I investigated how land use and human activities affect the sources and cycling of carbon (C) in subtropical rivers. Annually rivers receive a large amount of terrestrial C, process a portion of this C and return it to the atmosphere as CO 2 . The rest is transported to the ocean. Land use and human activities can affect the sources and fate of terrestrial C in rivers. However, studies on these effects are limited, especially in the humid subtropics. I combined measurements of the partial pressure of dissolved CO 2 (pCO 2 ), C isotopes ( 13 C and 14 C) and solid-state 13 C nuclear magnetic resonance (NMR) to study C cycling in three subtropical rivers in Texas, two small rivers (Buffalo Bayou and Spring Creek) and a midsized river (the Brazos). My pCO 2 data show that small humid subtropical rivers are likely a large source of atmospheric CO 2 in the global C cycle. My measurements on pCO 2 , C isotopic and chemical composition of dissolved inorganic C (DIC) and particulate organic C (POC) revealed four types of effects of land use and human activities on river C cycling. First, oyster shells and crushed carbonate minerals used in road construction are being dissolved and slowly drained into Buffalo Bayou and the lower Brazos and may be a source of river CO 2 released to the atmosphere. Second, river damming and nutrient input from urban treated wastewater stimulate algal growth and reduce CO 2 evasion of the middle Brazos. Third, urban treated wastewater discharge is adding old POC to the middle Brazos and decomposition of the old POC adds to the old riverine DIC pool. Fourth, agricultural activities coupled with high precipitation enhance loss of old organic C (OC) from deep soils to the lower Brazos, and decomposition of the old soil OC contributes to the old CO 2 evaded. I document for the first time the river C cycling effects of the use of carbonate minerals in construction and the riverine discharge of urban wastewater. Results presented here indicate the need to study disturbed river systems to better constrain the global C budget.

Diss. (sammanfattning) Uppsala : Sveriges lantbruksuniv., 2009. / Härtill 4 uppsatser.

No description available.

Inland waters are important systems for transforming, storing and transporting carbon along the aquatic continuum, but also by emitting carbon dioxide (CO2) and methane (CH4) to the atmosphere. In light of the last decades observed increase in dissolved organic carbon (DOC) in many inland waters across the northern hemisphere, a logical question arise whether other aquatic carbon species display similar trends. This study examined the measured concentrations of dissolved inorganic carbon (DIC) in a boreal catchment over a 14-year period. The objectives were to determine changes in DIC concentration over time and try to explain the causes for the observed changes. Data from 15 mostly forested sub-catchments were analyzed, both over the full time period, and grouped by season. Over the full 14-year period, only two of the sites exhibited significant trends in DIC concentration, both being negative. However, by seasonally grouping the data distinct patterns for the different seasons emerged. The autumn and winter data displayed no significant trends, whereas the spring flood data showed significant negative trends for almost all sites (14 out of 15). The summer data showed significant negative trends for seven sites, and positive for one site. The DIC concentration data were expectedly positively correlated with pH across most sites (13 out of 15). The correlation with DOC was negative for most sites (11 out of 15), possibly indicating different origins of the different carbon species. The DIC concentration was also negatively correlated with discharge for most sites (13 out of 15), suggesting a diluting effect with increased discharge. In conclusion, significant negative trends were observed during the spring flood and summer periods. Although the cause of these trends will require further investigation, the correlation analysis showed that the DIC concentration was closely related to the catchment hydrology. This suggests changes in terrestrial source areas where DIC is mobilized during spring and summer, and that these changes might continue during altered hydrometeorological conditions. The differences in DIC trends between sub-catchments further show the variability of the boreal landscape and highlight the need for local-scale process understanding when scaling to larger landscape units. We further conclude that trends in DIC concentration do not follow observed DOC changes over time, suggesting that DIC and DOC exports are mechanistically decoupled.

No description available.

No description available.

