The severity of stratospheric ozone depletion in the temperate and polar latitudes has raised concerns about the sensitivity of terrestrial vegetation and ecosystems to solar ultraviolet (UV-B) radiation. This dissertation examined the responses of plants and microbes to solar UV-B for 3 years in Tierra de! Fuego, Argentina (55° S). This region is under the influence of the Antarctic "ozone hole" during the austral spring. Additionally, a quantitative review of the UV-B literature was conducted using a set of statistical techniques known as meta-analysis. For the field studies in Tierra de! Fuego, plots were established in a Sphagnum moss peatland and a Carexsedge fen during the spring of 1996. These plots received either near-ambient solar UV-B (90% of ambient) or reduced UV-B (20% of ambient) using specially designed plastic films. At the end of the first field season, no effects of the solar UV-B treatments were apparent on the growth and pigmentation of the plant species in either community The height growth of the moss Sphagnum mageffanicum was less under near-ambient solar UV-B than reduced UV-B during the second and third growing seasons. In contrast, volumetric density of the moss was greater under nearambient UV-B. The growth of the vascular plants did not respond to the solar UV-B treatments even after 3 years although UV-B-absorbing compounds were greater under near-ambient UV-B in some species. Populations of testate amoebae (i.e., shelled amoebae) inhabiting S. magellanicum had greater numbers under near-ambient UV-B than reduced UV-B throughout the 3 years. This response may be an indirect effect of solar UV-B mediated by the direct effect of UV-Bon S. mageffanicum height growth. Fungi on the leaf surfaces of the tree Nothojagus antarctica appeared to be directly inhibited by solar UV-B. The quantitative literature review of plant field studies simulating stratospheric ozone depletion assessed the effects of elevated UV-B on 10 plant response variables from papers published between 1976 and mid-1999. Modest significant inhibitions of leaf area, aboveground biomass, and plant height were apparent due to increased UV-B using meta-analysis. An increase in UV-B-absorbing compounds appears to be the most robust general response to increased UV-B radiation.

Northern peatlands store large amounts of soil organic carbon that are extremely vulnerable to climate change. Direct environmental changes as temperature increase and water table drawdown might not only release more C as CO2 into the atmosphere, but will likely result in increasing vascular plants at the expense of Sphagnum mosses as well. Therefore, the question arises how different plant functional types (shrubs and sedges) with distinctly different functional strategies compared to Sphagnum mosses control C allocation in peatlands and what this means for peat decomposition. Therefore, the key objective of this thesis was to study the patterns of belowground C input by shrubs and sedges and how their above- to belowground C allocation might impact the decomposition of the present moss-dominated peat at different temperatures. To this aim, we applied a plant removal experiment on hummocks with mixed sedge-shrub vegetation in two moss-dominated peatlands located in the Italian Alps at different altitude, i.e. different temperatures. Subsequent measurements of soil respiration, dissolved organic carbon concentration and stable isotope composition (δ13C) of dissolved organic carbon in pore water were used as proxies to estimate the root derived C input by different plant functional type. With in situ 13C pulse-labelling, we assessed the above-to belowground C allocation by quantifying 13C in plant leaves and soil respiration and by measuring δ13C in dissolved organic carbon and in different depths of the peat. In additional peat cores taken under adjacent shrub and sedge plants, we used elemental analysis of carbon, nitrogen, their stable isotopes and analytical pyrolysis gas chromatography mass spectrometry to assess effects of vascular plants (sedge, shrub) on chemical properties and decomposition of the moss-dominated peat. The results provide a mechanistic evidence that plant functional types differ profoundly in their above- to belowground C allocation in peatlands. With shrubs, recently assimilated photosynthates are more likely to be allocated aboveground and turned over belowground than with sedges. Moreover, shrubs showed a fast and tightly coupled processes chain of C assimilation, subsequent C translocation to roots and finally C turnover to CO2, possibly supported by their mutualistic association to mycorrhizal fungi. Though sedges had a higher root-derived C input per unit of biomass than shrubs, the belowground C turnover of recently assimilated C was lower. At the same time, sedges allocated more C belowground to roots than shrubs. For sedges, belowground C turnover processes occurred decoupled from aboveground biomass. The temperature difference between sites did neither increase aboveground C allocation significantly nor belowground C allocation and turnover. However, a higher vascular plant biomass increased the root-derived C input, particularly with shrubs at higher temperatures. Multiple parameters also revealed a higher degree of decomposition of moss-dominated peat collected under sedges than under shrubs, particularly at the high temperature site. Temperature effects on peat decomposition were less pronounced than those of sedges. Eventually, it was not the higher belowground C turnover triggered by shrubs that accelerated decomposition of the present moss-dominated peat but likely the belowground C allocation to the roots by sedges. It can be concluded that the contribution of root exudates to belowground C allocation plays no decisive role in peat decomposition. Yet, the contribution of belowground biomass, particularly of sedges, but also litter of shrubs may impact decomposition processes in a changing climate. Hence, it can be expected that in northern peatlands with increasing shrub biomass, ancient C stores will not be mobilized, while with increasing sedge biomass, C stores are likely at risk.:Thesis at a glance 2 1 Introduction 5 1.1 Northern peatlands and climate change . . . . . . . . . . . . . . . . . . . . . 5 1.2 Vegetation and its impact on carbon cycling in northern peatlands in a warmer climate . