Organic geochemistry of Jurassic-Cretaceous source rocks and oil seeps from the profile across the Adriatic-Dinaric carbonate platform

Organic geochemical and stable isotope investigations were performed to provide an insight into the depositional environments, origin and maturity of the organic matter in Jurassic and Cretaceous formations of the External Dinarides. A correlation is made among various parameters acquired from Rock-Eval, gas chromatography-mass spectrometry data and isotope analysis of carbonates and kerogen. Three groups of samples were analysed. The first group includes source rocks derived from Lower Jurassic limestone and Upper Jurassic ``Leme'' beds, the second from Upper Cretaceous carbonates, while the third group comprises oil seeps genetically connected with Upper Cretaceous source rocks. The carbon and oxygen isotopic ratios of all the carbonates display marine isotopic composition. Rock-Eval data and maturity parameter values derived from biomarkers define the organic matter of the Upper Cretaceous carbonates as Type I-S and Type II-S kerogen at the low stage of maturity up to entering the oil-generating window. Lower and Upper Jurassic source rocks contain early mature Type III mixed with Type IV organic matter. All Jurassic and Cretaceous potential source rock extracts show similarity in triterpane and sterane distribution. The hopane and sterane distribution pattern of the studied oil seeps correspond to those from Cretaceous source rocks. The difference between Cretaceous oil seeps and potential source rock extracts was found in the intensity and distribution of n-alkanes, as well as in the abundance of asphaltenes which is connected to their biodegradation stage. In the Jurassic and Cretaceous potential source rock samples a mixture of aromatic hydrocarbons with their alkyl derivatives were indicated, whereas in the oil seep samples extracts only asphaltenes were observed.

Elemental (C/N ratios) and isotopic (δ15N(org), δ13C(org)) compositions of sedimentary organic matter from a high-altitude mountain lake (Meidsee, 2661 m a.s.l., Switzerland): Implications for Lateglacial and Holocene Alpine landscape evolution

The deposition of Late Pleistocene and Holocene sediments in the high-altitude lake Meidsee (located at an altitude of 2661 m a.s.l. in the Southwestern Alps) strikingly coincided with global ice-sheet and mountain-glacier decay in the Alpine forelands and the formation of perialpine lakes. Radiocarbon ages of bottom-core sediments point out (pre-) Holocene ice retreat below 2700 m a.s.l., at about 16, 13, 10, and 9 cal. kyr BP. The Meidsee sedimentary record therefore provides information about the high-altitude Alpine landscape evolution since the Late Pleistocene/Holocene deglaciation in the Swiss Southwestern Alps. Prior to 5 cal. kyr BP, the C/N ratio and the isotopic composition of sedimentary organic matter (delta N-15(org), delta C-13(org)) indicate the deposition of algal-derived organic matter with limited input of terrestrial organic matter. The early Holocene and the Holocene climatic optimum (between 7.0 and 5.5 cal. kyr BP) were characterized by low erosion (decreasing magnetic susceptibility, chi) and high content of organic matter (C-org > 13 wt.%), enriched in C-13(org) (>-18 parts per thousand) with a low C/N (similar to 10) ratio, typical of modern algal matter derived from in situ production. During the late Holocene, there was a long-term increasing contribution of terrestrial organic matter into the lake (C/N > 11), with maxima between 2.4 and 0.9 cal. kyr BP. A major environmental change took place 800 years ago, with an abrupt decrease in the relative contribution of terrestrial organic material into the lake compared with aquatic organic material which subsequently largely dominated (C/N drop from 16 to 10). Nonetheless, this event was marked by a rise in soil erosion (chi), in nutrients input (N and P contents) and in anthropogenic lead deposition, suggesting a human disturbance of Alpine ecosystems 800 years ago. Indeed, this time period coincided with the migration of the Walser Alemannic people in the region, who settled at relatively high altitude in the Southwestern Alps for farming and maintaining Alpine passes.

Organic geochemistry across the Permian-Triassic transition at the Idrijca Valley, Western Slovenia

Bulk and molecular stable C isotopic compositions and biomarker distributions provide evidence for a diverse community of algal and bacterial organisms in the sedimentary organic matter of a carbonate section throughout the Permian-Triassic (P/Tr) transition at the Idrijca Valley, Western Slovenia. The input of algae and bacteria in all the Upper Permian and Lower Scythian samples is represented by the predominance of C-15-C-22 n-alkanes, odd C-number alkylcyclohexanes, C-27 steranes and substantial contents Of C-21-C-30 acyclic isoprenoids. The occurrence of odd long-chain n-alkanes (C-22-C-30) and C29 steranes in all the samples indicate a contribution of continental material. The decrease of C-org and C-carb contents, increase of Rock-Eval oxygen indices, and C-13-enrichment of the kerogen suggest a decrease in anoxia of the uppermost Permian bottom water. The predominance of odd C-number alkylcycloalkanes, C-27 steranes, and C-17 n-alkanes with delta(13)C values similar to-30parts per thousand, and C-13-enrichment of the kerogens in the lowermost Scythian samples are evidence of greater algal productivity. This increased productivity was probably sustained by a high nutrient availability and changes of dissolved CO2 speciation associated to the earliest Triassic transgression. A decrease Of Corg content in the uppermost Scythian samples, associated to a C-13-depletetion in the carbonates (up to 4parts per thousand) and individual n-alkanes (up to 3.4parts per thousand) compared to the Upper Permian samples, indicate lowering of the primary productivity (algae, cyanobacteria) and/or higher degradation of the organic matter. (C) 2003 Elsevier Ltd. All rights reserved.

