Phase II (2019-'21) |
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II P1: FIRE Induced Element Cycling II P2: Nutrient cycling & vegetation II P3: Microorganisms & soil structure II P4: Linking bioturbation with fluxes II P5: Erosion-Climate-Vegetation coupling (SECCO) II P6: Bio-Geomorphology II P7: Biota, fracture, thresholds II P8: Stress constrained landscape modeling II P9: Bridging timescales with modeling II P10: Landscape evolution from Thermochronology II P11: DeepES - Weathering Geochemistry II P12: DeepES - Microbial element cycling II P13: DeepES - Geophysical Imaging II P14: DeepES - Microbial activity II P15: DeepES - Geomicrobiology II A1: Plant available water storage II A2: Bioweath |
Phase I (2016-'18) |
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I P1: Plant Traits and Decomposition I P2: Coupled Modelling I P3: Biofilms & Weathering I P4: Sediment storage & Connectivity I P5: Crustweathering I P6: Root Carbon I P7: Paleoclimate I P8: Imaging of Weathering front I P9: Sediment Transport I P10: Phosphorus solubilization I P11: Green & Grey world I P12: Biogenic Weathering I P13: Microbiological Stabilization I A3: Carbon & Nutrient Fluxes |
Investigator Names and Contact Info:
Chilean Collaborators Involved:
PhD-Student:
Supervisor: Prof. Dirk Scherler
MSc-Student:
Supervisor: Prof. Dirk Scherler
Project Summary:
BioScapes III is part of a series of independent EARTHSHAPE proposals that quantifies biotic, surface process, and paleoclimate interactions at the catchment scale and larger. The topography of the Earth’s surface is shaped by erosion and sediment transport that tend to balance tectonic rock uplift over geological time scales. Although it is widely understood that organisms directly and indirectly affect these processes, their long-term contribution to the evolution of landscapes is not well known. This deficit is rooted in the fact that biotic influences are complex and difficult to disentangle from climatic influences. In this project, we want to examine the influence of biota on erosion and sediment transport in the framework of a threshold-stochastic stream power model of river incision. We shall test the hypothesis that biota, the characteristics of soils, and vegetation, influence river incision primarily by modulating the magnitude-frequency distribution of flood events. To achieve this goal, we will focus on the Earthshape SPP key areas that are distributed across a large climate-and-vegetation gradient in the Coastal Cordillera of Central Chile, and address three key objectives: (1) quantify erosion rates with cosmogenic nuclide concentrations in fluvial sediments; (2) quantify the influence of biota on river discharge by analyzing a large data set of mean daily discharge records, combined with ecohydrological modeling; and (3) model the cosmogenic nuclide-derived erosion rates with a threshold-stochastic stream power model calibrated with discharge distributions and field observations. Our project combines geological/geochemical with ecohydrological/geoecological methods for bridging the different time scales, from the stream response to individual rain events to the long-term effect on landscape development.