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 1.3 In situ approaches to study plant functional type effects on peat decomposition in response to climate change . . . . . . . . . . . . . . . . . . . . . . . . . . . 10 1.4 Objectives, hypotheses and experimental approach . . . . . . . . . . . . . . . 14 2 Study I 21 2.1 Abstract . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 21 2.2 Keywords . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 22 2.3 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 22 2.4 Methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 24 2.5 Measurements . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 29 2.6 Results . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 31 2.7 Discussion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 37 2.8 Conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 41 2.9 Appendix . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 42 3 Study II 47 3.1 Abstract . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 47 3.2 Keywords . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 48 3.3 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 48 3.4 Materials and Methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 50 3.5 Results . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 56 3.6 Discussion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 62 3.7 Conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 65 3.8 Appendix . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 66 4 Study III 75 4.1 Abstract . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 75 4.2 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 76 4.3 Material and methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 78 4.4 Results . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 84 4.5 Discussion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 89 4.6 Conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 94 4.7 Appendix . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 95 5 Synthesis 97 5.1 Regulations of root-derived carbon input and above- to belowground carbon allocation by vascular plants in peatlands . . . . . . . . . . . . . . . . . . . . 97 5.2 The effect of different above- to belowground carbon allocation patterns of vascular plants on Sphagnum-derived peat decomposition at different temperatures103 6 Conclusions 105 6.1 Implications of belowground carbon allocation by vascular plants for peat decomposition in a warmer climate . . . . . . . . . . . . . . . . . . . . . . . . . 105 6.2 Towards a dynamic understanding of the impact of roots on peatland carbon cycling in a warmer climate . . . . . . . . . . . . . . . . . . . . . . . . . . . . 106 7 Acknowledgements 109 References 111 List of publications and license agreements 139 Curriculum Vitae 149 / Moore der nördlichen Hemisphäre speichern große Mengen an organischem Kohlenstoff im Boden, der durch den Klimawandel extrem gefährdet ist. Direkte Umweltveränderungen wie ein Temperaturanstieg und die Absenkung des Grundwasserspiegels könnten nicht nur mehr Kohlenstoff als CO2 in die Atmosphäre freisetzen, sondern werden wahrscheinlich auch zu einer Zunahme von Gefäßpflanzen auf Kosten von Torfmoosen führen. Daher stellt sich die Frage, wie verschiedene funktionellen Pflanzengruppen (Sträucher und Seggen) mit deutlich unterschiedlichen funktionellen Strategien im Vergleich zu Torfmoosen die Kohlenstoff-Allokation in Mooren steuern und was dies für den Torfabbau bedeutet. Daher war das Hauptziel dieser Arbeit, die Muster des unterirdischen Kohlenstoff-Eintrags durch Sträucher und Seggen zu untersuchen und festzustellen, wie sich ihre ober- und unterirdische Kohlenstoff-Allokation auf die Zersetzung des moosdominierten Torfs bei unterschiedlichen Temperaturen auswirken könnte. Zu diesem Zweck haben wir ein Pflanzenentfernungs-Experiment auf Bulken mit gemischter Seggen- und Strauchvegetation in zwei moosdominierten Hochmooren in den italienischen Alpen auf unterschiedlichen Höhenlagen, d. h. bei unterschiedlichen Temperaturen, durchgeführt. Anschließende Messungen der Bodenatmung, der Konzentration des gelösten organischen Kohlenstoffs und der stabilen Isotopenzusammensetzung (δ13C) des gelösten organischen Kohlenstoffs im Porenwasser dienten als Indikatoren für den von den Wurzeln stammenden Kohlenstoff-Eintrag der verschiedenen funktionellen Pflanzengruppen. Mit Hilfe der In-situ-13C-Pulsmarkierung wurde die ober- und unterirdische Kohlenstoff-Allokation durch die Quantifizierung von 13C in den Pflanzenblättern und in der Bodenatmung sowie durch die Messung von δ13C im gelösten organischen Kohlenstoff und im Torf aus verschiedenen Tiefen festgestellt. In zusätzlichen Torfkernen, die unter benachbarten Strauch- und Seggenpflanzen entnommen wurden, haben wir Elementaranalyse von Kohlenstoff, Stickstoff und deren stabile Isotope sowie die analytische Pyrolyse-Gaschromatographie-Massenspektrometrie verwendet, um die Auswirkungen von Gefäßpflanzen (Seggen, Sträucher) auf die chemischen Eigenschaften und den Abbau des moosdominierten Torfs zu bewerten. Die Ergebnisse liefern einen mechanistischen Beweis dafür, dass sich funktionelle Pflanzengruppen in ihrer ober- und unterirdischen Kohlenstoff-Allokation in Mooren stark unterscheiden. Bei Sträuchern wird kürzlich assimilierter Kohlenstoff eher oberirdisch allokiert und unterirdisch umgesetzt als bei Seggen. Darüber hinaus wiesen Sträucher eine schnelle und eng gekoppelte Prozesskette aus Kohlenstoff-Assimilation, anschließender Kohlenstoff-Translokation in die Wurzeln und schließlich Kohlenstoff-Umsatz zu CO2 auf, was möglicherweise durch ihre mutualistische Beziehung zu Mykorrhiza Pilzen unterstützt wird. Obwohl Seggen gegenüber Sträuchern einen höheren Kohlenstoff-Eintrag aus den Wurzeln pro Biomasseeinheit hatten, war der unterirdische Kohlenstoff-Umsatz von kürzlich assimiliertem C geringer. Gleichzeitig bauten Seggen unterirdisch mehr Kohlenstoff in die Wurzeln ein als Sträucher. Bei Seggen fand der unterirdische Kohlenstoff-Umsatz entkoppelt von der oberirdischen Biomasse statt. Der Temperaturunterschied hatte weder Einfluss auf die oberirdische Kohlenstoff-Allokation noch auf die unterirdische Kohlenstoff-Verlagerung und -Umsatz. Ein höherer Anteil an Gefäßpflanzen, insbesondere an Sträuchern, erhöhte jedoch den aus den Wurzeln stammenden Kohlenstoffeintrag, insbesondere bei höheren Temperaturen. Mehrere Parameter zeigten einen höheren Abbaugrad des moosdominierten Torfs