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.
Research article
| 
08 Oct 2018
Research article |
| 08 Oct 2018
| 08 Oct 2018
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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26 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
- Past, present, and future geo-biosphere interactions on the Tibetan Plateau and implications for permafrost T. Ehlers et al. 10.1016/j.earscirev.2022.104197
- How to map biomes: Quantitative comparison and review of biome‐mapping methods A. Champreux et al. 10.1002/ecm.1615
- Recently fixed carbon fuels microbial activity several meters below the soil surface A. Scheibe et al. 10.5194/bg-20-827-2023
- N2 fixation per unit microbial biomass increases with aridity A. Scheibe & M. Spohn 10.1016/j.soilbio.2022.108733
- Vegetation strategies for nitrogen and potassium acquisition along a climate and vegetation gradient: From semi-desert to temperate rainforest S. Stock et al. 10.1016/j.geoderma.2022.116077
- Regional carbon stock assessment and the potential effects of land cover change J. Fryer & I. Williams 10.1016/j.scitotenv.2021.145815
- The uncertain future of mountaintop-removal-mined landscapes 1: How mining changes erosion processes and variables C. Shobe et al. 10.1016/j.geomorph.2023.108984
- Nitrogen Gain and Loss Along an Ecosystem Sequence: From Semi-desert to Rainforest K. Abdallah et al. 10.3389/fsoil.2022.817641
- Geography, Temperature, and Water: Interaction Effects in a Small Native Amphibian M. Vidal et al. 10.1086/710537
- Impacts of Loss of Cryosphere in the High Mountains of Northwest North America J. Clague & D. Shugar 10.3390/quat6010001
- Landscapes through time T. Ehlers 10.1126/science.adg5546
- Climate, not Quaternary biogeography, explains skull morphology of the long-tailed macaque on the Sunda Shelf N. Grunstra et al. 10.1016/j.quascirev.2023.108121
- Feedbacks between the formation of secondary minerals and the infiltration of fluids into the regolith of granitic rocks in different climatic zones (Chilean Coastal Cordillera) F. Hampl et al. 10.5194/esurf-11-511-2023
- 3D shear wave velocity imaging of the subsurface structure of granite rocks in the arid climate of Pan de Azúcar, Chile, revealed by Bayesian inversion of HVSR curves R. Trichandi et al. 10.5194/esurf-12-747-2024
- 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
- 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
- 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: 29 Jun 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...
