Kandreho Formation Explained

Kandreho Formation
Period:Toarcian
Age:Toarcian
~
Type:Geological formation
Prilithology:Marly limestone
Namedfor:Kandreho
Namedby:Geiger
Year Ts:2004
Coordinates:-17.5°N 45.3°W
Paleocoordinates:-22.3°N 24°W
Region:Mahajanga Province
Country: Madagascar
Extent:Mahajanga Basin

The Kandreho Formation is an Early Jurassic (middle or late Toarcian) geological formation of the Mahajanga Basin of Madagascar. The marly limestones of the formation were deposited in a subtidal lagoonal environment. The formation overlies the Bouleiceras and Spiriferina beds of the early Toarcian and has been correlated to the Marrat Formation of Saudi Arabia.[1] Fossils of the marine crocodylian "Steneosaurus" as well as bivalves and the ammonite Nejdia have been found in the formation.[2] [3] The name Kandreho Formation was proposed by Geiger in 2004.[4]

Fossils

Crocodyliformes

See also

References

Bibliography

Notes and References

  1. Buffetaut . Eric . Termier . Geneviéve . Termier . Henri . 1981 . A teleosaurid (Crocodylia, Mesosuchia) from the Toarcian of Madagascar and its palaeobiogeographical significance . Paläontologische Zeitschrift . 55 . 3-4 . 313–319 . 10.1007/bf02988145 . 0031-0220.
  2. https://paleobiodb.org/classic/displayCollResults?collection_no=132380 Behazonaty, SW of the basin of the Kelifely
  3. Buffetaut et al., 1981, p.314
  4. Geiger, 2004, p.125