The Lower Sakamena Formation is a geological formation found in the Morondava Basin on the southern part of the island of Madagascar. It is widely regarded as dating to the Late Permian period, around 259-252 million years ago. It is well known for largely complete, articulated fossils of fish and reptiles that are found in concretions, along with more fragmentary therapsid and amphibian remains.
Geology and setting The Lower Sakamena Formation is generally thought to be Late Permian in age. The formation forms the lowest part of the 4000 m thick Sakamena Group (which is sometimes considered part of the Karoo Supergroup) within the Morondava Basin of southern Madagascar, of consists of predominantly coarse fluvial and lacustrine derived sediments, including sandstone and conglomerate as well as mudstone, deposited within a rift valley system with rift lakes. Articulated remains of vertebrates (which are sometimes preserved as moulds) are primarily found in concretions concentrated within certain horizons, though disarticulated vertebrate remains are also sometimes found separately from concretions.Smith, R. M. H. 2000. Sedimentology and taphonomy of Late Permian vertebrate fossil localities in Southwestern Madagascar. Paleontologia Africana 36:25–41
Paleoenvironment
The environment of the formation is thought to have been warm and humid with a temperate climate, with rainfall likely being seasonal and possibly monsoonal, with the immediate area surrounding the lakes likely being a riparian forest in which Glossopteris trees were likely a prominent component. The lower waters of the lakes within the rift system are likely to have been cold and anoxic (oxygen depleted), which helped to preserve animal remains by slowing decay. The articulated animal remains are suggested to largely have originated from mass mortality events when during heavily rain and floods, the anoxic waters in the lower part of the lakes became mixed with those in the upper part, killing aquatic animals as a result of oxygen deprivation in the case of fish or thermal shock. Articulated remains of terrestrial vertebrates were probably were washed in postmortem rather than being killed by the anoxic water.
Paleobiota After Smith (2000):
Vertebrates Vertebrates of the Lower Sakamena FormationGenusNoteImagesClaudiosaurusA probably aquatic neodiapsid reptileHovasaurusAn aquatic tangasaurid neodiapsid reptileBarasaurusAn owenettid procolophonian non-diapsid reptileCoelurosauravusA gliding weigeltisaurid neodiapsid reptileThadeosaurusA probably terrestrial tangasaurid neodiapsid reptileAcerosodontosaurusA probably aquatic tangasaurid neodiapsid reptileOudenodonA dicynodont therapsid known from a skull. Other indeterminate postcranial dicynodont remains are also known from the formationAtherstoniaA "palaeoniscoid"-grade ray-finned fishRhinesuchidae indetTemnospondyl amphibians known from fragmentary remainsTheriodontia indetAn indeterminate therapsid known from a lower jaw
Flora Flora of the Lower Sakamena FormationGenusNoteImagesGlossopterisA glossopterid seed-bearing tree known from leavesLepidopterisA peltasperm seed fern known from stemsSchizoneuraAn equisetalean related to modern horsetails known from stems
References