Total dissolved organic carbon and total dissolved nitrogen in sediment pore water of the central Arctic Ocean collected during POLARSTERN cruise ARK-XXVII/3 from August-September 2012

During the RV Polarstern cruise ARK-XXVII/3 to the Arctic Ocean in summer 2012, when sea ice declined to a record minimum bottom, water and sediment pore water samples were collected with a TV-guided multicorer at stations in the Nansen and Amundsen basin. 50 ml sediment pore water samples were collected from 0-1, 1-5 and 5-10 cm sediment depths from up to 4 parallel sediment cores at each station. Additionally, overlying bottom waters were carefully collected from undisturbed sediment cores. Acidified pore water samples (pH2) were used for analysis of DOC and TDN concentrations. The measurements were performed by hand injection via catalytic oxidation at high temperature on a TOC-V Shimadzu instrument.

Dissolved organic carbon concentrations, amino sugar concentrations and highly significantly correlating FT-ICR mass peak magnitudes obtained from solid phase extracted marine dissolved organic matter during POLARSTERN cruise ANT-XXV/1

Dissolved organic matter (DOM) was extracted with solid phase extraction (SPE) from 137 water samples from different climate zones and different depths along an Eastern Atlantic Ocean transect. The extracts were analyzed with Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) with electrospray ionization (ESI). D14C analyses were performed on subsamples of the SPE-DOM. In addition, the amount of dissolved organic carbon was determined for all water and SPE-DOM samples as well as the yield of amino sugars for selected samples. Linear correlations were observed between the magnitudes of 43% of the FT-ICR mass peaks and the extract D14C values. Decreasing SPE-DOM D14C values went along with a shift in the molecular composition to higher average masses (m/z) and lower hydrogen/carbon (H/C) ratios. The correlation was used to model the SPE-DOM D14C distribution for all 137 samples. Based on single mass peaks a degradation index was developed to compare the degradation state of marine SPE-DOM samples analyzed with FT-ICR MS. A correlation between D14C, degradation index, DOC values and amino sugar yield supports that SPE-DOM analyzed with FT-ICR MS reflects trends of bulk DOM. A relative mass peak magnitude ratio was used to compare aged SPE-DOM and fresh SPE-DOM regarding single mass peaks. The magnitude ratios show a continuum of different reactivities for the single compounds. Only few of the compounds present in the FT-ICR mass spectra are expected to be highly degraded in the oldest water masses of the Pacific Ocean. All other compounds should persist partly thermohaline circulation. Prokaryotic (bacterial) production, transformation and accumulation of this very stable DOM occurs probably primarily in the upper ocean. This DOM is an important contribution to very old DOM, showing that production and degradation are dynamic processes.

Emissão de gases de efeito estufa e estoque de carbono no sistema solo-planta em função do sistema de produção e da aplicação superficial de corretivo da acidez

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

QUANTIDADE DE FÓSFORO EXTRAÍDO PELAS SOLUÇÕES DE MEHLICH-1 E MEHLICH-3 EM RAZÃO DE DIFERENTES VELOCIDADES DE AGITAÇÃO, TEMPOS DE CONTATO E TEMPERATURAS

A extração de fósforo do solo pode ser comprometida pelas condições em que a análise é realizada e isso pode explicar a variabilidade nos resultados encontrados. O objetivo deste trabalho foi verificar a influência de desvios na velocidade de agitação, no tempo de contato e na temperatura sobre a extração do P pelos extratores Mehlich-1 (M-1) e Mehlich-3 (M-3) em amostras de solo. O estudo foi conduzido por meio de três experimentos executados com 11 amostras de solo provenientes da camada arável de Latossolo, Neossolo, Argissolo, Cambissolo, Planossolo, que são representativas das regiões geomorfológicas do Planalto e da Depressão Central do Estado do Rio Grande do Sul. Para todos os experimentos, adotou-se o delineamento experimental inteiramente casualizado em esquema fatorial 2 × 5 × 11, sendo dois extratores, cinco velocidades, temperaturas ou tempos de contato solo/solução e 11 tipos de solo, com quatro repetições. No primeiro experimento, a mistura solo:solução foi agitada em 80, 100, 120, 140 e 160 oscilações por min (opm). No segundo, após a agitação por 5 min, a mistura solo:solução foi deixada em repouso por períodos de tempo de oito, 12, 16, 20 e 24 h para retirada dos extratos. No terceiro, a temperatura de execução de todo o protocolo de análises foi mantida constante em 15, 20, 25, 30 e 35 °C. O aumento na velocidade de agitação de 120 até 160 opm aumentou a quantidade de P extraído pelos extratores. O aumento no tempo de contato antes da extração da alíquota elevou as quantidades de P extraído pelo M-1 e diminuiu para o M-3. Variações na temperatura não influenciaram significativamente o extrator M-1, mas o M-3 foi mais sensível a variações. Uma padronização na velocidade de agitação, no tempo de repouso e uma climatização dos laboratórios tornam-se necessárias para diminuir a interferência causada sobre as quantidades de P extraído pelos métodos M-1 e M-3 em amostras de solo.

