Methylierung von anorganischem Quecksilber im Intestinaltrakt des Kompostwurms Eisenia foetida

Im Rahmen dieser Arbeit wurde die Methylierung von Quecksilber in Intestinaltrakt des Kompostwurms Eisenia foetida untersucht. Des Weiteren wurden aerobe und anaerobe Mikroorganismen aus dem Darmtrakt von Eisenia fotida isoliert, identifiziert und auf ihr Potential zur Methylierung von Quecksilber getestet. Die Bestimmung von Methylquecksilber erfolgte mittels GC-ICPMS (Gaschromatographie mit induktiv gekoppelter Plasma-Massenspektrometrie) und GC-AFS (Gaschromatographie- Atomfluoreszenzspektrometrie). Für die GC-ICPMS erfolgte die Quantifizierung des Methylquecksilbers mittels der Isotopenverdünnungsmethode. Die Extraktion des Methylquecksilbers aus dem Wurmgewebe erfolgte durch einen alkalischen Aufschluss mit TMAH (Tetramethylammoniumhydroxid) und anschließender Derivatisierung des Methylquecksilbers durch Natriumtetrapropylborat. Für die Extraktion des gebildeten Methylquecksilbers aus Bakterienkulturen wurde eine Extraktion mit einer methanolischen Kaliumhydroxidlösung verwendet. Wie bei dem Wurmgewebe wurde das Methylqueckilsber ebenfalls mit Natriumtetrapropylborat derivatisiert.rnrnFür die Untersuchung einer in vivo Methylquecksilberbildung in bodenlebenden Invertebraten wurde der Kompostwurm Eisenia foetida als Modellorganismus verwendet. Die Tiere wurden aus einer Kultur in einen Boden überführt, der mit anorganischem Quecksilber versetzt wurde. Nach zehn Tagen Inkubationszeit wurden die Würmer entnommen und das Methylquecksilber extrahiert. Um eine mögliche Methylierung von Quecksilber durch Bodenorganismen auszuschließen wurde sowohl steriles als auch unsteriles Bodenmaterial verwendet. In den Wurmproben aus dem unsterilen Bodenmaterial konnte eine Konzentration an Methylquecksilber von 17,4 ng/g Trockengewicht (Boden ohne Zugabe von Quecksilber) und 62,4 ng/g Trockengewicht (Boden mit Quecksilberzugabe). Bei den Wurmproben aus sterilem Bodenmaterial lag die Konzentration an Methylquecksilber bei 17,2 ng/g Trockengewicht (Boden ohne Zugabe von Quecksilber) und 51,9 ng/g Trockengewicht (Boden mit Quecksilberzugabe).rnrnBei den Bakterienkulturen konnte in Reinkulturen keine Methylierung von Quecksilber nachgewiesen werden. In einer fakultativ anaeroben Mischkultur konnte eine Methylierung von Quecksilber beobachtet werden. Für die Identifizierung der Mikroorganismen wurde die 16s rDNA mittels PCR amplifiziert und anschließend über eine DGGE aufgetrennt. Die Banden wurden ausgeschnitten und sequenziert. Dabei konnten drei Enterobacteriaceen identifiziert werden.rn

Chemical characterization of soil organic matter in an oligotrophic, subtropical, freshwater wetland system: Sources, diagenesis and preservation

Freshwater wetland soils of the Everglades were studied in order to assess present environmental conditions and paleo-environmental changes using organic geochemistry techniques. Organic matter in dominant vegetation, peat and marl soils was characterized by geochemical means. Samples were selected along nutrient and hydrology gradients with the objective to determine the historical sources of organic matter as well as the extent of its preservation. Effective molecular proxies were developed to differentiate the relative input of organic matter from different biological sources to wetland soils. Thus historical vegetation shifts and hydroperiods were reconstructed using those proxies. The data show good correlations with historical water management practices starting at the turn of the century and during the mid 1900's. Overall, significant shortening of hydroperiods during this period was observed. The soil organic matter (SOM) preservation was assessed through elemental analysis and molecular characterizations of bulk 13C stable isotopes, solid state 13C NMR spectroscopy, UV-Vis spectroscopy, and tetramethyl ammonium hydroxide (TMAH) thermochemolysis-GC/MS. The relationship of the environmental conditions and degradation status of the soil organic matter (SOM) among the sites suggested that both high nutrient levels and long hydroperiod favor organic matter degradation in the soils. This is probably the result of an increase in the microbial activity in the soils which have higher nutrient levels, while longer hydroperiods may enhance physical/chemical degradation processes. The most significant transformations of biomass litter in this environment are controlled by very early physical/chemical processes and once the OM is incorporated into surface soils, the diagenetic change, even over extended periods of time is comparatively minimal, and SOM is relatively well preserved regardless of hydroperiod or nutrient levels. SOM accumulated in peat soils is more prone to continued degradation than the SOM in the marl soils. The latter is presumably stabilized early on through direct air exposure (oxidation) and thus, it is more refractory to further diagenetic transformations such as humification and aromatization reactions.

