This thesis investigates the abiotic control of carbon (C) and water vapour fluxes (FCO₂ and E, respectively) in a New Zealand Pinus radiata D. Don plantation and a nearby clearcut. It concentrates on the limitation of these fluxes imposed by growing season soil water deficit. This results from low precipitation (658 mm a⁻¹) in combination with a limited root zone water storage capacity of the very stony soil (> 30% by volume). The thesis analyses results from seven eddy covariance flux measurement campaigns between November 1994 and March 1996. The study site was located in Balmoral Forest, 100 km north-west of Christchurch (42° 52' S, 172° 45' E), in a (in November 1994) 8-year-old stand. One set of measurements was conducted in an adjacent clearcut. Ecosystem flux measurements were accompanied by separate measurements of ground fluxes and of the associated environmental variables. Flux analysis focussed on the underlying processes of assimilation (Ac), canopy stomatal conductance (Gc) and respiration (Reco), using biophysical models coupled to soil water balance and temperature subroutines. Aiming to link time inegrated net ecosystem C (NEP) to tree growth, sequestration in tree biomass (NPP) was quantified by regular measurements of stem diameter using allometric relationships. Average rates of FCO₂ and E were highest in spring (324 mmol m⁻² d⁻¹ and 207 mol m⁻² d⁻¹, respectively) when the abiotic environment was most favourable for Gc and Ac. During summer, fluxes were impeded by the depletion of available soil water (θ) and the co-occurrence of high air saturation deficit (D) and temperature (T) and were equal or smaller than during winter (FCO₂ = 46 mmol m⁻² d⁻¹ in summer and 115 mmol m⁻² d⁻¹ in winter; E = 57 and 47 mol m⁻² d⁻¹, respectively). With increasingly dry soil, fluxes and their associated ratios became predominantly regulated by D rather than quantum irradiance, and on particularly hot days the ecosystem was a net C source. Interannually, forest C and water fluxes increased strongly with rainfall, and the simultaneously reduced D and T. For two succeeding years, the second having 3 % more rain, modelled NEP was 515 and 716 g C m⁻² a⁻¹, Ac 1690 and 1841 g C m⁻² a⁻¹ and Reco 1175 and 1125 g C m⁻² a⁻¹. NEP / E increased in wetter (and cooler) years (1.3 and 1.5 g kg⁻¹), reflecting a relatively larger gain in NEP. Responding mainly to increased rainfall during commonly dry parts of the year (ie summer), and reflecting the otherwise benign maritime climate of New Zealand, NEP during the winter months could exceed NEP during the middle of the notional tree growing season. Annual Ac, NEP, and NPP were strongly linearly related. This relation did not hold during bi-weekly periods when the processes of intermediate C storage were influential. Separate knowledge of tree growth and C fluxes allowed quantification of autotrophic, and heterotrophic respiration (Rhet≈ 0.4 NEP), as well as fine-root turnover (≈0.2 NEP). The ratio of NEP and stem volume growth was conservative (0.24 t C m⁻³) and allows a direct connection to be made between ecosystem carbon fluxes and forest yield tables. In the absence of living roots, the clearcut flux measurements demonstrated the expected limitation of Rhet by soil temperature (Ts) and θ. However, an additional 'pumping effect' was discovered at the open site whereby turbulence increased CO₂ efflux considerably when the soil surface was wet. Accounting for the combined effects of Ts, θ and turbulence, annual Rhet at the clear-cut site (loss to the atmosphere) was »50 % of NEP (C sequestered from the atmosphere) in the nearby forest. Clearly, there is an important contribution of C fluxes during early stages of ecosystem development to the total C sequestered over the lifetime of a plantation.