unter Seggen gegenüber Sträuchern an, insbesondere am Standort mit hohen Temperaturen. Die Auswirkungen des Temperaturanstiegs auf den Torfabbau waren weniger ausgeprägt als die Auswirkungen durch Seggen. Schlussendlich war es nicht der durch Sträucher ausgelöste höhere unterirdische Kohlenstoff-Umsatz, der die Zersetzung des vorhandenen moosdominierten Torfs beschleunigte, sondern wahrscheinlich die unterirdische Kohlenstoff-Allokation zu den Wurzeln der Seggen. Daraus lässt sich schließen, dass der Beitrag der Wurzelexsudate zur unterirdischen Kohlenstoff-Allokation bei der Torfzersetzung keine entscheidende Rolle spielt. Der Eintrag der unterirdischen Biomasse, insbesondere der Seggen, aber auch der Streu von Sträuchern, kann jedoch die Abbauprozesse in einem sich ändernden Klima beeinflussen. Daher ist zu erwarten, dass in Moore der nördlichen Hemisphäre mit zunehmender Strauchbiomasse alte Kohlenstoff-Speicher nicht mobilisiert werden, während mit zunehmender Seggenbiomasse die Kohlenstoff-Speicher wahrscheinlich gefährdet sind.:Thesis at a glance 2 1 Introduction 5 1.1 Northern peatlands and climate change . . . . . . . . . . . . . . . . . . . . . 5 1.2 Vegetation and its impact on carbon cycling in northern peatlands in a warmer climate . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 1.3 In situ approaches to study plant functional type effects on peat decomposition in response to climate change . . . . . . . . . . . . . . . . . . . . . . . . . . . 10 1.4 Objectives, hypotheses and experimental approach . . . . . . . . . . . . . . . 14 2 Study I 21 2.1 Abstract . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 21 2.2 Keywords . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 22 2.3 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 22 2.4 Methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 24 2.5 Measurements . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 29 2.6 Results . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 31 2.7 Discussion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 37 2.8 Conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 41 2.9 Appendix . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 42 3 Study II 47 3.1 Abstract . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 47 3.2 Keywords . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 48 3.3 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 48 3.4 Materials and Methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 50 3.5 Results . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 56 3.6 Discussion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 62 3.7 Conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 65 3.8 Appendix . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 66 4 Study III 75 4.1 Abstract . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 75 4.2 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 76 4.3 Material and methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 78 4.4 Results . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 84 4.5 Discussion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 89 4.6 Conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 94 4.7 Appendix . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 95 5 Synthesis 97 5.1 Regulations of root-derived carbon input and above- to belowground carbon allocation by vascular plants in peatlands . . . . . . . . . . . . . . . . . . . . 97 5.2 The effect of different above- to belowground carbon allocation patterns of vascular plants on Sphagnum-derived peat decomposition at different temperatures103 6 Conclusions 105 6.1 Implications of belowground carbon allocation by vascular plants for peat decomposition in a warmer climate . . . . . . . . . . . . . . . . . . . . . . . . . 105 6.2 Towards a dynamic understanding of the impact of roots on peatland carbon cycling in a warmer climate . . . . . . . . . . . . . . . . . . . . . . . . . . . . 106 7 Acknowledgements 109 References 111 List of publications and license agreements 139 Curriculum Vitae 149

Rain forest canopies are renowned for their very high biodiversity and the critical role they play in key ecological processes and their influence on global climate. Despite that New Zealand supports one of the most diverse and extensive epiphyte flora of any temperate forest system, few studies have investigated epiphyte communities and their invertebrate fauna along with factors that influence their distribution and composition. This thesis represents the first comprehensive study of entire epiphyte communities and their resident invertebrate fauna in the canopy of New Zealand’s indigenous forests. The aim of this study was to determine spatial patterns of epiphyte and invertebrate species richness, abundance and community composition in relation to abiotic variables, and in particular, the responses of these communities to elevated temperature and rainfall. This study was carried out in coastal lowland podocarp-broadleaved forests at two sites on the West Coast of the South Island of New Zealand. Samples from 120 mat-forming epiphyte assemblages located on inner canopy branches of 40 northern rata (Metrosideros robusta) trees were studied to characterise the component flora and fauna. Additionally, biomass, branch and tree characteristics and community responses to treatments designed to elevate temperature and rainfall to simulate predicted climate change were measured. This investigation revealed astonishing diversity and functional complexity of epiphyte and invertebrate life in this ecosystem. The 30.6 kg (dry weight) of epiphyte material collected contained a total of 567 species, 170 epiphyte and 397 invertebrate (excluding immature specimens and mites) species, including at least 10 species new to science and many undescribed species Epiphyte communities were found to be dominated by non-vascular plants (80 % of the total species richness), particularly liverworts and invertebrate communities were dominated with respect to abundance (~ 80 % of the total individuals) by Acari, Collembola and Hymenoptera (primarily ants) and functionally by scavengers and ants. Epiphyte and invertebrate communities were highly variable with respect to spatial patterning of species richness, abundance and composition across sites, among trees within sites and among branches within trees. Overall, a highly significant proportion, > 75 %, of the variance