Phase II (2019-'21) |
---|
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) |
---|
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:
Prof. Maaike Bader, co-supervisors: Dr. Alfredo Saldaña and Dr. Rodrigo Ríos
MSc-Student:
Prof. Maaike Bader, co-supervisor: Rafaella Canessa
BSc-Student:
Prof. Maaike Bader, co-supervisor: Rafaella Canessa
Project Summary:
The input of organic carbon into the soil is one of the major drivers of weathering and erosion. This input, in turn, is primarily controlled by interactive effects of vegetation and climate. Understanding how climate and vegetation together determine soil organic carbon, as an energy source for microorganisms as weathering engines and as a stabilizing factor in erosion, is one of the major scientific goals of the EarthShape program (SPP 1803). With this project we aim to pursue this goal by studying organic carbon fluxes, from plant productivity to litter decomposition (and carbon dynamics in soils1), disentangling plant and climate effects. Based on our hypothesis that the relative importance of climate and plant traits may be scale dependent we will work at multiple spatial-climatic scales. These scales encompass three biomes along the Chilean coastal cordillera (arid, mediterranean and wet-temperate) and two contrasting study sites within each of these biomes. These two scale-levels and the comparison of soils below contrasting plant types within sites will allow us to partially decouple vegetation and climate effects. A further decoupling is achieved by translocating plant litter between the three biomes and sites in a fully-reciprocal experiment, studying decomposition of this litter over a period of two years. Vegetation is regarded from a functional point of view: carbon inputs, as determined by primary productivity and litter decomposition, will be described as functions of plant functional traits (chemical, physical and phenological) and trait diversity. The results of this project will include a statistical model predicting soil organic carbon inputs based on climate and vegetation traits, accounting for effects on plant productivity as well as litter decomposition. This improved process knowledge is important for understanding and modelling carbon cycles and geomorphology-related soil processes.