Natural archives such as lake sediments allow us to assess contemporary ecosystem responses to climate and environmental changes in a long-term context beyond the few decades to at most few centuries covered by monitoring or historical data. To achieve a comprehensive view of the changes preserved in sediment records, multi-proxy studies – ideally in high resolution – are necessary. However, this combination of including a range of analyses and high resolution constrains the amount of material available for analyses and increases the analytical costs. Infrared spectroscopic methods are a cost-efficient alternative to conventional methods because they offer a) a simple sample pre-treatment, b) a rapid measurement time, c) the non- or minimal consumption of sample material, and d) the potential to extract quantitative and qualitative information about organic and inorganic sediment components from a single measurement. The main objective of this doctoral thesis was twofold. The first part was to further explore the potential of Fourier transform infrared (FTIR) and visible-near infrared (VNIR) spectroscopy in paleolimnological studies as a) an alternative tool to conventional methods for quantifying biogenic silica (bSi) – a common proxy of paleoproductivity in lakes – in sediments and b) as a tool to infer past lake-water total organic carbon (TOC) levels from sediments. In a methodological study, I developed an independent application of FTIR spectroscopy and PLS modeling for determining bSi in sediments by using synthetic sediment mixtures with known bSi content. In contrast to previous models, this model is independent from conventional wet-chemical techniques, which had thus far been used as the calibration reference, and their inherent measurement uncertainties. The second part of the research was to apply these techniques as part of three multi-proxy studies aiming to a) improve our understanding of long-term element cycling in boreal and arctic landscapes in response to climatic and environmental changes, and b) to assess ongoing changes, particularly in lake-water TOC, on a centennial to millennial time scale. In the first applied study, high-resolution FTIR measurements of the 318-m long sediment record of Lake El’gygytgyn provided a detailed insight into long-term climate variability in the Siberian Arctic over the past 3.6 million years. Highest bSi accumulation occurred during the warm middle Pliocene (3.6-3.3 Ma), followed by a gradual but variable decline, which reflects the first onset of glacial periods and then the finally full establishment of glacial–interglacial cycles during the Quaternary. The second applied study investigated the sediment record of Torneträsk in subarctic northern Sweden also in relation to climate change, but only over the recent post-glacial period (~10 ka). By comparing responses to past climatic and environmental forcings that were recorded in this large-lake system with those recorded in small lakes from its catchment, I determined the significance and magnitude of larger-scale changes across the study region. Three different types of response were identified over the Holocene: i) a gradual response to the early landscape development following deglaciation (~10000-5300 cal yr BP); ii) an abrupt but delayed response following climate cooling during the late Holocene, which occurred c. 1300 cal yr BP – about 1000-2000 years later than in smaller lakes from the area; and iii) an immediate response to the ongoing climate change during the past century. The rapid, recent response in a previously rather insensitive lake-ecosystem emphasizes the unprecedented scale of ongoing climate change in northern Fennoscandia. In the third applied study, VNIR-inferred lake-water TOC concentrations from lakes across central Sweden showed that the ongoing, observed increase in surface water TOC in this region was in fact preceded by a long-term decline beginning already AD 1450-1600. These dynamics coincided with early human land use activities in the form of widespread summer forest grazing and farming that ceased over the past century. The results of this study show the strong impact of past human activities on past as well as ongoing TOC levels in surface waters, which has thus far been underestimated. The research in this thesis demonstrates that infrared spectroscopic methods can be an essential component in high-resolution, multi-proxy studies of past environmental and climate changes.

Northern lakes and ponds are abundant and emit large amounts of the potent climate forcer methane to the atmosphere at rates prone to change with amplified Arctic warming. In spite of being important, fluxes from surface waters are not well understood. Long-term measurements are lacking and the dominant and irregular transport mode ebullition (bubbling) is rarely quantified, which complicate the inclusion of lakes and ponds in the global methane budget. This thesis focuses on variations in emissions on both local and regional scales. A synthesis of methane fluxes from almost all studied sites constrains uncertainties and demonstrates that northern lakes and ponds are a dominant source at high latitudes. Per unit area variations in flux magnitudes among different types of water bodies are mainly linked to water depth and type of sediment. When extrapolated, total area is key and thus post-glacial lakes dominate emissions over water bodies formed by peat degradation or thermokarst processes. Further, consistent multiyear measurements in three post-glacial lakes in Stordalen, northern Sweden, reveal that seasonal ebullition, primarily driven by fermentation of acetate, can be predicted by easily measured parameters such as temperature and heat energy input over the ice-free season. Assuming that most water bodies respond similarly to warming, this thesis also suggests that northern lakes and ponds will release substantially more methane before the end of the century, primarily as a result of longer ice-free seasons. Improved uncertainty reductions of both current and future estimates rely on increased knowledge of landscape-level processes related to changes in aquatic systems and organic loading with permafrost thaw, as well as more high-quality measurements, seldom seen in contemporary data. Sampling distributed over entire ice-free seasons and across different depth zones is crucial for accurately quantifying methane emissions from northern lakes and ponds. / <p>At the time of the doctoral defense, the following paper was unpublished and had a status as follows: Paper 4: Manuscript.</p>