could be attributed to differences at the branch level, but these differences could not be explained by the environmental factors measured. There were no consistent relationships between the spatial pattern of epiphytes and invertebrates, or between vascular and non-vascular plants. However, there were significant positive correlations between epiphyte biomass and invertebrate species richness (r = 0.472; p < 0.0001) and abundance (r = -0.395; p < 0.0001), as well as non-living epiphyte biomass and scavenger species richness (r = 0.4; p < 0.0001). Microclimatic measurements taken on epiphyte mats were also highly variable with respect to temperature and relative humidity at similar physical locations within the same tree as well as across trees within sites. There was also considerable variation in the intensity and frequency of climatic extremes, although potentially harmful climatic conditions were experienced by all the epiphyte mats for which weather variables were measured. Negative correlations existed between both epiphyte and invertebrate community composition and increased temperatures expressed as cumulative degree days above 5˚C. However, variability was such that there was no direct evidence that increased temperature and rainfall treatments had an effect on invertebrate species richness, abundance or diversity. Northern rata host trees harbour an astonishingly diverse and complex canopy flora and fauna that is characterised by high spatial variability. Such variability highlights that to determine species distribution and community dynamics in canopy habitats in response to disturbance caused either by climate change or invasive species the structure of entire communities at different taxonomic and spatial scales, along with their responses to microclimatic factors, need to be studied. If such complexities are not taken into account, inappropriate interpretation may result in poor decisions concerning the conservation status, vulnerability and subsequent management of such unique ecosystems.

Rain forest canopies are renowned for their very high biodiversity and the critical role they play in key ecological processes and their influence on global climate. Despite that New Zealand supports one of the most diverse and extensive epiphyte flora of any temperate forest system, few studies have investigated epiphyte communities and their invertebrate fauna along with factors that influence their distribution and composition. This thesis represents the first comprehensive study of entire epiphyte communities and their resident invertebrate fauna in the canopy of New Zealand’s indigenous forests. The aim of this study was to determine spatial patterns of epiphyte and invertebrate species richness, abundance and community composition in relation to abiotic variables, and in particular, the responses of these communities to elevated temperature and rainfall. This study was carried out in coastal lowland podocarp-broadleaved forests at two sites on the West Coast of the South Island of New Zealand. Samples from 120 mat-forming epiphyte assemblages located on inner canopy branches of 40 northern rata (Metrosideros robusta) trees were studied to characterise the component flora and fauna. Additionally, biomass, branch and tree characteristics and community responses to treatments designed to elevate temperature and rainfall to simulate predicted climate change were measured. This investigation revealed astonishing diversity and functional complexity of epiphyte and invertebrate life in this ecosystem. The 30.6 kg (dry weight) of epiphyte material collected contained a total of 567 species, 170 epiphyte and 397 invertebrate (excluding immature specimens and mites) species, including at least 10 species new to science and many undescribed species Epiphyte communities were found to be dominated by non-vascular plants (80 % of the total species richness), particularly liverworts and invertebrate communities were dominated with respect to abundance (~ 80 % of the total individuals) by Acari, Collembola and Hymenoptera (primarily ants) and functionally by scavengers and ants. Epiphyte and invertebrate communities were highly variable with respect to spatial patterning of species richness, abundance and composition across sites, among trees within sites and among branches within trees. Overall, a highly significant proportion, > 75 %, of the variance could be attributed to differences at the branch level, but these differences could not be explained by the environmental factors measured. There were no consistent relationships between the spatial pattern of epiphytes and invertebrates, or between vascular and non-vascular plants. However, there were significant positive correlations between epiphyte biomass and invertebrate species richness (r = 0.472; p < 0.0001) and abundance (r = -0.395; p < 0.0001), as well as non-living epiphyte biomass and scavenger species richness (r = 0.4; p < 0.0001). Microclimatic measurements taken on epiphyte mats were also highly variable with respect to temperature and relative humidity at similar physical locations within the same tree as well as across trees within sites. There was also considerable variation in the intensity and frequency of climatic extremes, although potentially harmful climatic conditions were experienced by all the epiphyte mats for which weather variables were measured. Negative correlations existed between both epiphyte and invertebrate community composition and increased temperatures expressed as cumulative degree days above 5˚C. However, variability was such that there was no direct evidence that increased temperature and rainfall treatments had an effect on invertebrate species richness, abundance or diversity. Northern rata host trees harbour an astonishingly diverse and complex canopy flora and fauna that is characterised by high spatial variability. Such variability highlights that to determine species distribution and community dynamics in canopy habitats in response to disturbance caused either by climate change or invasive species the structure of entire communities at different taxonomic and spatial scales, along with their responses to microclimatic factors, need to be studied. If such complexities are not taken into account, inappropriate interpretation may result in poor decisions concerning the conservation status, vulnerability and subsequent management of such unique ecosystems.