Surface functionalization of alumina ceramic foams with organic ligands.

Different anchoring groups have been studied with the aim of covalently binding organic linkers to the surface of alumina ceramic foams. The results suggested that a higher degree of functionalization was achieved with a pyrogallol derivative - as compared to its catechol analogue - based on the XPS analysis of the ceramic surface. The conjugation of organic ligands to the surface of these alumina materials was corroborated by DNP-MAS NMR measurements.

De l'agriculture urbaine à la都市農業 (toshinogyo) Une analyse de leur émergence dans le cas de Genève et Tokyo

Il y a aujourd'hui un relatif consensus autour de l'émergence de l'agriculture urbaine. Les projets d'agriculture urbaine se développeraient, car il y aurait une nécessité à réinstaurer des relations entre l'urbain et l'agricole. Les dispositifs qui ont été mis en place par la modernité comme le zonage, l'économie de marché, les transports, l'usage de fertilisants ou les filières agroalimentaires auraient en effet fait disparaître ces relations qu'il s'agirait aujourd'hui de reconnecter. L'agriculture urbaine serait alors présentée comme une stratégie alternative à cette distinction. Elle serait le résultat de relations réciproques - et donc équivalentes - entre l'urbain et l'agricole. Elle serait alors à la fois urbaine et agricole. Nous pensons qu'il faut sortir aujourd'hui de cette conception d'agriculture urbaine. Nous remettons tout d'abord en question le fait que l'agriculture urbaine aurait pour objectif de reconnecter l'urbain et l'agricole. Cela présuppose qu'il n'y aurait plus de relations durant la modernité entre l'agricole et l'urbain. Or, comme le montre l'étude des aspects spatiaux, fonctionnels et sociaux de ces relations sous la modernité pour les cas de Genève et de Tokyo, ces relations existeraient toujours, voire même s'intensifieraient. Nous cherchons aussi à montrer qu'il faut faire évoluer l'idée que l'agriculture urbaine étant le résultat de relations réciproques entre l'urbain et l'agricole, elle se devait d'être à la fois urbaine et agricole. Dans les faits, l'agriculture urbaine apparaît plus souvent comme un projet de l'urbain au bénéfice de celui-ci, que comme un projet partagé entre l'urbain et l'agricole. Enfin, nous mettons en avant que l'agriculture urbaine n'aurait pas la capacité de reconnecter de façon effective l'agricole et l'urbain. Ainsi, l'agriculture urbaine n'est pas en mesure de se substituer aux dispositifs mis en place par la modernité. Elle ne peut rendre les villes autonomes en denrées alimentaires, établir des symbioses agro-urbaines ou remettre en question le système des filières agroalimentaires. Dans ce contexte, nous défendons la thèse que la conception d'agriculture urbaine doit aujourd'hui évoluer vers celle de toshinogyo. L'objectif est alors de rendre visibles les relations entre l'agricole et l'urbain. Les dispositifs mis en place sous la modernité n'ont pas eu pour effet de supprimer les relations entre l'urbain et l'agricole, mais de les rendre invisibles. Il s'agit aujourd'hui de leur redonner une visibilité. En devenant cette prise qui rend visibles ces relations, la toshinogyo ne serait alors plus tenue d'être urbaine et agricole à la fois, de même qu'elle ne s'opposerait pas aux dispositifs modernes, mais en serait complémentaire. Dans le contexte Genevois, le passage de l'agriculture urbaine à la toshinogyo est loin d'être encore évident. Dans le cas de Tokyo, l'optique de la toshinogyo est clairement affirmée et pourrait alors donner des amorces de pistes à suivre.

Characterization of volatile organic gunshot residues in fired handgun cartridges by headspace sorptive extraction

In forensic investigation of firearm-related cases, determination of the residual amount of volatile compounds remaining inside a cartridge could be useful in estimating the time since its discharge. Published approaches are based on following the decrease of selected target compounds as a function of time by using solid phase micro-extraction (SPME). Naphthalene, as well as an unidentified decomposition product of nitrocellulose (referred to as "TEA2"), are usually employed for this purpose. However, reliability can be brought into question given their high volatility and the low reproducibility of their extracted quantities. In order to identify alternatives and therefore develop improved dating methods, an extensive study on the composition and variability of volatile residues in nine different types of cartridges was carried out. Analysis was performed using headspace sorptive extraction (HSSE), which is a more exhaustive technique compared to SPME. 166 compounds were identified (several of which for the first time), and it was observed that the final compositional characteristics of each residue were strongly dependent on its source. Variability of single identified compounds within and between different types of cartridge, as well as their evolution over time, was also studied. Many explosion products containing up to 4 aromatic rings were found to be globally present in high proportions amongst residues. 27 of them (excluding naphthalene) also presented detectable decreases during the first 24 h. Therefore, they could be used as complementary target analytes in future dating methods.