Structurée en trois principaux chapitres, cette étude présente une approche pluridisciplinaire en combinant desanalyses spatiales et temporelles de la variabilité interannuelle des saisons de pluies d’une base de données agroclimatique,des essais phénologiques mensuelles d’une sélection de variétés photopériodiques de mil et de sorgholocales et améliorées, et l’utilisation conjointe d’un modelé de culture calibre pour les effets de la latitude et d’unSystème d’Information Géographique (SIG). Elle permet de tirer des conclusions originales et d’identifier lesenvironnements cibles prometteurs pour la vulgarisation des variétés de mil et de sorgho photopériodiques enAfrique de l’Ouest. Elle met en évidence l’existence de relations significatives entre les réponses phénologiques,le degré de sensibilité à la photopériode des variétés et les facteurs environnementaux, dont les principales sont :‒ La variabilité interannuelle des pluies en Afrique de l’Ouest durant les cinquante dernières années (1950-2000) est marquée par une diminution globale de la pluviométrie annuelle caractérisée par une variabilitéaccrue des dates de début de saison des pluies dans les latitudes basses que dans les latitudes élevées etune variabilité interannuelles des dates de fin de saison plus notable sur les latitudes du Nord plus quedans les basses latitudes au sud.‒ La distribution spatiale des variétés de mil et de sorgho photopériodiques est étroitement liée à larépartition spatiale et temporelle de la variabilité des dates de débuts et de fin de la saison de pluies. Lesvariétés photopériodiques se localisent essentiellement dans les basses latitudes ou la variabilité des datesde début de saison est plus élevée que celle des dates de fin de saison plus stable.‒ La réponse phénologique des variétés de mil et de sorgho photopériodiques est strictement dépendantede la date de semis et de la latitude. Les effets de la latitude sur la phénologie et la réactionphotopériodique des variétés est proportionnelle à la distance entre la zone de culture d’une variété et salatitude d’origine.‒ Le modèle de développement des céréales photopériodiques « Impatience » calibré et corrigé à cet effet(effet de la latitude) prévois et défini avec plus de précision les zones d’adaptation variétale optimale pourles variétés de mil et de sorgho photopériodiques en Afrique de l’Ouest.‒ L’adéquation entre la durée du cycle phénologique calibrée par le modèle de culture corrigé de l’effet dela latitude et celle observée dans les systèmes agraires à base de mil et de sorgho photopériodiques dansles agro-systèmes villageois au Mali valide le modèle les cartes d’adaptation variétale optimale. / Structured in three main chapters; this study addresses multidisciplinary approach combining spatial and temporalanalysis of interannual variability of rainfall, multi-locations trials of a large and representative sample of photoperiodicvarieties of sorghum and millet combined with a photoperiod response crop model and Geographic Information System(GIS). It allowed identifying specific target environment to promote the vulgarization of photoperiodic varieties ofsorghum and millet in West Africa. This study depicted significant relationships between phenology, PP sensitivityresponses and environmental factors, where the mains components are listed below:‒ The interannual rainfall variability in West Africa over the past fifty years (1950-2000) was marked by ageneral decrease in annual rainfall characterized by high variability in the onset of growing period at lowerlatitudes and an increase in the interannual variability of the end of growing period in the northern latitudeswith least significant variability through climatic periods.‒ The spatial distribution of PP sensitivity varieties of millet and sorghum is closely related to the spatial andtemporal distribution of the interannual variability of the onset and end dates of growing period. Photoperiodsensitive varieties are located mainly at lower latitudes where the interannual variability in the onset of thegrowing period is much higher than the end of the growing period.‒ Phonological response and expression of photoperiod sensitivity are strictly dependent on sowing date andlatitude. Effects of latitude on the expression of photoperiod sensitivity and phenology are proportional tolatitude.‒ The "impatience" sub-crop model calibrated and corrected for latitudinal effect predicts and identifies moreaccurately optimal varietal adaptation areas for sorghum and millet varieties in West Africa.‒ The adequacy between calibrated duration of the phonological cycle by the crop model adjusted for latitudinaleffect and that observed in farming systems in agro-systems in Mali, allowed to validate the predicted optimalvarietal adaptation maps by defined the model.

No description available.

