As relações de género no âmbito do jogo simbólico numa sala de três anos

O presente estudo foi realizado no âmbito da Prática de Ensino Supervisionado do Mestrado em Educação Pré-escolar, tem como objectivo a obtenção do grau de Mestre. A temática abordada surgiu da experiencia profissional realizada com vinte e duas crianças de três anos. Esta pesquisa foi concretizada segundo uma investigação qualitativa. Esta pesquisa partiu de uma observação participante e baseada essencialmente na recolha de dados em formato de notas de campo e entrevistas semi orientadas. De uma observação inicial surgiu a seguinte temática: compreender as relações de género no âmbito do jogo simbólico, no contexto do pré-escolar, mais concretamente na sala de três anos. Com este estudo adquiri, sistematizei, aprofundei e desenvolvi conceitos e conhecimentos que vão contribuir para a minha vida profissional de forma significativa enquanto educadora. A temática proposta é de grande relevância para pais e agentes educativos. A família é o primeiro modelo de referência da criança atribuindo significado à distinção de papéis sociais. Uma identidade bem desenvolvida abrange diversas vertentes. Uma das primeiras a ser consciencializada é a identidade sexual por volta dos dois anos e meio, seguindo-se a interiorização da identidade de género. Ao sentir-se menino ou menina as crianças identificam-se com o progenitor ou com alguém de referência do mesmo sexo que o seu. Na sociedade, as questões relacionadas com identidades sexuais são uma constante. A atribuição de papéis específicos a cada grupo identitário é ancestral. Esta realidade apesar das transformações inerentes, ainda se verifica na actualidade, sendo percepcionada pelas crianças muito cedo. As crianças ao brincarem emitam acções que residem no património sócio cultural da sociedade onde se inserem. O que observam e vivenciam não também não é excluído destas brincadeiras, sendo modificadas e integradas em função das necessidades emocionais da criança. Para cada criança o significado que retira da brincadeira é único e edificador da sua própria identidade, fazendo o género parte integrante dessa identidade. Compreender como as crianças brincam, como se associam, que modelos adoptam e em que idade interioriza cada fase de descoberta da sua identidade é fundamental na orientação destes futuros adultos e no trabalho de futuros educadores. E sabe-se que brincar é mais de que um privilégio, é uma necessidade e um direito consagrado. Neste sentido recai sobre as famílias, sobre as escolas e a toda a sociedade a responsabilidade de promover tempo e espaço para que as crianças se possam viver associando-se e desenvolvendo jogos simbólicos livremente. É minha intenção que outros profissionais de educação reflictam sobre o jogo simbólico e as questões de género nas suas salas, como contributo para um maior respeito pela individualidade de cada criança.

Ecosystem size matters: The dimensionality of intralacustrine diversification in Icelandic stickleback is predicted by lake size

Cases of evolutionary diversification can be characterized along a continuum from weak to strong genetic and phenotypic differentiation. Several factors may facilitate or constrain the differentiation process. Comparative analyses of replicates of the same taxon at different stages of differentiation can be useful to identify these factors. We estimated the number of distinct phenotypic groups in threespine stickleback populations from nine lakes in Iceland and in one marine population. Using the inferred number of phenotypic groups in each lake, genetic divergence from the marine population, and physical lake and landscape variables, we tested if ecosystem size, approximated by lake size and depth, or isolation from the ancestral marine gene pool predict the occurrence and the extent of phenotypic and genetic diversification within lakes. We find intralacustrine phenotypic diversification to be the rule rather than the exception, occurring in all but the youngest lake population and being manifest in ecologically important phenotypic traits. Neutral genetic data further indicates non-random mating in four out of nine studied lakes, and restricted gene flow between sympatric phenotypic groups in two. Although neither the phenotypic variation nor the number of intralacustrine phenotypic groups were associated with any of our environmental variables, the number of phenotypic traits that were differentiated was significantly positively related to lake size, and evidence for restricted gene flow between sympatric phenotypic groups was only found in the largest lakes where trait specific phenotypic differentiation was highest.

Étude du syncrétisme de l’assiko à travers le geste et le foyer socioculturel d’un guitariste Bassa.

