid- to late Holocene...
