Bunodosine 391: An Analgesic Acylamino Acid from the Venom of the Sea Anemone Bunodosoma cangicum

A new acylamino acid, bunodosine 391 (BDS 391), was isolated from the venom of the sea anemone Bunodosoma cangicum. The structure was elucidated by spectroscopic analyses (2D NMR, ESIMS/MS) and verified by its synthesis. Intraplantar injection of BDS 391 into the hind paw of a rat induced a potent analgesic effect. This effect was not altered by naloxone (an opioid receptor antagonist), but was completely reversed by methysergide (a serotonin receptor antagonist), indicating that the effect is mediated by activation of serotonin receptors:

Biología de Anopheles (Kerteszia) neivai H., D. & K., 1913 (Diptera: Culicidae) en la Costa Pacifica de Colombia: IV - Estructura etárea y transmisión de malaria

Con el fin de determinar la dinamica de transmisión de malaria en el poblado de Charambirá (Chocó), Colombia, se estudió la estructura etárea de Anopheles neivai (reconocido vector en la Costa Pacífica) con base en su estado gonadotrófico. Se recolectaron mosquitos intradomiciliarmente durante el crepúsculo vespertino con cebos humanos y aspiradores bucales. Los mosquitos recolectados se mantuvieron en cajas cilíndricas de cartón con papel humedecido y dispensadores alimenticios hasta su disección al día siguiente. De los 200 mosquitos disecados entre septiembre y octubre de 1986,68 (34%) presentaban huellas de menos de tres oviposturas y los restantes (66%) habían efectuado al menos tres oviposturas. La diferencia entre el primer grupo considerado como mosquitos "no infectivos" y el segundo considerado como los "potencialmente infectivos" fue altamente significativa (X² = 10,68; P = 0,001). El 1,5% de A. neivai estudiados presentaban huellas correspondientes a 10 oviposturas mostrando una marcada longevidad y múltiples alimentaciones sanguíneas. Los resultados sugieren que existe un alto riesgo de contraer malaria en Charambirá durante el crepúsculo vespertino.

Proteómica microbiana: análise comparativa da bactéria redutora de sulfato Desulfovibrio desulfuricans ATCC 27774 e das actinobactérias Salinispora arenicola e Salinispora pacifica

As bactérias redutoras de sulfato (BRS) são um grupo diversificado de micro-organismos anaeróbios que obtêm energia a partir da redução dissimilativa do sulfato. Algumas espécies de BRS possuem versatilidade a nível respiratório, como é o caso de Desulfovibrio desulfuricans ATCC 27774, devido à utilização de aceitadores finais de eletrões alternativos. Neste contexto, o objetivo da primeira parte desta dissertação consistiu na identificação das ferramentas metabólicas (proteínas) envolvidas na flexibilidade respiratória desta bacteria induzidas por diferentes aceitadores de eletrões (nitrato vs sulfato). Assim, os extratos proteicos totais de células de D. desulfuricans crescidas em meios VMN com nitrato ou sulfato, foram analisados por eletroforese bidimensional (2DE), num gradiente de pH 4 - 7. Nas condições experimentais testadas, foram observados 604 e 519 spots de proteínas nos géis de células crescidas em meio contendo nitrato ou sulfato, respetivamente. Pela avaliação estatística foi possível observar aproximadamente 25 % de spots diferenciais. Os resultados obtidos sugerem que na presença de nitrato, a bactéria não só cresce mais rapidamente e com maior rendimento, como também produz uma maior quantidade de proteínas. Estes dados foram relacionados com a adaptação de D. desulfuricans ao substrato respiratório alternativo. Tal como esperado, nos ensaios das atividades enzimáticas das redutases do nitrito e do nitrato, foi possível observar maior atividade nos extratos das células crescidas em nitrato do que em sulfato. As actinobactérias marinhas do género Salinispora, têm vindo a ser exploradas como fontes de biofármacos naturais. Assim, na segunda parte deste trabalho, realizou-se um estudo preliminar, que pretendeu caracterizar as proteínas envolvidas na biossíntese destes compostos bioactivos em S. arenicola e de S. pacifica. Para tal, foi utilizada uma abordagem proteómica diferencial, baseada em 2DE. Surpreendentemente, os perfis proteicos das duas espécies mostraram-se bastante distintos, tendo-se identificado apenas 37 spots comuns entre os 650 observados no gel de S. arenicola e 510 no gel de S. pacifica.

Sommola aurea de pacifica conscientia, vel modo de confessare ([Reprod.])

