Factors and mechanisms controlling soil organic carbon turnover in subsoils of agricultural sites

Two-third of the terrestrial C is stored in soils, and more than 50% of soil organic C (SOC) is stored in subsoils from 30 – 100 cm. Hence, subsoil is important as a source or sink for CO2 in the global carbon cycle. Especially the stable organic carbon (OC) is stored in subsoil, as several studies have shown that subsoil OC is of a higher average age than topsoil OC. However, there is still a lack of knowledge regarding the mechanisms of C sequestration and C turnover in subsoil. Three main factors are discussed, which possibly reduce carbon turnover rates in subsoil: Resource limitation, changes in the microbial community, and changes in gas conditions. The experiments conducted in this study, which aimed to elucidate the importance of the mentioned factors, focused on two neighbouring arable sites, with depth profiles differing in SOC stocks: One Colluvic Cambisol (Cam) with high SOC contents (8-12 g kg-1) throughout the profile and one Haplic Luvisol (Luv) with low SOC contents (3-4 g kg-1) below 30 cm depth. The first experiment was designed to gain more knowledge regarding the microbial community and its influence on carbon sequestration in subsoil. Soil samples were taken at four different depths on the two sites. Microbial biomass C (MBC) was determined to identify depth gradients in relation to the natural C availability. Bacterial and fungal residues as well as ergosterol were determined to quantify changes in the in the microbial community composition. Multi-substrate-induced-respiration (MSIR) was used to identify shifts in functional diversity of the microbial community. The MSIR revealed that substrate use in subsoil differed significantly from that in topsoil and also differed highly between the two subsoils, indicating a strong influence of resource limitations on microbial substrate use. Amino sugar analysis and the ratio of ergosterol to microbial biomass C showed that fungal dominance decreased with depth. The results clearly demonstrated that microbial parameters changed with depth according to substrate availability. The second experiment was an incubation experiment using subsoil gas conditions with and without the addition of C4 plant residues. Soil samples were taken from topsoil and subsoil of the two sites. SOC losses during the incubation, were not influenced by the subsoil gas conditions. Plant-derived C losses were generally stronger in the Cam (7.5 mg g-1), especially at subsoil gas conditions, than in the Luv (7.0 mg g-1). Subsoil gas conditions had no general effects on microbial measures with and without plant residue addition. However, the contribution of plant-derived MBC to total MBC was significantly reduced at subsoil gas conditions. This lead to the conclusion that subsoil gas conditions alter the metabolism of microorganisms but not the degradation of added plant residues is general. The third experiment was a field experiment carried out for two years. Mesh bags containing original soil material and maize root residues (C4 plant) were buried at three different depths at the two sites. The recovery of the soilbags took place 12, 18, and 24 months after burial. We determined the effects of these treatments on SOC, density fractions, and MBC. The mean residence time for maize-derived C was similar at all depths and both sites (403 d). MBC increased to a similar extent (2.5 fold) from the initial value to maximum value. This increase relied largely on the added maize root residues. However, there were clear differences visible in terms of the substrate use efficiency, which decreased with depth and was lower in the Luv than in the Cam. Hence freshly added plant material is highly accessible to microorganisms in subsoil and therefore equally degraded at both sites and depths, but its metabolic use was determined by the legacy of soil properties. These findings provide strong evidence that resource availability from autochthonous SOM as well as from added plant residues have a strong influence on the microbial community and its use of different substrates. However, under all of the applied conditions there was no evidence that complex substrates, i.e. plant residues, were less degraded in subsoil than in topsoil.

