During the Paleozoic,
Gondwana merged with
Laurasia, forming supercontinent
Pangea.
In this era, when the sea level was about 300 to 400 m higher than today, the syneclises (intercratonic sedimentary basins) of the
Neoproterozoic
South American Platform
were flooded by the sea (marine transgressions).
Evidences of these floodings are for example the Devonian (400 Ma) layers of the
Ponta Grossa formation (Paraná supersequence) at Chapada dos Guimarães
National Park (
(
Paraná Basin / Mato Grosso).