Responses of three tropical seagrass species to CO2 enrichment

Increased atmospheric carbon dioxide leads to ocean acidification and carbon dioxide (CO2) enrichment of seawater. Given the important ecological functions of seagrass meadows, understanding their responses to CO2 will be critical for the management of coastal ecosystems. This study examined the physiological responses of three tropical seagrasses to a range of seawater pCO2 levels in a laboratory. Cymodocea serrulata, Halodule uninervis and Thalassia hemprichii were exposed to four different pCO2 treatments (442-1204 µatm) for 2 weeks, approximating the range of end-of-century emission scenarios. Photosynthetic responses were quantified using optode-based oxygen flux measurements. Across all three species, net productivity and energetic surplus (PG:R) significantly increased with a rise in pCO2 (linear models, P < 0.05). Photosynthesis-irradiance curve-derived photosynthetic parameters-maximum photosynthetic rates (P max) and efficiency (alpha) also increased as pCO2 increased (linear models, P < 0.05). The response for productivity measures was similar across species, i.e. similar slopes in linear models. A decrease in compensation light requirement (Ec) with increasing pCO2 was evident in C. serrulata and H. uninervis, but not in T. hemprichii. Despite higher productivity with pCO2 enrichment, leaf growth rates in C. serrulata did not increase, while those in H. uninervis and T. hemprichii significantly increased with increasing pCO2 levels. While seagrasses can be carbon-limited and productivity can respond positively to CO2 enrichment, varying carbon allocation strategies amongst species suggest differential growth response between species. Thus, future increase in seawater CO2 concentration may lead to an overall increase in seagrass biomass and productivity, as well as community changes in seagrass meadows.

Fisiologia e formação de partículas lipídicas durante o crescimento da levedura Yarrowia lipolytica IMUFRJ 50682.

A levedura Yarrowia lipolytica tem sido muito investigada, especialmente por ser um microrganismo oleaginoso, ou seja, capaz de acumular grandes quantidades de lipídios, o que ocorre majoritariamente em organelas denominadas partículas lipídicas. Estes lipídios apresentam várias potenciais aplicações biotecnológicas, como por exemplo na produção de óleo microbiano (single cell oil) e na produção de biodiesel. Durante este projeto de mestrado, objetivou-se estudar a fisiologia de duas linhagens da levedura Y. lipolytica, sendo uma tradicionalmente estudada pela comunidade científica internacional (linhagem w29) e outra isolada da Baía da Guanabara, no Rio de Janeiro (linhagem IMUFRJ 50682). Foram realizados cultivos em frascos agitados tipo Erlenmeyer com defletores tampados com algodão (volume total 500 mL, volume de meio 100 mL, 28 oC e 200 rotações por minuto), durante os quais foi possível: 1) escolher um meio de cultivo de composição totalmente definida, com tiamina como único fator de crescimento, adequado a estudos de fisiologia quantitativa com esta levedura; 2) verificar que Y. lipolytica não é capaz de crescer com sacarose ou xilose como única fonte de carbono; 3) verificar que Y. lipolytica cresce com velocidade específica de crescimento máxima (Máx) de 0,49 h-1 num meio complexo contendo glicose, extrato de levedura e peptona (meio YPD), 0,31 h-1 em meio definido com glicose como única fonte de carbono e 0,35 h-1 no mesmo meio, mas com glicerol como única fonte de carbono, sem excreção de metabólitos para o meio de cultivo; 4) verificar que ocorreu limitação por oxigênio nos cultivos em frasco agitado, sendo este o motivo pelo qual as células deixaram de crescer exponencialmente; 5) verificar que o uso de ureia, em vez de sulfato de amônio, como fonte de nitrogênio, contribui para uma variação menor do pH durante os cultivos, sem prejuízo ao crescimento da levedura; 6) observar que, ao se restringir a oferta de nitrogênio à levedura (aumento da relação C/N inicial no meio de 12,6 para 126), as células têm sua morfologia alterada e apresentam maior quantidade de partículas lipídicas; 7) determinar uma composição elementar para a biomassa de Y. lipolytica (CH1,98O0,58N0,13), em que os átomos de carbono encontram-se em média mais reduzidos do que na biomassa de leveduras como Saccharomyces cerevisiae e Dekkera bruxellensis. Foram também realizados cultivos em biorreator em batelada (1 L de volume útil, 28 oC, aerobiose plena e pH controlado em 5,0), durante os quais foi possível: a) estabelecer um protocolo de cultivo para Y. lipolytica em biorreator (que envolvem agitação mecânica, aeração e uso de anti-espumante, entre outras diferenças em relação aos cultivos em frasco); b) confirmar os valores dos principais parâmetros fisiológicos apresentados por esta levedura, anteriormente obtidos a partir de cultivos em frasco; c) confirmar que o fator de conversão de substrato a células (Yx/s) é maior para cultivos realizados com glicerol como fonte única de carbono (0,53 g/g para a linhagem IMUFRJ 50682), do que com glicose (0,48 g/g para a mesma linhagem). Finalmente, cultivos realizados em quimiostato com glicerol como fonte de carbono e energia, limitados por amônio (fonte de nitrogênio, relação C/N 126), às vazões específicas de 0,25 h-1 e 0,15 h-1, permitiram observar que o número de partículas lipídicas por célula de Y. lipolytica permaneceu em torno de 2 em ambas as situações e houve uma diminuição no teor de nitrogênio nas células quando a velocidade específica de crescimento diminuiu de 0,25 para 0,15 h-1.