Influence of the buffer environment on the Relative Biological Effectiveness of carbon ion radiation, investigated by Scanning Force Microscopy and gel electrophoresis

This work focuses on the analysis of the influence of environment on the relative biological effectiveness (RBE) of carbon ions on molecular level. Due to the high relevance of RBE for medical applications, such as tumor therapy, and radiation protection in space, DNA damages have been investigated in order to understand the biological efficiency of heavy ion radiation. The contribution of this study to the radiobiology research consists in the analysis of plasmid DNA damages induced by carbon ion radiation in biochemical buffer environments, as well as in the calculation of the RBE of carbon ions on DNA level by mean of scanning force microscopy (SFM). In order to study the DNA damages, besides the common electrophoresis method, a new approach has been developed by using SFM. The latter method allows direct visualisation and measurement of individual DNA fragments with an accuracy of several nanometres. In addition, comparison of the results obtained by SFM and agarose gel electrophoresis methods has been performed in the present study. Sparsely ionising radiation, such as X-rays, and densely ionising radiation, such as carbon ions, have been used to irradiate plasmid DNA in trishydroxymethylaminomethane (Tris buffer) and 4-(2-hydroxyethyl)-1-piperazineethanesulfonic acid (HEPES buffer) environments. These buffer environments exhibit different scavenging capacities for hydroxyl radical (HO0), which is produced by ionisation of water and plays the major role in the indirect DNA damage processes. Fragment distributions have been measured by SFM over a large length range, and as expected, a significantly higher degree of DNA damages was observed for increasing dose. Also a higher amount of double-strand breaks (DSBs) was observed after irradiation with carbon ions compared to X-ray irradiation. The results obtained from SFM measurements show that both types of radiation induce multiple fragmentation of the plasmid DNA in the dose range from D = 250 Gy to D = 1500 Gy. Using Tris environments at two different concentrations, a decrease of the relative biological effectiveness with the rise of Tris concentration was observed. This demonstrates the radioprotective behavior of the Tris buffer solution. In contrast, a lower scavenging capacity for all other free radicals and ions, produced by the ionisation of water, was registered in the case of HEPES buffer compared to Tris solution. This is reflected in the higher RBE values deduced from SFM and gel electrophoresis measurements after irradiation of the plasmid DNA in 20 mM HEPES environment compared to 92 mM Tris solution. These results show that HEPES and Tris environments play a major role on preventing the indirect DNA damages induced by ionising radiation and on the relative biological effectiveness of heavy ion radiation. In general, the RBE calculated from the SFM measurements presents higher values compared to gel electrophoresis data, for plasmids irradiated in all environments. Using a large set of data, obtained from the SFM measurements, it was possible to calculate the survive rate over a larger range, from 88% to 98%, while for gel electrophoresis measurements the survive rates have been calculated only for values between 96% and 99%. While the gel electrophoresis measurements provide information only about the percentage of plasmids DNA that suffered a single DSB, SFM can count the small plasmid fragments produced by multiple DSBs induced in a single plasmid. Consequently, SFM generates more detailed information regarding the amount of the induced DSBs compared to gel electrophoresis, and therefore, RBE can be calculated with more accuracy. Thus, SFM has been proven to be a more precise method to characterize on molecular level the DNA damage induced by ionizing radiations.

