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Mitchell, Edward
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Mitchell, Edward
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Professeur ordinaire
Email
edward.mitchell@unine.ch
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Voici les éléments 1 - 8 sur 8
- PublicationMétadonnées seulementCut-over peatland regeneration assessment using organic matter and microbial indicators (bacteria and testate amoebae)(2008)
;Laggoun-Défarge, Fatima; ;Gilbert, Daniel ;Disnar, Jean-Robert ;Comont, Laure ;Warner, BarryButtler, Alexandre1. Cut-over peatlands cover large surfaces of high potential value for enhancing biodiversity and carbon sequestration if successfully restored. Unfortunately, evaluation of restoration success is not straightforward. We assessed the bioindicator value of organic matter (OM), testate amoebae (protozoa) and bacteria in peat from two regeneration stages and a reference site of a cut-over bog. 2. Contrasting biochemical signatures of peat OM were observed along the regenerating profiles, allowing clear differentiation between the newly regenerated peat and the old peat. Where peat macrofossils were absent sugar biomarkers were used to infer peat botanical origin and OM alteration. 3. Over the succession, the OM composition of the new peat differed. Peat from the more recent stage was dominated by Sphagnum-derived tissues and characterized by lower carbohydrate preservation and higher bacterial biomass than the advanced regeneration stage. 4. Surface testate amoeba communities also changed from the recent to the advanced stages of regeneration, indicating a shift from wet and moderately acidic conditions to drier and more acidic conditions. Over this regeneration sequence (i) the biomass and average size of species declined but were higher at the unexploited site and (ii) species richness and diversity increased but density declined. 5. Synthesis and applications. Although secondary succession in the cut-over bog led to an ecosystem similar to that of the reference site in terms of surface vegetation, OM and testate amoebae continued to reflect disturbances associated with peat harvesting. Nevertheless, the described dynamics of both microbial and biochemical variables over the succession showed similarities between the advanced stage and the reference site: a higher testate amoeba diversity was associated with better carbohydrate preservation and a more heterogeneous botanical composition of the peat. The inferred water table depth and pH based on testate amoebae indicators proved to be an alternative approach for assessing restoration processes, in contrast to labour-intensive repeated measurements in the field. The botanical and biochemical composition of peat OM provided additional information on past anthropogenic perturbations of the bog and could be used for restoration monitoring. The combination of several indicators therefore provides a more complete assessment of ecological conditions that could be valuable for the management of cut-over peatlands. - PublicationAccès libreEffects of experimental warming on carbon sink function of a temperate pristine mire : the PEATWARM project(2008)
;Laggoun-Défarge, Fatima ;Gilbert, Daniel ;Buttler, Alexandre ;Epron, Daniel ;Francez, Andre-Jean ;Grasset, Laurent; ;Guimbaud, ChristopheRoy, J.-C.Within the PEATWARM project, we use Sphagnumpeatlands as a model to analyse their vulnerability to climate change using an experimental system (ITEX) that simulates in situan increase in average temperature. We aim to determine the effects of temperature increase on the vegetation, the balance of above- and belowground gas fluxes (CO2and CH4), the microbial diversity and activity in Sphagnummosses and in peat, and the dynamics of labile and recalcitrant organic matter of peat. The ultimate objective is the creation of a biogeochemical model of C coupled with N and S cycles that includes interactions between these key compartments. - PublicationAccès libreCut-over peatland regeneration assessment using organic matter and microbial indicators (bacteria and testate amoebae)(2007)
;Laggoun-Défarge, Fatima; ;Gilbert, Daniel ;Disnar, Jean-Robert ;Comont, Laure ;Warner, Barry G.Buttler, Alexandre1. Cut-over peatlands cover large surfaces of high potential value for enhancing biodiversity and carbon sequestration if successfully restored. Unfortunately, evaluation of restoration success is not straightforward. We assessed the bioindicator value of organic matter (OM), testate amoebae (protozoa) and bacteria in peat from two regeneration stages and a reference site of a cut-over bog.
2. Contrasting biochemical signatures of peat OM were observed along the regenerating profiles, allowing clear differentiation between the newly regenerated peat and the old peat. Where peat macrofossils were absent sugar biomarkers were used to infer peat botanical origin and OM alteration.
3. Over the succession, the OM composition of the new peat differed. Peat from the more recent stage was dominated by Sphagnum-derived tissues and characterized by lower carbohydrate preservation and higher bacterial biomass than the advanced regeneration stage. 4. Surface testate amoeba communities also changed from the recent to the advanced stages of regeneration, indicating a shift from wet and moderately acidic conditions to drier and more acidic conditions. Over this regeneration sequence (i) the biomass and average size of species declined but were higher at the unexploited site and (ii) species richness and diversity increased but density declined.