Dans cette thèse, nous avons abordé plusieurs thématiques liées aux modes de variabilité climatique dans l'Atlantique tropical à l'échelle interannuelle. Les analyses statistiques nous ont permis dans un premier temps de mettre en évidence les deux principaux modes dominants de cette variabilité interannuelle: un mode équatorial et un mode méridien. Le mode équatorial est responsable d'anomalies de température de surface de la mer (SST) principalement dans le Golfe de Guinée et est identifié par des variations de la pente du niveau de la mer dans la bande équatoriale. Il est dû à des rétroactions dynamiques entre le vent, le niveau de la mer et la SST. Quant au mode méridien, il se manifeste par des fluctuations inter-hémisphériques de SST et est contrôlé par des rétroactions dynamiques et thermodynamiques entre le vent, l'évaporation et la SST. L'évaluation du couplage de ces variables clés du mode méridien nous a permis de proposer un modèle conceptuel pour expliquer les principaux mécanismes responsables des oscillations du mode méridien. Le modèle a montré que le mode méridien résulte de la superposition d'un mécanisme auto-entretenu basé sur les rétroactions positives et négatives générant des oscillations régulières de haute fréquence (2-3 ans) et d'un autre mécanisme d'oscillation basse fréquence (4-9 ans) lié à l'influence d'ENSO du Pacifique Est. Comme l'évolution de ces deux modes est fortement liée au déplacement méridien de la zone de convergence intertropicale (ITCZ) qui transporte les pluies, nous avons ensuite identifié la signature de ces modes sur la salinité de la surface de la mer à l'aide observations in situ et d'une simulation numérique régionale. Les processus océaniques et/ou atmosphériques responsables de la signature de chaque mode ont été également identifiés grâce à un bilan de sel dans la couche de mélange du modèle validé. Le bilan de sel a révélé que le forçage atmosphérique, lié à la migration de l'ITCZ, contrôle la région équatoriale tandis que l'advection, due à la modulation des courants, du gradient vertical et le mélange à la base de la couche de mélange, explique les variations de SSS dans les régions sous l'influence des panaches. [...] / In this thesis, we investigate several topics related to the interannual climatic modes in the tropical Atlantic. Statistical analyses allows us to extract the two main dominant modes of interannual variability: an equatorial mode and a meridional mode. The equatorial mode is responsible for Sea Surface Temperature (SST) anomalies mainly found in the Gulf of Guinea and is linked to variations of the sea-level slope in the equatorial band. It is due to dynamic feedbacks between zonal wind, sea level and SST. The meridional mode is characterised by inter-hemispheric SST fluctuations and is controlled by dynamic and thermodynamic feedbacks between the wind, evaporation and SST. After quantifying the coupling between key variables involved in the meridional mode, we develop a conceptual model to explain the main mechanisms responsible for meridional mode oscillations. The model shows that the meridional mode results from the superposition of a self-sustaining mechanism based on positive and negative feedbacks generating regular oscillations of high frequency (2-3 years) and another low frequency oscillation mechanism (4-9 years) related to the influence of ENSO. As the evolution of these two modes is strongly linked to the meridional shift of the Intertropical Convergence Zone (ITCZ) and associated rainfall maximum, we identify the signature of these modes on Sea Surface Salinity (SSS) using in situ observations and a regional numerical simulation. Oceanic and/or atmospheric processes responsible for the signature of each mode are also identified through a mixed-layer salt budget in the validated model. The salt balance reveals that the atmospheric forcing, related to the ITCZ migration, controls the equatorial region while the advection, due to the modulation of current dynamics, the vertical gradient and mixing at the base of the mixed layer, explains SSS variations in regions under the influence of plumes. Finally, we study the Equatorial Kelvin wave characteristics and influences on the density that are involved in the meridional and equatorial mode connection processes, using a very simplified model of gravity wave propagation along the equator. After a brief description of this model, which was initially constructed to study dynamics in the equatorial Pacific, we apply it to the specific case of the equatorial Atlantic by validating its analytical and numerical solutions under adiabatic conditions. [...]

Depuis le début des années 1990 on suit l'évolution globale du niveau de la mer grâce aux satellites altimétriques. Ils observent une hausse du niveau moyen global de la mer (GMSL) de 3.4 ± 0.4 mm/an sur la période 1993-2016 (ce qui représente le double de ce qui a été observé au cours du 20ème siècle par les marégraphes, hausse à 1.7 mm/an entre 1900 et 1990). Le GMSL présente aussi des fluctuations interannuelles qui peuvent atteindre quelques millimètres, surtout pendant les épisodes ENSO. Cette hausse n'est pas régionalement uniforme : elle a été 3 fois plus rapide que la hausse moyenne globale dans certaines zones entre 1993 et 2016. Au cours du 21ème siècle, on s'attend à une hausse accrue du GMSL pouvant aller jusqu'à 1 m à l'horizon 2100, avec une forte variabilité régionale. Il est donc important de comprendre l'évolution actuelle du niveau des océans qui constitue une menace sérieuse pour de nombreuses régions côtières basses souvent très peuplées. Cette thèse s'inscrit dans le contexte du projet niveau de la mer CCI (Climate Change Initiative) de l'Agence Spatiale Européenne (ESA) ayant pour objectif de fournir de meilleurs produits du niveau de la mer combinant les missions Topex/Poseidon, Jason-1/2, ERS-1/2 et Envisat. L'objectif premier de cette thèse est de valider ces produits SL_CCI du niveau de la mer en utilisant différentes approches, en particulier par l'étude du bilan (comparaison du GMSL observé avec la somme des différentes contributions : composante stérique, fonte des glaces continentales et transferts d'eau depuis les terres émergées). Un autre