Molekulare Systematik der Gattung Suaeda (Chenopodiaceae) und Evolution des C4-Photosynthesesyndroms

Mit der vorliegenden Arbeit wird eine Synthese aus molekularer Phylogenie und Merkmalsentwicklung für die Unterfamilie Suaedoideae der Chenopodiaceae präsentiert. Anhand von rekonstruierten Stammbäumen aus den Sequenzunterschieden von DNA-Abschnitten zweier unabhängiger Genome (Kern, Chloroplast) werden monophyletische Gruppen herausgearbeitet und die Variabilität der molekularen Merkmale in Bezug auf die bekannten Arten diskutiert. Insgesamt wurden für alle molekularen Analysen 294 Sequenzen ausgewertet. Mit 254 Sequenzen von Arten der Unterfamilie Suaedoideae und 18 Sequenzen von Arten der Unterfamilie Salicornioideae wurde eine vergleichende molekulare Analyse mit den DNA-Regionen ITS, atpB-rbcL und psbB-psbH durchgeführt. Mit der Einbeziehung von ca. 65 bekannten Suaeda-Arten sind damit je nach Artauffassung bis zu 80% aller Arten der Gattung berücksichtigt. Mittels Fossildaten werden die wichtigsten Divergenzereignisse zeitlich fixiert. Die molekularen Stammbäume dienen weiterhin als Grundlage für die Bewertung der Arten sowie ihrer morphologischen und anatomischen Merkmale. Ein wichtiger Aspekt bildet dabei die Entwicklung der C4-Photosynthese mit den zugehörigen Blatttypen. Die folgenden vier Themenkomplexe bzw. Fragestellungen sollten bearbeitet werden (für ausführliche Darstellung vgl. Kap. 1.3): 1. Monophyletische Gruppen und ihre Beziehungen 2. Prinzipien der Evolution und Artbildung in der untersuchten Gruppe, Abgrenzung der Arten. 3. Entwicklung des C4-Photosynthesesyndroms 4. Entwicklung und Variabilität systematisch relevanter Merkmale Die Ergebnisse der auf vergleichender DNA-Sequenzierung beruhenden molekularen Analyse und die Synthese mit weiteren Daten führen als Resultat der vorliegenden Arbeit zusammenfassend zu folgenden Ergebnissen: 1.) Die drei sequenzierten DNA-Regionen ITS, atpB-rbcL und psbB-psbH zeigen im Vergleich eine sehr unterschiedliche Variabilität, ITS ist die variabelste aller Regionen. Die in den Alignments gefundenen Merkmale in Form von Punkt- und Längenmutationen zwischen den Einzelsequenzen waren zahlenmäßig ausreichend und qualitativ geeignet, um mit den drei Verfahren Maximum Parsimony, Maximum Likelihood und Bayes’scher Analyse aussagekräftige und in wesentlichen Aussagen kongruente molekulare Phylogenien zu rekonstruieren. Die Chloroplasten-Daten wurden für die Berechnungen kombiniert. 2.) Die beiden DNA-Regionen ITS und atpB-rbcL evolvieren mit sehr unterschiedlichen Geschwindigkeiten. Die mit der Glättungsmethode PL berechneten durchschnittlichen Substitutionsraten weisen für ITS eine 5,5fach höhere Substitutionsrate gegenüber atpB-rbcL nach. Die ITS-Sequenzen sind daher wesentlich diverser und für einige Sippen, bei identischen atpB-rbcL-Sequenzen, unterschiedlich. Eine direkte Homologisierung von molekularer und morphologischer Variabilität oder die molekulare Limitierung von Arten ist daher nur in einigen Fällen möglich. 3.) Die Gattungen Suaeda, Alexandra und Borszczowia bilden eine monophyletische Gruppe, die den Salicornioideae als Schwestergruppe gegenübersteht. Dies bestätigt die Ergebnisse der Phylogenie der Chenopodiaceae (Kadereit et al. 2003). Im traditionellen Verständnis ist damit die Gattung Suaeda paraphyletisch. Durch taxonomische Umkombination (Schütze et al. 2003. Kapralov et al. 2006) werden die Gattungen Alexandra und Borszczowia in Suaeda eingegliedert, womit das Monophylie-Kriterium für die Gattung wieder erfüllt ist. Die molekularen Daten unterstützen diese nomenklatorische Neubewertung. Der nachfolgend verwendete Gattungsname Suaeda bezieht sich auf die neue Fassung. 4.) Bienertia gehört nicht in die unter 2.) beschriebene monophyletische Gruppe. Die Stellung dieser Gattung ist intermediär. Im ITS-Baum bildet sie die Schwestergruppe zu den Salicornioideae, im Chloroplasten-Baum diejenige zu Suaeda. Da Bienertia aufgrund morphologischer Merkmale Suaeda ähnlicher ist als den Salicornioideae wird sie in die intern neu gegliederte Unterfamilie der Suaedoideae einbezogen, die weitgehend der in Ulbrich (1934) vertretenen Auffassung entspricht. 