Estudo da cinética de crescimento de células de inseto Sf21 e infecção por baculovírus Anticarsia gemmatalis (AgMNPV) para a produção de bioinseticida.

O interesse em estudar o cultivo das células de inseto está relacionado entre outros usos a sua utilização na produção de biopesticidas. Há muitos anos os pesticidas químicos vêm contribuindo no controle de pragas na agricultura. Entretanto, o uso desses compostos prolongadamente tem resultado na seleção de insetos resistentes e em poluição ambiental. Diante disso, torna-se necessário o desenvolvimento e aprimoramento dos bioinseticidas. No Brasil, o baculovírus Anticarsia gemmatalis multiple nucleopolyhedrovirus (AgMNPV) foi o principal agente de controle biológico da praga da soja Anticarsia gemmatalis. Assim, estudos que viabilizem a produção desses vírus in vitro possibilitariam uma produção mais controlada e de melhor qualidade desses biopesticidas. Neste trabalho, investigou-se a suscetibilidade à infecção por AgMNPV de diferentes linhagens celulares de Sf21 e o crescimento dessas células em diferentes sistemas: cultivos em schotts, em spinner e em biorreator, variando-se a idade do inóculo (IA) e a concentração celular inicial (X0). Constatou-se variação no perfil de infecção das linhagens, sendo as linhagens mais adequadas para a produção de bioinseticida as linhagens de Sf21 denominadas EMBRAPA, UFRN e GibcoG, uma vez que estas apresentaram mais do que 40 % das células com poliedros em cultivos em suspensão, enquanto a linhagem denominada GibcoSF teve menos de 2 % das células infectadas com poliedros. Ao se estudar o efeito do número de subcultivos na morfologia e crescimento celular, foi averiguado um aumento no diâmetro de 10 % e no volume de 26 % das células UFRN em relação às células GibcoSF. Além disso, o crescimento das células UFRN foi 49% menor do que das células GibcoSF. Quando realizado o Delineamento Composto Central Rotacional (DCCR) para se analisar o efeito da IA e a X0 na taxa de crescimento específica máxima (?max) e na concentração celular máxima (Xvmax) em cultivos em schott com células UFRN, obteve-se um modelo empírico. Quando analisadas as variáveis IA e X0 separadamente, não foram encontradas diferenças significativas para as respostas Xvmax e ?max em relação a X0. Para a IA, entretanto, obteve-se os resultados mais satisfatórios para os inóculos com IA de 72 e 96 horas: Xvmax de 5,97.106 cel/mL e 5,99.106 cel/mL, e ?max de 0,70 dia-1 e 0,63 dia-1, respectivamente. Nos cultivos em spinner com células UFRN, foi observada a formação de grumos, o que levou a Xvmax de 2,00.106 cel/mL. No cultivo em biorreator com células UFRN, foi obtido um Xvmax de 6,21.106 cel/mL, ?max de 0,70 dia-1, Qo2 na fase exponencial de 67,3 ± 3,6 .10-18 molO2/cel/s, rendimento de glicose em célula igual a 1,0.109 cel/g de glicose e um rendimento de glutamina em células de 3,0.109 cel/mL. Comprovou-se, portanto, a existência de alterações na infecção entre diferentes linhagens de Sf21; a importância do estado fisiológico da célula nos subcultivos, a ocorrência de mudanças no crescimento celular de acordo com os sistemas de cultivo e o efeito do número de subcultivos na morfologia e crescimento de células Sf21.