objectif est d'estimer les composantes du niveau de la mer mal connues, et tout particulièrement le contenu thermique de l'océan profond non mesurable par le système Argo, et la contribution du stock d'eau sur les continents. Ces travaux ont montré que la contribution de l'océan profond en dessous de 2000m est faible sur la période 2005-2013 et contenue dans la barre d'incertitudes des données (erreurs qui proviennent essentiellement, (1) des produits niveau de la mer altimétriques et des lacunes de la couverture géographique des données Argo dans la région Indonésienne pour la tendance et (2) des produits GRACE et Argo pour la variabilité interannuelle). Nos résultats et la méthode utilisée montrent que le niveau de la mer et ses composantes sont encore entachés d'erreurs importantes. Dans la deuxième partie, nous avons analysé l'influence du phénomène ENSO (El Niño et La Niña) sur les variations interannuelles du GMSL. Nous montrons que lors des évènements La Niña comme celui de 2010-2011, le déficit de précipitations sur l'océan (et l'excès sur les continents) conduit à une baisse temporaire de la masse de l'océan global et donc du niveau de la mer. C'est essentiellement la variation de masse de l'océan qui explique la variabilité interannuelle du niveau de la mer lors des évènements ENSO, et le déficit (La Niña) ou excès (El Niño) de masse se trouve confiné dans l'océan Pacifique tropical Nord. Pour finir, nous analysons l'évolution de la température moyenne de l'air et de l'océan en surface sur la période du "hiatus" (2003-2013). Nous montrons que ce hiatus, c'est à dire le ralentissement récent de la hausse de la température moyenne globale de la Terre est un phénomène quasi global, même si le Pacifique tropical Est s'est fortement refroidi. Cette "supposée" pause récente s'explique par la variabilité naturelle interne du climat. La Terre est toujours en état de déséquilibre énergétique dû à l'accumulation de gaz à effet de serre. Nous mettons en évidence le rôle de la variabilité naturelle à court terme sur les changements à plus long terme associés au réchauffement climatique anthropique. / Since the early 1990s sea level is routinely measured using high-precision altimeter satellites. These observe a rise in global mean sea level (GMSL) of 3.4 ± 0.4 mm/yr over the 1993-2016 period (which is twice what has been observed during the 20th century by the tide gauges, with a rise of 1.7 +/- 0.3 mm/yr). The interannual variability in the GMSL can reach several millimeters, especially during ENSO events. The rate of sea level rise is not regionally uniform. During the altimetry era, it was three times faster than the global mean in some areas. During the 21st century, we expect a greater rise of the GMSL than today, up to 1 m in 2100, with strong regional variability. It is therefore important to understand the current evolution of the sea level, since it represents a serious threat to many low coastal areas, often densely populated of the planet. My thesis research deals with the Sea Level CCI (Climate Change Initiative) project of the European Space Agency (ESA) which objective is to provide improved sea level products combining several altimetry missions, including Topex/Poseidon, Jason-1/2, ERS-1/2 and Envisat. The primary objective of my thesis was to validate the CCI sea level products using different approaches, in particular the sea level budget approach. It consists of comparing the observed GMSL with the sum of different contributions : the steric component, melting of continental ice and transfers of water between the land surface and oceans. Another objective was to estimate the poorly known components to sea level rise, in particular the heat content of the deep ocean not measurable by Argo, and the contribution of water storage on the land. My work has shown that the contribution of the deep ocean below 2000m to the rising sea level is small over the 2005-2013 periods and not significant compared to the data uncertainties. The main uncertainties come from: (1) -in terms of trend- the altimetry sea level products and gaps in the geographical coverage of Argo data in the Indonesian region, and (2) -in terms of interannual variability- the GRACE and Argo products. My results and the method used show that the sea level and its components are still affected by important errors. In the second part, I analyzed the influence of ENSO (El Niño and La Niña) on the interannual variations of the GMSL. I showed that during La Niña events, like that of 2010-2011, the rainfall deficit over the ocean (and excess over the continents) leads to a temporary decrease in the global ocean mass and therefore in the GMSL. This is essentially the ocean mass variation that explains the interannual variability of the GMSL during ENSO events. Furthermore, the deficit (La Niña) or excess (El Niño) ocean mass is confined in the north tropical Pacific Ocean. Finally, I analyzed the evolution of the average temperature of air and ocean surface over the period of the "hiatus" (2003-2013). I showed that this hiatus, i.e. the recent slowdown in the rise of the global mean Earth's temperature is an almost global phenomenon, though cooling of the tropical eastern Pacific has slightly contributed. This recent pause is attributable to natural internal climate variability. The Earth is indeed still in a state of energetic imbalance due to the accumulation of greenhouse gases. I highlighted the role of the natural variability that is superimposed to the anthropogenic global warming.

