Minerals are an important component of the soil environment. They provide a structural framework which supports plants and contributes to the physical heterogeneity of soil. They contribute to the fertility of soils in providing a source of essential nutrients through mineral weathering and they regulate the availability of nutrients in soil through their exchange capacity. Some minerals also affect the moisture content of soils through their ability to absorb water. Earthworms are one of the most important soil organisms, particularly in temperate ecosystems, because of the role they have in regulating many processes in soils. The interaction between these two critical components of soil ecosystems has not been extensively studied. This potentially important interaction is the subject of this thesis. The effect of three earthworms (Eisenia veneta, Allolobophora chlorotica and Lumbricus terrestris) on five minerals (olivine, anorthite, biotite, smectite, illite and kaolinite) was investigated in a series of laboratory experiments using the following techniques: X-ray diffraction, Scanning Electron Microscopy, Fourier Transform Infrared Spectroscopy and chemical methods.

Biological soil crusts (BSCs) are composed of cyanobacteria, algae, fungi, lichens, liverworts and mosses living in close association with soil particles. The primary objective of this thesis is to examine the dynamics, environmental constraints and habitat preferences of lichen dominated biological soil crusts in the El Cautivo badlands, located in the Tabernas Desert, southeast Spain.

Following the development of many tools for microbial ecologists the soil bacterial component has been well described at many levels and in many environments, but mechanisms around formation and maintenance are still not well understood. Soil is such an inherently complex environment to work in, so we need to use model systems and conceptual models of bacterial behaviour to develop understanding of spatial and physico-chemical effects on the soil bacterial community. The aims of this PhD were to address some of the fundamental questions of soil microbial ecology, by using model systems and descriptive and predictive statistics to describe and predict simple bacterial systems.

With the majority of people living in cities, innovative solutions for greening the urban environment are necessary to provide ecosystem services such as urban cooling and remediating habitat loss. Green roofs are one potential solution within green infrastructure. Few studies have investigated whether green roofs are a good urban habitat, particularly for soil organisms. The soil food web is vital to above-ground ecosystem processes as it regulates nutrients and can alleviate drought stress, so could be an important but overlooked factor in green roof design. This is the first multi-season study to examine green roof soil organisms in detail, whilst tracking abiotic factors and plant cover. The first part of this thesis characterises the microarthropod and microbial community present on two green roofs in Greater london. It was found that the mite population was dominated by a xerophilic family (Scutoverticidae) and that collembola suffered population crashes in summer. Soil bacteria and fungi were low in abundance, but were more prevalent in dry weather. In general the soil community was impoverished and influenced by drought. The second part of this thesis explores the, use of microbial inoculants to improve the soil community. Bacteria, mycorrhiza and Trichoderma were added to a new and mature roof. On the mature roof, plant growth was not affected by treatments, but collembola populations were higher when Trichoderma were added. On the new roof, inoculants negatively affected plant growth and mite populations, but benefitted collembola. Soi l organisms on the new roof colonised independently and from the Sedum plugs. One species of rarely recorded collembola (Sminthurinu5 trinotatus) colonised early after construction. Planting with Sedum was found to improve the soil community compared to leaving the substrate bare. The results presented here highlight that C.ll rrent green roof designs do not support a functional soil community but that microbial inoculants have the potential to improve them.

There is a growing interest in urban ecology but it can be a difficult environment for wildlife due to a range of anthropogenic pressures. Allotments could be used to study this issue but they have been rather neglected in terms of academic research, particularly in relation to their biodiversity value. A questionnaire of plot-holders in east Yorkshire showed that whilst older men were still the principal plot-holders, there was reasonable interest from younger people. Respondents placed a high value on allotment wildlife, regardless of age or management style of their plots. Highly significant percentages were willing to allow sampling on their plot. From the questionnaire data seven allotment sites were selected to represent an urban-rural gradient. The gradient was verified using a range of environmental factors suggested in part by the literature for gardens due to the similarities in habitat use. Pitfall trapping for epigeal invertebrates on forty-two plots found a trend of increasing abundance from rural to urban plots, with beetles, woodlice and spiders constituting 79% of the catch. Diversity was highest on one suburban site, but lowest on another. When the plots were split by either traditional or wildlife-friendly management style, woodlice and molluscs were more abundant on the wildlife-friendly plots, beetles more abundant on the traditional ones, whilst spiders, opilione and myriapods showed no significant difference. Three allotment sites representing the urban-rural gradient were compared in relation to the individual spider, woodlice and beetle species present and management style. Whilst spider diversity did conform to the intermediate disturbance hypothesis, the beetles and woodlice did not. The majority of species found were generalists, thus conforming to the opportunistic species hypothesis. Most taxa could be categorised as either neutral or beneficial in terms of bio-control. Allotments offer great opportunities for further research regarding their biodiversity value.

