O número de projetos de restauração de ecossistemas florestais no Brasil aumentou nas últimas décadas e, consequentemente, aumentaram as exigências na avaliação e na busca por indicadores de sucesso. Apesar dos avanços na ecologia da restauração, existem lacunas no conhecimento em relação ao funcionamento e à autossustentabilidade dos ecossistemas restaurados. Esta pesquisa teve o objetivo de responder às seguintes questões: (1) É possível detectar padrões nos atributos de riqueza, estrutura e grupos funcionais nas matas ciliares nativas da Floresta Estacional Semidecidual (FES), que podem ser utilizados como metas da restauração florestal nesta região? (2) Quais as variáveis de biodiversidade, estrutura florestal e grupos funcionais, nas áreas restauradas, que seguem trajetórias previsíveis com o tempo? (3) Quanto tempo é necessário para que estas variáveis atinjam os valores de referência das matas ciliares nativas? (4) Quais são os fatores bióticos, abióticos, de técnica de plantio e de manutenção pós-plantio que influenciam nas trajetórias das matas ciliares restauradas? O estudo foi desenvolvido em região de FES, onde amostramos quatro matas nativas (referências) e 26 plantios de restauração, com idade entre quatro e 53 anos, que utilizamos para modelar as trajetórias em cronoseqüência. Em cada área, dez parcelas de 100 \'M POT.2\' foram aleatoriamente distribuídas, dentro de uma faixa de até 50 m de largura a partir da margem. Identificamos e contabilizamos os indivíduos de espécies arbóreas e arbustivas, plantadas ou regenerantes, a partir de 50 cm de altura e os agrupamos em três classes de tamanho segundo o diâmetro à altura do peito (DAP): DAP < 1 cm, 1 cm \'< ou =\' DAP < 5 cm e DAP \'> ou =\' 5 cm. Na classe de maior tamanho registramos o DAP e estimamos a altura de cada indivíduo. Classificamos as espécies de acordo com a sua síndrome de dispersão, ritmo de crescimento, tolerância à sombra, capacidade de fixar N, grau de ameaça e raridade. Para cada parcela, medimos a abertura do dossel, contabilizamos o número de lianas, pteridófitas e árvores com epífitas e coletamos uma amostra de solo, para formar uma amostra composta para cada local de estudo. Calculamos a biomassa acima do solo para árvores com DAP \'> ou =\' 5 cm, a riqueza total estimada por Jackknife e a riqueza rarefeita para 100 indivíduos. Por meio de entrevistas, observações em campo e análises da paisagem, obtivemos dados representativos de fatores abióticos, bióticos e de manejo que poderiam influenciar as trajetórias das comunidades arbóreas restauradas. Modelamos a trajetória de cada variável relativa à comunidade arbustivo-arbórea em função do tempo e estimamos o tempo que será necessário para igualar os ecossistemas de referência para cada variável. Entre as variáveis analisadas, selecionamos, como indicadores para monitoramento da evolução e sustentabilidade do ecossistema restaurado, as que fossem mais previsíveis (melhor qualidade dos modelos) e que representassem processos ecológicos mais relevantes. Os atributos que não variaram entre florestas nativas e que puderam ser utilizados como referência foram: riqueza observada, riqueza estimada para 100 indivíduos com DAP \'> ou =\' 5 cm, riqueza estimada por Jackknife para indivíduos com DAP \'> ou =\' 1 cm, densidade de indivíduos com DAP \'> ou =\' 1 cm, área basal, biomassa, cobertura de copas, proporção de indivíduos tolerantes à sombra e proporções de espécies zoocóricas, de crescimento lento, tolerantes à sombra, fixadoras de nitrogênio e de distribuição rara. No geral, as trajetórias foram mais bem ajustadas aos modelos logarítmicos, mas a riqueza de regenerantes de maior tamanho (DAP \'> ou =\' 5) ajustou-se melhor ao modelo linear. A riqueza nesta classe de tamanho não atingiu o nível de regenerantes dos ecossistemas de referência no período estudado. As trajetórias seguiram padrões semelhantes, independentes das técnicas de plantio ou do número de espécies plantadas. Variáveis de estrutura florestal foram homogêneas entre as matas nativas. Nos plantios, são facilmente medidas e evoluem rapidamente. Assim, metas da restauração podem ser estabelecidas com base nos parâmetros