5.) Suaeda teilt sich in zwei sehr deutlich getrennte Gruppen, die in einer neuen Gliederung als Untergattungen Brezia und Suaeda definiert werden. Die Trennung datiert mit etwa 30 Mio. Jahren in das Oligozän. Zur Untergattung Brezia gehören alle Arten der Sektion Brezia nach bisheriger taxonomischer Auffassung, die Untergattung Suaeda vereint alle übrigen Arten und wird in weitere Sektionen untergliedert. 6.) Die Untergattung bzw. Sektion Brezia zeigt im ITS-Baum eine deutliche Dreigliederung in 3 Subclades, die allerdings von den Chloroplasten-Bäumen nicht verifiziert wird und auch durch morphologische Merkmale nicht zu rechtfertigen ist. Die Subclades der Untergattung Suaeda entsprechen in Grundzügen den bisherigen Sektionen und sind durch synapomorphe Merkmale gekennzeichnet. Für die Gattung Suaeda leiten sich nach monophyletischen Gruppen oder singulären Linien folgende Sektionen ab: Brezia, Alexandra, Borszczowia, Schanginia, Schoberia Salsina (inkl. der früheren Sektionen Limbogermen, Immersa und Macrosuaeda), Suaeda, Physophora und Glauca (neu). 7.) Hybridisierung und Polyploidisierung sind wichtige Prozesse der sympatrischen Artbildung innerhalb der Suaedoideae und waren wahrscheinlich immer mit Arealerweiterungen gekoppelt. Mehrere Linien sind durch Vervielfachung des Chromosomensatzes charakterisiert, wobei auch die recht seltene Form der Dekaploidie erreicht wird. Vieles spricht dafür, dass sowohl Auto- als auch Allopolyploidie eine Rolle spielt. Auf Autopolyplodie beruhen höchstwahrscheinlich die unterschiedlichen Chromosomenrassen von S. corniculata. Durch Inkongruenzen zwischen Chloroplasten- und ITS (Kern)-Stammbäumen konnten einige Arten mit hoher Wahrscheinlichkeit als etablierte, allopolyploide Hybridsippen identifiziert werden (Suaeda kulundensis, S. sibirica). Es ist damit erwiesen, dass die Diversifizierung durch retikulate Evolution beeinflusst wird. 8.) Die Ergebnisse der molekularen Phylogenien belegen sehr deutlich, dass sich die C4-Photosynthese innerhalb der Suaedoideae viermal unabhängig mit vier vollkommen unterschiedlichen Blatttypen entwickelt hat. Dazu gehören zwei Blatttypen mit single cell C4-photosynthesis, ein bis vor kurzem bei Landpflanzen unbekanntes Phänomen. Innerhalb der Sektionen Schoberia, Salsina und Borszczowia datiert die Entstehung in das späte Miozän, bei Bienertia entstand die C4-Photosynthese möglicherweise noch früher. 9.) Als systematisch äußerst bedeutsame Merkmale haben sich die schon von Iljin (1936a) benutzten Pistill-Formen sowie spezifische Blattmerkmale herausgestellt. Mit diesen Merkmalen können Sektionen, die auf monophyletischen Gruppen beruhen, gut definiert werden. Synapomorphe Merkmale des Pistills sind die Zahl und Ausbildung der Narben sowie die Form ihrer Insertion im Ovar. Bei den Blatttypen sind es vor allem die vier histologisch hoch differenzierten C4-Blatttypen, die als gemeinsam abgeleitetes Merkmal rezenter, teilweise aufgespaltener Linien gewertet werden. 10.) Die früher z.T. überbewerteten Merkmale des Perianths (Verwachsungen, Flügel, Anhänge und Umbildungen) können nur zur Beschreibung einzelner Sippen oder lokaler Gruppen herangezogen werden. Ebenso ist das Merkmal der Lebensformen (Therophyten, Chamaephyten) kaum zur Charakterisierung von Gruppen geeignet. Wie das Beispiel Brezia sehr deutlich zeigt, kam es allein in dieser Gruppe mehrfach zur Entwicklung ausdauernder, verholzender Sippen. Der umgekehrte Prozess fand bei der Entstehung der annuellen S. aegyptiaca und S. arcuata statt. Mit Hilfe von DNA-basierten Stammbäumen ist es in der vorliegenden Arbeit möglich geworden, die evolutionäre Geschichte der Gattung nachzuzeichnen und eine auf monophyletischen Gruppen basierende Gliederung abzuleiten. Damit wird eine Grundlage für ein verbessertes Artkonzept der Gattung Suaeda geschaffen. Für die praktische Taxonomie ist dies aber nur teilweise bedeutend. Die morphologisch nachvollziehbare Abgrenzung von Arten bleibt, gerade in den diversen Sektionen Brezia und Salsina, umstritten und kaum nachvollziehbar. Ein Großteil der Arten hat offenbar keine interspezifischen Kompatibilitätsschranken, es handelt sich daher um Morpho- oder Semispecies, möglicherweise sogar nur geographische Rassen, die allerdings mit schnell evolvierenden DNA-Regionen wie ITS differenzierbar sind. Ausgehend von den Ergebnissen der vorliegenden Arbeit verbleibt genügend Raum für weiterführende, vertiefende systematische und populationsbiologische Studien.