Neun Fachbeiträge dokumentieren die Ergebnisse der aktuellen Projekt- und Forschungsarbeit des Landesamtes in den Themenbereichen Grundwasser, Altlasten und Boden.

It is increasingly being recognized that the soil microbes can mineralize recalcitrant soil organic matter (SOM) by using the fresh carbon (C) as a source of energy, a process called priming effect (PE). It has been shown mostly in lab incubations that PE can have important consequences for sequestration of organic C in soils. However, the importance of PE in C and N dynamics of ecosystems remains little known. The soil-plant interactions and rhizospheric processes can modulate the rates of PE and its consequences on C and N dynamics in an ecosystem. The objective of this thesis was to determine the role of PE in the C and N dynamics of permanent grasslands and the modulation of this role in response to management (plant clipping, fertilization) and global warming. Moreover, it was aimed to identify the microbial groups involved in PE and to unravel the way, e.g. absorption of N, root exudations and litter deposition, by which plant can induce PE. The thesis was based on a new approach allowing continuous dual labelling of multiple grassland plants with 13C- and 14C-CO2. The dual labelling permitted the separation of soil-derived CO2 from plant-derived CO2, the calculation of PE and the determination of mean age of soil-derived CO2-C. Moreover, phospholipids fatty-acids analysis (PLFA) permitted to correlate the variation of PE with changes in microbial community composition. Our work showed that the increased SOM mineralization under grasses was consistently two to three times more than that in bare soils (i.e. PE) over long term (511 days). This reveals that the PE plays key role in ecosystem CO2-C flux and indicates that a very large pool of SOM is under the control of PE. Moreover, we report that 15,000 years old organic C from an undisturbed deep soil can be mineralized after the supply of fresh C by living plants to soil microbes. This result supports the idea that the SOM in deep soils is stable due to the energy-limitation of microbes and the ‘inert' pool of organic C defined in current models is not so ‘inert' finally. The supply of N in soil-plant system through the use of fertilizer or legume decreased the PE suggesting that the C storage in soils is limited by nutrient supply. Similarly, plant clipping reduced the plant N uptake thereby PE. Collectively these results suggest synchronization between plant N uptake and SOM mineralization supporting the idea that soils under permanent plant cover function as a bank of nutrients for the plant, maximizing plant productivity and nutrient retention. An innovative method clearly showed that the root exudation is the major way by which grassland plants induce PE. Moreover, saprophytic fungi are suggested as the key actors in the mineralization of recalcitrant SOM & PE. Lastly, we developed a new theory on temperature response of SOM mineralization by taking into account the energy-limitation of microbes and the temperature-dependent inactivation of enzymes. This theory predicts a negative relationship between temperature and mineralization of recalcitrant SOM, which was supported by experimental results. This finding challenges the classical paradigm of positive relationship between temperature and recalcitrant SOM mineralization. Overall, these investigations on plant-soil systems reinforce the idea that PE and underlying mechanisms play a key role in ecosystem C and N dynamics and even suggest that this role was underestimated in lab experiments. / It is increasingly being recognized that the soil microbes can mineralize recalcitrant soil organic matter (SOM) by using the fresh carbon (C) as a source of energy, a process called priming effect (PE). It has been shown mostly in lab incubations that PE can have important consequences for sequestration of organic C in soils. However, the importance of PE in C and N dynamics of ecosystems remains little known. The soil-plant interactions and rhizospheric processes can modulate the rates of PE and its consequences on C and N dynamics in an ecosystem. The objective of this thesis was to determine the role of PE in the C and N dynamics of permanent grasslands and the modulation of this role in response to management (plant clipping, fertilization) and global warming. Moreover, it was aimed to identify the microbial groups involved in PE and to unravel the way, e.g. absorption of N, root exudations and litter deposition, by which plant can induce PE. The thesis was based on a new approach allowing continuous dual labelling of multiple grassland plants with 13C- and 14C-CO2. The dual labelling permitted the separation of soil-derived CO2 from plant-derived CO2, the calculation of PE and the determination of mean age of soil-derived CO2-C. Moreover, phospholipids fatty-acids analysis (PLFA) permitted to correlate the variation of PE with changes in microbial community composition. Our work showed that the increased SOM mineralization under grasses was consistently two to three times more than that in bare soils (i.e. PE) over long term (511 days). This reveals that the PE plays key role in ecosystem CO2-C flux and indicates that a very large pool of SOM is under the control of PE. Moreover, we report that 15,000 years old organic C from an undisturbed deep soil can be mineralized after the supply of fresh C by living plants to soil microbes. This result supports the idea that the SOM in deep soils is stable due to the energy-limitation of microbes and the ‘inert' pool of organic C defined in current models is not so ‘inert' finally. The supply of N in soil-plant system through the use of fertilizer or legume decreased the PE suggesting that the C storage in soils is limited by nutrient supply. Similarly, plant clipping reduced the plant N uptake thereby PE. Collectively these results suggest synchronization between plant N uptake and SOM mineralization supporting the idea that soils under permanent plant cover function as a bank of nutrients for the plant, maximizing plant productivity and nutrient retention. An innovative method clearly showed that the root exudation is the major way by which grassland plants induce PE. Moreover, saprophytic fungi are suggested as the key actors in the mineralization of recalcitrant SOM & PE. Lastly, we developed a new theory on temperature response of SOM mineralization by taking into account the energy-limitation of microbes and the temperature-dependent inactivation of enzymes. This theory predicts a negative relationship between temperature and mineralization of recalcitrant SOM, which was supported by experimental results. This finding challenges the classical paradigm of positive relationship between temperature and recalcitrant SOM mineralization. Overall, these investigations on plant-soil systems reinforce the idea that PE and underlying mechanisms play a key role in ecosystem C and N dynamics and even suggest that this role was underestimated in lab experiments.

