Lower Sakamena Formation
Coordinates22.5476111°S 45.423666°E
CountryMadagascar
ExtentMorondava Basin
AgeLopingian
~
OtherlithologySandstone, conglomerate, Mudstone
UnitofSakamena Group
UnderliesMiddle Sakamena Formation
OverliesSakoa Formation
PeriodLopingian

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,[1] 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.[2]

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.[2][3]

Paleobiota

After Smith (2000):[2]

Vertebrates

Vertebrates of the Lower Sakamena Formation
GenusNoteImages
ClaudiosaurusA probably aquatic neodiapsid reptile
HovasaurusAn aquatic tangasaurid neodiapsid reptile
BarasaurusAn owenettid procolophonian non-diapsid reptile
CoelurosauravusA gliding weigeltisaurid neodiapsid reptile
ThadeosaurusA probably terrestrial tangasaurid neodiapsid reptile
AcerosodontosaurusA probably aquatic tangasaurid neodiapsid reptile
OudenodonA dicynodont therapsid known from a skull. Other indeterminate postcranial dicynodont remains are also known from the formation
AtherstoniaA "palaeoniscoid"-grade ray-finned fish
Rhinesuchidae indetTemnospondyl amphibians known from fragmentary remains
Theriodontia indetAn indeterminate therapsid known from a lower jaw

Flora

Flora of the Lower Sakamena Formation
GenusNoteImages
GlossopterisA glossopterid seed-bearing tree known from leaves
LepidopterisA peltasperm seed fern known from stems
SchizoneuraAn equisetalean related to modern horsetails known from stems

References

  1. ^ Wescott, William A. & Diggens, John N. (October 1998). "Depositional history and stratigraphical evolution of the Sakamena group (Middle Karoo Supergroup) in the southern Morondava Basin, Madagascar". Journal of African Earth Sciences. 27 (3–4): 461–479. Bibcode:1998JAfES..27..461W. doi:10.1016/S0899-5362(98)00073-6
  2. ^ Smith, R. M. H. 2000. Sedimentology and taphonomy of Late Permian vertebrate fossil localities in Southwestern Madagascar. Paleontologia Africana 36:25–41
  3. ^ Buffa, Valentin; Jalil, Nour-Eddine; Falconnet, Jocelyn; Vincent, Peggy (March 2025). "The neodiapsid Thadeosaurus colcanapi from the upper Permian of Madagascar". Papers in Palaeontology. 11 (2). Bibcode:2025PPal...11E0008B. doi:10.1002/spp2.70008. ISSN 2056-2799