estruturais das matas nativas e tais variáveis seriam bons indicadores inclusive em plantios de restauração mais jovens. As variáveis que tendem a alcançar mais rapidamente os valores de referência são: área basal (12 anos), biomassa (13 anos), altura média das maiores árvores (26 anos), cobertura de gramíneas (33 anos), cobertura de copas (35 anos), riqueza de regenerantes com DAP \'> ou =\' 1 cm (52 anos), densidade de regenerantes com DAP \'> ou =\' 1 cm (52 anos) e riqueza total (53 anos). A área basal e a biomassa ultrapassaram em muito os valores de referência, o que pode indicar um filtro restritivo para a regeneração natural, caso a densidade dos indivíduos na classe de maior tamanho (geralmente plantados) não diminua naturalmente com o tempo. Para alguns grupos de espécies (zoocóricas, fixadoras de N, espécies raras e ameaçadas), as proporções em termos de riqueza e de densidade não apresentaram trajetórias previsíveis, mas algumas matas ciliares restauradas atingiram e ultrapassam os valores de referência. Excluímos o fator idade para identificar os fatores que influenciaram as trajetórias das variáveis selecionadas como indicadores, calculando um índice de sucesso (proporção entre o dado observado em cada local e o estimado para a mesma variável com base no modelo). Entre as seis variáveis selecionadas como indicadores, uma foi influenciada somente pela distância de fragmento-fonte (riqueza de regenerantes com DAP \'> ou =\' 5) e outra apena pela proporção de partículas finas no solo (área basal). Apesar da proporção do terreno ocupada por gramíneas não influenciar nas trajetórias, o controle da mato-competição com herbicida resultou em maiores valores de riqueza de plantas em regeneração. Independentemente das técnicas de plantio e dos tipos de manejo dos projetos de restauração, a estrutura florestal e os processos funcionais dos ecossistemas restaurados tendem a se tornar mais semelhantes aos ecossistemas de referência com o tempo, desde que haja fontes de propágulos e disponibilidade de água e nutrientes no solo. Os resultados obtidos apontam para uma influência muito pequena ou nula das técnicas de plantio e manejo, se comparados com a influência dos fatores ambientais e da paisagem sobre as trajetórias das matas ciliares em restauração. / A remarkable increase in the number of forest restoration projects has been recorded in Brazil in the last decade. As a consequence of this increase, the demand for monitoring and indicators of restoration success has also increased. Despite the advances in restoration ecology, there are still gaps in knowledge about the functioning and self-sustainability of restored ecosystems. In order to fill some of these gaps, in this study we aimed at to answer the following questions: (1) Are there patterns in the attributes of richness, structure, and functional groups on the native riparian Seasonally Semideciduous Forest (SSF), which may be used as goals to forest restoration in this region? (2) What are the variables representing biodiversity, forest structure and functional groups in the restored areas, which follow predictable paths over time? (3) How long it takes for these variables to achieve the reference values of native riparian forests? (4) Among the biotic, abiotic and technical factors analyzed, which can be considered as drivers of the successional trajectories of the restored forests? We assessed four native forests (as references) and 26 restored forests in the SSF region (a sub-type of the Atlantic Forest) in a chronosequence from four to 53 years since planting. At each site, the sample area comprised ten plots of 100 \'M POT.2\' randomly distributed within a range of 50 m away from the margin. We identified and counted all individuals of tree and shrub species from 50 cm in height, planted or regenerating, categorized in three size classes according to diameter at breast height (DBH): DBH < 1 cm, 1 cm \'< ou =\' DBH < 5 cm DBH \'> ou =\' 5 cm. We measured DBH and estimated the height of each individual from the upper class. We categorized the species according to their dispersion syndrome, growth rate, shade tolerance, Nitrogen-fixing ability, degree