Éditeur(s) : HAL CCSD
Résumé :  
absent
Annual Meeting of the Association for Tropical Biology and Conversation
Paramaribo, Suriname

hal-01032073
https://hal.archives-ouvertes.fr/hal-01032073

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
We explored the relationship between soil processes, estimated through soil respiration (Rsoil), and the spatial variation in forest structure, assessed through the distribution of tree size, in order to understand the determinism of spatial variations in Rsoil in a tropical forest. The influence of tree size was examined using an index (Ic) calculated for each tree as a function of (1) the trunk cross section area and (2) the distance from the measurement point. We investigated the relationships between Ic and litterfall,root mass and Rsoil, respectively. Strong significant relationships were found between Ic and both litterfall and root mass. Rsoil showed a large range of variations over the 1-ha experimental plot, from 1.5 to 12.6 gC m−2 d−1. The best relationship between Ic and Rsoil only explained 17% of the spatial variation in Rsoil. These results support the assumption that local spatial patterns in litter production and root mass depend on tree distribution in tropical forests. Our study also emphasizes the modest contribution of tree size distribution-which is mainly influenced by the presence of the biggest trees (among the large range size of the inventoried trees greater than 10 cm diameter at 1.30 m above ground level or at 0.5 m above the buttresses)-in explaining spatial variations in Rsoil.
ISSN: 0032-079X

hal-00797064
https://hal.archives-ouvertes.fr/hal-00797064

Éditeur(s) : HAL CCSD Cambridge University Press (CUP)
Résumé : The objective of this study was to analyse the factors explaining spatial variation in soil respiration over topographic transects in a tropical rain forest of French Guiana. The soil of 30 plots along six transects was characterized. The appearance of the 'dry to the touch' character at a depth of less than 1.2 m was used to discriminate soils exhibiting vertical drainage from soils exhibiting superficial lateral drainage and along with colour and texture, to define five classes from well-drained to strongly hydromorphic soils. Spatial variation in soil respiration was closely related to topographic position and soil type. Increasing soil water content and bulk density and decreasing root biomass and soil carbon content explained most of the decrease in soil respiration from the plateaux (vertically drained hypoferralic acrisol) to the bottomlands (haplic gleysol). These results will help to stratify further field experiments and to identify the underlying determinants of spatial variation in soil respiration to develop mechanistic models of soil respiration.
ISSN: 0266-4674

hal-01032046
https://hal.archives-ouvertes.fr/hal-01032046
DOI : 10.1017/S0266467406003415

Éditeur(s) : HAL CCSD Wiley
Résumé : This work aimed at understanding the role of mycorrhizal status in phosphorus efficiency of tree seedlings in the tropical rainforest of French Guyana. * Mycorrhizal colonization, growth, phosphorus content, net photosynthesis and root respiration were determined on three occasions during a 9-month growth period for seedlings of two co-occurring species (Dicorynia guianensis and Eperua falcata) grown at three soil phosphorus concentrations, with or without inoculation with arbuscular mycorrhizas. * Seedlings of both species were unable to absorb phosphorus in the absence of mycorrhizal association. Mycorrhizal seedlings exhibited coils that are specific of Paris-type mycorrhizae. Both species benefited from the mycorrhizal symbiosis in terms of phosphorus acquisition but the growth of E. falcata seedlings was unresponsive to this mycorrhizal improvement of phosphorus status, probably because of the combination of high seed mass and P reserves, with low growth rate. * The two species belong to two different functional groups regarding phosphorus acquisition, D. guianensis being an obligate mycotrophic species.
ISSN: 0028-646X

hal-01032209
https://hal.archives-ouvertes.fr/hal-01032209
DOI : 10.1111/j.1469-8137.2004.00978.x

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
Disentangling the autotrophic and heterotrophic components of soil CO2 efflux is critical to understanding the role of soil system in terrestrial carbon (C) cycling. In this study, we combined a stable C-isotope natural abundance approach with the trenched plot method to determine if root exclusion significantly affected the isotopic composition (δ13C) of soil CO2 efflux (RS). This study was performed in different forest ecosystems: a tropical rainforest and two temperate broadleaved forests, where trenched plots had previously been installed. At each site, RS and its δ13C (δ13CRs) tended to be lower in trenched plots than in control plots. Contrary to RS, δ13CRs differences were not significant. This observation is consistent with the small differences in δ13C measured on organic matter from root, litter and soil. The lack of an effect on δ13CRs by root exclusion could be from the small difference in δ13C between autotrophic and heterotrophic soil respirations, but further investigations are needed because of potential artefacts associated with the root exclusion technique.
ISSN: 0032-079X

bioemco-00353850
https://hal-bioemco.ccsd.cnrs.fr/bioemco-00353850
DOI : 10.1007/s11104-008-9844-5

