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“ The island of Madagascar has been separated from the African mainland for 80 million years, so long that most of its animals are now very different from any to be found elsewhere. ”

David Attenborough, Islands

The Maevarano Formation is a Late Cretaceous sedimentary rock formation found in the Mahajanga Province (known as "Majunga" in French) of northwestern Madagascar.

Paleoenvironment[]

The Maevarano Formation is recognized as an alluvial plain where the discharge of rivers fluctuate. The area is also believed to have had reddish soil, with floodplains that supported vegetation able to grow in the relatively dry climate. The region, at times semi-arid (like it is today), at times undergoing strong dry and wet seasons, was eventually claimed by rising sea levels that pushed the shoreline back. This may or may not have been the result of the Cretaceous-Paleogene Extinction Event, a catastrophe that wiped out three-quarters of life on Earth.

Appearances[]

The Maevarano Formation serves as the setting of the fifth segment of Freshwater, the third and fourth segments of Islands, and the third segment of Swamps.

Paleofauna[]

References[]

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