of threaten, and rarity. For each plot, we measured the canopy openness, and recorded the number of lianas, pteridophytes and number of trees with epiphytes. We also collected composite soil samples for chemical and physical analyses, from each study site. We estimated the aboveground biomass for trees with DBH \'> ou =\' 5 cm, total richness and richness rarefied to 100 individuals. By interviews, field observations, and landscape studies, we obtained information on other ecological factors and management practices that could affect the paths of the restored plant communities. We modeled the trajectory of each variable of the plant community over time, and estimated the period of time required for the restored forests to reach the reference ecosystems. Amongst the analyzed variables, we selected as indicators for monitoring the evolution and sustainability of the restored ecosystem those that were more predictable (best quality models) and that represent the most relevant ecological processes. The attributes that did not change among the native forests and could be used as references were: observed richness, estimated richness for 100 individuals with DBH \'> ou =\' 5 cm, total richness estimated by Jackknife DBH \'> ou =\' 1 cm, density DBH \'> ou =\' 1 cm, basal area, biomass, canopy cover, proportion of shade-tolerant individuals, and proportion of zoochoric species, slow growing, shade tolerant, nitrogen fixers, and rare distribution. Overall, the trajectories were best fitted to the logarithmic models, but richness (DBH \'> ou =\' 5 cm) was better adjusted to the linear model. In the upper size class, richness did not reach the \"species pool\" of the reference ecosystems in the 53 years period analyzed. The trajectories followed similar patterns, regardless of the planting techniques or the number of planted species. Variables representing forest structure were similar among the native forests and quickly recovered in comparison to those related to biodiversity. Thus, the restoration goals can be established based on native forests parameters and such variables would be good indicators even in young restoration plantings. The variables reaching more quickly the reference values were: basal area (12 years), biomass (13 years), average height of the largest trees (26 years), grass cover (33 years), canopy cover (35 years), richness of regenerants with DBH \'> ou =\' 1 cm (52 years), density of regenerants with DBH 1 cm (52 years), and total richness (53 years). The basal area and biomass greatly exceeded the reference values, which may indicate a restrictive filter for the forest dynamics if the density of individuals in the upper class (most planted) does not decrease naturally over time. For some functional groups (zoochoric, N-fixing, rare, and endangered species), the proportions of species and relative densities did not follow predictable trajectories, but some of the restored riparian areas reached and exceeded the reference values. In order to identify the factors driving the paths of the variables selected as indicators, we excluded the age factor, calculating an index of success (the ratio between observed and estimated values for the variable, the first directly measured for each site and the last obtained by the linear models). Among the six variables selected as indicators, some were influenced only by the distance of the source fragment (seedling richness of DBH \'> ou =\' 5 cm) and others only by the proportion of fine particles in the soil (basal area). While the ground cover by grasses does not influence the trajectories, weed control with herbicides resulted in higher plant richness in regeneration. Regardless of planting techniques and management practices, the forest structure and functional processes of restored ecosystems tend to become more similar to reference ecosystems over time, as long as there are propagule sources in the vicinity and availability of soil water and nutrients. Our findings pointed to a weak, if any, effect from the planting techniques or management and a high influence of environmental and landscape factors on the trajectories of a riparian forest restoration.