Éditeur(s) : HAL CCSD
Résumé :  
absent
Programme National coordonné ANR " ECCO "
Toulouse, France

hal-01032072
https://hal.archives-ouvertes.fr/hal-01032072

Éditeur(s) : HAL CCSD
Résumé :  
absent
33. European Geosciences Union General Assembly
Vienne, Austria

hal-01032070
https://hal.archives-ouvertes.fr/hal-01032070

Éditeur(s) : HAL CCSD
Résumé :  
absent
9. Journées d'Ecologie Fonctionnelle
Biarritz, France

hal-01032071
https://hal.archives-ouvertes.fr/hal-01032071

Éditeur(s) : HAL CCSD Springer Verlag (Germany)
Résumé :  
We explored the relationship between soil processes, estimated through soil respiration (Rsoil), and the spatial variation in forest structure, assessed through the distribution of tree size, in order to understand the determinism of spatial variations in Rsoil in a tropical forest. The influence of tree size was examined using an index (Ic) calculated for each tree as a function of (1) the trunk cross section area and (2) the distance from the measurement point. We investigated the relationships between Ic and litterfall, root mass and Rsoil, respectively. Strong significant relationships were found between Ic and both litterfall and root mass. Rsoil showed a large range of variations over the 1-ha experimental plot, from 1.5 to 12.6 gC m−2 d−1. The best relationship between Ic and Rsoil only explained 17% of the spatial variation in Rsoil. These results support the assumption that local spatial patterns in litter production and root mass depend on tree distribution in tropical forests. Our study also emphasizes the modest contribution of tree size distribution-which is mainly influenced by the presence of the biggest trees (among the large range size of the inventoried trees greater than 10 cm diameter at 1.30 m above ground level or at 0.5 m above the buttresses)-in explaining spatial variations in Rsoil.
Plant and Soil

hal-01032200
https://hal.archives-ouvertes.fr/hal-01032200
DOI : 10.1007/s11104-011-0848-1

Éditeur(s) : HAL CCSD
Résumé :  
absent
Séminaire du "Dipartimento di Scienze Ambientali"
Naples, Italy

hal-01032045
https://hal.archives-ouvertes.fr/hal-01032045

Éditeur(s) : HAL CCSD
Résumé : Carbon isotopic signature has been measured at the different stages of the soil CO2 efflux production in trenched and control plots to improve the knowledge about the physical and biochemical processes of the soil respiration. All the measurements of _13C have been performed using a mass-spectrometer.We have compared the isotopic signatures of the CO2 going out of the soil, the CO2 of the soil atmosphere, the organic carbon in the material that could be considered as the main soil respiration sources (live and dead roots, soil organic matter, aerial litter) and the CO2 produced by these sources in incubation jars. The aims of this study were to evaluate the possibilities to combine these different data sets to estimate the partitioning of soil respiration between its autotrophic and heterotrophic components, and to get more insight into potential fractionation during biochemical or diffusion processes. Measurements were conducted in a beech forest located at Hesse in the North East of France (site equipped with a flux tower and belonging to the CarboEurope network) and in a neotropical primary rainforest located at Paracou (French Guiana). Preliminary results show first a very tenuous difference between CO2 isotopic signatures of efflux coming from the trenched and control plots and, secondly, _13C significant divergences between bulk organic material and CO2 produced in the corresponding incubation jars. Our ability to use this kind of data for partitioning soil respiration into its main components will be discussed.
European Geosciences Union. General Assembly 2006
Vienne, Austria

