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Projekt Druckansicht

Transformation of organic carbon in the terrestrial-aquatic interface

Antragstellerinnen / Antragsteller Professor Dr. Michael Mutz; Dr. Katrin Premke
Fachliche Zuordnung Hydrogeologie, Hydrologie, Limnologie, Siedlungswasserwirtschaft, Wasserchemie, Integrierte Wasserressourcen-Bewirtschaftung
Förderung Förderung von 2013 bis 2017
Projektkennung Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 237042772
 
Erstellungsjahr 2017

Zusammenfassung der Projektergebnisse

A deeper knowledge of aquatic organic carbon transformation, its physical and the microbial key player are of high relevance for the modelling of carbon flow through landscapes and for the understanding of the global carbon cycle. The results gained from this project significantly improve our understanding of mechanisms involved in regulation of organic carbon transformation in aquatic and semiaquatic ecosystems with emphasis on ephemeral streams and its sediment structure. Consequently, they contribute to a better understanding of the relevance and the understanding of organic carbon mineralisation and involved microbial community composition in regards to different sediment strata and patches across those ecosystems. Significant progress could be obtained on three different aspects: Firstly, the relevance of recalcitrant terrestrial organic carbon in respect to microbial assimilation and mineralization has been further clarified. We provide new insight into how different mechanisms are pronounced/ control the contribution of fungi and bacteria in aquatic carbon cycling in relation to the composition of the organic matter pool. Using a 13C stable-isotope approach we combined for the first time continuous measurements of carbon mineralization with the analysis of microbial phospholipids to link microbial activities to relative changes in the abundance of fungal and bacterial heterotrophs. Elucidation of the relationship between organic matter quality and microbial activities is fundamental to improve our understanding on how freshwater ecosystems interact with the global carbon cycling. Thus our study adds valuable information to this field of research. Secondly, effects of periodic sediment shifting occurring in migrating sand ripples were investigated in regard to microbial carbon mineralization and different carbon qualities in microcosm experiments. We could show for the first time that the mechanical disturbance in migrating ripples modulates the sedimentassociated microorganisms affecting its structure and functions. Change in regimen from stable to migrating ripple sediment and vise-versa, showed a different structure-function response that depended on age of the biofilm. However, further experiments are needed to clarify the role of structural variability of biofilms to its response to periodic migrating and further on the regulating factors during the transition from stable to migrating. Finally, we conducted stable isotope tracer study in experimental outdoor streams with different scenarios. We manipulated algal abundance using different light intensities and aimed at examining how their relevance for leaf litter metabolism by stream biofilms relates to variations in streambed heterogeneity, droughts and rewetting’s. We show for the first time that cycling of terrestrial carbon in benthic biofilms is shaped by streambed heterogeneity. Our findings provide evidence that a higher solute transfer may reduce spatial barriers between biofilm organisms and thus enhance the metabolic interactions among microbial auto- and heterotrophs. Accordingly, our study has profound implications for the previously postulated effects of autochthonous carbon on terrestrial carbon decomposition in stream ecosystems and, therefore, greatly adds to current research on microbial turnover of terrestrial carbon in aquatic ecosystems. Moreover, our study provides knowledge on resistance and resilience of temperate microbial communities to drought and rewetting and linking these to shading and sediment structure. The experiment provided also evidence that despite these shifts, stream metabolic functions were highly resilient and modulated by shading. Thus, our results suggest that sediment structure alterations and riparian vegetation are strong modulators of stream metabolism and should be regarded in management preparing temperate streams to predicted drought stress.

Projektbezogene Publikationen (Auswahl)

 
 

Zusatzinformationen

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