The global carbon (C) balance is vulnerable to disturbances that alter terrestrial C uptake and loss. Moderate disturbances that kill or defoliate only a subset of canopy trees such as insect defoliation, drought, and age-related senescence are increasing in extent and frequency; yet, little is known about the effect of moderate disturbance on forest production and the mechanisms sustaining or supporting the recovery of the C cycle across a range of moderate disturbance severities. We used a broad plot-scale gradient of upper canopy tree mortality within a large manipulation of forest disturbance to: 1) quantify how aboveground wood net primary production (ANPPw) responds to a range of moderate disturbance severities and; 2) identify the primary mechanisms supporting ANPPw resistance or resilience following moderate disturbance. We found that ANPPw was highly resistant to moderate disturbance, with production levels sustained following the senescence of 9 to > 60 % of the upper canopy tree basal area. As upper canopy gap fraction increased with rising disturbance severity, greater light availability to the subcanopy enhanced leaf-level C uptake and the growth of this formerly light-limited canopy stratum, compensating for upper canopy production losses. As a result, whole-ecosystem production efficiency (ANPPw/LAI) increased at high levels of disturbance severity and leaf area loss. These findings provide a mechanistic explanation for sustained ANPPw across the disturbance gradient, in which the physiological and growth enhancement of undisturbed vegetation was proportional to the level of disturbance severity. Our results have important ecological and management implications, showing that moderate disturbances may minimally alter ecosystem functions such as C storage.