hal-01032380
https://hal.archives-ouvertes.fr/hal-01032380

Éditeur(s) : HAL CCSD
Résumé : Carbon isotopic signature has been measured at the different stages of the soil CO2 efflux production in trenched and control plots to improve the knowledge about the physical and biochemical processes of the soil respiration. All the measurements of d13C have been performed using a mass-spectrometer. We have compared the isotopic signatures of the CO2 going out of the soil, the CO2 of the soil atmosphere, the organic carbon in the material that could be considered as the main soil respiration sources (live and dead roots, soil organic matter, aerial litter) and the CO2 produced by these sources in incubation jars. The aims of this study were to evaluate the possibilities to combine these different data sets to estimate the partitioning of soil respiration between its autotrophic and heterotrophic components, and to get more insight into potential fractionation during biochemical or diffusion processes. Measurements were conducted in a beech forest located at Hesse in the North East of France (site equipped with a flux tower and belonging to the CarboEurope network) and in a neotropical primary rainforest located at Paracou (French Guiana). Preliminary results show first a very tenuous difference between CO2 isotopic signatures of efflux coming from the trenched and control plots and, secondly, d13C significant divergences between bulk organic material and CO2 produced in the corresponding incubation jars. Our ability to use this kind of data for partitioning soil respiration into its main components will be discussed.
AGU Fall Meeting
San Francisco, United States

hal-01032042
https://hal.archives-ouvertes.fr/hal-01032042

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé :  
The maintenance in the long run of a positive carbon balance under very low irradiance is a prerequisite for survival of tree seedlings below the canopy or in small gaps in a tropical rainforest. To provide a quantitative basis for this assumption, experiments were carried out to determine whether construction cost (CC) and payback time for leaves and support structures, as well as leaf life span (i) differ among species and (ii) display an irradiance-elicited plasticity. Experiments were also conducted to determine whether leaf life span correlates to CC and payback time and is close to the optimal longevity derived from an optimization model. Saplings from 13 tropical tree species were grown under three levels of irradiance. Specific-CC was computed, as well as CC scaled to leaf area at the metamer level. Photosynthesis was recorded over the leaf life span. Payback time was derived from CC and a simple photosynthesis model. Specific-CC displayed only little interspecific variability and irradiance-elicited plasticity, in contrast to CC scaled to leaf area. Leaf life span ranged from 4 months to >26 months among species, and was longest in seedlings grown under lowest irradiance. It was always much longer than payback time, even under the lowest irradiance. Leaves were shed when their photosynthesis had reached very low values, in contrast to what was predicted by an optimality model. The species ranking for the different traits was stable across irradiance treatments. The two pioneer species always displayed the smallest CC, leaf life span, and payback time. All species displayed a similar large irradiance-elicited plasticity.
ISSN: 0022-0957

hal-01032198
https://hal.archives-ouvertes.fr/hal-01032198
DOI : 10.1093/jxb/err092

Éditeur(s) : HAL CCSD
Résumé :  
absent
4. International Symposium on Dynamics of Physiological Processes in Roots of Woody Plants
Bangor, United Kingdom

hal-01031399
https://hal.archives-ouvertes.fr/hal-01031399

Éditeur(s) : HAL CCSD Springer Verlag
Résumé :  
The high spatial variability of soil respiration in tropical rainforests is well evaluated, but influences of biotic factors are not clearly understood. This study underlines the influence of tree species characteristics on soil respiration across a 16-monospecific plot design in a tropical plantation of French Guiana. A large variability of soil CO2 fluxes was observed among plots (i.e. 2.8 to 6.8 μmol m−2 s −1 ) with the ranking being constant across seasons. There were no significant relationships between soil respiration and soil moisture or soil temperature, neither spatially, nor seasonally. The variability of soil respiration was mainly explained by quantitative factors such as leaf litterfall and basal area. Surprisingly, no significant relationship was observed between soil respiration and root biomass. However, the influence of substrate quality was revealed by a strong relationship between soil respiration and litterfall P (and litterfall N, to a lesser extent).
ISSN: 0032-079X

hal-01032069
https://hal.archives-ouvertes.fr/hal-01032069
DOI : 10.1007/s11104-008-9866-z

