Identifying change trajectories and evolutive phases on coastal landscapes. Case study: Sao Sebastiao Island, Brazil

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)Environmental planning decisions depend on an understanding of how the preservation or degradation process has progressed through time, and consequently, on how to define strategies that will be conducive to environmental conservation. The landscape ecology literature has been addressing methodological deficiencies regarding landscape evaluation and interpretation, mainly with respect to express heterogeneity, where it is difficult to recognize the matrix through landscape configuration. We argue that a better representation of the spatio-temporal landscape occurs integrating driving forces that are capable of initiating and perpetuating changes in the landscape, modeling the complex geometric pattern inherent in landscape structure, and defining the change vectors in a continuum of scales. The aim of this study is to develop a methodology that allows the identification of structure patterns resulting from the relation among driving forces, change vectors and evolutive phases in a coastal landscape. This paper, then, considers four factors: driving forces identified through the construction of a historical survey; land use and cover maps (LUCC) at broad scale, cross tabulation, flux diagram, and dominance index; the landscape evolution phases identified using LUCC and driving forces; and landscape cracking and change-vectors defined at fine scale using conservation and degradation indexes. This strategy reveals the existence of specific geometric patterns and change vectors for each evolution phase of the landscape. It also allows the identification of sites where management actions should be directed toward helping decision makers. (C) 2012 Elsevier B.V. All rights reserved.1061115123Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq

Biogeochemical processes and the diversity of Nhecolândia lakes, Brazil

The Pantanal of Nhecolândia, the world's largest and most diversified field of tropical lakes, comprises approximately 10,000 lakes, which cover an area of 24,000 km² and vary greatly in salinity, pH, alkalinity, colour, physiography and biological activity. The hyposaline lakes have variable pHs, low alkalinity, macrophytes and low phytoplankton densities. The saline lakes have pHs above 9 or 10, high alkalinity, a high density of phytoplankton and sand beaches. The cause of the diversity of these lakes has been an open question, which we have addressed in our research. Here we propose a hybrid process, both geochemical and biological, as the main cause, including (1) a climate with an important water deficit and poverty in Ca2+ in both superficial and phreatic waters; and (2) an elevation of pH during cyanobacteria blooms. These two aspects destabilise the general tendency of Earth's surface waters towards a neutral pH. This imbalance results in an increase in the pH and dissolution of previously precipitated amorphous silica and quartzose sand. During extreme droughts, amorphous silica precipitates in the inter-granular spaces of the lake bottom sediment, increasing the isolation of the lake from the phreatic level. This paper discusses this biogeochemical problem in the light of physicochemical, chemical, altimetric and phytoplankton data.<br>O Pantanal da Nhecolândia é o maior e mais diversificado campo de lagos da região tropical do planeta, com cerca de 10.000 lagos de variadas salinidade, pH, alcalinidade, cor, fisiografia e atividade biológica dispostos em uma área de 24.000 km². Os lagos hipossalinos têm pH variável, baixa alcalinidade, macrófitas e baixa densidade de fitoplâncton. Os lagos salinos tem pH acima de 9 ou 10, elevada alcalinidade, alta densidade de fitoplâncton e praias de areia. A causa da diversidade desses lagos é uma questão ainda em aberto que é abordada nesta pesquisa. Propõe-se como principal causa um processo híbrido, geoquímico e biológico, baseado em (1) clima com um déficit hídrico importante e pobreza em Ca2+na água superficial e do freático e (2) na elevação do pH durante florações de cianobactérias. Estes dois aspectos desestabilizam a tendência geral de pH neutro para as águas superficiais da Terra. Este desequilíbrio resulta em aumento do pH e dissolução da areia quartzosa do fundo dos lagos salino-alcalinos. Durante secas extremas há precipitação de sílica amorfa nos espaços inter-granulares dos sedimentos de fundo destes lagos, aumentando seu isolamento do freático. O artigo discute este processo biogeoquímico, à luz de dados físico-químicos, químicos, fitoplânctonicos e de altimetria de precisão