Collection : Italian books before 1601 ; 527.5

Studies on a sea anemone ,anthopleura nicrescens(verrill) from the south west coast of India

The present study was undertaken with a view to understanding some aspects of the morphology, bionomics and physiology of the sea anemone A.nigrescens. This species was selected for the study since it is abundantly available along the coast throughout the year and can successfully reared in the laboratory without much effort. The present study deals with the following aspects of A.nigrescens. description of the species, habitat, food and feeding, digestion, studies on salinity tolerance, studies on oxygen consumption, studies on tolerance to desiccation, asexual reproduction and regeneration.

Desarrollo de habilidades sociales necesarias para la gestión pacifica de conflictos en el área escolar

La propuesta que se presenta tiene como fin desarrollar habilidades sociales en niños del Colegio Cofraternidad de San Fernando, de la Localidad de Ciudad Bolívar, que les permita solucionar problemas interpersonales por medio de estrategias no agresivas, para mejorar su convivencia tanto en la Institución Educativa, como en otros contextos

Killer Whales and Marine Mammal Trends in The North Pacific—A Re-Examination of Evidence for Sequential Megafauna Collapse and the Prey-Switching Hypothesis

Springer et al. (2003) contend that sequential declines occurred in North Pacific populations of harbor and fur seals, Steller sea lions, and sea otters. They hypothesize that these were due to increased predation by killer whales, when industrial whaling’s removal of large whales as a supposed primary food source precipitated a prey switch. Using a regional approach, we reexamined whale catch data, killer whale predation observations, and the current biomass and trends of potential prey, and found little support for the prey-switching hypothesis. Large whale biomass in the Bering Sea did not decline as much as suggested by Springer et al., and much of the reduction occurred 50–100 yr ago, well before the declines of pinnipeds and sea otters began; thus, the need to switch prey starting in the 1970s is doubtful. With the sole exception that the sea otter decline followed the decline of pinnipeds, the reported declines were not in fact sequential. Given this, it is unlikely that a sequential megafaunal collapse from whales to sea otters occurred. The spatial and temporal patterns of pinniped and sea otter population trends are more complex than Springer et al. suggest, and are often inconsistent with their hypothesis. Populations remained stable or increased in many areas, despite extensive historical whaling and high killer whale abundance. Furthermore, observed killer whale predation has largely involved pinnipeds and small cetaceans; there is little evidence that large whales were ever a major prey item in high latitudes. Small cetaceans (ignored by Springer et al.) were likely abundant throughout the period. Overall, we suggest that the Springer et al. hypothesis represents a misleading and simplistic view of events and trophic relationships within this complex marine ecosystem.

Calcium carbonate, biogenic opal, and organic carbon content and d15N ratios of sediments from the Bering Sea

Millennial-scale paleoceanographic changes in the Bering Sea during the last 71 kyrs were reconstructed using geochemical and isotope proxies (biogenic opal, CaCO3, and total organic carbon (TOC), nitrogen and carbon isotopes of sedimentary organic matters) and microfossil (radiolaria and foraminifera) data from two cores (PC23A and PC24A) which were collected from the northern continental slope area at intermediate water depths. Biogenic opal and TOC contents were generally high with high sedimentation rates during the last deglaciation. Laminated sediment depositions during the Early-Holocene (EH) and Bølling-Allerød (BA) were closely related with the increased primary productivity recorded by high biogenic opal and TOC contents and high d15N values. Enhanced surface-water productivity was attributed to increased nutrient supply from strengthened Bering Slope Current (BSC) and from increased amount of glacial melt-water, resulting in high C/N ratios and low d13C values, and high proportion of Rhizoplegma boreale during the last deglaciation. In contrast, low surface-water productivity during the last glacial period was due to depleted nutrient supply caused by strong stratification and to restricted phytoplankton bloom by extensive sea ice distribution under cold climates. Extensive formation of sea ice produces more oxygen-rich intermediate-water, leading to oxic bottom-water conditions due to active ventilation, which favored good preservation of oxic benthic foraminifera species. Remarkable CaCO3 peaks coeval with high biogenic opal and TOC contents in both cores during MIS 3 to MIS 4 are most likely correlated with Dansgaard-Oeschger (D-O) events. High d15N and d13Corg values during D-O interstadials support increased surface-water productivity resulting from nutrients supplied mainly by intensified BSC. During the EH, BA and D-O interstadials, dominant benthic foraminifera species indicate dysoxic bottom-water conditions as a result of increased surface-water productivity and weak ventilation of intermediate-water with mitigated sea ice development caused by strengthening of the Alaskan Stream. It is of note that the bottom-water conditions and formation of intermediate-water in the Bering Sea during the last glacial period are related to the variation of dissolved oxygen concentration of the bottom-water in the northeastern Pacific and to strong ventilation of intermediate-water in the northwestern Pacific. Thus, the millennial-scale paleoceanographic events in the Bering Sea during the D-O interstadials are closely associated with the intermediate-water ventilation, ultimately leading to weakening of North Pacific Intermediate Water.