Éditeur(s) : HAL CCSD
Résumé : Diffusion du document : INRA Documentation de Centre, Domaine de Duclos, 97170 Petitt-Bourg (Guadeloupe, France) Diplôme : DEA
il s'agit d'un type de produit dont les métadonnées ne correspondent pas aux métadonnées attendues dans les autres types de produit : DISSERTATION
Because soil respiration representes 80% of ecosystem respiration, it is a major flux between biosphere and atmosphere. We examined the effects of root and litter exclusion on soil CO! efflux (Rsu1) using trenching and litter exclusion in a tropical plantation constituted of trees seedlings installed in 16 mono-specific stands 20 years ago near Kourou, French Guyana. Soil CO2 efflux was measured using an infra red gas analyser (PP System,EGM4 ) at 16 randomly distributed plot in each treatment: control, root exclusion, litter exclusion and both root and litter exclusion. in the plantation. We measured R'1l1during four periods, and we have collected soil samples, litter biomass and measured moisture at 5 cm depth in the soil. Soil CO, efflux varied significantly among species from 2,8±O,7f1mo l. m''. s' (mean ± standard deviation) to 7.4± 1.7fLmol. n'-' . s ' for Qualea rosea and Vochys ia tomentosa, respectively. 1'0 significant correlation was found between RSIlI variability and soil moisture, which is mostly related to soil texture in the experimental site. Soil CO2 efflux was significantly reduced in litter exclusion treatment and root exclusion plots (6 months litter and/or root exclusion) during ail measurements period and for ail species, compared to control plots. The reduction of soil CO, efflux was higher in plot without root than in plot without litter of control plot (42% and 25%, respectively). There was an import ant specific diversity in these reductions . We estimated the contribution of roof respiration (Rr) to total Rso1 by calculating the difference between Rso1 control and Rsn l root exclusion plot corrected for the decomposition of root that were killed following t re n e h in ~. Thus the heterotrophic component of soil carbon efflux accounts for 46% of total carbon efflux (1,9f1 mol. rn" . s•') while root respiration accounts for 54% of soil carbon release (2,3 ~t mo l. m-2 S-I) . Because there was a negative and significant correlation between microbial respiration (Rrn) and C/N of mature leaves it seemed to be possible to predict Rm if we known the mature leaves quality. In addition a good estimate theorical R ~, values from R~, measured in different treatments.
La respiration du sol en représentant une part de 80% de la respiration de l'écosystème apparaît être un flux majeur entre la biosphère et l'atmosphère. Nous avons étudié les effets de l'exclusion racinaire et de la litière sur le flux de CO, du sol (R ~ , ) en utilisant la méthode de " Trench-plots" et de suppression de litière dans une plantation d'arbres tropicaux. Ces arbres, âgés de 20 ans ont été plantés sur un sol uniforme, près de Kourou en Guyane française, en 16 placeaux mono-spécifiques. Pour mesurer les flux de CO2 provenant du sol, nous avons utilisé un analyseur différentiel de gaz infrarouge portable muni d'une chambre. Les mesures ont été faites sur 4 traitements différents tels que : le contrôle, l'exclusion racinaire, l'exclusion de litière et l'exclusion de litière et de racine et ce, répétés sur chacune des 16 placettes mono-spécifiques. Cette étude comporte 4 campagnes de mesures. Nous avons également effectué des prélèvements de sol de litière et nous avons fait des mesures d’humidité de sol à une profondeur de 5 cm. Les flux de C01 du sol varient fortement entre espèces de 2.8±O.7 ~t m o 1. m-2. sol à 7 A± 1. 7 ~t m o l. m•1 sol pour Qua/ev rosea ct Vochysto tomentasa, respectivement. Il n'existe pas de corrélation significative entre les variations de Rw l ct celles de l'humidité du sol (indication sur la texture du sol de la plantation ). Nous avons observé que Rso1 était significativement plus faible dans les placeaux sans racines et/ou sans litière (6 mois après la mise en place de l'expérimentation) pour toutes les campagnes de mesures et pour toutes les espèces que dans les placeaux contrôlés. Cette réduction du flux de CO2 du sol est plus forte dans les "trench-plots " que dans les traitement s d'exclusion de litière avec 42 et 25% respectivement. Un effet "traitement " et un effet "espèce" important expliquent 3 1"/.. ct 13% de la variabilité totale de R~. Nous avons cherché à connaître la contribution des racines dans les valeurs de R""I. en comparant le flux de CO2 provenant du sol sur des "trench -plot s'' au flux de COl provenant du sol dans les placeaux contrôlés . Cette estimation a été corrigée pour prendre en compte la décomposition des racines tuées par les tranchées. Ainsi, la composante appartenant aux micro -organismes représente 46% du flux total de carbone provenant du sol (1.9Jlmo l. m-2 S•I ) alors que la respiration des racines représente 54% du dégagement de carbone (2 ,3~lmol. m ol . 5-La respiration des micro-organismes pourrait être estimée en mesurant le C/N des feuilles matures puisqu'il existe une corrélation significative et négative entre les deux. Enfin les résultats obtenus sur les différents traitements permettent d'obtenir une bonne estimation de la respiration du sol avec un RSIlI théorique corrélé à 66% avec les valeurs réelles mesurées.
https://hal.archives-ouvertes.fr/hal-01189239