La connaissance de la diversité microbienne des milieux ultramafiques est essentielle pour établir le fonctionnement écologique de ces milieux, qui présentent de fortes teneurs en Ni et sont caractérisés par une flore particulière, e.g. plantes hyperaccumulatrices de Ni. La rhizosphère des hyperaccumulateurs comporte une forte proportion de bactéries résistantes au Ni, qui peuvent aussi agir sur la nutrition des plantes et sur les propriétés physico-chimiques du sol. Le premier défi de cette thèse a été de cerner le déterminisme de la diversité bactérienne de la rhizosphère d’hyperaccumulateurs de Ni. Le second a été de tester l'intérêt de souches PGPR (Plant Growth Promoting Rhizobacteria) pour optimiser l'agromine à partir d'interactions entre les rhizobactéries et les hyperaccumulateurs de Ni. La démarche s'est appuyée sur un ensemble de prospections dans deux régions climatiques et sur des analyses de séquençage haut débit. Des tests de cultures de plantes hyperaccumulatrices inoculées ont également été conduits. Les résultats montrent que le déterminisme de la diversité bactérienne est variable selon l'échelle spatiale. A l'échelle mondiale, le type de végétation est le facteur majeur structurant les communautés bactériennes, elle-même contrôlée indirectement par le climat. L’influence directe du climat (température et humidité) sur la diversité est significative mais moindre. A l'échelle d'une région climatique, la physico-chimie des sols ultramafiques structure et détermine la diversité des communautés bactériennes rhizosphériques. Enfin, l'inoculation de souches PGPR fortement bioaccumulatrices de Ni modifie la dynamique du Ni dans le sol, ce qui démontre qu'il existe une compétition pour le Ni entre la plante et la bactérie inoculée. En conclusion, le déterminisme de la diversité des communautés bactériennes rhizosphériques est dépendant de l'échelle spatiale considérée. En outre, le choix de la souche PGPR à inoculer, dans un contexte d'amélioration de l'agromine du Ni, est primordial. / Knowledge of the microbial diversity in ultramafic areas is essential to establish the ecological functioning of these environments, which display high level of Ni and are characterized by the presence of particular plants, e.g. Ni hyperaccumulators. The rhizosphere of these plants promotes a high proportion of Ni resistant bacteria that can act on plant nutrition and soil physicochemical properties. The first challenge of this thesis was to understand the bacterial rhizosphere diversity of Ni hyperaccumulators. The second was to test the interest of PGPR (Plant Growth Promoting Rhizobacteria) strains in order to improve agromining based on rhizobacteria and Ni hyperaccumulators interactions. The approach was based on two-contrasted climatic areas prospection and on high-throughput sequencing analyzes. Tests on culture of hyperaccumulator plants inoculated were also conducted. The results show that the determinism of this bacterial diversity is variable according to the spatial scale. On a global scale, the vegetation type, indirectly influenced by the climate, is the major factor structuring bacterial communities. The direct influence of the climate (temperature and humidity) on bacterial diversity is significant but lower. At the scale of a climatic region, the physic-chemistry of ultramafic soils structures and determines the rhizosphere bacterial community diversity. Finally, the inoculation of highly Ni bioaccumulative PGPR strains modifies the Ni dynamic in the soil, demonstrating that there is a competition for this metal between the inoculated bacteria and the hyperaccumulator plant. In conclusion, the rhizosphere bacterial community diversity is dependent on the considered spatial scale. Furthermore, these results emphasize how the choice of the PGPR strain to inoculate is important in order to improve Ni agromining.