1.° Historiae Romanae breviarium, secundùm Titum Livium per libros et decadas ordinatum. — 2.° C. J. Caesaris ad Oppium Cornelium epistolae duae de suis cum Pompeio rebus. — 3.° Anonymi chronicon ab orbe condito ad annum Christi 1300.

Mazarinaeus

1.° Anonymi in Hippocratis librum de natura hominis commentarius. — 2.° Trium Galeni librorum de temperamentis epitome. — 3.° Compendium de epidemia, per collegium Facultatis Medicorum Parisiis ordinatum anno 1348. et è duobus manuscriptis exscriptum, altero Sanvictoriensi, altero Renati Morelli, Medici. — 4.° Tractatus de epidemia, à quodam practico de Montepessulano conscriptus anno 1349.

Mentellianus

Adattamento e acclimatazione a diverse temperature di lieviti psicrofili obbligati e facoltativi e di lieviti mesofili. Studio della produzione di acidi grassi polinsaturi omega-3 e omega-6 per via fermentativa.

Adaptation and acclimation to different temperatures of obligate psychrophilic, facultative psychrophilic and mesophilic yeasts. Production of ω-3 and ω-6 polyunsaturated fatty acids by fermentative way. Obligate psychrophilic, facultative psychrophilic and mesophilic yeasts were cultured in a carbon rich medium at different temperatures to investigate if growth parameters, lipid accumulation and fatty acid composition were adaptive and/or acclimatory responses. Acclimation of facultative psychrophiles and mesophiles to lower temperature negatively affected their specific growth rate. Obligate psychrophiles exhibited the highest biomass yield (YX/S), followed by facultative psychrophiles, then by mesophiles. The growth temperature did not influence the YX/S of facultative psychrophiles and mesophiles. Acclimation to lower temperature caused the increase in lipid yield (YL/X) in mesophilic yeasts, but did not affect YL/X in facultative psychrophiles. Similar YL/X were found in both facultative and obligated psychrophiles, suggesting that lipid accumulation is not a distinctive character of adaptation to permanently cold environments. The extent of unsaturation of fatty acids was one major adaptive feature of the yeasts which colonize permanently cold ecosystems. Remarkable amounts of α-linolenic acid were found in obligate psychrophiles at the expenses of linoleic acid, whereas it was generally scarce or absent in all the others strains. Increased unsaturation of fatty acids was also an acclimatory response of mesophiles and facultative psychrophiles to lower temperature. It’s well known that omega-3 polyunsaturated fatty acids (PUFAs) display a variety of beneficial effects on various organ systems and diseases, therefore a process for the microbial production of omega-3 PUFAs would be of great interest. This work sought also to investigate if one of the better psychrophilic yeast, Rhodotorula glacialis DBVPG 4785, stimulated by acclamatory responses, produced omega-3 PUFAs. In fact, the adaptation of psychrophilic yeasts to cold niches is related to the production of higher amounts of lipids and to increased unsaturation degree of fatty acids, presumably to maintain membrane fluidity and functionality at low temperatures. Bioreactor fermentations of Rhodotorula glacialis DBVPG 4785 were carried out at 25, 20, 15, 10, 5, 0, and -3°C in a complex medium with high C:N ratio for 15 days. High biomass production was attained at all the temperatures with a similar biomass/glucose yield (YXS), between 0.40 and 0.45, but the specific growth rate of the strain decreased as the temperature diminished. The coefficients YL/X have been measured between a minimum of 0.50 to a maximum of 0.67, but it was not possible to show a clear effect of temperature. Similarly, the coefficient YL/S ranges from a minimum of 0.22 to a maximum of 0.28: again, it does not appear to be any significant changes due to temperature. Among omega-3 PUFAs, only α-linolenic acid (ALA, 18:3n-3) was found at temperatures below to 0°C, while, it’s remarkable, that the worthy arachidonic acid (C20:4,n-6), stearidonic acid (C20:4,n-3) C22:0 and docosahexaenoic acid (C22:6n-3) were produced only at the late exponential phase and the stationary phase of batch fermentations at 0 and -3°C. The docosahexaenoic acid (DHA) is a beneficial omega-3 PUFA that is usually found in fatty fish and fish oils. The results herein reported improve the knowledge about the responses which enable psychrophilic yeasts to cope with cold and may support exploitation of these strains as a new resource for biotechnological applications.