hal-01189239
https://hal.archives-ouvertes.fr/hal-01189239
PRODINRA : 18212

Éditeur(s) : HAL CCSD Wiley
Résumé :  
The lack of information on the ways seasonal drought modifies the CO2 exchange between Neotropical rainforest ecosystems and the atmosphere and the resulting carbon balance hinders our ability to precisely predict how these ecosystems will respond as global environmental changes force them to face increasingly contrasting conditions in the future. To address this issue, seasonal variations in daily net ecosystem productivity (NEPd) and two main components of this productivity, daily total ecosystem respiration (REd) and daily gross ecosystem productivity (GEPd), were estimated over 2 years at a flux tower site in French Guiana, South America (511605400N, 5215404400W). We compared seasonal variations between wet and dry periods and between dry periods of contrasting levels of intensity (i.e. mild vs. severe) during equivalent 93-day periods. During the wet periods, the ecosystem was almost in balance with the atmosphere (storage of 9.0 gCm_2). Seasonal dry periods, regardless of their severity, are associated with higher incident radiation and lower REd combined with reduced soil respiration associated with low soil water availability. During the mild dry period, as is normally the case in this region, the amount of carbon stored in the ecosystem was 32.7 gCm_2. Severe drought conditions resulted in even lower REd, whereas the photosynthetic activity was only moderately reduced and no change in canopy structure was observed. Thus, the severe dry period was characterized by greater carbon storage (64.6 gCm_2), emphasizing that environmental conditions, such as during a severe drought, modify the CO2 exchange between Neotropical rainforest ecosystems and the atmosphere and potentially the resulting carbon balance.
ISSN: 1354-1013

hal-01032067
https://hal.archives-ouvertes.fr/hal-01032067
DOI : 10.1111/j.1365-2486.2008.01610.x

Éditeur(s) : HAL CCSD
Résumé : Carbon isotopic signature has been measured at the different stages of the soil CO2 efflux production in trenched and control plots to improve the knowledge about the physical and biochemical processes of the soil respiration. All the measurements of _13C have been performed using a mass-spectrometer.We have compared the isotopic signatures of the CO2 going out of the soil, the CO2 of the soil atmosphere, the organic carbon in the material that could be considered as the main soil respiration sources (live and dead roots, soil organic matter, aerial litter) and the CO2 produced by these sources in incubation jars. The aims of this study were to evaluate the possibilities to combine these different data sets to estimate the partitioning of soil respiration between its autotrophic and heterotrophic components, and to get more insight into potential fractionation during biochemical or diffusion processes. Measurements were conducted in a beech forest located at Hesse in the North East of France (site equipped with a flux tower and belonging to the CarboEurope network) and in a neotropical primary rainforest located at Paracou (French Guiana). Preliminary results show first a very tenuous difference between CO2 isotopic signatures of efflux coming from the trenched and control plots and, secondly, _13C significant divergences between bulk organic material and CO2 produced in the corresponding incubation jars. Our ability to use this kind of data for partitioning soil respiration into its main components will be discussed.
Geophysical Research Abstracts

hal-01031785
https://hal.archives-ouvertes.fr/hal-01031785

Éditeur(s) : HAL CCSD
Résumé :  
absent
Réunion du projet Galiléo "Traçage isotopique du carbone dans les écosystèmes forestiers"
Napoli, Italy

hal-01032064
https://hal.archives-ouvertes.fr/hal-01032064

Éditeur(s) : HAL CCSD
Résumé :  
absent
Journées d'Ecologie Fonctionnelle
Super Besse, France

hal-01031728
https://hal.archives-ouvertes.fr/hal-01031728