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:
Postdoc:
supervisor: Prof. K. Tielbörger, co-supervisor: Prof. Y. Oelmann
Postdoc:
supervisor: Prof. K. Tielbörger, co-supervisor: Prof. Y. Oelmann
PhD:
supervisor: Prof. Y. Oelmann, co-supervisors: Dr. H. Neidhardt, Prof. K. Tielbörger
PhD:
supervisor: Prof. Y. Oelmann, co-supervisors: Dr. H. Neidhardt, Prof. K. Tielbörger
MSc:
supervisor: Prof. Y. Oelmann, co-supervisors: Dr. H. Neidhardt
MSc:
supervisor: Prof. Y. Oelmann, co-supervisors: Dr. H. Neidhardt
BSc:
supervisor: Prof. T. Tielbörger
BSc:
supervisor: Prof. K. Tielbörger, co-supervisors: Dr. R. Canessa
BSc:
supervisor: Prof. Y. Oelmann, co-supervisors: Dr. H. Neidhardt
in cooperation with Dr. Thomas Hoffmann, project 6
BSc:
supervisor: Prof. Y. Oelmann, co-supervisors: Dr. H. Neidhardt
Project summary:
One component why biota might shape the Earth’s surface is related to their active role as “weathering engine”. However, efficient nutrient cycling of both plants and soil microorganisms might reduce their need to access nutrients contained in bedrock especially under increasingly progressed weathering towards more humid climate. In addition, nutrient cycling is affected by even higher trophic levels i.e., herbivory. However, it is virtually unknown how climate, especially rainfall, interacts with herbivory in affecting nutrient cycling and litter decomposition. Our overall goal is to dissect the relative importance of biotic (plants, microorganisms, herbivores) and abiotic factors (geology, climate) on processes related to weathering and biogeochemical nutrient cycling. We will directly link biological and geochemical processes by a) doing in-depth studies on processes at the interface between the green, the brown, and the grey world that build on the foundations laid in Phase 1, and by b) doing integrated analyses of this data and of new data collected by a large interdisciplinary consortium collaborating in our drought experiment. We expand our initial focus on plant-soil-geology feedbacks related to litter both ‘downwards’ and ‘upwards’. Specifically, we will focus on a) nutrient limitation and nutrient efficiency of plants and soil microorganisms, and b) the influence of herbivory on decomposability of litter that both potentially affect biogeochemical rock weathering. To that end, we combine the EarthShape space-for-time approach with mechanistically orientated field experiments that manipulate climate conditions on-site. With this approach, we address the following overarching questions: Can spatial climate gradients, i.e. the result of long-term climatic impact on the earth surface, serve as proxy for short- to medium-term temporal climatic changes? Which processes (‘green vs. brown vs. grey’) can be best described by spatial gradients? We will be able to answer these questions based on observations and experiments in the field as well as plant and herbivory experiments in the greenhouse. To assess nutrient cycling, we will measure nutrients in plants, soil and soil microorganisms complemented by innovative stable isotope tracers. By addressing the explicit role of a whole suite of biota in nutrient cycling, we will reveal their potential role as “weathering engine” which is a backbone of EarthShape. Additionally, our study is the first in Chile to investigate climate change impacts on ecosystem processes using large field experiments.
Fig.: Conceptual model of the proposed work programme. Asterisks * indicate the central focus of Phase 1 with measurements that will be complemented in Phase 2. Dashed lines and the grey box show the tight connection to weathering processes, and thus the close integration into the EarthShape SPP.