Ce mémoire porte sur le rôle du geste musical dans le développement de styles musicaux devenus syncrétiques. Il s’attarde à définir dans le détail le style de guitare populaire assiko propre aux Bassa du Cameroun du Sud lequel est représenté internationalement par le guitariste et percussionniste traditionnel Atna Njock. Grâce à une approche dialogique et participative, les techniques du jeu assiko sont explorées et comparées à des exemples de jeu de guitare européenne, afro-américaines et africaines. Les influences qui définissent le jeu d’Atna découlent de la culture Bassa et de son histoire marquée par l’influence coloniale et missionnaire, mais sont aussi alimentées par la «philosophie» (voire la spiritualité) et le passé musical de l’artiste. L’approche participative fournit une perspective émique, c’est-à-dire interne à la culture, de la gestuelle et de la structure du jeu assiko même si nous confrontons les propos du musicien à notre propre regard analytique. La comparaison avec divers instruments de percussion auxquels Atna a été initié montre comment ceux-ci ont forgé son jeu guitaristique. Son rôle de « garant » de la tradition musicale Bassa influence son approche et se manifeste par une préoccupation particulière pour l’« authenticité » dans la reproduction des rythmes d’un « langage » musical donné. Ses liens avec la culture Bassa, s’expriment notamment par le biais de sa reproduction du style de jeu de son maître, Jean Bikoko « Aladin ». La contribution particulière d’Atna à la technique de guitare de Bikoko est comprise comme un ajout à la lignée ancestrale. Une analyse d’un morceau du répertoire assiko issu du plus récent album d’Atna illustre d’ailleurs comment son incorporation de styles « modernes » reproduit les processus traditionnels en intégrant des éléments culturels étrangers.

Raw-data to morphometric investigations about the Neogene planktonic foraminifer Globorotalia menardii and related forms from ODP Hole 154-925B (Céara Rise, western tropical Atlantic)

Evolutionary prospection is the study of morphological evolution and speciation in calcareous plankton from selected time-slices and key sites in the world oceans. In this context, the Neogene menardiform globorotalids serve as study objects for morphological speciation in planktic foraminifera. A downcore investigation of test morphology of the lineage of G. menardii-limbata-multicamerata during the past 8 million years was carried out in the western tropical Atlantic ODP Hole 925B. A total of 4669 specimens were measured and analyzed from 38 stratigraphic levels and compared to previous studies from DSDP Sites 502 and 503. Collection of digital images and morphometric measurements from digitized outlines were achieved using a microfossil orientation and imaging robot called AMOR and software, which was especially developed for this purpose. Most attention was given to the evolution of spiral height versus axial length of tests in keel view, but other parameters were investigated as well. The variability of morphological parameters in G. menardii, G. limbata, and G. multicamerata through time are visualized by volume density diagrams. At Hole 925B results show gradual test size increase in G. menardii until about 3.2 Ma. The combination of taxonomic determination in the light microscope with morphometric investigations shows strong morphological overlap and evolutionary continuity from ancestral to extant G. menardii (4-6 chambers in the final whorl) to the descendent but extinct G. limbata (seven chambers in the final whorl) and to G. multicamerata (>=8 chambers in the final whorl). In the morphospace defined by spiral height (dX) and axial length (dY) Globorotalia limbata and G. multicamerata strongly overlap with G. menardii. Distinction of G. limbata from G. menardii is only possible by slight differences in the number of chambers of the final whorl, nuances in spiral convexity, upper keel angles, radii of osculating circles, or by differences in reflectance of their tests. Globorotalia multicamerata can be distinguished from the other two forms by more than eight chambers in the final whorl. It appeared as two stratigraphically separate clusters during the Pliocene. Between 2.88 and 2.3 Ma G. menardii was severely restricted in size and abundance. Thereafter, it showed a rapid and prominent expansion of the upper test size extremes between 2.3 and 1.95 Ma persisting until present. The size-frequency distributions at Hole 925B are surprisingly similar to trends of menardiform globorotalids from Caribbean DSDP Site 502. There, the observations were explained as an adaptation to changes in the upper water column due to the emergence of the Isthmus of Panama. In light of more recent paleontological and geological investigations about the completion of the permanent land connection between North and South America since about 3 Ma the present study gives reason to suspect the sudden test size increase of G. menardii to reflect immigration of extra-large G. menardii from the Indian Ocean or the Pacific. It is hypothesized that during the Late Pliocene dispersal of large G. menardii into the southern to tropical Atlantic occurred during an intermittent episode of intense Agulhas Current leakage around the Cape of Good Hope and from there via warm eddy transport to the tropical Atlantic (Agulhas dispersal hypothesis).

