Rodolfo José Angulo

TL;DR: In this article, the authors discuss all the key radiocarbon-dated samples used to establish regional trends in relative sea-level on the eastern coast of Brazil and conclude that there is widespread evidence for a progressive decline, possibly with uneven rates, of relative sea level since the end of the mid-Holocene sea level maximum (PMT) above present sea level and a subsequent fall to the present time.

TL;DR: In this paper, the authors analyze the palaeo-sea-level indicators (vermetid tubes, shells, wood fragments and shell-midden deposits) related to the sea-level maximum of the mid-Holocene and two secondary oscillations that would have occurred between 4100-3800 years B.P and 3000-2700 years C.P.

TL;DR: In this article, radiocarbon dates from vermetid shells collected in the southernmost sector of the Brazilian rocky coast presented dates ranging from 5410±80 to 190±65 years B.P., with associated paleosea levels varying from +2.10 m to +0.20 m above present sea level.

TL;DR: In this paper, the authors proposed a model of evolutionary development for mangroves on the Brazilian Braganca Peninsula driven by relative sea-level changes from the middle to late Holocene.

TL;DR: The Paranagua coastal plain is a 600 km 2 barrier system located in south Brazil (25° 30′ S) and is largely made up of Pleistocene and Holocene beach ridges as discussed by the authors.