Au cours des dernières décennies, l'Indonésie a connu des transformations spectaculaires des terres avec une expansion des plantations de palmiers à huile au détriment des forêts tropicales. L'Indonésie est actuellement l'une des régions ayant le plus haut taux de transformation de la surface terrestre dans le monde à cause de l'expansion des plantations de palmiers à huile et d'autres agricultures qui remplacent les forêts à grande échelle. Comme la végétation est un modificateur du climat près du sol, ces transformations à grande échelle ont des impacts majeurs sur les variables biophysiques de surface telles que la température de surface, l'albédo, les indices de végétation (NDVI), sur le bilan énergétique de surface et le partitionnement énergétique. Ce travail de thèse vise à quantifier les impacts des changements d’usage des terres en Indonésie sur les variables biophysiques de surface. Pour évaluer ces changements à l'échelle régionale, des données de télédétection sont nécessaires. Étant une variable clé de nombreuses fonctions écologiques, la température de surface (LST) est directement affectée par les changements de la couverture terrestre. Nous avons analysé la LST à partir de la bande thermique d'une image Landsat et produit une carte de température de surface avec une haute résolution (30m) pour les basses terres de la province de Jambi à Sumatra (Indonésie), une région qui a subi de grandes transformations au cours des dernières décennies. La comparaison des LST, albédo, NDVI et évapotranspiration (ET) entre sept différents types de couverture terrestre (forêts, zones urbaines, terres incultes, plantations de palmiers à huile jeunes et matures, plantations d'acacias et de caoutchouc) montre que les forêts ont des températures de surface inférieures à celles des autres types de couvert végétal, ce qui indique un effet de réchauffement local après la conversion des forêts vers des plantations. Les différences de LST atteignaient 10,1 ± 2,6 ºC (moyenne ± écart-type) entre les forêts et les terres déforestées. Les différences de températures de surface s'expliquent par un effet de refroidissement évaporatif des forêts, qui compense l'effet de réchauffement de l'albédo. Basé sur des différences observées dans les variables biophysiques entre les plantations de palmiers à huile jeunes et matures, nous avons analysé trois images Landsat couvrant une chronoséquence de plantations de palmiers à huile pour étudier la dynamique des variables biophysiques de surface pendant le cycle de rotation de 20-25 ans des plantations de palmiers à huile. Nos résultats montrent que les différences entre les plantations de palmiers à huile à différents stades du cycle de rotation du palmier à huile se reflètent dans les différences du bilan énergétique de surface, du partitionnement énergétique et des variables biophysiques. Au cours du cycle de rotation des plantations de palmiers à huile, les différences de température à la surface diminuent graduellement et se rapprochent de zéro autour du stade mature de la plantation de palmiers à huile de 10 ans. Parallèlement, le NDVI augmente et l'albédo diminue à proximité des valeurs typiques des forêts. Le bilan énergétique de surface et le partitionnement énergétique montrent des tendances de développement liés aux variables biophysiques et à l'âge des plantations de palmiers à huile. Les nouvelles plantations et les jeunes plantations (<5 ans) ont un rayonnement net plus faible que les plantations de palmiers à huile matures, mais ont des températures de surface plus élevées que les plantations de palmiers à huile matures. Les changements dans les variables biophysiques, le bilan énergétique et la répartition de l'énergie au cours du cycle d’une rotation du palmier à huile peuvent s'expliquer par l'effet de refroidissement évaporatif précédemment identifié dans les forêts, qui compense l'effet de réchauffement de l'albédo. L'un des principaux déterminants de ce mécanisme est la couverture végétale au cours des différentes phases du cycle de rotation du palmier à huile. Le NDVI en tant qu'indicateur du couvert végétal a montré une relation inverse cohérente avec LST de différentes plantations de palmiers à huile âgés, une tendance qui est également observée pour différents types d'utilisation des terres dans cette étude. Une analyse régionale et à plus long terme de la tendance LST entre 2000 et 2015 basée sur les données MODIS montre que dans la journée la température moyenne de Jambi a augmenté de 1,05 ºC, suivant la tendance des changements observés et dépassant les effets du réchauffement climatique. Afin d'évaluer les effets de l'expansion du palmier à huile sur le climat, le bilan énergétique de surface, le partitionnement énergétique et les processus biophysiques jouent un rôle important et le cycle complet de rotation des plantations de palmiers à huile doit être envisagé. Basé sur nos résultats, nous construisons le cycle de rotation des plantations de palmiers à huile et les changements qui se produisent au cours du développement de la végétation de palmiers à huile. Cette étude fournit des preuves que l'expansion des plantations de palmiers à huile et d'autres cultures commerciales entraîne des changements dans les variables biophysiques, réchauffant la surface du sol et augmentant ainsi l'augmentation de la température de l'air à cause du changement climatique. En utilisant des données Landsat à haute résolution, nous avons pu inclure les effets du changement d'utilisation des terres sur les variables biophysiques. Comprendre les effets du changement de la couverture terrestre sur les variables biophysiques peut soutenir des politiques concernant la conservation des forêts existantes, la planification et l'expansion des plantations de palmiers à huile et les mesures de boisement possibles. La connaissance des variables biophysiques, du bilan radiatif et de la répartition énergétique au cours du cycle de rotation du palmier à huile peut inclure de nouvelles pratiques de gestion susceptibles de réduire les conditions environnementales et microclimatiques extrêmes dans la phase initiale des plantations de palmiers à huile.