Mikrobielle Gemeinschaften werden direkt und indirekt von einem komplexen System verschiedenster Interaktionen zwischen biotischen und abiotischen Faktoren beeinflusst. So zum Beispiel von verschiedenen Pflanzenarten und ihren jeweiligen Eigenschaften, dem Nährstoffgehalt des Bodens, sowie dem pH-Wert. Im Gegenzug gestalten Mikroorganismen als wichtige Treiber der C- und N-Kreisläufe ihre Umwelt. Im Rahmen der vorliegenden Arbeit wurden mehrere Studien unter kontrollierten Feld- und Laborbedingungen, sowie unter natürlichen Bedingungen im Freiland durchgeführt, um verschiedene Einflussfaktoren zu bestimmen und den Grad ihres Einflusses zu ermitteln. Die Zusammensetzung der prokaryotischen Gemeinschaften in den verschiedenen Bodenproben wurden mit Hilfe phylogenetischer Marker, der 16S-rRNA Gene und der 16S-rRNA, analysiert. Die erhaltenen Amplikon-basierten Daten wurden dann prozessiert und die Indices für Artenvielfalt und Artenreichtum berechnet. Zusätzlich wurden Betadiversitätsanalysen durchgeführt, um Unterschiede in der Zusammensetzung der bakteriellen Gemeinschaft zwischen den verschiedenen Behandlungen sichtbar zu machen. Des Weiteren wurden die erhaltenen DGGE Profile für Clusteranalysen verwendet, um Ähnlichkeiten oder Unterschiede in der Struktur der Bakteriengemeinschaft zwischen den verschiedenen Behandlungen aufzuzeigen. Die vorliegende Arbeit gibt einen Einblick über den Einfluss der Baumarten, Baumartendiversität, des Laubes und des Probennahmezeitpunktes auf die Zusammensetzung und Diversität von Bakteriengemeinschaften in Böden. Die erhaltenen Daten zeigten, dass die Laubschicht der Haupteinflussfaktor auf die Zusammensetzung der bakteriellen Gemeinschaft in der Rhizosphäre von jungen Buchen und Eschen ist. Des Weiteren zeigte sich, das verschiedene Baumarten, deren Diversität, sowie saisonale Unterschiede nur einen geringen Einfluss auf die Struktur der bakteriellen Gemeinschaft haben. Zusätzlich konnte gezeigt werden, dass die mikrobielle Gemeinschaftsstruktur nicht signifikant von Buchen- und Eschensetzlingen beeinflusst wird, vermutlich aufgrund des frühen Entwicklungsstadiums der verwendeten Baumsetzlinge. Weiterhin konnte gezeigt werden, dass die Buchensetzlinge das Wachstum von Bakterien inhibierten, während das Pilzwachstum gefördert wurde. Dies wurde vermutlich hervorgerufen durch eine Verschiebung des pH-Wertes im Boden verursacht durch buchenspezifische Wurzelausscheidungen. Morphologisch unterschiedliche Baumarten beeinflussen die Struktur und Diversität mikrobieller Gemeinschaften auf verschiedenen Wegen. Die Analyse der Bakterien- und Pilzgemeinschaften in natürlichen Waldböden unter erwachsenen Buchen und Fichten zeigte einen signifikanten Einfluss der untersuchten Baumarten auf deren Zusammensetzung. Es konnte ein Einfluss des pH-Werts auf die Bakterien- und Pilzvielfalt unter den analysierten Fichtenbeständen gezeigt werden. Des Weiteren wurden die Auswirkungen hoher NO3- Depositionen auf die CH4 und N2O Gasflüsse und die aktiven Bakterien- und Archeengemeinschaften in gemäßigten Laubwaldböden mit Hilfe von Mesokosmen untersucht. Es konnte ein starker Effekt der NO3- Düngung auf die CH4 Aufnahmeraten und N2O Emissionen des gedüngten Laubwaldbodens gezeigt werden. Die N-Düngung hemmte die CH4 Aufnahme des Bodens, während die N2O Emission stieg. Die Bakteriengemeinschaft in den gedüngten Mikrokosmen verschob sich im Verlauf des Versuches in Richtung einer denitrifizierenden Gemeinschaft, dominiert durch die Gattung Rhodanobacter. Darüber hinaus konnte eine Reduzierung der bakteriellen Vielfalt und der CO2 Emission innerhalb der N-gedüngten Mikrokosmen gezeigt werden. Des Weiteren sanken die CO2 Emissionsraten in beiden Behandlungen im Verlauf des Experiments. Dies deutet auf eine reduzierte Aktivität der vorhandenen Bodenmikroorganismen hin, möglicherweise hervorgerufen durch eine C Limitierung des verwendeten Waldbodens. Obwohl eine Verschiebung in der relativen Häufigkeit der auftretenden nitrifizierenden Archeen der Gattung Nitrosotalea nachgewiesen wurde, konnte eine signifikante Veränderung in der Zusammensetzung der gesamten Archeengemeinschaft nicht beobachtet werden. Die Ergebnisse zeigten jedoch einen erheblichen Beitrag methylotropher, methanotropher und nitrifizierender Bakterien, welche in geringer Zahl auftraten, in Bezug auf die gemessene CH4 Aufnahme. Des Weiteren wurden die Auswirkungen der Anwesenheit von Ameisen und ihrer Aktivitäten auf die Aktivität und Vielfalt der mikrobiellen Gemeinschaften im Boden und Ameisennest untersucht. Ameisen transportierten den von Läusen gewonnenen Honigtau in den Boden und verursachten damit eine Abnahme der mikrobiellen Biomasse in der Streuschicht, während die δ15N-Signatur, die basale Atmung und die mikrobielle Biomasse im Boden erhöht wurden. Im Gegensatz dazu konnten mittels Cluster-Analyse der erstellten DGGE Profile keine deutlichen Unterschiede der mikrobiellen Gemeinschaftsstruktur in den untersuchten Mikrokosmen gezeigt werden. Im Gegensatz dazu beeinflusste die Nestbauaktivität und der Eintrag von organischen Substanzen in den Boden durch die Ameisen jedoch die Struktur der Bakteriengemeinschaften im Freiland. Die Cluster-Analyse der erhaltenen DGGE Profile zeigte Unterschiede in der Zusammensetzung der bakteriellen Gemeinschaft in Abhängigkeit vom Probenentnahmeort und der Ameisenaktivität. Außerdem konnte gezeigt werden, dass sich die Struktur der Bakteriengemeinschaft in den Ameisennestern von der im Umgebungsboden unterschied. Ein sekundäres Projekt dieser Arbeit war die Erfassung und der Vergleich der mikrobiellen Gemeinschaften in biologischen Bodenkrusten zweier unterschiedlicher Standorte in extrazonalen, trockenen Bergsteppen der nördlichen Mongolei. Die Studie zeigte deutliche Unterschiede in der mikrobiellen Gemeinschaftsstruktur der beiden Standorte, welche sich im Grad der Störung unterschieden.