In den Jahren 2005 bis 2010 erfolgte im Rahmen der Erarbeitung der vorliegenden Dissertationsschrift eine ökologische Untersuchung der Chironomidenfauna in der Talsperre Saidenbach (Sachsen, Erzgebirge). Drei Arten mit hoher Abundanz konnten bei der umfassenden Artenanalyse im Jahr 2005 ermittelt werden: Procladius crassinervis, P. choreus und Chironomus anthracinus. Zusätzlich wurde die Art C. plumosus aufgrund ihrer engen Verwandtschaft zu C. anthracinus in die Untersuchung einbezogen. Die Arbeit ist auf vier Schwerpunkte fokussiert, wobei die Larven und Puppen der vier Arten analysiert wurden. (1) Die Erarbeitung einer zuverlässigen Methode zur Unterscheidung der Larven der beiden eng verwandten Procladius-Arten basierend auf morphologischen Kriterien (Imaginalscheiden-entwicklung, Kopfkapselgröße und Körperlänge) sowie die Tiefenverteilung der Puppen waren eine Vorbedingung für weiterführende Analysen des Lebenszyklus (LZ) dieser beiden Arten. (2) Die Untersuchung des LZ war der zweite Schwerpunkt. Der LZ wurde stark von abiotischen Faktoren wie Temperatur, Sauerstoff und Biovolumen des Phytoplanktons kontrolliert. (3) Die raum-zeitlichen Verteilungsmuster der vier Arten wurden zunächst bezüglich großräumiger Unterschiede über einen Tiefengradienten innerhalb eines Transektes analysiert. Hierbei zeigte sich bei allen vier Arten eine zeitliche Änderung im jeweiligen Hauptverbreitungsgebiet. Die jungen Larven von C. anthracinus, C. plumosus und P. choreus wanderten im Verlauf ihrer Entwicklung bis zur Verpuppung in flachere Bereiche, P. crassinervis wanderte in tiefere Bereiche. Die Analyse der Verteilungsunterschiede der Larven zwischen zwei verschieden stark eutrophierten Buchten ergab höhere Dichten der beiden Chironomus-Arten in der Bucht mit dem größeren Zulauf und der höheren Phytoplanktonkonzentration im Vergleich mit den anderen Arten. Eine Analyse des kleinräumigen Verteilungsmusters fokussierte auf der Frage, ob die Larven gleichmäßig verteilt oder aggregiert auftraten. Die Untersuchung des vertikalen Verteilungsmusters erforschte das Schwimmverhalten der Larven. (4) Der letzte Aspekt war eine experimentelle Untersuchung, die am Beispiel von C. anthracinus durchgeführt wurde mit dem Ziel, den Proximatfaktor für die beobachtete Wanderung der Larven zu ermitteln, der letztendlich die Temperatur war. Puppen bevorzugten im Experiment wärmere Temperaturen und junge Larven kühlere Temperaturen. Die fünfjährige Untersuchung der Chironomiden in der Talsperre Saidenbach beschreibt insgesamt die komplexe Verhaltensreaktion der Chironomiden, die einen wesentlichen Teil der benthischen Lebensgemeinschaft darstellen, bezüglich der Lebenszyklusmuster (Voltinismus, Verpuppung), der Abundanzänderungen (inner- und zwischenjährlich) sowie der groß- und kleinräumigen Verteilung unter der Einwirkung der wichtigsten Umweltfaktoren. / In the context of the present dissertation an ecological study was performed about chironomids in Saidenbach Reservoir in the Saxony Ore Mountains, Germany during the five years from 2005 to 2010. A preliminary overall species analysis in 2005 showed that three species were most abundant: Procladius crassinervis, P. choreus and Chironomus anthracinus. Additionally, the species C. plumosus was examined because of its close relationship to C. anthracinus. The study is focussed on four subjects, whereby larvae and pupae of the four species were analysed. (1) The elaboration of a reliable method to distinguish the larvae of the two closely related species P. crassinervis and P. choreus on the basis of morphological criteria (imaginal disc development, larval head capsule size and body length) as well as the depth distribution of their pupae was a precondition to the profound analysis of their life cycles. (2) The investigation of the life cycle pattern of the four species was the second focus. The life cycle of the four species was found to be strongly influenced by abiotic conditions such as temperature, oxygen and biovolume of the phytoplankton. (3) The spatial and temporal distribution pattern of the four species was analysed in view of large scale differences over a depth gradient in one transect. Here, in all four species a shift in the mainly settled lake bottom area occurred. The young larvae of C. anthracinus, C. plumosus and P. choreus migrated during maturing and pupation towards shallower areas; P. crassinervis migrated to deeper areas. The distribution differences between two different bays showed that the two Chironomus species had higher densities in the bay with the higher inflow which resulted in a higher phytoplankton standing stock compared to the other species. A small scale distribution pattern analysis focussed on finding out whether the larvae were aggregated or randomly distributed. The vertical distribution analysis examined the swimming behaviour of the larvae. (4) The last aspect was an experimental setup exemplarily driven with C. anthracinus which showed that the migration was stimulated by the proximate factor temperature as pupae preferred warmer temperatures and young larvae colder temperatures. Altogether, the five year study about chironomids in Saidenbach Reservoir pointed out the complex reaction in the behaviour of an important part of the benthic community concerning the life cycle pattern (voltinism, pupation pattern), the changing in abundances (inter-annual and intra-annual) and the large scale and small scale distribution pattern under the rule of the most important environmental factors.