The thesis was conducted to investigate soil fertility changes and assess the sustainability of agroecological management in different land-use systems of the southern Ecuadorian Andes using quantitative and qualitative methods. Ecuador still holds the highest deforestation rate of all Latin American countries which also has a large impact in the research area by forest conversion into agricultural land. Agricultural land-use systems in the research area are multifaceted due to heterogeneous biophysical and socio-economic conditions. To map this diversity, land-use systems were investigated in Yantzaza (low-external-input), El Tambo (irrigated cash crops) and San Lucas (integrated nutrient management). Yet, management effects on soil fertility have not been assessed systematically in Ecuadorian farming systems which hampers the evaluation whether agroecological management is sustainable. Therefore, the present study used a set of quantitative and qualitative approaches to assess soil fertility changes at plot and farm scale with a nutrient balance/chronosequence approach and local expert knowledge. Nutrient balances were modeled with Nutmon after adaptation of difficult-to-quantify flows to the local conditions facilitating area and land-use specific calculation. Soil nutrient balances in the research area were diverse and varied between −151 to 66 kg ha-1 a-1, −4 to 33 kg ha-1 a-1 and −346 to 39 kg ha-1 a-1 for NPK, respectively. The evaluation of socio-economic and soil fertility explanatory variables revealed that up to 70% of the balances’ variability could be explained. Land-uses with a strong market orientation such as annual crops in El Tambo received large amounts of external inputs which were often focused on mineral N fertilization causing strongly negative PK balances. In contrast, P balances were mainly positive after the application of organic fertilizers and nutrient recycling as was found in perennial crops of San Lucas. NP balances in annual crops of Yantzaza were most negative due to the low-external-input system with nonexistent fertilization as well as leaching and burning of crop residues. Highest soil nutrient stocks were found in land-uses benefiting from a surplus of within-farm flows. The quantification of soil nutrient stocks and their temporal changes were carried out with a chronosequence approach in Yantzaza. SOC stocks in annual/perennial crops and pastures decreased between 14% and 19% after forest conversion by slash-and-burn. Annual sites were abandoned not later than five years after forest conversion due to a shortage of available N and P closely linked to low-external-input management. Stocks for TN, TP, TS and exchangeable bases increased above forest level in perennial crops and pastures 6-20 years after forest conversion. Yet a strong decrease in SOC and soil nutrient stocks was found in oldest perennial and pasture sites compared to medium aged sites. This was traced back to adverse site processes such as the decay of clay humus complexes, leaching as well as poor pasture management. To assess sustainability of the agroecological management, a set of sustainability indicators was implemented including N balances, yearly N stock change and SOC stocks as well as total (TN) and available (PO4-P) soil nutrient stocks. Sustainability assessment took place based on individual land-uses and nutrients within each pilot study since soil fertility change did not show a consistent trend within one research area. Despite mainly negative soil nutrient balances, the impact on the yearly soil nutrient stock change was often negligible due to large soil nutrient pools. Annual and perennial crops of Yantzaza and pastures of San Lucas exceeded the threshold value of 1% for yearly TN stock losses. Yet, only annual crops in Yantzaza, having the highest yearly TN stock losses of 4.9%, also showed severe TN and SOC losses between 15-25% below those of the forest reference area. Therefore, the present agroecological management of annuals in Yantzaza is not sustainable which was also indicated by the abandonment of these sites not later than 5 years after forest conversion due to soil fertility decline. Hence, it is proposed to install an integrated agricultural management in annual crops of Yantzaza using nutrient recycling and fertilization for the replenishment of soil nutrient stocks. Nutrient balance studies indicated an average N-fertilizer application of more than 200 kg ha-1 a-1 for annual crops in El Tambo and low SOC stocks in soils of the colluvial foot slopes. Therefore, a laboratory incubation experiment was conducted to investigate fertilization effects of urea and newly introduced guinea pig manure on the microbial activity in colluvial and eroded soils of El Tambo. While urea fertilization induced an acceleration of SOM mineralization, a combined fertilization (urea + GPM) increased the amount of microbial biomass and provided mineral nitrogen for immediate plant uptake. SOM stocks in colluvial soils were 40% below those of eroded soils which was partly due to the positive priming effect after urea fertilization. A participatory appraisal with local farmers resulted in the adaptation of the present harvest residue management aiming at SOM maintenance in colluvial soils. Yet, the calculation of the potential for SOM replenishment indicated that only the maize residue biomass had the potential to compensate for SOM mineralization losses. Therefore, it is recommended to support SOM replenishment by additional organic inputs since SOM has to be maintained in the long-term to enable agricultural productivity.

