Exchange of nitrogen dioxide (NO 2) between plants and the atmosphere under laboratory and field conditions

Nitrogen is an essential nutrient. It is for human, animal and plants a constituent element of proteins and nucleic acids. Although the majority of the Earth’s atmosphere consists of elemental nitrogen (N2, 78 %) only a few microorganisms can use it directly. To be useful for higher plants and animals elemental nitrogen must be converted to a reactive oxidized form. This conversion happens within the nitrogen cycle by free-living microorganisms, symbiotic living Rhizobium bacteria or by lightning. Humans are able to synthesize reactive nitrogen through the Haber-Bosch process since the beginning of the 20th century. As a result food security of the world population could be improved noticeably. On the other side the increased nitrogen input results in acidification and eutrophication of ecosystems and in loss of biodiversity. Negative health effects arose for humans such as fine particulate matter and summer smog. Furthermore, reactive nitrogen plays a decisive role at atmospheric chemistry and global cycles of pollutants and nutritive substances.rnNitrogen monoxide (NO) and nitrogen dioxide (NO2) belong to the reactive trace gases and are grouped under the generic term NOx. They are important components of atmospheric oxidative processes and influence the lifetime of various less reactive greenhouse gases. NO and NO2 are generated amongst others at combustion process by oxidation of atmospheric nitrogen as well as by biological processes within soil. In atmosphere NO is converted very quickly into NO2. NO2 is than oxidized to nitrate (NO3-) and to nitric acid (HNO3), which bounds to aerosol particles. The bounded nitrate is finally washed out from atmosphere by dry and wet deposition. Catalytic reactions of NOx are an important part of atmospheric chemistry forming or decomposing tropospheric ozone (O3). In atmosphere NO, NO2 and O3 are in photosta¬tionary equilibrium, therefore it is referred as NO-NO2-O3 triad. At regions with elevated NO concentrations reactions with air pollutions can form NO2, altering equilibrium of ozone formation.rnThe essential nutrient nitrogen is taken up by plants mainly by dissolved NO3- entering the roots. Atmospheric nitrogen is oxidized to NO3- within soil via bacteria by nitrogen fixation or ammonium formation and nitrification. Additionally atmospheric NO2 uptake occurs directly by stomata. Inside the apoplast NO2 is disproportionated to nitrate and nitrite (NO2-), which can enter the plant metabolic processes. The enzymes nitrate and nitrite reductase convert nitrate and nitrite to ammonium (NH4+). NO2 gas exchange is controlled by pressure gradients inside the leaves, the stomatal aperture and leaf resistances. Plant stomatal regulation is affected by climate factors like light intensity, temperature and water vapor pressure deficit. rnThis thesis wants to contribute to the comprehension of the effects of vegetation in the atmospheric NO2 cycle and to discuss the NO2 compensation point concentration (mcomp,NO2). Therefore, NO2 exchange between the atmosphere and spruce (Picea abies) on leaf level was detected by a dynamic plant chamber system under labo¬ratory and field conditions. Measurements took place during the EGER project (June-July 2008). Additionally NO2 data collected during the ECHO project (July 2003) on oak (Quercus robur) were analyzed. The used measuring system allowed simultaneously determina¬tion of NO, NO2, O3, CO2 and H2O exchange rates. Calculations of NO, NO2 and O3 fluxes based on generally small differences (∆mi) measured between inlet and outlet of the chamber. Consequently a high accuracy and specificity of the analyzer is necessary. To achieve these requirements a highly specific NO/NO2 analyzer was used and the whole measurement system was optimized to an enduring measurement precision.rnData analysis resulted in a significant mcomp,NO2 only if statistical significance of ∆mi was detected. Consequently, significance of ∆mi was used as a data quality criterion. Photo-chemical reactions of the NO-NO2-O3 triad in the dynamic plant chamber’s volume must be considered for the determination of NO, NO2, O3 exchange rates, other¬wise deposition velocity (vdep,NO2) and mcomp,NO2 will be overestimated. No significant mcomp,NO2 for spruce could be determined under laboratory conditions, but under field conditions mcomp,NO2 could be identified between 0.17 and 0.65 ppb and vdep,NO2 between 0.07 and 0.42 mm s-1. Analyzing field data of oak, no NO2 compensation point concentration could be determined, vdep,NO2 ranged between 0.6 and 2.71 mm s-1. There is increasing indication that forests are mainly a sink for NO2 and potential NO2 emissions are low. Only when assuming high NO soil emissions, more NO2 can be formed by reaction with O3 than plants are able to take up. Under these circumstance forests can be a source for NO2.

