Kandreho Formation

Summary

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. Fossils of the marine crocodylian Andrianavoay (originally classed as a species of Steneosaurus) as well as bivalves and the ammonite Nejdia have been found in the formation.[1][2] The name Kandreho Formation was proposed by Geiger in 2004.[3]

Kandreho Formation
Stratigraphic range: Toarcian
~180–176 Ma
TypeGeological formation
Lithology
PrimaryMarly limestone
Location
Coordinates17°30′S 45°18′E / 17.5°S 45.3°E / -17.5; 45.3
Approximate paleocoordinates22°18′S 24°00′E / 22.3°S 24.0°E / -22.3; 24.0
RegionMahajanga Province
Country Madagascar
ExtentMahajanga Basin
Type section
Named forKandreho
Named byGeiger
Year defined2004
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Outcrop of the formation in Madagascar

Gallery edit

See also edit

References edit

  1. ^ Behazonaty, SW of the basin of the Kelifely at Fossilworks.org
  2. ^ Buffetaut et al., 1981, p.314
  3. ^ Geiger, 2004, p.125

Bibliography edit

  • Buffetaut, É.; G. Termier, and H. Termier. 1981. A teleosaurid (Crocodylia, Mesosuchia) from the Toarcian of Madagascar and its palaeobiogeographical significance. Paläontologische Zeitschrift 55. 313–319. Accessed 2018-08-30.
  • Geiger, Markus. 2004. Sedimentary and stratal patterns in Jurassic successions of western Madagascar - Facies, stratigraphy, and architecture of Gondwana breakup and drift sequences (PhD thesis), 1–179. Universität Bremen. Accessed 2018-08-30.