Quantitative and Qualitative Aspects of Dissolved Organic Carbon Leached from Senescent Plants in an Oligotrophic Wetland

We conducted a series of experiments whereby dissolved organic matter (DOM) was leached from various wetland and estuarine plants, namely sawgrass (Cladium jamaicense), spikerush (Eleocharis cellulosa), red mangrove (Rhizophora mangle), cattail (Typha domingensis), periphyton (dry and wet mat), and a seagrass (turtle grass; Thalassia testudinum). All are abundant in the Florida Coastal Everglades (FCE) except for cattail, but this species has a potential to proliferate in this environment. Senescent plant samples were immersed into ultrapure water with and without addition of 0.1% NaN3 (w/ and w/o NaN3, respectively) for 36 days. We replaced the water every 3 days. The amount of dissolved organic carbon (DOC), sugars, and phenols in the leachates were analyzed. The contribution of plant leachates to the ultrafiltered high molecular weight fraction of DOM (>1 kDa; UDOM) in natural waters in the FCE was also investigated. UDOM in plant leachates was obtained by tangential flow ultrafiltration and its carbon and phenolic compound compositions were analyzed using solid state 13C cross-polarization magic angle spinning nuclear magnetic resonance (13C CPMAS NMR) spectroscopy and thermochemolysis in the presence of tetramethylammonium hydroxide (TMAH thermochemolysis), respectively. The maximum yield of DOC leached from plants over the 36-day incubations ranged from 13.0 to 55.2 g C kg−1 dry weight. This amount was lower in w/o NaN3 treatments (more DOC was consumed by microbes than produced) except for periphyton. During the first 2 weeks of the 5 week incubation period, 60–85% of the total amount of DOC was leached, and exponential decay models fit the leaching rates except for periphyton w/o NaN3. Leached DOC (w/ NaN3) contained different concentrations of sugars and phenols depending on the plant types (1.09–7.22 and 0.38–12.4 g C kg−1 dry weight, respectively), and those biomolecules comprised 8–34% and 4–28% of the total DOC, respectively. This result shows that polyphenols that readily leach from senescent plants can be an important source of chromophoric DOM (CDOM) in wetland environments. The O-alkyl C was found to be the major C form (55±9%) of UDOM in plant leachates as determined by 13C CPMAS NMR. The relative abundance of alkyl C and carbonyl C was consistently lower in plant-leached UDOM than that in natural water UDOM in the FCE, which suggests that these constituents increase in relative abundance during diagenetic processing. TMAH thermochemolysis analysis revealed that the phenolic composition was different among the UDOM leached from different plants, and was expected to serve as a source indicator of UDOM in natural water. Polyphenols are, however, very reactive and photosensitive in aquatic environments, and thus may loose their plant-specific molecular characteristics shortly. Our study suggests that variations in vegetative cover across a wetland landscape will affect the quantity and quality of DOM leached into the water, and such differences in DOM characteristics may affect other biogeochemical processes.

Ferulates and lignin structural composition in cork

The structure of lignin and suberin, and ferulic acid (FA) content in cork from Quercus suber L. were studied. Extractive-free cork (Cork), suberin, desuberized cork (Cork(sap)), and milled-cork lignins (MCL) from Cork and Cork(sap) were isolated. Suberin composition was determined by GC-MS/FID, whereas the polymers structure in Cork, Corksap, and MCL was studied by Py-TMAH and 2D-HSQC-NMR. Suberin contained 94.4% of aliphatics and 3.2% of phenolics, with 90% of omega-hydroxyacids and alpha,omega-diacids. FA represented 2.7% of the suberin monomers, overwhelmingly esterified to the cork matrix. Py-TMAH revealed significant FA amounts in all samples, with about 3% and 6% in cork and cork lignins, respectively. Py-TMAH and 2D-HSQC-NMR demonstrated that cork lignin is a G-lignin (>96% G units), with a structure dominated by beta-O-4' alkyl-aryl ether linkages (80% and 77% of all linkages in MCL and MCLsap, respectively), followed by phenylcoumarans (18% and 20% in MCL and MCLsap, respectively), and smaller amounts of resinols (ca. 2%) and dibenzodioxocins (1%). HSQC also revealed that cork lignin is heavily acylated (ca. 50%) exclusively at the side-chain gamma-position. Ferulates possibly have an important function in the chemical assembly of cork cell walls with a cross-linking role between suberin, lignin and carbohydrates.

Limiti e potenzialità della pirolisi analitica nella quantificazione delle microplastiche nell'ambiente

I rifiuti plastici, oggigiorno, rappresentano una grande minaccia per l’ambiente, per gli ecosistemi e per la salute umana, tanto da essere al centro della attenzione di numerosi studi. La preoccupazione maggiore è destata dalle microplastiche (frammenti di dimensioni inferiori ai 5 mm) che per la loro dimensione, la loro ubiquità e la loro lunga persistenza in ambiente possono interferire in maniera allarmante con gli organismi viventi. L’ampia gamma di dimensioni delle microplastiche e la natura complessa delle loro forme, colori e tipi di polimero hanno impedito ai ricercatori di sviluppare una classificazione coerente data anche dall'attuale assenza di una standardizzazione nel metodo di campionamento, preparazione e analisi del campione. Infatti lo studio di questa tipologia di inquinanti può essere effettuato mediante diverse metodologie analitiche sia di tipo spettroscopico che termico. Con questo studio si è cercato di valutare le potenzialità della pirolisi analitica (PyGCMS) per la quantificazione e identificazione di sei polimeri: PE, PP, PS, PET, PVC e PA. Tramite un attento confronto con la letteratura sono stati identificati alcuni punti critici nell'analisi quantitativa di alcuni polimeri in miscela. In particolare, la miscela PET/PA è risultata essere soggetta a grandi interferenze date dalla comparsa di prodotti pirolitici secondari che ne impediscono una corretta quantificazione. Inoltre un diverso rapporto dei polimeri nella miscela binaria va a modificare la risposta quantitativa rendendola non prevedibile. L’uso di derivatizzanti come agenti metilanti sembra ridurre alcuni effetti di interazione in pirolisi, ma non sembra essere così vantaggioso come riportato in altri studi. Complessivamente la pirolisi analitica risulta una tecnica applicabile alla identificazione e quantificazione delle microplastiche, ma emerge dallo studio una scarsa conoscenza in letteratura delle interazioni in fase pirolitica tra prodotti di pirolisi di diversi polimeri.