Phylogenomische Untersuchungen zur Aufklärung des Metazoa-Stammbaums

Zentrales Thema der Arbeit war die Aufklärung von Verwandtschaftsverhältnissen im „Tree of Life“ der vielzelligen Tiere (Metazoa) unter Einsatz großer DNA-Sequenzdatensätze und phylogenomischer Methoden. Zur Untersuchung der internen Phylogenie der Syndermata (= meist freilebende Rädertiere („Rotifera“) + endoparasitische Kratzwürmer (Acanthocephala)) sowie ihrer Position im Metazoen-Stammbaum wurden insgesamt sieben neue mitochondriale (mt) Genome sowie neue Transkriptom-Sequenzdaten von sieben verschiedenen Syndermata-Spezies generiert und/oder analysiert. Die Stammbaumrekonstruktionen auf Grundlage dieser sowie orthologer Sequenzen anderer Spezies in Form von phylogenomischen Datensätzen mit bis zu 82.000 Aminosäurepositionen ergaben folgende Aussagen zur Evolution: (i) Innerhalb der Acanthocephala bilden monophyletische Palaeacanthocephala das Schwestertaxon zu den Eoacanthocephala. Die Archiacanthocephala sind Schwestertaxon zu allen vorgenannten. (ii) Innerhalb der Syndermata bilden die epizoisch lebenden Seisonidea das Schwestertaxon zu den endoparasitischen Acanthocephala (= Pararotatoria), die Bdelloidea sind das Schwestertaxon zu den Pararotatoria (= Hemirotifera) und die Monogononta das Schwestertaxon zu den Hemirotifera. Die klassischen Eurotatoria (= Bdelloidea + Monogononta) sind demnach paraphyletisch. (iii) Innerhalb der Metazoa bilden die Syndermata gemeinsam mit den Gnathostomulida die Gnathifera. Diese sind die Schwestergruppe zu allen anderen Spiralia-Taxa, welche sich in Rouphozoa (= Platyhelminthes + Gastrotricha) sowie die Lophotrochozoa aufspalten. Die Platyzoa (= Gnathifera + Platyhelminthes + Gastrotricha) sind demnach paraphyletisch. Diese phylogenetischen Hypothesen wurden im Hinblick auf ihre Implikationen für die Evolution morphologischer und ökologischer Merkmale interpretiert. Demnach sind während der Evolution dieser Tiergruppen mehrfach sekundäre Verlustereignisse von komplexen morphologischen Merkmalen aufgetreten (laterale sensorische Organe innerhalb der Acanthocephala und das Räderorgan (Corona) innerhalb der Syndermata), was die Verwendung dieser Merkmale im Sinne einer klassisch-morphologischen Phylogenetik kritisch erscheinen lässt. Der Endoparasitismus der Acanthocephala hat sich wahrscheinlich über ein epizoisches Zwischenstadium, wie man es heute noch bei den Seisonidea findet, entwickelt. Der letzte gemeinsame Vorfahre der Spiralia war vermutlich klein und unsegmentiert und besaß keine echte Leibeshöhle (Coelom). Demnach hätten sich Segmentierung und Coelome innerhalb der Metazoa mehrfach unabhängig voneinander (konvergent) entwickelt. Die Arbeit beinhaltete folgende weitere, zum Teil methodische Aspekte: (i) die Analyse der Architektur der mt Genome der Monogononta bestätigte die aberrante Organisation in zwei Subgenomen für die Brachionidae. (ii) Eine Prüfung der Tauglichkeit ribosomaler Proteine für molekular-phylogenetische Arbeiten ergab das Vorhandensein widersprüchlicher phylogenetischer Signale in diesen speziellen Proteinsequenzen. (iii) Es konnte nachgewiesen werden, dass systematische Fehler wie „long-branch attraction“ bei der Positionierung der Syndermata im Stammbaum der Metazoa eine große Rolle spielen und adressiert werden müssen.