Distribution and Growth Morphology of the Recent Microbialites: the Case of Lagoa Salgada, Rio de Janeiro - Brazil
| Autor: | Douglas Rosa da Silva, Kátia Leite Mansur, Leonardo Fonseca Borghi de Almeida |
|---|---|
| Rok vydání: | 2019 |
| Předmět: |
biology
Terrigenous sediment Thin section Geography Planning and Development Geochemistry Geology Development Areal distribution biology.organism_classification chemistry.chemical_compound chemistry Stromatolite Geologic time scale robial mats Recent stromatolite Carbonate Economic Geology Microbial mat Lithification General Environmental Science |
| Zdroj: | Anuário do Instituto de Geociências; Vol 42, No 1 (2019); 439-453 Anuário do Instituto de Geociências Universidade Federal do Rio de Janeiro (UFRJ) instacron:UFRJ |
| ISSN: | 1982-3908 0101-9759 |
| Popis: | Organosedimentary deposits formed by interaction of carbonate and terrigenous sediments are commonly found in the Lagoa Salgada, a holocenic environment located on the north of Rio de Janeiro state which records environmental and biological information of their evolution. Microbial mats are widespread however stromatolites are very prominent and exposed nowadays in the lagoon. Microbial mats were distinguished into two main morphologies, colloform and polygonal mats. It is interesting to note that the colloform ones are not lithified unlike the polygonal ones. Related to stromatolites three main morphologies were defined and classified based on their external morphology and internal structure. Internal structure was further analyzed by sample cutting and thin section study to confirm field classification. Stromatolites are mostly bioherms dome-like and vary from 10 to 40cm high. Morphologically stromatolites are columnar or branched to columnar and coalescence among them are very common resulting in stratiform morphologies. Stromatolitic domal-like bioherms though showing similar internal structure were separated in small and large according to their size; the differences in size are clearly observed and have different areal distribution, which possibly reflects changes in the lagoon paleogeography during the geological time. Also, the identification of differences in the internal structure of stromatolites allows the formulation of hypothesis supporting environmental changes in the Lagoa Salgada. |
| Databáze: | OpenAIRE |
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