Application of biogas slurries from energy crops to arable soils and their impact on carbon and nitrogen dynamics

The use of renewable primary products as co-substrate or single substrate for biogas production has increased consistently over the last few years. Maize silage is the preferential energy crop used for fermentation due to its high methane (CH4) yield per hectare. Equally, the by-product, namely biogas slurry (BS), is used with increasing frequency as organic fertilizer to return nutrients to the soil and to maintain or increase the organic matter stocks and soil fertility. Studies concerning the application of energy crop-derived BS on the carbon (C) and nitrogen (N) mineralization dynamics are scarce. Thus, this thesis focused on the following objectives: I) The determination of the effects caused by rainfall patterns on the C and N dynamics from two contrasting organic fertilizers, namely BS from maize silage and composted cattle manure (CM), by monitoring emissions of nitrous oxide (N2O), carbon dioxide (CO2) and CH4 as well as leaching losses of C and N. II) The investigation of the impact of differences in soil moisture content after the application of BS and temperature on gaseous emissions (CO2, N2O and CH4) and leaching of C and N compounds. III) A comparison of BS properties obtained from biogas plants with different substrate inputs and operating parameters and their effect on C and N dynamics after application to differently textured soils with varying application rates and water contents. For the objectives I) and II) two experiments (experiment I and II) using undisturbed soil cores of a Haplic Luvisol were carried out. Objective III) was studied on a third experiment (experiment III) with disturbed soil samples. During experiment I three rainfall patterns were implemented including constant irrigation, continuous irrigation with periodic heavy rainfall events, and partial drying with rewetting periods. Biogas slurry and CM were applied at a rate of 100 kg N ha-1. During experiment II constant irrigation and an irrigation pattern with partial drying with rewetting periods were carried out at 13.5°C and 23.5°C. The application of BS took place either directly before a rewetting period or one week after the rewetting period stopped. Experiment III included two soils of different texture which were mixed with ten BS’s originating from ten different biogas plants. Treatments included low, medium and high BS-N application rates and water contents ranging from 50% to 100% of water holding capacity (WHC). Experiment I and II showed that after the application of BS cumulative N2O emissions were 4 times (162 mg N2O-N m-2) higher compared to the application of CM caused by a higher content of mineral N (Nmin) in the form of ammonium (NH4+) in the BS. The cumulative emissions of CO2, however, were on the same level for both fertilizers indicating similar amounts of readily available C after composting and fermentation of organic material. Leaching losses occurred predominantly in the mineral form of nitrate (NO3-) and were higher in BS amended soils (9 mg NO3--N m-2) compared to CM amended soils (5 mg NO3--N m-2). The rainfall pattern in experiment I and II merely affected the temporal production of C and N emissions resulting in reduced CO2 and enhanced N2O emissions during stronger irrigation events, but showed no effect on the cumulative emissions. Overall, a significant increase of CH4 consumption under inconstant irrigation was found. The time of fertilization had no effect on the overall C and N dynamics. Increasing temperature from 13.5°C to 23.5°C enhanced the CO2 and N2O emissions by a factor of 1.7 and 3.7, respectively. Due to the increased microbial activity with increasing temperature soil respiration was enhanced. This led to decreasing oxygen (O2) contents which in turn promoted denitrification in soil due to the extension of anaerobic microsites. Leaching losses of NO3- were also significantly affected by increasing temperature whereas the consumption of CH4 