Biogenic emission of halocarbons

Within this doctoral thesis, biogenic emissions of several globally relevant halocarbons (methyl chloride, methyl bromide, methyl iodide, dibromomethane, chloroform and bromoform) have been investigated in different environments. An airborne study was focused on the tropical rainforest ecosystem, while shipborne measurements investigated naturally occurring oceanic plankton blooms. Laboratory experiments using dried plant material were made to elucidate abiotic production mechanisms occurring in organic matter. Airborne measurements over the tropical rainforest of Suriname and French Guyana (3 - 6 °N, 51 - 59 °W) revealed net fluxes of 9.5 (± 3.8 2σ) µg m-2 h-1 methyl chloride and 0.35 (± 0.15 2σ) µg m-2 h-1 chloroform emitted in the long dry season (October) 2005. An extrapolation of these numbers to all tropical forests helped to narrow down the range of the recently discovered and poorly quantified methyl chloride source from tropical ecosystems. The value for methyl chloride obtained (1.5 (± 0.6 2σ) Tg yr-1) affirms that the contribution of the tropical forest ecosystem is the major source in the global budget of methyl chloride. The extrapolated global net chloroform flux from tropical forests (56 (± 23 2σ) Gg yr-1) is of minor importance (5 - 10 %) compared to the global sources. A source of methyl bromide from this region could not be verified. The abiotic formation of methyl chloride and methyl bromide from dead plant material was tested in a laboratory study. The release from plant tissue representative of grassland, deciduous forest, agricultural areas and coastal salt marshes (hay, ash, tomato and saltwort) has been monitored. Incubations at different temperatures (25 - 50 °C) revealed significant emissions even at ambient temperature, and that the emissions increased exponentially with temperature. The strength of the emission was found to be additionally dependent on the availability of halide and the methoxyl group within the plant tissue. However, high water content in the plant material was found to inhibit methyl halide emissions. The abiotic nature of the reaction yielding methyl halides was confirmed by its high activation energy calculated via Arrhenius plots. Shipborne measurements of the atmospheric mixing ratios of methyl chloride, methyl bromide, methyl iodide, dibromomethane and bromoform have been conducted along a South Atlantic transect from the 27.01. - 05.02.2007 to characterize halocarbon emissions from a large-scale natural algae bloom encountered off the coast of Argentina. Mixing ratios of methyl chloride and methyl bromide were not significantly affected by the occurrence of the phytoplankton bloom. Emissions of methyl iodide, dibromomethane and bromoform showed pronounced mixing ratio variations, triggered by phytoplankton abundance. Methyl iodide was strongly correlated with dimethyl sulfide throughout the sampled region. A new technique combining satellite derived biomass marker (chlorophyll a) data with back trajectory analysis was successfully used to attribute variations in mixing ratios to air masses, which recently passed over areas of enhanced biological production.

Heiltraditionen und Biodiversität: Die traditionelle Medizin der Baatombu Nordbenins

Im Zentrum der vorliegenden Untersuchung steht die Nutzung von Medizinalpflanzen vor dem Hintergrund einer zurückgehenden Phytodiversität in Nordbenin. Die Dissertation ba-siert auf ethnologischen Forschungen, die in das interdisziplinäre Forschungsprojekt BIOTA (Biodiversity Monitoring Transect Analysis in Africa) eingebunden sind. Das BIOTA-Projekt untersucht die Wirkung menschlichen Handelns (insbesondere Nutzung) auf die Biodiversi-tät und versucht aus diesen Erkenntnissen Maßnahmen zum Erhalt der biologischen Vielfalt abzuleiten. Die vorliegende Studie basiert auf einem 13-monatigen Feldforschungsaufenthalt im Zeitraum von April 2004 bis August 2006 in der nordbeninischen Gemeinde Ouassa-Pehunco. Meine Informanten sind überwiegend traditionelle Heiler, mit denen ich standardi-sierte und offene Interviews durchführte, deren Behandlungsverfahren und Heilzeremonien ich teilnehmend beobachtete sowie dokumentierte und auf deren Initiative hin ich mich bei dem Aufbau eines Medizinalpflanzengartens einbrachte (cf. Kap. 1). In diesem Forschungsfeld situiere ich mich mit der Frage nach dem Einfluss einer verän-derten Pflanzenvielfalt auf die traditionelle medizinische Versorgung der Baatombu Nordbe-nins. Die Beantwortung dieser Frage erfolgt in mehreren Schritten. 1. Die Phytodiversität nimmt, wie von naturwissenschaftlicher Seite bestätigt, in der Region ab. 2. Lokale Heilkun-dige nehmen diesen Rückgang an verfügbaren Heilpflanzen ebenso wahr. 3. Die Abnahme der Pflanzenbestände führen die Heiler vor allem auf den Baumwollanbau und die demogra-fischen Entwicklungen der Region zurück - dies entspricht ebenfalls den Auffassungen von Naturwissenschaftlern, die eine Verdichtung der landwirtschaftlichen Bodennutzung fest-stellten. 4. Heilkundige und Heilpflanzenverkäuferinnen vermerken eine zunehmende Nach-frage nach lokaler Pflanzenmedizin aufgrund der steigenden Bevölkerungszahlen. 5. Die pflanzenbasierte Gesundheitsversorgung der lokalen Bevölkerung ist jedoch relativ gesi-chert, da die Heiler sich alternativ wirkender Medizinalpflanzen bedienen, ihre Therapiefor-men der veränderten Lage anpassen (z.B. geringere Dosierungen) und sie regelmäßig genutz-te Pflanzen im Medizinalpflanzengarten Guson wieder anpflanzen. Ein wichtiger Aspekt der Arbeit ist, dass die Heilpraktiken der Baatombu nicht allein auf naturheilkundlichem Erfahrungswissen beruhen, sondern in magisch-religiöse Vorstellungen eingebettet sind (cf. Kap. 2). Demzufolge untersuche ich die lokalen Krankheits- und Ge-sundheitsvorstellungen und die symbolischen Klassifikationen von Heilpflanzen und Krank-heiten (cf. Kap. 3). Ich stellte fest, dass nach Auffassung von Heilkundigen soziokulturelle Faktoren wie der Zeitpunkt und der Ort einer Sammlung sowie entsprechende Ernte-Rituale die medizinische Wirksamkeit von Pflanzen maßgeblich bedingen (cf. Kap. 5). Die Umwelt-klassifikation der Heiler (Landschafts- und Vegetationstypen) richtet sich demzufolge nach dem medizinischen Wert, den sie einer Heilpflanze zuschreiben (cf. Kap.4). Basierend auf diesen Erkenntnissen wurde von einigen engagierten Heilern und mit Un-terstützung von BIOTA, der GTZ und der Deutschen Botschaft der Medizinalpflanzengarten Guson eingerichtet, der eine Antwort auf die regionale Ressourcenverknappung darstellt und in seiner Anlage dem lokalen ökologischen und heilkundlichen Wissen der Heiler entspricht (cf. Kap. 6). Den Anwendungsbezug der Forschung nutzten die Heiler, um sich als Interes-sensgemeinschaft für den Erhalt der benötigten pflanzlichen Ressourcen einzusetzen.

