1998
DOI: 10.1006/ecss.1998.0368
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Characterization of Energy Gradient in Enclosed Bays of Ubatuba Region, South-eastern Brazil

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Cited by 78 publications
(113 citation statements)
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“…Despite the generally low energy conditions, three areas can be distinguished, each varying in its silt, clay and organic matter content: a finer and richer Central and North Zone; a West Inner Zone with fine sand, silt and clay besides a moderate organic matter content, and a South Zone plus the largest rivers, characterized by medium sand and low values of organic matter. These results follow the general pattern found in the northeast coast of São Paulo State as showed early by Mahiques et al 1998.…”
Section: Discussionsupporting
confidence: 89%
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“…Despite the generally low energy conditions, three areas can be distinguished, each varying in its silt, clay and organic matter content: a finer and richer Central and North Zone; a West Inner Zone with fine sand, silt and clay besides a moderate organic matter content, and a South Zone plus the largest rivers, characterized by medium sand and low values of organic matter. These results follow the general pattern found in the northeast coast of São Paulo State as showed early by Mahiques et al 1998.…”
Section: Discussionsupporting
confidence: 89%
“…2), but can be characterized as a low energy environment also. In this region, the Ubatuba Bay exhibits a constriction in the coastline that induces wave refraction (Mahiques et al 1998) and acts as a barrier for the intrusion of waves from the open sea. As it is known, wave action is one of the principal hydrodynamic phenomena responsible for the bottom sedimentary processes in coastal areas (Furtado and Mahiques 1989) and can explain the features observed.…”
Section: Discussionmentioning
confidence: 99%
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“…1), during 1974-1976. Ubatuba sites are sheltered from wave action, with predominantly muddy sand bottoms (Mahiques et al, 1998). Schizoporella colonies were fixed to rocks at about 1 m below MLWS, together with other sessile organisms such as the macroalgae Acanthophora spicifera, Laurencia papillosa and Sargassum filipendula, the sponges Zygomycale parishii, Tedania ignis, Haliclona erina, Halichondria magniconulosa, and colonies of cnidarians and tunicates.…”
Section: Methodsmentioning
confidence: 99%