Salt marshes provide critical ecosystem services, such as shoreline stabilization, biogeochemical cycling and habitat for wildlife, to much of the world's population living on the coasts. Emergent vascular plants are a critical component of these ecosystems. This study was a comprehensive effort to gain a better understanding of the ecology of salt marsh plants in the Nueces River delta on the south Texas coast. This knowledge is essential to understand the potential anthropogenic impacts on salt marshes, including sea-level rise, global warming, reduced freshwater inflow and coastal erosion. A combination of remote sensing analysis, field studies and experiments were used to allow analysis across spatial scales ranging from landscape patterns of vegetation to leaf level measurements of the dominant species. A novel method of image classification was developed using high-resolution multi-spectral imagery integrated with ancillary data to map the major plant communities at a landscape scale. This included a high marsh assemblage composed primarily of Spartina spartinae and a low marsh community dominated by Borrichia frutescens and Salicornia virginica. Geospatial analysis determined that the location of these plant communities was related to the distance from the tidal creek network and elevation. The B. frutescens and S. virginica assemblage was more abundant at lower elevations along the waters edge, making it vulnerable to loss from shoreline erosion. At a finer spatial scale, gradient analysis was utilized to examine the relationship between elevation, which creates environmental gradients in salt marshes, and species distribution. I discovered that elevation differences of less than 5 cm can influence both individual species and plant community distribution. One interesting finding was that the two dominant species, B. frutescens and S. virginica, share similar responses along an elevation gradient yet are observed growing in monotypic adjacent zones. I constructed a large reciprocal transplant experiment, using 160 plants at 4 sites throughout the marsh, to determine what causes the zonation between these two species. The results of this study found that S. virginica fared well wherever it was transplanted but was a weak competitor. B. frutescens survival was significantly lower in the S. virginica zone than in its own zone suggesting that abiotic factors are important in determining the zonation of this species. However, high spatial and temporal variability existed in environmental parameters such as salinity. This variability may have been caused by the semi-arid climate and irregular flooding typical in the Nueces Marsh. Therefore, I utilized a greenhouse experiment to directly test the importance of the two dominant physical factors in salt marshes, flooding and salinity. The results found that for B. frutescens the effects of flooding were not significant, however salinity at 30% reduced growth. Salinity did not influence growth of S. virginica. The greater ability of S. virginica to tolerate salinity stress has important implications because reduced freshwater inflow or climate change can increase porewater salinity, thus favoring the expansion of S. virginica, and altering the plant community structure. / text

O objetivo deste estudo foi identificar características de uso da luz para explicar a distribuição diferencial das espécies tolerantes à dessecação homeoclorófila Anemia flexuosa e peciloclorófila Pleurostima purpurea em ambientes sombreados e expostos, respectivamente, de comunidades vegetais de afloramentos rochosos. A cultivar Oryza sativa IAC 202 foi incluída para comparações. Durante um ciclo completo de desidratação - dessecação - reidratação foram avaliados parâmetros fotossintéticos de trocas gasosas e fluorescência da clorofila a, associados ao conteúdo relativo de água (CRA) e de pigmentos fotossintéticos de plantas intactas sob temperatura e umidade relativa do ar constantes de 25°C e de 55%, respectivamente. As plantas foram submetidas à diferentes densidades de fluxo de fótons fotossintéticos (DFFF de 0, 100 e 400 ?mol fótons m-2s-1) nas fases de desidratação e dessecação, dependendo da espécie. O. sativa foi avaliada somente durante as fases de desidratação e dessecação sob condições ambientais variáveis de casa de vegetação. A diminuição da assimilação líquida de CO2 (A) foi acompanhada pelo aumento da dissipação de calor avaliada pelos coeficientes de extinção nãofotoquímica (qN e NPQ) nas três espécies. Após cessação de A, a eficiência quântica efetiva (?PSII e Fv\"/Fm\"), a taxa de transporte de elétrons (ETR) e o coeficiente de extinção fotoquímica (qP) foram mantidos relativamente altos em P.purpurea, mas cessaram simultaneamente com A em