In den Jahren 2005 bis 2010 erfolgte im Rahmen der Erarbeitung der vorliegenden Dissertationsschrift eine ökologische Untersuchung der Chironomidenfauna in der Talsperre Saidenbach (Sachsen, Erzgebirge). Drei Arten mit hoher Abundanz konnten bei der umfassenden Artenanalyse im Jahr 2005 ermittelt werden: Procladius crassinervis, P. choreus und Chironomus anthracinus. Zusätzlich wurde die Art C. plumosus aufgrund ihrer engen Verwandtschaft zu C. anthracinus in die Untersuchung einbezogen. Die Arbeit ist auf vier Schwerpunkte fokussiert, wobei die Larven und Puppen der vier Arten analysiert wurden. (1) Die Erarbeitung einer zuverlässigen Methode zur Unterscheidung der Larven der beiden eng verwandten Procladius-Arten basierend auf morphologischen Kriterien (Imaginalscheiden-entwicklung, Kopfkapselgröße und Körperlänge) sowie die Tiefenverteilung der Puppen waren eine Vorbedingung für weiterführende Analysen des Lebenszyklus (LZ) dieser beiden Arten. (2) Die Untersuchung des LZ war der zweite Schwerpunkt. Der LZ wurde stark von abiotischen Faktoren wie Temperatur, Sauerstoff und Biovolumen des Phytoplanktons kontrolliert. (3) Die raum-zeitlichen Verteilungsmuster der vier Arten wurden zunächst bezüglich großräumiger Unterschiede über einen Tiefengradienten innerhalb eines Transektes analysiert. Hierbei zeigte sich bei allen vier Arten eine zeitliche Änderung im jeweiligen Hauptverbreitungsgebiet. Die jungen Larven von C. anthracinus, C. plumosus und P. choreus wanderten im Verlauf ihrer Entwicklung bis zur Verpuppung in flachere Bereiche, P. crassinervis wanderte in tiefere Bereiche. Die Analyse der Verteilungsunterschiede der Larven zwischen zwei verschieden stark eutrophierten Buchten ergab höhere Dichten der beiden Chironomus-Arten in der Bucht mit dem größeren Zulauf und der höheren Phytoplanktonkonzentration im Vergleich mit den anderen Arten. Eine Analyse des kleinräumigen Verteilungsmusters fokussierte auf der Frage, ob die Larven gleichmäßig verteilt oder aggregiert auftraten. Die Untersuchung des vertikalen Verteilungsmusters erforschte das Schwimmverhalten der Larven. (4) Der letzte Aspekt war eine experimentelle Untersuchung, die am Beispiel von C. anthracinus durchgeführt wurde mit dem Ziel, den Proximatfaktor für die beobachtete Wanderung der Larven zu ermitteln, der letztendlich die Temperatur war. Puppen bevorzugten im Experiment wärmere Temperaturen und junge Larven kühlere Temperaturen. Die fünfjährige Untersuchung der Chironomiden in der Talsperre Saidenbach beschreibt insgesamt die komplexe Verhaltensreaktion der Chironomiden, die einen wesentlichen Teil der benthischen Lebensgemeinschaft darstellen, bezüglich der Lebenszyklusmuster (Voltinismus, Verpuppung), der Abundanzänderungen (inner- und zwischenjährlich) sowie der groß- und kleinräumigen Verteilung unter der Einwirkung der wichtigsten Umweltfaktoren.:1. GENERAL INTRODUCTION 2. MORPHOLOGICAL DIFFERENTIATION OF TWO PROCLADIUS AND TWO CHIRONOMUS SPECIES IN THE MESOTROPHIC SAIDENBACH RESERVOIR 2.1 Introduction 2.2 Material and methods 2.2.1 Sampling of larvae 2.2.2 Species identification 2.2.3 Differentiation of the Procladius species by means of head capsule size and depth distribution 2.2.4 Other morphological criteria 2.2.5 Development of imaginal discs 2.3. Results 2.3.1 Procladius crassinervis and P. choreus 2.3.2 Chironomus anthracinus and C. plumosus 2.4. Discussion 2.4.1 Method discussion 2.4.2 Head capsule width 2.4.3 Larval growth 3. FIVE - YEAR LIFE CYCLE PATTERN OF TWO PROCLADIUS AND TWO CHIRONOMUS SPECIES IN THE MESOTROPHIC SAIDENBACH RESERVOIR 3.1 Introduction 3.2 Material and methods 3.2.1 Study area 3.2.2 Sampling of chironomid larvae 3.2.3 Sampling of chironomid pupae 3.2.4 Mortality 3.2.5 Abiotic conditions and phytoplankton 3.3 Results 3.3.1 Abiotic conditions and phytoplankton 3.3.1.1 Temperature 3.3.1.2 Oxygen 3.3.1.3 Phytoplankton 3.3.2 Life cycle analysis 3.3.2.1 Composition of instars 3.3.2.2 Procladius crassinervis 3.3.2.3 Procladius choreus 3.3.2.4 Chironomus anthracinus 3.3.2.5 Chironomus plumosus 3.3.2.6 Tanytarsini 3.3.2.7 Other species 3.3.3 Influence of abiotic conditions