Articles | Volume 6, issue 4
https://doi.org/10.5194/esurf-6-829-2018
© 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/esurf-6-829-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Effect of changing vegetation and precipitation on denudation – Part 1: Predicted vegetation composition and cover over the last 21 thousand years along the Coastal Cordillera of Chile
Christian Werner
CORRESPONDING AUTHOR
Senckenberg Biodiversity and Climate Research Centre (BiK-F),
Senckenberganlage 25, 60325 Frankfurt, Germany
Manuel Schmid
Department of Geosciences, University of Tuebingen, Wilhelmstrasse
56, 72074 Tuebingen, Germany
Todd A. Ehlers
Department of Geosciences, University of Tuebingen, Wilhelmstrasse
56, 72074 Tuebingen, Germany
Juan Pablo Fuentes-Espoz
Department of Silviculture and Nature Conservation, University of
Chile, Av. Santa Rosa 11315, La Pintana, Santiago RM, Chile
Jörg Steinkamp
Senckenberg Biodiversity and Climate Research Centre (BiK-F),
Senckenberganlage 25, 60325 Frankfurt, Germany
Matthew Forrest
Senckenberg Biodiversity and Climate Research Centre (BiK-F),
Senckenberganlage 25, 60325 Frankfurt, Germany
Johan Liakka
Nansen Environmental and Remote Sensing Center, Bjerknes Centre for
Climate Research, Thormøhlens gate 47, 5006 Bergen, Norway
Antonio Maldonado
Centro de Estudios Avanzados en Zonas Áridas (CEAZA), Raúl
Bitrán 1305, La Serena, Chile
Thomas Hickler
Senckenberg Biodiversity and Climate Research Centre (BiK-F),
Senckenberganlage 25, 60325 Frankfurt, Germany
Department of Physical Geography, Geosciences, Goethe University,
Altenhoeferallee 1, 60438 Frankfurt/Main, Germany
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- Satellite measurement of forest disturbance, recovery and deposit distribution following explosive volcanic eruptions M. Udy et al. 10.1016/j.jvolgeores.2024.108204
- Comparison of soil production, chemical weathering, and physical erosion rates along a climate and ecological gradient (Chile) to global observations M. Schaller & T. Ehlers 10.5194/esurf-10-131-2022
- Combined seismic and borehole investigation of the deep granite weathering structure—Santa Gracia Reserve case in Chile R. Trichandi et al. 10.1002/esp.5457
- The effects of late Cenozoic climate change on the global distribution of frost cracking H. Sharma et al. 10.5194/esurf-10-997-2022
- Comparison of regolith physical and chemical characteristics with geophysical data along a climate and ecological gradient, Chilean Coastal Cordillera (26 to 38° S) M. Schaller et al. 10.5194/soil-6-629-2020
- Formation of soil phosphorus fractions along a climate and vegetation gradient in the Coastal Cordillera of Chile E. Brucker & M. Spohn 10.1016/j.catena.2019.04.022
- Strontium isotopes trace biological activity in the Critical Zone along a climate and vegetation gradient R. Oeser & F. von Blanckenburg 10.1016/j.chemgeo.2020.119861
- The Territory as a Victim: Geological Assessment to Analyzing the Impact of Colombia’s Armed Conflict on Geo-Bio Megadiversity at the Sierra Nevada de Santa Marta J. Zapata-Herrera et al. 10.3389/esss.2024.10112
- High economic costs of reduced carbon sinks and declining biome stability in Central American forests L. Baumbach et al. 10.1038/s41467-023-37796-z
- Alluvial channel response to environmental perturbations: fill-terrace formation and sediment-signal disruption S. Tofelde et al. 10.5194/esurf-7-609-2019
- From rock eating to vegetarian ecosystems — Disentangling processes of phosphorus acquisition across biomes M. Koester et al. 10.1016/j.geoderma.2020.114827
- Effect of rock uplift and Milankovitch timescale variations in precipitation and vegetation cover on catchment erosion rates H. Sharma et al. 10.5194/esurf-9-1045-2021
Latest update: 22 Nov 2024
Short summary
Vegetation is crucial for modulating rates of denudation and landscape evolution, and is directly influenced by climate conditions and atmospheric CO2 concentrations. Using transient climate data and a state-of-the-art dynamic vegetation model we simulate the vegetation composition and cover from the Last Glacial Maximum to present along the Coastal Cordillera of Chile. In part 2 we assess the landscape response to transient climate and vegetation cover using a landscape evolution model.
Vegetation is crucial for modulating rates of denudation and landscape evolution, and is...