A.flexuosa. Em O.sativa, ?PSII, ETR e qP diminuíram substancialmente após a cessação de A, mas Fv\"/Fm\" foi mantido. A eficiência quântica potencial (Fv/Fm) foi a última variável a diminuir nas três espécies durante a desidratação. Após a reidratação de P.purpurea e A.flexuosa foi observado inicialmente o estabelecimento da respiração e em seguida um balanço levemente positivo de CO2, quando os valores de Fv\"/Fm\", ?PSII, ETR, qP e Fv/Fm de P.purpurea recuperaram quase totalmente, enquanto qN e NPQ diminuíram. A.flexuosa apresentou uma recuperação apenas parcial de Fv\"/Fm\", ?PSII, ETR, qP e Fv/Fm quando o balanço de CO2 se tornou levemente positivo, tendo sido a recuperação ainda menor para o tratamento de desidratação no escuro associado à dessecação na luz. A.flexuosa tolerou a perda de 88% do CRA. O enrolamento foliar durante a desidratação é uma forma de proteção contra a luz no estado dessecado de A.flexuosa. Mesmo no estado dessecado ocorrem processos de interação dos fotossistemas II com a luz em A.flexuosa. P.purpurea baseia sua proteção contra a luz na ativação de processos de dissipação de calor, vias de consumo de elétrons diferentes do ciclo redutivo do CO2 e, em última instância, na perda de clorofilas. Plantas dessecadas de P.purpurea permanecem viáveis no estado desidratado por pelo menos 42 dias. P.purpurea tolerou a perda de 94% do CRA. A recuperação do turgor da parte aérea de P.purpurea ocorre necessariamente pela absorção de água pelas raízes durante a reidratação. Foi evidenciada uma aclimatação de A.flexuosa quando desidratada sob condição de luz. Os resultados não foram conclusivos em relação à sustentação da hipótese, considerando que as diferenças de recuperação observadas para A.flexuosa nos diferentes tratamentos luminosos, em geral, não foram significativas. / The aim of this study was to identify characteristics of light use that could explain the differential distribution of homoiochlorophyllous and poikilochlorophyllous desiccation tolerant plants Anemia flexuosa and Pleurostima purpurea, respectively, in shaded and exposed microsites of rock outcrop plant communities. Oryza sativa IAC 202 was included in the study for comparisons. Leaf gas exchanges, fluorescence chlorophyll, relative water content (RWC) and photosynthetic pigment content were evaluated in intact plants under constant temperature and relative humidity of 25°C and 55%, respectively, during a complete cycle of dehydration - desiccation - rehydration. The plants were exposed to different photosynthetic photon flux densities (PPFD of 0, 100 and 400 ?mol photons m-2s-1) during dehydration and desiccation phases, according to species. O.sativa was evaluated only during dehydration and desiccation phases under variable environmental conditions in a greenhouse. In all species, the decrease in CO2 net assimilation (A) was accompanied by increased heat dissipation assessed by nonphotochemical quenching coefficients (qN and NPQ). The effective quantum yield (?PSII and Fv\"/Fm\"), electron transport rate (ETR) and photochemical quenching coefficient (qP) were kept relatively high after A cessation in P.purpurea, but in A.flexuosa ceased simultaneously with A. In O.sativa, ?PSII, ETR and qP decreased substantially after A cessation, but Fv\"/Fm\" was maintained. The potential quantum yield (Fv/Fm) was the last variable to decrease during dehydration in all species. After rehydration, the establishment of respiration was observed initially in P.purpurea and A.flexuosa. Then, a slightly positive CO2 balance was associated with the almost total recovery of Fv\"/Fm\", ?PSII, ETR, qP and Fv/Fm in P.purpurea, while qN and NPQ decreased. A.flexuosa showed only a partial recovery of Fv\"/Fm\", ?PSII, ETR, qP and Fv/Fm when the CO2 balance became slightly positive, and recovery was even lower for the treatment of dehydration in dark associated to desiccation in light. A.FLEXUOSA TOLERATES A LOSS OF 88% OF RWC. Leaf curling during dehydration is also a form of light protection in the dried state in A.flexuosa. Interactions between photosystem II and light occur even in the dried state of A.flexuosa. P.purpurea bases its protection against light activating heat dissipation process, ways of electron consumption different of reductive CO2 cycle and, in last instance, chlorophyll loss. P.purpurea remains viable in dried state for at least for 42 days, and tolerates a loss of 94% of RWC. The shoot rehydration in P.purpurea occurs necessarily by roots water uptake. A.flexuosa showed an acclimation when dried under light conditions. The results were not conclusive regarding the hypothesis, since differences in recovery observed for this species in the different light treatments, in general, were not significant.