No description available.

No description available.

This research investigates soil respiration (Rs) in a boreal jack pine (Pinus banksiana Lamb.) fire scar chronosequence at Sharpsand Creek, Ontario, Canada. During two field campaigns in 2006 and 2007, Rs was measured in a chronosequence of fire scars in the range 0 to 59 years since fire. Mean Rs adjusted for soil temperature (Ts) and soil moisture (Ms) (Rs T,M) ranged from 0.56 μmol CO2/m2/s (32 years post fire) to 8.18 μmol CO2/m2/s (58 years post fire). Coefficient of variation (CV) of Rs adjusted for Ts and Ms ranged from 20% (16 years post fire) to 56% (58 years post fire). Across the field site, there was a significant exponential relationship between Rs adjusted for soil organic carbon (Cs) and Ts (P = 1.24*10-06; Q10 = 2.21) but no effect of Ms on Rs adjusted for Cs and Ts for the range 0.21 to 0.77 volumetric Ms (P = 0.702). Rs T,M significantly (P = 0.030) decreased after burning mature forest, though no significant (P > 0.1) difference could be detected between recently burned and unburned young forest. Rs was measured in recently burned boreal jack pine fire scar age categories that differed in their burn history and there was a significant difference in Rs T,M between previously 32 v 16 year old (P = 0.000) and previously 32 v 59 year old (P = 0.044) scars. There was a strong significant exponential increase in S R T,M with time since fire (r2 = 0.999; P = 0.006) for the chronosequence 0, 16 and 59 years post fire, and for all these age categories, Rs T,M was significantly different from one another (P < 0.05). The Joint UK Land Environment Simulator (JULES) was used to model vegetation re-growth over successional time at Sharpsand Creek, though it appeared to perform poorly in simulating leaf area index and canopy height. JULES probably over estimated heterotrophic Rs at Sharpsand Creek when Ts corrected simulated values were compared with measured Rs T,M. The results of this study contribute to a better quantitative understanding of Rs in boreal jack pine fire scars and will facilitate improvements in C cycle modelling. Further work is needed in quantifying autotrophic and heterotrophic contributions to soil respiration in jack pine systems, monitoring soil respiration for extended time periods after fire and improving the ability of JULES to simulate successional vegetation re-growth.

