Holocene paleo-sea level changes along the coast of Rio de Janeiro, southern Brazil: Comment on Castro et al. (2014)
AUTOR(ES)
ANGULO, RODOLFO J., GIANNINI, PAULO C.F., SOUZA, MARIA CRISTINA DE, LESSA, GUILHERME C.
FONTE
An. Acad. Bras. Ciênc.
DATA DE PUBLICAÇÃO
10/11/2016
RESUMO
ABSTRACT The present work discusses and reinterprets paleo-sea level indicators used to build Holocene sea-level curve for the coast of Rio de Janeiro at former works. We conclude that: (a) the paleo-sea levels inferred by vermetid remains show that sea-level has fallen over the past 4400 years, at least; (b) the paleo-sea level inferred by the beachrock facies and dated shells of Jaconé shows that sea-level was near the present elevation between 8198 and 5786 years before present; and (c) several shells from other beachrocks were deposited probably thousands of years after the specimens died and consequently do not allow precise reconstructions of paleo-sea levels. These conclusions differ from the conclusions of the original paper.
Documentos Relacionados
- Reply to Castro et al. 2018 on “Holocene paleo-sea level changes along the coast of Rio de Janeiro, southern Brazil”.
- Comments to Angulo et al. 2016 on “Sea-level fluctuations and coastal evolution in the state of Rio de Janeiro, southeastern - Brazil” by Castro et al. 2014
- Sea-level fluctuations and coastal evolution in the state of Rio de Janeiro, southeastern Brazil
- Paleochannels related to late quaternary sea-level changes in Southern Brazil
- Comment on Coomes et al. ‘Scaling of xylem vessels and veins within the leaves of oak species’