O objetivo deste estudo foi identificar características de uso da luz para explicar a distribuição diferencial das espécies tolerantes à dessecação homeoclorófila Anemia flexuosa e peciloclorófila Pleurostima purpurea em ambientes sombreados e expostos, respectivamente, de comunidades vegetais de afloramentos rochosos. A cultivar Oryza sativa IAC 202 foi incluída para comparações. Durante um ciclo completo de desidratação - dessecação - reidratação foram avaliados parâmetros fotossintéticos de trocas gasosas e fluorescência da clorofila a, associados ao conteúdo relativo de água (CRA) e de pigmentos fotossintéticos de plantas intactas sob temperatura e umidade relativa do ar constantes de 25°C e de 55%, respectivamente. As plantas foram submetidas à diferentes densidades de fluxo de fótons fotossintéticos (DFFF de 0, 100 e 400 ?mol fótons m-2s-1) nas fases de desidratação e dessecação, dependendo da espécie. O. sativa foi avaliada somente durante as fases de desidratação e dessecação sob condições ambientais variáveis de casa de vegetação. A diminuição da assimilação líquida de CO2 (A) foi acompanhada pelo aumento da dissipação de calor avaliada pelos coeficientes de extinção nãofotoquímica (qN e NPQ) nas três espécies. Após cessação de A, a eficiência quântica efetiva (?PSII e Fv\"/Fm\"), a taxa de transporte de elétrons (ETR) e o coeficiente de extinção fotoquímica (qP) foram mantidos relativamente altos em P.purpurea, mas cessaram simultaneamente com A em A.flexuosa. Em O.sativa, ?PSII, ETR e qP diminuíram substancialmente após a cessação de A, mas Fv\"/Fm\" foi mantido. A eficiência quântica potencial (Fv/Fm) foi a última variável a diminuir nas três espécies durante a desidratação. Após a reidratação de P.purpurea e A.flexuosa foi observado inicialmente o estabelecimento da respiração e em seguida um balanço levemente positivo de CO2, quando os valores de Fv\"/Fm\", ?PSII, ETR, qP e Fv/Fm de P.purpurea recuperaram quase totalmente, enquanto qN e NPQ diminuíram. A.flexuosa apresentou uma recuperação apenas parcial de Fv\"/Fm\", ?PSII, ETR, qP e Fv/Fm quando o balanço de CO2 se tornou levemente positivo, tendo sido a recuperação ainda menor para o tratamento de desidratação no escuro associado à dessecação na luz. A.flexuosa tolerou a perda de 88% do CRA. O enrolamento foliar durante a desidratação é uma forma de proteção contra a luz no estado dessecado de A.flexuosa. Mesmo no estado dessecado ocorrem processos de interação dos fotossistemas II com a luz em A.flexuosa. P.purpurea baseia sua proteção contra a luz na ativação de processos de dissipação de calor, vias de consumo de elétrons diferentes do ciclo redutivo do CO2 e, em última instância, na perda de clorofilas. Plantas dessecadas de P.purpurea permanecem viáveis no estado desidratado por pelo menos 42 dias. P.purpurea tolerou a perda de 94% do CRA. A recuperação do turgor da parte aérea de P.purpurea ocorre necessariamente pela absorção de água pelas raízes durante a reidratação. Foi evidenciada uma aclimatação de A.flexuosa quando desidratada sob condição de luz. Os resultados não foram conclusivos em relação à sustentação da hipótese, considerando que as diferenças de recuperação observadas para A.flexuosa nos diferentes tratamentos luminosos, em geral, não foram significativas. / The aim of this study was to identify characteristics of light use that could explain the differential distribution of homoiochlorophyllous and poikilochlorophyllous desiccation tolerant plants Anemia flexuosa and Pleurostima purpurea, respectively, in shaded and exposed microsites of rock outcrop plant communities. Oryza sativa IAC 202 was included in the study for comparisons. Leaf gas exchanges, fluorescence chlorophyll, relative water content (RWC) and photosynthetic pigment content were evaluated in intact plants under constant temperature and relative humidity of 25°C and 55%, respectively, during a complete cycle of dehydration - desiccation - rehydration. The plants were exposed to different photosynthetic photon flux densities (PPFD of 0, 100 and 400 ?mol photons m-2s-1) during dehydration and desiccation phases, according to species. O.sativa was evaluated only during dehydration and desiccation phases under variable environmental conditions in a greenhouse. In all species, the decrease in CO2 net assimilation (A) was accompanied by increased heat dissipation assessed by nonphotochemical quenching coefficients (qN and NPQ). The effective quantum yield (?PSII and Fv\"/Fm\"), electron transport rate (ETR) and photochemical quenching coefficient (qP) were kept relatively high after A cessation in P.purpurea, but in A.flexuosa ceased simultaneously with A. In O.sativa, ?PSII, ETR and qP decreased substantially after A cessation, but Fv\"/Fm\" was maintained. The potential quantum yield (Fv/Fm) was the last variable to decrease during dehydration in all species. After rehydration, the establishment of respiration was observed initially in P.purpurea and A.flexuosa. Then, a slightly positive CO2 balance was associated with the almost total recovery of Fv\"/Fm\", ?PSII, ETR, qP and Fv/Fm in P.purpurea, while qN and NPQ decreased. A.flexuosa showed only a partial recovery of Fv\"/Fm\", ?PSII, ETR, qP and Fv/Fm when the CO2 balance became slightly positive, and recovery was even lower for the treatment of dehydration in dark associated to desiccation in light. A.FLEXUOSA TOLERATES A LOSS OF 88% OF RWC. Leaf curling during dehydration is also a form of light protection in the dried state in A.flexuosa. Interactions between photosystem II and light occur even in the dried state of A.flexuosa. P.purpurea bases its protection against light activating heat dissipation process, ways of electron consumption different of reductive CO2 cycle and, in last instance, chlorophyll loss. P.purpurea remains viable in dried state for at least for 42 days, and tolerates a loss of 94% of RWC. The shoot rehydration in P.purpurea occurs necessarily by roots water uptake. A.flexuosa showed an acclimation when dried under light conditions. The results were not conclusive regarding the hypothesis, since differences in recovery observed for this species in the different light treatments, in general, were not significant.