Age estimations of calcareous nannofossil biohorizons of the middle Paleocene to early Eocene at ODP Site 208-1262 (Table 1, Appendix B)

Over the last several decades debates on the 'tempo and mode' of evolution have centered on the question whether morphological evolution preferentially occurs gradually or punctuated, i.e., with long periods of stasis alternating with short periods of rapid morphological change and generation of new species. Another major debate is focused on the question whether long-term evolution is driven by, or at least strongly influenced by changes in the environment, or by interaction with other life forms. Microfossils offer a unique opportunity to obtain the large datasets as well as the precision in dating of subsequent samples to study both these questions.We present high-resolution analyses of selected calcareous nannofossils from the deep-sea section recovered at ODP Site 1262 (Leg 208) in the South-eastern Atlantic. The studied section encompasses nannofossil Zones NP4-NP12 (equivalent to CP3-CP10) and Chrons C27r-C24n. We document more than 70 biohorizons occurring over an about 10 Myr time interval, (~62.5 Ma to ~52.5 Ma), and discuss their reliability and reproducibility with respect to previous data, thus providing an improved biostratigraphic framework, which we relate to magnetostratigraphic information, and present for two possible options of a new Paleocene stratigraphic framework based on cyclostratigraphy. This new framework enabled us to tentatively reconstruct steps in the evolution of early Paleogene calcareous nannoplankton through documentation of transitional morphotypes between genera and/or species and of the phylogenetic relations between the genera Fasciculithus, Heliolithus, Discoasteroides and Discoaster, as well as between Rhomboaster and Tribrachiatus. The exceptional record provided by the continuous, composite sequence recovered at Walvis Ridge allows us to describe the mode of evolution among calcareous nannoplankton: new genera and/or new species usually originated through branching of lineages via gradual, but relatively rapid, morphological transitions, as documented by the presence of intermediate forms between the end-member ancestral and descendant forms. Significant modifications in the calcareous nannofossil assemblages are often "related" to significant changes in environmental conditions, but the appearance of structural innovations and radiations within a single genus also occurred during "stable" environmental conditions. These lines of evidence suggest that nannoplankton evolution is not always directly triggered by stressed environmental conditions but could be also driven by endogenous biotic control.

Cicely, and other stories,

"These stories first appeared in the Youth's companion and Forward."

Morphological variability of Globorotalia menardii in DSDP Sites 68-502 and 68-503

Variability in the test of Globorotalia menardii during the past 8 million years has been investigated at DSDP Site 502A (Caribbean Sea) and DSDP Site 503A (Eastern Equatorial Pacific). Measurements were made of spire height (delta x), maximum diameter (delta y), the tangent angles of the upper and lower peripheral keels (phi 1, phi 2, respectively), the number of chambers in the final whorl, and the area of the silhouette in keel view. Four morphotypes alpha, beta, gamma, and delta were distinguished. Morphotype alpha was found in strata ranging in age from the Late Miocene through the Holocene. It shows a continuous increase in delta x and delta y until the Late Pleistocene. During and after the final closure of the ancient Central American Seaway (between 2.4 Ma and 1.8 Ma) there was a rapid increase in the area of the test in keel view. At the Caribbean Sea site, morphotype beta evolved during the past 0.22 Ma. It is less inflated than alpha and has a more delicate test. In the morphospace of delta x vs. delta y, morphotypes alpha and beta can be distinguished by a separation line delta y = 3.2 * delta x - 160 (delta x and delta y in µm). Plots of morphotype alpha are below that line, those of beta are above it. Morphotype alpha is taken to be Globorotalia menardii menardii Parker, Jones & Brady (1865) and includes G. menardii 'A' Bolli (1970). Morphotype beta is identified as G. menardii cultrata (d'Orbigny). Morphotypes gamma and delta are extinct Upper Miocene to Pliocene forms which evolved from morphotype alpha. They have a narrower phi 1 angle and more chambers (>=7) than morphotype alpha commonly with 5 to 6 chambers (7 in transitional forms). In contemporaneous samples morphotype delta can be distinguished from gamma by a smaller value of phi 1 and 8 or more chambers in the final whorl. Morphotype gamma is taken to be G. limbata (Fornasini, 1902) and includes the junior synonym G. menardii 'B' Bolli (1970). Morphotype delta is G. multicamerata Cushman & Jarvis (1930). With the exception of the Late Pleistocene development of G. menardii cultrataonly in the Caribbean the morphological changes of G. menardii at DSDP Sites 502A and 503A are similar. The development from the ancestral G. menardii menardii of the G. limbata - G. multicamerata lineage during the Pliocene and of G. menardii cultrata during the Late Pleistocene suggests responses at the two sites to a changing palaeoceanography during and after the formation of the Isthmus of Panama.

