Articles | Volume 14, issue 10
https://doi.org/10.5194/cp-14-1543-2018
© 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-14-1543-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
23 Oct 2018
Research article |
| 23 Oct 2018
| 23 Oct 2018
Fire, vegetation, and Holocene climate in a southeastern Tibetan lake: a multi-biomarker reconstruction from Paru Co
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University of Venice, 30172, Venice, Italy
Institute for the Dynamics of Environmental Processes – CNR, 30172, Venice, Italy
Dario Battistel
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University of Venice, 30172, Venice, Italy
Geosciences and Environmental Change Science Center, U.S. Geological Survey, Denver Federal Center, Denver, CO 80225, USA
Felipe Matsubara Pereira
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University of Venice, 30172, Venice, Italy
Torben Kirchgeorg
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University of Venice, 30172, Venice, Italy
Maria del Carmen Villoslada Hidalgo
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University of Venice, 30172, Venice, Italy
Broxton W. Bird
Department of Earth Sciences, Indiana University–Purdue University, Indianapolis, IN 46208, USA
Carlo Barbante
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University of Venice, 30172, Venice, Italy
Institute for the Dynamics of Environmental Processes – CNR, 30172, Venice, Italy
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Latest update: 17 Nov 2024
Short summary
Holocene fires and vegetation are reconstructed using different molecular markers with a single analytical method, applied for the first time to lake sediments from Tibet. The early Holocene shows oscillations between grasses and conifers, with smouldering fires represented by levoglucosan peaks, and high-temperature fires represented by PAHs. The lack of human FeSts excludes local human influence on fire and vegetation changes. Late Holocene displays an increase in local to regional combustion.
Holocene fires and vegetation are reconstructed using different molecular markers with a single...