Abstract Succession is a compositional change of species and other ecosystem characteristics over time. Mire development, i.e., long-term mire succession is basically driven by an increase in peat layer height, promoting changes in hydrology, vegetation and nutrient status of a particular mire. Due to this, ecosystem processes, such as production and loss of carbon due to decomposition (i.e. carbon gas functions), change with increasing successional mire stage. An adequate method for studying the changes in ecosystem C functions is to measure CO2 and CH4 fluxes between the ecosystem and atmosphere. Succession and carbon dynamics of boreal pristine mires have been much studied. However the link between these phenomena is largely unknown. Further, if and how the C gas functions of mires change during mire succession it is rather poorly understood. The main objective of this thesis was to study how ecosystem functions, measured as CO2 and CH4 exchange, change during mire development. The study also aims to explore the drivers of succession in mire development, i.e., mire succession. Successional mire C dynamics were studied along an eight-kilometer-long successional sequence of primary paludified mires located in the land uplift coast of the Bothnian Bay. Due to the short distance between sites, they all have been under the same climatic control for most of their development. The gradual replacement of plant species with different photosynthetic potential, phenology and assimilating green area resulted in lower-level and temporal variation of CO2 exchange patterns at the later successional stages. Similar to this, CH4 also had the lowest interannual variation in the later stages. In general, CH4 emissions increased with mire age even though this trend did not emerge during the rainy season. Further, this study showed that the wintertime C function pattern was related to the C pattern during the previous summer confirming the important effect of growing season patterns on wintertime C dynamics. In addition to the fundamental effect of vegetation as a driver of succession which was also confirmed in this study, the role of hydrological conditions appeared to be equally important. More constant hydrological conditions at later successional stages resulted in lower temporal variation in CH4 and CO2 fluxes. The present results suggest that the stability of ecosystem C gas functions increases during mire development due to increasing autogenic control. / Tiivistelmä Sukkessio on ekosysteemin lajistossa ja sen muissa ominaisuuksissa ajan kuluessa tapahtuva muutos. Suon kehitystä eli pitkäaikaista suosukkessiota vie eteenpäin turpeen paksuuskasvu, joka saa aikaan muutoksia suoekosysteemin hydrologiassa, kasvillisuudessa ja ravinnetilassa. Tästä johtuen myös suoekosysteemin erilaiset prosessit, kuten tuotanto sekä hajoamisen kautta tapahtuva hiilen vapautuminen eli hiilikaasutoiminta muuttuu suon ikääntyessä. Ekosysteemin hiilikaasutoiminnassa tapahtuvia muutoksia voidaan tutkia muun muassa mittaamalla ekosysteemin ja ilmakehän välisiä hiilidioksidi- ja metaanivirtoja. Boreaalisten luonnontilaisten soiden sukkessiota ja hiilidynamiikkaa on tutkittu runsaasti, mutta niiden välistä yhteyttä ei sen sijaan juuri tunneta. Tämän vuoksi ei tiedetä kuinka soiden hiilikaasutoiminta mahdollisesti muuttuu suon kehityksen aikana eli suosukkession edetessä. Tämän tutkimuksen päätavoitteena oli tutkia kuinka hiilidioksidin ja metaanin vaihdolla mitattu ekosysteemitoiminta muuttuu suon kehityksen aikana. Tutkimus pyrki myös selvittämään suosukkessiota kontrolloivat tekijät. Eri-ikäisten soiden hiilikaasudynamiikkaa tutkittiin mittaamalla hiilikaasuja Perämeren maankohoamisrannikolla kahdeksan kilometrin pituisella sukkessiogradientilla, joka koostuu primaarisoistumisen kautta syntyneistä soista. Soiden lyhyestä keskinäisestä etäisyydestä johtuen ne ovat olleet saman ilmastollisen kontrollin alaisena suurimman osan kehityksestään. Vaiheittainen kasvilajien muutos sukkessiogradientilla yhdessä kasvilajien erilaisen yhteyttämispotentiaalin, fenologian ja yhteyttävän lehtipinta-alan kanssa johti hiilidioksidivaihdon alhaisempaan tasoon sekä pienempään ajalliseen vaihteluun vanhemmilla sukkessiovaiheilla. Myös metaanin vaihdolla oli alhaisimmat vuosien väliset vaihtelut vanhemmilla vaiheilla. Yleisesti ottaen metaanipäästöt kasvoivat suon iän myötä, vaikkakaan tätä trendiä ei havaittu sateisena kasvukautena. Lisäksi tutkimus osoitti, että talviaikaiset hiilivirrat (CO2, CH4) seurasivat kesäaikaisen hiilidynamiikan vaihtelua. Kasvillisuuden keskeinen rooli ekosysteemin sukkessiossa havaittiin myös tässä tutkimuksessa. Kasvillisuuden ohella merkittäväksi suosukkessiota sääteleväksi tekijäksi osoittautui hydrologisten olojen vaikutus. Tasaisemmat hydrologiset olot vanhemmilla sukkessiovaiheilla johtivat vähäisempään ajalliseen vaihteluun metaani- ja hiilidioksidivirroissa. Tutkimuksen tulokset viittaavat siihen, että ekosysteemin hiilidynamiikka stabilisoituu suon kehityksen aikana lisääntyvän autogeenisen kontrollin kautta.

No description available.