Reflexiones sobre la investigación acción en el abordaje de las memorias e identidades indígenas kollas en la ciudad de La Plata

Este trabajo tiene como finalidad presentar los principales lineamientos de lo que constituye mi proyecto tesis de investigación de posgrado explicitando los objetivos generales y particulares que se buscan alcanzar. Asimismo, se presentan cuestiones referidas a los desafíos que plantea el trabajo con entrevistas y observaciones participantes, especialmente las que atañen prácticas de grupos tradicionalmente silenciados y relegados al olvido como son las comunidades indígenas de Argentina. La posibilidad de entablar vínculos estrechos con miembros de estas comunidades que permitan dar cuenta de las experiencias personales y colectivas, las memorias sociales compartidas, las herencias ancestrales y culturales, constituye el resultado de un trabajo sostenido en el largo plazo. En este caso, el desarrollo de ésta investigación se plantea como un proceso conjunto y participativo, fruto de una experiencia de extensión universitaria que permitió el acercamiento y vinculación con la comunidad kolla, Asociación Civil Warmikunamanta Antipak Sonqokuna. En consecuencia, se buscará abrir a la reflexión sobre la producción de saberes en ciencias sociales, especialmente en los estudios sobre sociedades indígenas del siglo XXI

California Calling

Thesis (Master's)--University of Washington, 2016-06

Certain observations concerning the effects of epistasis on complex traits and the evolution of genomes.

Thesis (Ph.D.)--University of Washington, 2016-05

Centromere identification and inactivation on a neo-Y chromosome fusion in threespine stickleback fish (Gasterosteus aculeatus)

Thesis (Ph.D.)--University of Washington, 2016-05

Armenian Orchestral Music

Thesis (D.M.A.)--University of Washington, 2016-06

Being, Belonging, and Connecting: Filipino Youths' Narratives of Place(s) and Wellbeing in Hawai'i

Thesis (Ph. D.)--University of Washington, 2016-04

Phylogeny, molecular and fossil dating, and biogeographic history of Annonaceae and Myristicaceae (Magnoliales)

Annonaceae and Myristicaceae, the two largest families of Magnoliales, are pantropical groups of uncertain geographic history. The most recent morphological and molecular phylogenetic analyses identify the Asian-American genus Anaxagorea as sister to all other Annonaceae and the ambavioids, consisting of small genera endemic to South America, Africa, Madagascar, and Asia, as a second branch. However, most genera form a large clade in which the basal lines are African, and South American and Asian taxa are more deeply nested. Although it has been suggested that Anaxagorea was an ancient Laurasian line, present data indicate that this genus is basically South American. These considerations may mean that the family as a whole began its radiation in Africa and South America in the Late Cretaceous, when the South Atlantic was narrower, and several lines dispersed from Africa-Madagascar into Laurasia as the Tethys closed in the Tertiary. This scenario is consistent with the occurrence of annonaceous seeds in the latest Cretaceous of Nigeria and the Eocene of England and with molecular dating of the family. Based on distribution of putatively primitive taxa in Madagascar and derived taxa in Asia, it has been suggested that Myristicaceae had a similar history. Phylogenetic analyses of Myristicaceae, using morphology and several plastid regions, confirm that the ancestral area was Africa-Madagascar and that Asian taxa are derived. However, Myristicaceae as a whole show strikingly lower molecular divergence than Annonaceae, indicating either a much younger age or a marked slowdown in molecular evolution. The fact that the oldest diagnostic fossils of Myristicaceae are Miocene seeds might be taken as evidence that Myristicaceae are much younger than Annonaceae, but this is implausible in requiring transoceanic dispersal of their large, animal-dispersed seeds.

Chic chicks: the evolution of chick ornamentation in rails

Competition over access to food has led to the evolution of a variety of exaggerated visual and vocal displays in altricial nestling birds. Precocial chicks that are fed by their parents also vary widely in appearance ranging from those with inconspicuous coloration to those with brightly colored bills, fleshy parts, and plumes. These ornaments are lost by the end of the period of parental dependence, suggesting they function in competition over parental care. We use a comparative approach to evaluate which ecological or life-history variables may have favored the evolution of conspicuous ornamentation in precocial chicks. We compiled data on chick morphology, ecology, and social organization of species in the Family Rallidae, a group with highly variable downy chicks. Chick ornamentation in the form of brightly colored bills, fleshy patches, or plumes is observed in 36 of 97 species for which downy chicks are described. Phylogenetic reconstructions suggest that nonornamentation is the ancestral state. Chick ornamentation has evolved multiple times within the Rallidae and is significantly associated with large clutch sizes and polygamous mating systems. Chick ornamentation was also weakly associated with adult ornamentation and adult dimorphism. We argue that these results support the hypothesis that lineages with higher levels of sibling competition are more likely to evolve ornamented chicks.