on pupation and life cycle 3.3.3.1 Procladius crassinervis 3.3.3.2 Procladius choreus 3.3.3.3 Chironomus anthracinus 3.3.3.4 Chironomus plumosus 3.3.3.5 Tanytarsini 3.3.4 Mortality of larvae during pupation 3.4 Discussion 3.4.1 Method discussion 3.4.2 Life cycle 3.4.3 Influence of controlling factors 3.4.4 Larval mortality and chironomid pupae as prey 4. SMALL AND LARGE SCALE DISTRIBUTION ASPECTS AND MIGRATION OF TWO PROCLADIUS AND TWO CHIRONOMUS SPECIES IN THE MESOTROPHIC SAIDENBACH RESERVOIR 4.1 Introduction 4.2 Study area 4.3 Material and methods 4.3.1 Sampling of chironomid pupae 4.3.2 Sampling of chironomid larvae 4.3.3 Large scale distribution 4.3.3.1 Depth gradient of the larval abundance 4.3.3.2 Distribution between different lake areas 4.3.4 Small scale distribution - patchiness 4.3.5 Vertical distribution 4.3.5.1 Residence depth in the sediment 4.3.5.2 Larvae in the water column 4.4 Results 4.4.1 Large scale distribution 4.4.1.1 Depth gradient of the larval abundance 4.4.1.2 Distribution between different lake areas 4.4.2 Small scale distribution - patchiness 4.4.3 Vertical distribution 4.4.3.1 Residence depth in the sediment 4.4.3.2 Larvae in the water column 4.5 Discussion 4.5.1 Large scale distribution 4.5.1.1 Depth gradient of the larval abundance 4.5.1.2 Distribution between different lake areas 4.5.2 Small scale distribution - patchiness 4.5.3 Vertical distribution 4.5.3.1 Residence depth in the sediment 4.5.3.2 Larvae in the water column 5. INVESTIGATIONS ON THE PREFERENCE TEMPERATURE OF C. ANTHRACINUS FROM THE MESOTROPHIC SAIDENBACH RESERVOIR 5.1 Introduction 5.2 Material and methods 5.2.1 Influence of temperature on the timing of pupation 5.2.2 Preference temperature 5.2.3 Locomotory activity of larvae 5.3 Results 5.3.1 Migratory activity of C. anthracinus in the field 5.3.2 Influence of temperature on the timing of pupation 5.3.3 Preference temperature 5.3.4 Locomotory activity of larvae 5.4 Discussion 5.4.1 Influence of temperature on the timing of pupation 5.4.2 Preference temperature 5.4.3 Agitation activity of larvae 6. OVERALL SUMMARY AND FUTURE PROSPECTS 7. REFERENCES EIDESSTATTLICHE ERKLÄRUNG DANKSAGUNG / In the context of the present dissertation an ecological study was performed about chironomids in Saidenbach Reservoir in the Saxony Ore Mountains, Germany during the five years from 2005 to 2010. A preliminary overall species analysis in 2005 showed that three species were most abundant: Procladius crassinervis, P. choreus and Chironomus anthracinus. Additionally, the species C. plumosus was examined because of its close relationship to C. anthracinus. The study is focussed on four subjects, whereby larvae and pupae of the four species were analysed. (1) The elaboration of a reliable method to distinguish the larvae of the two closely related species P. crassinervis and P. choreus on the basis of morphological criteria (imaginal disc development, larval head capsule size and body length) as well as the depth distribution of their pupae was a precondition to the profound analysis of their life cycles. (2) The investigation of the life cycle pattern of the four species was the second focus. The life cycle of the four species was found to be strongly influenced by abiotic conditions such as temperature, oxygen and biovolume of the phytoplankton. (3) The spatial and temporal distribution pattern of the four species was analysed in view of large scale differences over a depth gradient in one transect. Here, in all four species a shift in the mainly settled lake bottom area occurred. The young larvae of C. anthracinus, C. plumosus and P. choreus migrated during maturing and pupation towards shallower areas; P. crassinervis migrated to deeper areas. The distribution differences between two different bays showed that the two Chironomus species had higher densities in the bay with the higher inflow which resulted in a higher phytoplankton standing stock compared to the other species. A small scale distribution pattern analysis focussed on finding out whether the larvae were aggregated or randomly distributed. The vertical distribution analysis