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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Cited
13 citations as recorded by crossref.
- Do degree and rate of silicate weathering depend on plant productivity? R. Oeser & F. von Blanckenburg 10.5194/bg-17-4883-2020
- Effect of changing vegetation and precipitation on denudation – Part 2: Predicted landscape response to transient climate and vegetation cover over millennial to million-year timescales M. Schmid et al. 10.5194/esurf-6-859-2018
- 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
- Geomorphic and Sedimentary Effects of Modern Climate Change: Current and Anticipated Future Conditions in the Western United States A. East & J. Sankey 10.1029/2019RG000692
- Regional carbon stock assessment and the potential effects of land cover change J. Fryer & I. Williams 10.1016/j.scitotenv.2021.145815
- Nitrogen Gain and Loss Along an Ecosystem Sequence: From Semi-desert to Rainforest K. Abdallah et al. 10.3389/fsoil.2022.817641
- 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
- Geography, Temperature, and Water: Interaction Effects in a Small Native Amphibian M. Vidal et al. 10.1086/710537
- 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
13 citations as recorded by crossref.
- Do degree and rate of silicate weathering depend on plant productivity? R. Oeser & F. von Blanckenburg 10.5194/bg-17-4883-2020
- Effect of changing vegetation and precipitation on denudation – Part 2: Predicted landscape response to transient climate and vegetation cover over millennial to million-year timescales M. Schmid et al. 10.5194/esurf-6-859-2018
- 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
- Geomorphic and Sedimentary Effects of Modern Climate Change: Current and Anticipated Future Conditions in the Western United States A. East & J. Sankey 10.1029/2019RG000692
- Regional carbon stock assessment and the potential effects of land cover change J. Fryer & I. Williams 10.1016/j.scitotenv.2021.145815
- Nitrogen Gain and Loss Along an Ecosystem Sequence: From Semi-desert to Rainforest K. Abdallah et al. 10.3389/fsoil.2022.817641
- 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
- Geography, Temperature, and Water: Interaction Effects in a Small Native Amphibian M. Vidal et al. 10.1086/710537
- 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: 21 Mar 2023
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...