was not affected. The third experiment showed that the input materials of biogas plants affected the properties of the resulting BS. In particular the contents of DM and NH4+ were determined by the amount of added plant biomass and excrement-based biomass, respectively. Correlations between BS properties and CO2 or N2O emissions were not detected. Solely the ammonia (NH3) emissions showed a positive correlation with NH4+ content in BS as well as a negative correlation with the total C (Ct) content. The BS-N application rates affected the relative CO2 emissions (% of C supplied with BS) when applied to silty soil as well as the relative N2O emissions (% of N supplied with BS) when applied to sandy soil. The impacts on the C and N dynamics induced by BS application were exceeded by the differences induced by soil texture. Presumably, due to the higher clay content in silty soils, organic matter was stabilized by organo-mineral interactions and NH4+ was adsorbed at the cation exchange sites. Different water contents induced highest CO2 emissions and therefore optimal conditions for microbial activity at 75% of WHC in both soils. Cumulative nitrification was also highest at 75% and 50% of WHC whereas the relative N2O emissions increased with water content and showed higher N2O losses in sandy soils. In summary it can be stated that the findings of the present thesis confirmed the high fertilizer value of BS’s, caused by high concentrations of NH4+ and labile organic compounds such as readily available carbon. These attributes of BS’s are to a great extent independent of the input materials of biogas plants. However, considerably gaseous and leaching losses of N may occur especially at high moisture contents. The emissions of N2O after field application corresponded with those of animal slurries.

Nitrogen and carbon dynamics in grassland soils and plants after application of digestate

A better understanding of effects after digestate application on plant community, soil microbial community as well as nutrient and carbon dynamics is crucial for a sustainable grassland management and the prevention of species and functional diversity loss. The specific research objectives of the thesis were: (i) to investigate effects after digestate application on grass species and soil microbial community, especially focussing on nitrogen dynamic in the plant-soil system and to examine the suitability of the digestate from the “integrated generation of solid fuel and biogas from biomass” (IFBB) system as fertilizer (Chapter 3). (ii) to investigate the relationship between plant community and functionality of soil microbial community of extensively managed meadows, taking into account temporal variations during the vegetation period and abiotic soil conditions (Chapter 4). (iii) to investigate the suitability of IFBB-concept implementation as grassland conservation measure for meadows and possible associated effects of IFBB digestate application on plant and soil microbial community as well as soil microbial substrate utilization and catabolic evenness (Chapter 5). Taken together the results indicate that the digestate generated during the IFBB process stands out from digestates of conventional whole crop digestion on the basis of higher nitrogen use efficiency and that it is useful for increasing harvestable biomass and the nitrogen content of the biomass, especially of L. perenne, which is a common species of intensively used grasslands. Further, a medium application rate of IFBB digestate (50% of nitrogen removed with harvested biomass, corresponding to 30 50 kg N ha-1 a-1) may be a possibility for conservation management of different meadows without changing the functional above- and belowground characteristic of the grasslands, thereby offering an ecologically worthwhile alternative to mulching. Overall, the soil microbial biomass and catabolic performance under planted soil was marginally affected by digestate application but rather by soil properties and partly by grassland species and legume occurrence. The investigated extensively managed meadows revealed a high soil catabolic evenness, which was resilient to medium IFBB application rate after a three-year period of application.