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Gobat, Jean-Michel
Nom
Gobat, Jean-Michel
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Professeur honoraire
Email
jean-michel.gobat@unine.ch
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Voici les éléments 1 - 4 sur 4
- PublicationMétadonnées seulementContrasted effects of increased N and CO2 supply on two keystone species in peatland restoration and implications for global change(2002-5-2)
; ;Buttler, Alexandre ;Grosvernier, Philippe ;Rydin, Hakan ;Siegenthaler, Andy1 Significant areas of temperate bogs have been damaged by peat harvesting but may regenerate. These secondary mires, if well managed, may act as strong C sinks, regulate hydrology and buffer regional climate. 2 The potential effects of bog regeneration will, however, depend on the successful establishment of the principal peat formers - Sphagnum mosses. The influence of hydrology and microclimate on Sphagnum re-growth is well studied but effects of elevated CO2 and N deposition are not known. 3 We carried out two in-situ experiments in a cutover bog during three growing seasons in which we raised either CO2 (to 560 p.p.m.) or N (by adding NH4NO3, 3 g m(-2) year(-1)). The two treatments had contrasting effects on competition between the initial coloniser Polytrichum strictum (favoured by high N) and the later coloniser Sphagnum fallax (favoured by high CO2). 4 Such changes may have important consequences for bog regeneration and hence for carbon sequestration in cutover bogs, with potential feedback on regional hydrological and climatic processes. - PublicationAccès libreContrasted effects of increased N and CO2 supply on two keystone species in peatland restoration and implications for global change(2002)
; ;Buttler, Alexandre ;Grosvernier, Philippe ;Rydin, HÃ…kan ;Siegenthaler, Andy1 Significant areas of temperate bogs have been damaged by peat harvesting but may regenerate. These secondary mires, if well managed, may act as strong C sinks, regulate hydrology and buffer regional climate.
2 The potential effects of bog regeneration will, however, depend on the successful establishment of the principal peat formers –Sphagnum mosses. The influence of hydrology and microclimate on Sphagnum re-growth is well studied but effects of elevated CO2 and N deposition are not known.
3 We carried out two in-situ experiments in a cutover bog during three growing seasons in which we raised either CO2 (to 560 p.p.m.) or N (by adding NH4NO3, 3 g m−2 year−1). The two treatments had contrasting effects on competition between the initial coloniser Polytrichum strictum (favoured by high N) and the later coloniser Sphagnum fallax (favoured by high CO2).
4 Such changes may have important consequences for bog regeneration and hence for carbon sequestration in cutover bogs, with potential feedback on regional hydrological and climatic processes. - PublicationMétadonnées seulementEffects of elevated CO2 and nitrogen deposition on natural regeneration processes of cut-over ombrotrophic peat bogs in the Swiss Jura mountains(: Springer, 1999-5-2)
;Grosvernier, Philippe; ;Buttler, Alexandre; ;Visconti, Guido ;Beniston, Martin ;Iannorelli, Emilio DBarba, DiegoIn the Swiss Jura mountains most of the remaining ombrotrophic pear bogs have been exploited to some extent for peat. In these sires, natural regeneration processes are taking place. The dominant process is paludification, where a cut over drained surface is colonised by key species, usually either Polytrichum strictum or Eriophortum vaginatum. These early colonisers of bare pear surfaces create microclimatic conditions that enable the re-colonisation of Sphagnum mosses, usually S. fallax. In later stages of the succession S. fallax grows to Form a continuous carpet and the key species gradually suffer from competition for light availability. We studied the effect of elevated CO2 (560 ppm) and nitrogen deposition (30 kg ha(-1) year(-1)) on the competition between Sphagnum fallax and Polytrichum strictum year in a three years field experiment (EU project BERI - Bog Ecosystem Research Initiative) using miniFACE systems (small size Free Air Carbon dioxide Enrichment). The cover and growth in length of the two species was monitored. The height difference between the emerging Polytrichum and the top of the Sphagnum mosses was also recorded at regular intervals, Effect Of CO2: Sphagnum covet increased in the first year but this trend was not confirmed subsequently, whereas Polytrichum cover was not affected by elevated CO2 Both Sphagnum and Polytrichum had a reduced growth in length under elevated CO2. However, the growth of Sphagnum was less reduced than that of Polytrichum and therefore the height difference between Sphagnum and Polytrichum decreased. Effect of N: Sphagnum cover declined and Polytrichum cover doubled over the three years period in the high N plots. Sphagnum growth in length was not significant affected by N, but Polytrichum grew more in the high N plots. As a results the height difference between Sphagnum and Polytrichum increased. These results suggest that elevated CO2 and nitrogen deposition may have contrasting effects on bog regeneration. The positive effect of elevated CO2 on Sphagnum mosses may be counterbalanced by higher N deposition levels. - PublicationMétadonnées seulementEcology of testate amoebae (Protozoa : Rhizopoda) in Sphagnum peatlands in the Jura mountains, Switzerland and France(1999-5-2)
; ;Buttler, Alexandre ;Warner, BarryTestate amoebae (Protozoa) living in Sphagnum peatlands are important environmental and paleoecological indicators. The distribution of these animals is closely related to soil moisture variables. This study examines the ecology of sphagnicolous testate amoebae near the southern limit of bogs in Europe. A total of 64 samples were collected for analysis of testate amoebae from six peatlands in the Jura region of Switzerland and France. Eleven site-specific ecological variables, six of which were soil-moisture related variables, were measured at each site. The data were subjected to weighted averaging, jack-knifing, cluster analysis, canonical correspondence analysis, and the indicator value method to model relationships between testate amoebae distributions and environmental variables. Testate amoebae abundance showed a direct relationship with pear pH and depth to water table. Strong relationships were with sites that had a water table less than 41 cm deep. In drier sites with water table depth greater than 41 cm, other factors such as soil porosity and water holding capacity were more important compared to the wetter sites. Though there was a strong relationship between restate amoebae faunas and soil moisture content and porosity, these two variables could not be confidently predicted. Testate amoebae in peatlands in this region appear to be sensitive to peat pH and water tables. Further work is needed to explore relationships between restate amoebae, soil moisture, and porosity.