Paleosols
Mostrando 1-7 de 7 artigos, teses e dissertações.
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1. Micromorphology of Paleosols of the Marília Formation and their Significance in the Paleoenvironmental Evolution of the Bauru Basin, Upper Cretaceous, Southeastern Brazil
ABSTRACT Deduction of associated paleoenvironments and paleoclimate, definition of the chronosequence of paleosols, and paleogeographic reconstruction have become possible through the application of micromorphology in paleopedology. Micromorphology has also been useful in recognition of weathering processes and definition of minerals formed in succession. In
Rev. Bras. Ciênc. Solo. Publicado em: 13/02/2017
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2. Pedodiagenetic Characterization of Cretaceous Paleosols in Southwest Minas Gerais, Brazil
ABSTRACT The influence of post-burial geological processes on preserving pedogenic properties has great importance in identifying ancient paleosols both in the field and in a laboratory. However there are not many publications that focus on characterizing paleosol diagenesis. As temperature and pressure progressively increase, evidence of pedogenesis is modi
Rev. Bras. Ciênc. Solo. Publicado em: 06/02/2017
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3. Paelossolos da formação Marília : subsídios para a interpretação paleogeográfica na área de Duartina-SP / Marília formation paleosols : subsidies for the paleogeographic interpretation in the area of Duartina-SP
O estudo de paleossolos tem se mostrado como uma importante ferramenta interdisciplinar na interpretação paleoambiental. Neste sentido, a interpretação de evidências paleopedológicas em paleossolos da Formação Marília (Maastrichtiano), membro litoestratigráfico superior do Grupo Bauru, se mostra de grande valia para a interpretação paleogeográfi
Publicado em: 2011
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4. Significados paleoambientais e paleoclimáticos dos Paleossolos : uma revisão
The majority of paleosols are described from continental deposits, most commonly from alluvial strata. In these continental records to much little is revealed of conditions between events of sedimentation. In alluvial sedimentary environments, a record of these conditions is not lost and gone forever. They may be interpreted from fossil soils formed on depos
Publicado em: 2010
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5. Caracterização de paleossolos da formação Marilia : Serra de Echaporã - SP / Caracterization of paleosols in the Marilia formation : Serra de Echaporã - SP
Esta pesquisa foi realizada em um afloramento na rodovia SP - 421, no sentido Marília - Echaporã. O objetivo foi identificar e caracterizar os paleossolos que ocorrem neste ponto na Formação Marília, utilizando técnicas da pedologia, micromorfologia e macromorfologia. Através das técnicas empregadas, foi possível identificar três tipos de paleossol
Publicado em: 2008
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6. Sistema pedológico Planosolo-Plintossolo no Pantanal de Barão de Melgaço-MT / Pedological system Solonetz-Plinthosol in the Pantanal of Barão de Melgaço-MT
The Pantanal is the largest continental flood plains, comprising a mosaic of different habitats, maintaining plant diversity, animal and soil. It consists of eleven sub-regions, one of which the of the Pantanal of Barão de Melgaço, which is located north of the Quaternary sedimentary basin. It presents a spatial heterogeneity that is related to the diversi
Publicado em: 2008
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7. The Paleoproterozoic snowball Earth: A climate disaster triggered by the evolution of oxygenic photosynthesis
Although biomarker, trace element, and isotopic evidence have been used to claim that oxygenic photosynthesis evolved by 2.8 giga-annum before present (Ga) and perhaps as early as 3.7 Ga, a skeptical examination raises considerable doubt about the presence of oxygen producers at these times. Geological features suggestive of oxygen, such as red beds, laterit
National Academy of Sciences.