Mediterranean-type climate in the South Aegean (Eastern Mediterranean) during the Late Miocene: Evidence from isotope and element proxies

The present-day climate in the Mediterranean region is characterized by mild, wet winters and hot, dry summers. There is contradictory evidence as to whether the present-day conditions (“Mediterranean climate”) already existed in the Late Miocene. This thesis presents seasonally-resolved isotope and element proxy data obtained from Late Miocene reef corals from Crete (Southern Aegean, Eastern Mediterranean) in order to illustrate climate conditions in the Mediterranean region during this time. There was a transition from greenhouse to icehouse conditions without a Greenland ice sheet during the Late Miocene. Since the Greenland ice sheet is predicted to melt fully within the next millennia, Late Miocene climate mechanisms can be considered as useful analogues in evaluating models of Northern Hemispheric climate conditions in the future. So far, high resolution chemical proxy data on Late Miocene environments are limited. In order to enlarge the proxy database for this time span, coral genus Tarbellastraea was evaluated as a new proxy archive, and proved reliable based on consistent oxygen isotope records of Tarbellastraea and the established paleoenvironmental archive of coral genus Porites. In combination with lithostratigraphic data, global 87Sr/86Sr seawater chronostratigraphy was used to constrain the numerical age of the coral sites, assuming the Mediterranean Sea to be equilibrated with global open ocean water. 87Sr/86Sr ratios of Tarbellastraea and Porites from eight stratigraphically different sampling sites were measured by thermal ionization mass spectrometry. The ratios range from 0.708900 to 0.708958 corresponding to ages of 10 to 7 Ma (Tortonian to Early Messinian). Spectral analyses of multi-decadal time-series yield interannual δ18O variability with periods of ~2 and ~5 years, similar to that of modern records, indicating that pressure field systems comparable to those controlling the seasonality of present-day Mediterranean climate existed, at least intermittently, already during the Late Miocene. In addition to sea surface temperature (SST), δ18O composition of coral aragonite is controlled by other parameters such as local seawater composition which as a result of precipitation and evaporation, influences sea surface salinity (SSS). The Sr/Ca ratio is considered to be independent of salinity, and was used, therefore, as an additional proxy to estimate seasonality in SST. Major and trace element concentrations in coral aragonite determined by laser ablation inductively coupled plasma mass spectrometry yield significant variations along a transect perpendicular to coral growth increments, and record varying environmental conditions. The comparison between the average SST seasonality of 7°C and 9°C, derived from average annual δ18O (1.1‰) and Sr/Ca (0.579 mmol/mol) amplitudes, respectively, indicates that the δ18O-derived SST seasonality is biased by seawater composition, reducing the δ18O amplitude by 0.3‰. This value is equivalent to a seasonal SSS variation of 1‰, as observed under present-day Aegean Sea conditions. Concentration patterns of non-lattice bound major and trace elements, related to trapped particles within the coral skeleton, reflect seasonal input of suspended load into the reef environment. δ18O, Sr/Ca and non-lattice bound element proxy records, as well as geochemical compositions of the trapped particles, provide evidence for intense precipitation in the Eastern Mediterranean during winters. Winter rain caused freshwater discharge and transport of weathering products from the hinterland into the reef environment. There is a trend in coral δ18O data to more positive mean δ18O values (–2.7‰ to –1.7‰) coupled with decreased seasonal δ18O amplitudes (1.1‰ to 0.7‰) from 10 to 7 Ma. This relationship is most easily explained in terms of more positive summer δ18O. Since coral diversity and annual growth rates indicate more or less constant average SST for the Mediterranean from the Tortonian to the Early Messinian, more positive mean and summer δ18O indicate increasing aridity during the Late Miocene, and more pronounced during summers. The analytical results implicate that winter rainfall and summer drought, the main characteristics of the present-day Mediterranean climate, were already present in the Mediterranean region during the Late Miocene. Some models have argued that the Mediterranean climate did not exist in this region prior to the Pliocene. However, the data presented here show that conditions comparable to those of the present-day existed either intermittently or permanently since at least about 10 Ma.