Catchment characteristics and soil and water chemistry of the San Francisco basin and subbasins, Ecuador

In this study, the Mean Transit Time and Mixing Model Analysis methods are combined to unravel the runoff generation process of the San Francisco River basin (73.5 km**2) situated on the Amazonian side of the Cordillera Real in the southernmost Andes of Ecuador. The montane basin is covered with cloud forest, sub-páramo, pasture and ferns. Nested sampling was applied for the collection of streamwater samples and discharge measurements in the main tributaries and outlet of the basin, and for the collection of soil and rock water samples. Weekly to biweekly water grab samples were taken at all stations in the period April 2007-November 2008. Hydrometric data, Mean Transit Time and Mixing Model Analysis allowed preliminary evaluation of the processes controlling the runoff in the San Francisco River basin. Results suggest that flow during dry conditions mainly consists of lateral flow through the C-horizon and cracks in the top weathered bedrock layer, and that all subcatchments have an important contribution of this deep water to runoff, no matter whether pristine or deforested. During normal to low precipitation intensities, when antecedent soil moisture conditions favour water infiltration, vertical flow paths to deeper soil horizons with subsequent lateral subsurface flow contribute most to streamflow. Under wet conditions in forested catchments, streamflow is controlled by near surface lateral flow through the organic horizon. Exceptionally, saturation excess overland flow occurs. By absence of the litter layer in pasture, streamflow under wet conditions originates from the A horizon, and overland flow.

Description of, and 238U, 234U, 232Th and 230Th measurements on a nodule from R/V Sonne station SO79_62KD, Central East Pacific Ocean

Two diagenetic manganese nodules from the Peru Basin were investigated by thermal ionization mass spectrometry and high resolution alpha spectrometry for uranium and thorium. The TIMS concentrations for nodule 62KD (63KG) vary as follows: 0.12-1.01 ppb (0.06-0.59) 230Th, 0.51-1.98 ppm (0.43-1.40) 232Th, 0.13-0.80 ppb (0.09-0.49) 234U, and 1.95-13.47 ppm (1.66-8.24) 238U. Both nodules have average growth rates of ~110 mm per million years. However, from the variations of excess 230Th with depth we estimate partial accumulation rates which range from 50 to 400 mm per million years. The 234U dating method cannot be applied due to remobilization of U from the sediment and subsequent incorporation into the nodules' crystal lattice, reflected by decay corrected 234U values far above the ocean water value. Sections of fast nodule growth are related to those layers having high Mn/Fe ratios (up to 200) and higher densities. As a possible explanation we develop a scenario that describes similar glacial/interglacial trends in both nodules as a record of regional changes of sediment and/or deep water chemistry.

Description and 238U, 234U, 232Th and 230Th measurements of the manganese nodule analysed from station SO79_63KG, R/V SONNE

Thorium and uranium isotopes were measured in a diagenetic manganese nodule from the Peru basin applying alpha- and thermal ionization mass spectrometry (TIMS). Alpha-counting of 62 samples was carried out with a depth resolution of 0.4 mm to gain a high-resolution Th-230(excess) profile. In addition, 17 samples were measured with TIMS to obtain precise isotope concentrations and isotope ratios. We got values of 0.06-0.59 ppb (Th-230), 0.43-1.40 ppm (Th-232), 0.09-0.49 ppb (U-234) and 1.66-8.24 ppm (U-238). The uranium activity ratio in the uppermost samples (1-6 mm) and in two further sections in the nodule at 12.5+/-1.0 mm and 27.3-33.5 mm comes close to the present ocean wa ter value of 1.144+/-0.004. In two other sections of the nodule, this ratio is significantly higher, probably reflecting incorporation of diagenetic uranium. The upper 25 mm section of the Mn nodule shows a relatively smooth exponential decrease in the Th-230(excess) concentration (TIMS). The slope of the best fit yields a growth rate of 110 mm/Ma up to 24.5 mm depth. The section from 25 to 30.3 mm depth shows constant Th-230(excess) concentrations probably due to growth rates even faster than those in the top section of the nodule. From 33 to 50 mm depth, the growth rate is approximately 60 mm/Ma. Two layers in the nodule with distinct laminations (11-15 and 28-33 mm depth) probably formed during the transition from isotopic stage 8 to 7 and in stage 5e, respectively. The Mn/Fe ratio shows higher values during interglacials 5 and 7, and lower ones during glacials 4 and 6. A comparison of our data with data from adjacent sediment cores suggests (a) a variable sb supply of hydrothermal Mn to sediments and Mn nodules of the Peru basin or (b) suboxic conditions at the water sediment interface during periods with lower Mn/Fe ratios.