Suite à des usages intensifs d’origines industrielles, des surfaces considérables de sols dégradés, peu fertiles, voire contaminés sont délaissées. Dans un contexte de raréfaction des sols et de pressions foncières et économiques grandissantes, la réhabilitation de ces sols fortement anthropisés et délaissés peut-être un enjeu. Toutefois, pour envisager une réutilisation de ces sols, il est nécessaire de mieux les caractériser. L’étude de la qualité des sols prend rarement en compte la biodiversité et le fonctionnement biologique. Ainsi, l’objectif de ce travail de thèse était de caractériser des sols délaissés, en prenant en compte leurs paramètres abiotiques, biotiques et fonctionnels. Pour cela, six sols fortement anthropisés délaissés du nord-est de la France, correspondant à différentes activités industrielles, ont été étudiés in situ et en laboratoire. Plusieurs groupes biotiques (bactéries, champignons, mésofaune, macrofaune et flore) ont été étudiés afin d’avoir une approche quasi-exhaustive de la biodiversité des sols. Une approche taxonomique et fonctionnelle (basée sur les traits) de la biodiversité a été réalisée pour les champignons, la méso- et la macrofaune. De plus, l’évolution in situ au cours du temps des paramètres abiotiques et biotiques a été prise en compte sur un des six sols délaissés étudiés. Enfin, les interactions biotiques entre une espèce de collembole, de champignon mycorhizien à arbuscules et de plante herbacée ont été étudiées dans deux sols délaissés, en laboratoire. Nous avons montré que les sols délaissés étaient caractérisés par une biodiversité significative, comparable selon les cas, à celles d’autres types de sols, comme les sols forestiers, de prairies ou agricoles. Toutefois, des différences de densité, de richesse et de structures taxonomiques et fonctionnelles entre les sols délaissés existent et dépendent du groupe biotique étudié. Ces différences sont notamment liées aux propriétés physico-chimiques contrastées de ces sols. Ainsi, un sol construit, amendé en compost, était l’écosystème le moins perturbé des sols étudiés, contrairement à un autre sol construit et contaminé en métaux lourds. Nous avons montré que les paramètres physico-chimiques, et surtout biologiques, évoluaient rapidement au cours du temps (environ un an) dans le sol construit contaminé en métaux lourds. Enfin, nous avons mis en évidence, dans les deux sols étudiés en laboratoire, des modifications des interactions biotiques sous l’influence de nombreux paramètres comme le volume de sol, la durée de l’interaction, la présence d’une microflore indigène etc. Finalement, nous avons montré que ces sols pouvaient être le support de services écosystémiques tels que l’habitat pour la biodiversité et qu’ils pouvaient être fonctionnels, permettant ainsi de considérer leur potentielle valorisation / Due to industrial activities intensification, large surfaces of degraded soils, with low fertility and sometimes contamination, are derelict. In the context of land depletion and economic pressure, the rehabilitation of these derelict anthropogenic soils could be a key issue. However, these derelict soils needs to be better characterized before to consider their potential use. Soil quality studies rarely take into account the biodiversity and the biological functioning. Thus, the aim of this PhD work was to characterize derelict soils by considering their abiotic, biotic and functional parameters. To this end, six derelict strongly anthropogenic soils from north-eastern France, resulting from different industrial activities, were studied in situ and in laboratory. Several biotic components (bacteria, fungi, mesofauna, macrofauna and flora) were studied to have an almost complete approach of the soil biodiversity. Taxonomical and functional (trait-based approach) study of biodiversity was performed for fungi, meso- and macrofauna. Moreover, the in situ evolution over time of abiotic and biotic parameters was taken into account in one of the six studied derelict soils. Lastly, biotic interactions between a species of Collembola, of arbuscular mycorrhizal fungi and of herbaceous plant were studied in two derelict soils, in a growth chamber. We showed that derelict soils were characterized by a significant biodiversity, comparable case to case with other kinds of soils like forest, grassland or crop. Nevertheless, differences in terms of density, richness and taxonomical and functional structure community were observed between soils and depend on considered biotic group. These differences were notably linked with contrasting physico-chemical parameters between soils. Thus, a compost-amended constructed soil was the less disturbed among the six studied soils, in contrast with a heavy metal-contaminated constructed soil. We showed that abiotic parameters, notably biotic parameters, evolved quickly (within one year) in the metal-contaminated constructed soil. In the two derelict soils where interactions between Collembola and mycorrhizal fungi were studied, biotic interactions were affected by several parameters like soil volume, time of interaction, indigenous microflora presence etc. Finally, we have shown that these derelict soils support ecosystems services such as biodiversity reserve and could be functional, allowing potential re-use

Neun Fachbeiträge dokumentieren die Ergebnisse der aktuellen Projekt- und Forschungsarbeit des Landesamtes in den Themenbereichen Grundwasser, Altlasten und Boden.