5.Synthesis and applications. Although secondary succession in the cut-over bog led to an ecosystem similar to that of the reference site in terms of surface vegetation, OM and testate amoebae continued to reflect disturbances associated with peat harvesting. Nevertheless, the described dynamics of both microbial and biochemical variables over the succession showed similarities between the advanced stage and the reference site: a higher testate amoeba diversity was associated with better carbohydrate preservation and a more heterogeneous botanical composition of the peat. The inferred water table depth and pH based on testate amoebae indicators proved to be an alternative approach for assessing restoration processes, in contrast to labour-intensive repeated measurements in the field. The botanical and biochemical composition of peat OM provided additional information on past anthropogenic perturbations of the bog and could be used for restoration monitoring. The combination of several indicators therefore provides a more complete assessment of ecological conditions that could be valuable for the management of cut-over peatlands. - PublicationMétadonnées seulementReconciling commercial exploitation of peat with biodiversity in peatland ecosystems(2006)
;Artz, Rebekka ;Campbell, Colin ;Francez, André-Jean ;Laggoun-Défarge, Fatima ;Vasander, Harri ;Schloter, Michael ;Epron, Daniel ;Gilbert, Daniel; ;Schwarz, GChapman, Steve - PublicationMétadonnées seulementReconciling commercial exploitation of peat with biodiversity in peatland ecosystems (EU Project RECIPE)(2004)
; ;Chapman, Steve ;Buttler, Alexandre ;Combe, Jean ;Francez, André-Jean ;Gilbert, Daniel ;Harms, Hauke ;Laggoun-Défarge, Fatima ;Schloter, MichaelVasander, Harri - PublicationMétadonnées seulementBiochemical characteristics of peat organic matter and distribution of testate amoebae in two naturally regenerating cutover Sphagnum peatlands of the Jura Mountains(2004)
;Laggoun-Défarge, Fatima; ;Gilbert, Daniel ;Warner, Barry ;Comont, Laure ;Disnar, Jean-RobertButtler, Alexandre - PublicationAccès libreExploitation of northern peatlands and biodiversity maintenance: a conflict between economy and ecology(2003)
;Chapman, Steve ;Buttler, Alexandre ;Francez, André-Jean ;Laggoun-Défarge, Fatima ;Vasander, Harri ;Schloter, Michael ;Combe, Jean ;Grosvernier, Philippe ;Harms, Hauke ;Epron, Daniel ;Gilbert, DanielPeatlands are ecosystems of exceptional conservation value because of their beauty, biodiversity, importance in global geochemical cycles, and the paleoenvironmental records they preserve. Commercial extraction and drainage for forestry or agriculture have caused the destruction of many peatlands, especially in or close to urban areas of the northern temperate zone. Are these commercial and environmental interests irreconcilable? A close analysis suggests that limited peat extraction may actually increase biodiversity in some cases, and may be sustainable over the long term. As we learn more about how peatlands spontaneously regenerate following disturbance, and what conditions govern the re-establishment of a diverse community and the ability to sequester carbon, we increase our chances of being able to restore damaged peatlands. Preserving the chronological records hidden in the peat profile, the natural heritage value of peatlands, and the bulk of sequestered carbon, however, will remain incompatible with any form of exploitation. - PublicationAccès libreAbove- and belowground linkages in Sphagnum peatland: climate warming affects plant-microbial interactions
;Jassey, Vincent E. J. ;Chiapusio, Geneviève ;Binet, Philippe ;Buttler, Alexandre ;Laggoun-Défarge, Fatima ;Delarue, Frédéric ;Bernard, Nadine; ;Toussaint, Marie-Laure ;Francez, André-JeanGilbert, DanielPeatlands contain approximately one third of all soil organic carbon (SOC). Warming can alter above- and belowground linkages that regulate soil organic carbon dynamics and C-balance in peatlands. Here we examine the multiyear impact of in situ experimental warming on the microbial food web, vegetation, and their feedbacks with soil chemistry. We provide evidence of both positive and negative impacts of warming on specific microbial functional groups, leading to destabilization of the microbial food web. We observed a strong reduction (70%) in the biomass of top-predators (testate amoebae) in warmed plots. Such a loss caused a shortening of microbial food chains, which in turn stimulated microbial activity, leading to slight increases in levels of nutrients and labile C in water. We further show that warming altered the regulatory role of Sphagnum-polyphenols on microbial community structure with a potential inhibition of top predators. In addition, warming caused a decrease in Sphagnum cover and an increase in vascular plant cover. Using structural equation modelling, we show that changes in the microbial food web affected the relationships between plants, soil water chemistry, and microbial communities. These results suggest that warming will destabilize C and nutrient recycling of peatlands via changes in above- and belowground linkages, and therefore, the microbial food web associated with mosses will feedback positively to global warming by destabilizing the carbon cycle. This study confirms that microbial food webs thus constitute a key element in the functioning of peatland ecosystems. Their study can help understand how mosses, as ecosystem engineers, tightly regulate biogeochemical cycling and climate feedback in peatlands.