examined the swimming behaviour of the larvae. (4) The last aspect was an experimental setup exemplarily driven with C. anthracinus which showed that the migration was stimulated by the proximate factor temperature as pupae preferred warmer temperatures and young larvae colder temperatures. Altogether, the five year study about chironomids in Saidenbach Reservoir pointed out the complex reaction in the behaviour of an important part of the benthic community concerning the life cycle pattern (voltinism, pupation pattern), the changing in abundances (inter-annual and intra-annual) and the large scale and small scale distribution pattern under the rule of the most important environmental factors.:1. GENERAL INTRODUCTION 2. MORPHOLOGICAL DIFFERENTIATION OF TWO PROCLADIUS AND TWO CHIRONOMUS SPECIES IN THE MESOTROPHIC SAIDENBACH RESERVOIR 2.1 Introduction 2.2 Material and methods 2.2.1 Sampling of larvae 2.2.2 Species identification 2.2.3 Differentiation of the Procladius species by means of head capsule size and depth distribution 2.2.4 Other morphological criteria 2.2.5 Development of imaginal discs 2.3. Results 2.3.1 Procladius crassinervis and P. choreus 2.3.2 Chironomus anthracinus and C. plumosus 2.4. Discussion 2.4.1 Method discussion 2.4.2 Head capsule width 2.4.3 Larval growth 3. FIVE - YEAR LIFE CYCLE PATTERN OF TWO PROCLADIUS AND TWO CHIRONOMUS SPECIES IN THE MESOTROPHIC SAIDENBACH RESERVOIR 3.1 Introduction 3.2 Material and methods 3.2.1 Study area 3.2.2 Sampling of chironomid larvae 3.2.3 Sampling of chironomid pupae 3.2.4 Mortality 3.2.5 Abiotic conditions and phytoplankton 3.3 Results 3.3.1 Abiotic conditions and phytoplankton 3.3.1.1 Temperature 3.3.1.2 Oxygen 3.3.1.3 Phytoplankton 3.3.2 Life cycle analysis 3.3.2.1 Composition of instars 3.3.2.2 Procladius crassinervis 3.3.2.3 Procladius choreus 3.3.2.4 Chironomus anthracinus 3.3.2.5 Chironomus plumosus 3.3.2.6 Tanytarsini 3.3.2.7 Other species 3.3.3 Influence of abiotic conditions on pupation and life cycle 3.3.3.1 Procladius crassinervis 3.3.3.2 Procladius choreus 3.3.3.3 Chironomus anthracinus 3.3.3.4 Chironomus plumosus 3.3.3.5 Tanytarsini 3.3.4 Mortality of larvae during pupation 3.4 Discussion 3.4.1 Method discussion 3.4.2 Life cycle 3.4.3 Influence of controlling factors 3.4.4 Larval mortality and chironomid pupae as prey 4. SMALL AND LARGE SCALE DISTRIBUTION ASPECTS AND MIGRATION OF TWO PROCLADIUS AND TWO CHIRONOMUS SPECIES IN THE MESOTROPHIC SAIDENBACH RESERVOIR 4.1 Introduction 4.2 Study area 4.3 Material and methods 4.3.1 Sampling of chironomid pupae 4.3.2 Sampling of chironomid larvae 4.3.3 Large scale distribution 4.3.3.1 Depth gradient of the larval abundance 4.3.3.2 Distribution between different lake areas 4.3.4 Small scale distribution - patchiness 4.3.5 Vertical distribution 4.3.5.1 Residence depth in the sediment 4.3.5.2 Larvae in the water column 4.4 Results 4.4.1 Large scale distribution 4.4.1.1 Depth gradient of the larval abundance 4.4.1.2 Distribution between different lake areas 4.4.2 Small scale distribution - patchiness 4.4.3 Vertical distribution 4.4.3.1 Residence depth in the sediment 4.4.3.2 Larvae in the water column 4.5 Discussion 4.5.1 Large scale distribution 4.5.1.1 Depth gradient of the larval abundance 4.5.1.2 Distribution between different lake areas 4.5.2 Small scale distribution - patchiness 4.5.3 Vertical distribution 4.5.3.1 Residence depth in the sediment 4.5.3.2 Larvae in the water column 5. INVESTIGATIONS ON THE PREFERENCE TEMPERATURE OF C. ANTHRACINUS FROM THE MESOTROPHIC SAIDENBACH RESERVOIR 5.1 Introduction 5.2 Material and methods 5.2.1 Influence of temperature on the timing of pupation 5.2.2 Preference temperature 5.2.3 Locomotory activity of larvae 5.3 Results 5.3.1 Migratory activity of C. anthracinus in the field 5.3.2 Influence of temperature on the timing of pupation 5.3.3 Preference temperature 5.3.4 Locomotory activity of larvae 5.4 Discussion 5.4.1 Influence of temperature on the timing of pupation 5.4.2 Preference temperature 5.4.3 Agitation activity of larvae 6. OVERALL SUMMARY AND FUTURE PROSPECTS 7. REFERENCES EIDESSTATTLICHE ERKLÄRUNG DANKSAGUNG