Trajetórias construídas em caminhos (não) planejados: os sentidos formativos da escrita no estágio supervisionado obrigatório do curso de Pedagogia da UFMA

This research is taking as study aim the mediatory teaching action, its involvement with educational guidance reports of Supervised Obligatory Student Teaching in curriculum managing by formal teachers is more related to the form as each one understands the mediatory action of the pedagogy teaching activities than to the adherence of a common project, that is: the Course Pedagogy Project (CPP). Thus, our aim is meant to understand the attribution from the formal teachers to curriculum managing process, having as forms its action in the supervised obligatory student teaching at UFMA Pedagogy Course. On one side, we look for traces about established relation by them between their professional experience and their report guidance in current course. On the other hand, a research concern comes up to us on the forming meaning of the report writing by UFMA Pedagogy Teachers Course. In order to do that, we used interviews interpreted by means of methodology understanding interview. Starting from oral speeches, we understand that the managing formation in this course is linked to postures not identical and adjustable to conditions the teachers have access. We identify a curriculum subject group and a group that by their conformation adapted is considered as object group of curriculum practices. As for the mediatory action in writing formation process, we noticed that they contribute to teacher information at UFMA in the reflexive critic perspective and or in the bureaucratic reproduction perspective. The report writing at the end of the Supervised Obligatory internship is characteristic of quality quantity assessment display, as bureaucratic process and as reflexive display and didactic pedagogy activity intervention. We defend that the teachers´ guidance under critical reflections, where the writing has a social role, must overcome individual dimension, they must be debated as collective and organized practices. We hope to contribute with such a research on teacher mediatory actions and their implementing with help of reporting writing guidance in the Supervised Obligatory Student Teaching in the Curriculum Teacher managing process.

Grain size composition of ocean and sea bottom sediments

On the basis of a long term research of the authors a database model of grain size composition of unlithified marine and ocean bottom sediments has been created. An improved method of water-mechanical analysis has been offered. Grain size parameters of main types of bottom sediments have been measured and calculated. The genetic interpretation of results and regularities of sandy, aleuritic and pelitic material in basins of sedimentation are under discussion.

Distribution of planktonic and benthic foraminifers in bottom sediments from Core LV28-42-5, Sea of Okhotsk

Distribution of diatoms and planktonic and benthic foraminifers, as well as correlation of components of sandy grain size fraction were studied in the Quaternary sediment core LV28-42-5 (720 cm long) col¬lected on the southeastern slope (1045 m depth) of the Institute of Oceanology Rise, Sea of Okhotsk. This study allowed to reconstruct principle features of paleoceanographic evolution. In the course of penultimate and last continental glaciations (isotope stages 6 and 4-2) and during the later period of the last interglacial (substages 5.d-5.a) the following conditions were characteristic of this area: low temperatures of surface water, terrigenous sediment accumulation including coarse grained ice-rafted material, minimum bioproductivity and microfossil content in sediments, low sea level, reduced water exchange with the ocean, low position of old deep Pacific water. During the interglacial optimum (substage 5.e), as well as in the last deglaciation and Holocene (stage 1) water temperature and bioproductivity increased, sea level rose, and active surface water exchange between the Sea of Okhotsk and the Pacific Ocean and the Sea of Japan took place. This resulted in intensive inflow of the old deep Pacific water into the Sea of Okhotsk and elevation of its upper boundary by few hundred meters. During the later intervals of these warm periods a dichothermal structure of the upper water layer formed and diatom oozes accumulated.

(Table 1) Composition of organic matter from sediments of the triple junction area in the Indian Ocean

Bituminous substances in metalliferous sediments from the region of the triple junction in the Indian Ocean were studied. Specific peculiarities of their structure confirming location in "hot conditions" were revealed. Hydrocarbons are genetically connected with hydrothermal matter, and thus they could be considered as a geochemical indicator of hydrothermal processes in the ocean.

Sediment age, abundance of planktonic foraminifera shells, degree of their dissolution, percentage of benthic foraminifera in total foram fauna, Core GC-11, Sea of Okhotsk

Taxonomic composition and distribution of planktonic foraminifera are studied in section of Core GC-11 penetrated through Upper Quaternary sediments of the Bowers Ridge western slope, south Bering Sea. It is shown that structure of foraminiferal assemblage and productivity varied substantially during the last 32000 calendar years in response to changes in surface water temperatures and water mass circulation in the North Pacific including the Bering Sea. Productivity was maximal during the deglaciation epoch, being notably lower in Holocene and minimal at glaciation time.