Influence of the "Hypsithermal Age" and "Neoglaciation" climatic conditions on the Brazilian coast.

Autores

  • KENITIRO SUGUIO Instituto de Geociências/ USP

DOI:

https://doi.org/10.22456/1807-9806.20296

Palavras-chave:

''Hypsithermal Age", "Neoglaciation", Holoce paleoclimate.

Resumo

Meanwhile the highest relative sea-level is the present one in southeastern United States (Gulf of Mexico) or in Netherlands coast, most of the Brazilian coast exhibited Holocene sea-levels higher than the present in the past. The Brazilian curves, representing the relative sea-level changes during last 7.000 years, are outlined using sedimentological, biological and prehistorical past sea-level records. This paper shows that these relative sea-level records, during the Holocene, can be suitably used to demonstrate the influence of the worldwide known paleoclimatic events, like the “Hypsithermal Age” and “Neoglaciation” on the Brazilian coast.


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Publicado

2001-12-31

Como Citar

SUGUIO, K. (2001). Influence of the "Hypsithermal Age" and "Neoglaciation" climatic conditions on the Brazilian coast. Pesquisas Em Geociências, 28(2), 213–222. https://doi.org/10.22456/1807-9806.20296