Structure and chemistry of TECHNO encrustations

Using as a starting point the results giving 'traditional' growth rates as determined by the decrease of radioelements (part I) and the hypothesis of rapid formation, the different mineralogical, structure and chemical characteristics of the sample have been studied to try to understand the possible mode of formation of this encrustation. A rapid formation would account for (1) the very peculiar structure of the sample composed of oriented botryoids and the bundle-like structure of the outermost oxide layer; (2) the fact that this sample represents a substitution of a preexisting hyaloclastite; (3) the different chemical gradients, mainly iron, thorium and uranium; (4) the fact that this sample which cannot have been maintained at the sediment-water interface by bioturbation is not covered by a great thickness of sediments. On the other hand, an unsolved problem remains: Why different radionuclides used for dating give growth rates of the same order of magnitude and different 'exposition ages'.

Volume changes of Jacobshavn Isbrae between 1985, 1997 and 2007

Following three decades of relative stability, Jakobshavn Isbrae, West Greenland, underwent dramatic thinning, retreat and speed-up starting in 1998. To assess the amount of ice loss, we analyzed 1985 aerial photos and derived a 40 m grid digital elevation model (DEM). We also obtained a 2007 40 m grid SPOT DEM covering the same region. Comparison of the two DEMs over an area of ~4000 km**2 revealed a total ice loss of 160 ± 4 km**3, with 107 ± 0.2 km**3 in grounded regions (0.27 mm eustatic sea-level rise) and 53 ± 4 km**3 from the disintegration of the floating tongue. Comparison of the DEMs with 1997 NASA Airborne Topographic Mapper data indicates that this ice loss essentially occurred after 1997, with +0.7 ± 5.6 km**3 between 1985 and 1997 and -160 ± 7 km**3 between 1997 and 2007. The latter is equivalent to an average specific mass balance of -3.7 ± 0.2 m/a over the study area. Previously reported thickening of the main glacier during the early 1990s was accompanied by similar-magnitude thinning outside the areas of fast flow, indicating that the land-based ice continued reacting to longer-term climate forcing.

Mass balance of Stubacher Sonnblickkees, Hohe Tauern Range, Eastern Alps, Austria

Results of the direct, glaciological determination of the mass budget of Stubacher Sonnblick kees in the Hohe Tauern group are summarized for the years 1971/72 through 1977/78. Tabulation of budget quantities, accumulation and ablation areas and distribution of budget terms for 50 m altitude intervals is supplemented by comments on observations and field work.

Research on the BET surface area and packing of molecules on the activated carbon

Adsorption of different aromatic compounds (two of them are electrolytes) onto an untreated activated carbon (F100) is investigated. The experimental isotherms are fitted into Langmuir homogenous and heterogeneous Model. Theoretical maximum adsorption capacities that are based on the BET surface area of the adsorbent cannot be close to the real value. The affinity and the heterogeneity of the adsorption system observed to be related to the pK(a) of the solutes. The maximum adsorption capacity (Q(max)) of activated carbon for each solute dependent on the molecular area as well as the type of functional group attached on the aromatic compound and also pH of solution. The arrangement of the molecules on the carbon surface is not face down. Furthermore, it is illustrated that the packing arrangement is most likely edge to face (sorbate-sorbent) with various tilt angles. For characterization of the carbon, the N-2 and CO2 adsorption were used. X-ray Photoelectron Spectroscopy (XPS) measurement was used to surface elemental analysis of activated carbon.

Radiocarbon dating of mumiyo samples from Antarctica

Radiocarbon dating is a nimportant tool for reconstructing Late Quaternary paleoenvironmental history of the Antarctic continent. Because of the scarcity of datable material, new suitable substances are welcomed. We present here novel paleoenvironmental records subfosil stomach oil deposits (mumiyo). This waxy organic material is found in petrel breeding colonies, especialy in those of snow petrels, Pagodroma nivea. The substance is formed by acumulation and solidifica tion of stomach oil regurgitated for the purpose of defense. We demonstrate and outline the usefulnes and limitations of 14C dating mumiyo for determining dates of local ice retreat, moraines and petrel ocupation history.