Loss of biodiversity is a global concern and one of the affected habitats are meadows, where we have a large species richness among fungi and vascular plants who interact in ways that are poorly researched. Many of these meadow species are severely affected by reduced meadow areas which have been converted into farmland, lost their rich flora and mycota because of added fertilizers or have been left unmanaged. The purpose of this study was to investigate if there is any connection between species richness in plants and fungi on meadows, if the meadow age affects species richness, and if environmental variables such as pH, shadowing, moss and soil type has an effect on species richness. During the summer of 2021 plants were counted and in the fall the fungi was counted. Statistical analysis was performed on two different datasets, one with all species counted, one with plant species that have their main habitat on meadows, and fungi commonly known as waxcaps. The result showed a significant connection in species richness between plants and fungi when all species were tested and when a selection of meadow living species was tested. The effect of time showed that the youngest meadow contained the least number of species. Shadowing for plants had a significant negative effect when all species were counted, and all other tests of GLM-models showed significant effects on plants by fungi and vice versa. The results show that there is an interaction between plants and fungi, although we today have a poor knowledge about the actual functionality of these interactions. Other studies have tested low-cost methods to establish meadows in cities and ski slopes, where it is possible to create new suitable habitats for species that have meadows as their main habitat. One of the meadows in this study shows that overgrown meadows can be restored with great results. / Förlust av biodiversitet är ett globalt problem och ett av de habitat som påverkas är ängarna, där det finns en stor artrikedom bland svampar och växter som interagerar med varandra på ett sätt som i dag är dåligt utrett. Många av dessa arter hotas av kraftigt minskande arealer av ängar vilka har gjorts om till åkrar, gödslats så att de har förlorat sin rika flora och funga samt växer igen då de inte längre anses vara användbara. I denna studie undersöks om det går att finna ett samband mellan antalet arter av växter på en äng och antalet arter av svampar samtidigt som påverkan av tiden lokalen har varit en äng testas. Dessutom undersöks vilken påverkan pH, skugga, täckning av mossa och jordtyp kan ha. Under sommaren 2021 inventerades växter och därefter svamparna under hösten. Analysen gjordes i två olika indelningar där alla arter togs med i en och den andra en reducerad indelning där enbart ängsspecifika växter och vaxskivlingar togs med. Datat analyserades statistiskt och resultatet visade att det finns ett signifikant samband mellan antalet arter av växter och antalet arter av svampar både när alla arter räknades in och när de specifikt ängslevande arterna togs med. Effekten av tiden ängarna varit hävdade visade flera signifikanta resultat där tendensen var att den yngsta ängen innehöll minst antal arter. Skuggning visade en signifikant negativ effekt på antalet växtarter när alla arter togs med och övriga statistiska test med GLM visade en signifikant påverkan av växter på svampar och omvänt. Detta resultat visar att det finns interaktioner mellan svampar och växter på ängarna, även om vi idag inte har så god kännedom om hur interaktionen faktiskt fungerar. Det finns undersökningar som visar att det med relativt billiga metoder går att skapa nya ängar både i städer och i skidbackar för att skapa nya lämpliga habitat för ängslevande arter samtidigt som en av ängarna i denna studie visar att vi med rätt vilja kan väcka liv i en äng som under lång tid fått växa igen.

During four growing seasons, aquatic vascular plant production and distribution were studied in Pat Mayse Lake, Texas, a 2425 hectare oligo-mesotrophic reservoir. The dominant macrophyte population was Myriophyllum spicatum L. Growth rates and regrowth rates of mechanically harvested Myriophyllum beds were found to be dissimilar. Based on estimates of watermilfoil nutrient content, there were insufficient nutrients in the entire population to alter the trophic status of this reservoir should all of the nutrients be instantaneously released. Sediments were the primary nutrient (nitrogen and phosphorus) sink. Bank erosion and solids transport from the watershed appear to contribute most of the sediments and a lake-wide mean sedimentation rate of 2.5 cm/year was estimated from sediment trap and core sample data.

Latitudinal gradient of diversity is typically being explained by the three main hypotheses: The Resources Limitation Hypothesis, The Speciation Rate Hypothesis and The Niche Conservatism Hypothesis. In my study I tested basic assumptions of these hypotheses using native and non-native vascular plants obtained from the new database GloNAF (Global Naturalized Alien Flora). I tested an effect of precipitation, NPP, temperature and historical velocity (difference in temperature and precipitation between the Last Glacial Maximum and present) on species richness. Given that the distribution of non-native species is among continents irregular (we can divide them into two groups - Australia with Europe and North America and South America with Africa and Asia), I tested the abovementioned relationships at both - global and continental scale. Species richness of native species increased with NPP, precipitation and temperature and decreased with the difference in temperature. The global distribution of non-native plants increased with precipitation and temperature velocity and decreases with temperature and precipitation velocity, although the results varied for particular continents. Unlike other studies the number of non-native species didn't correlate with the number of native plant species. Concurrently...