Menuha Formation

Menuha Formation Stratigraphic range: Upper Cretaceous (Santonian-Early Campanian) PreЄ Є O S D C P T J K Pg N
Menuha Formation exposed in Makhtesh Ramon.
Type	Sedimentary
Unit of	Mount Scopus Group
Underlies	Mishash Formation
Overlies	Zihor Formation
Thickness	14 to 50 m
Lithology
Primary	chalk, marly chalk
Other	conglomeratic chalk, limestone
Location
Region	Makhtesh Ramon, Negev desert
Country	Israel
Extent	Israel

The Menuha Formation is the name given to an Upper Cretaceous (Santonian-Early Campanian) chalk, marly chalk and conglomeratic chalk unit exposed throughout the Makhtesh Ramon region of southern Israel and parts of northern Israel (Avni, 1991).

Stratigraphy and paleoenvironment

The Menuha Formation records the earliest occurrence of tectonic activity within the Ramon anticline, forming the present erosive valley known as "Makhtesh Ramon" as an outcome of a sequence of erosive events evolving since the Late Cretaceous (Avni, 1993). It consists of white and yellow/brown chalk that is often glauconitic and sometimes conglomeratic or marly. The Menuha Formation likely represents a temperate to subtropical, open shelf environment deposited during the formation of the Ramon anticline. Reworked conglomeratic chalks in the western section represent marginal facies derived from this structural uplift.

The paleoenvironment is based on the occurrences of several shark and fish teeth, oysters, trace fossils, phosphatic peloids, and foraminiferans. The isolated teeth represent at least ten different species:

• Cretalamna appendiculata
• Cretoxyrhina mantelli
• Squalicorax falcatus?
• Squalicorax kaupi
• Scapanorhynchus rapax
• Scapanorhynchus raphiodon?
• Carcharias samhammeri
• Carcharias cf. C holmdelensis
• Hadrodus priscus
• Micropycnodon kansasensis?

References

• Avni, Y. (1991). "The geology, paleogeography and landscape evolution in the central Negev Highlands and the western Ramon structure". Geological Survey of Israel, Report GSI/6/91: 153 p. 

• Avni, Y. (1993). "The structural and landscape evolution of the western Ramon structure". Israel Journal of Earth Sciences 42: 177–188. 

• Wilson, M.A.; Zaton, M.; Avni, Y. (2012). "Origin, paleoecology and stratigraphic significance of bored and encrusted concretions from the Upper Cretaceous (Santonian) of southern Israel". Palaeobiodiversity and Palaeoenvironments: DOI 10.1007/s12549–012–0082–8. 

• 

  Thalassinoides burrowing system throughout the Menuha Formation chalk.

• 

  Cretalamna appendiculata tooth, Menuha Formation.

• 

  Squalicorax kaupi tooth, Menuha Formation.

• 

  Squalicorax falcatus? tooth, Menuha Formation.

• 

  Carcharias samhammeri tooth, Menuha Formation.

• 

  Carcharias cf. C holmdelensis tooth, Menuha Formation.

• 

  Cretoxyrhina mantelli tooth, Menuha Formation.

• 

  Scapanorhynchus rapax tooth, Menuha Formation.

• 

  Scapanorhynchus raphiodon? tooth, Menuha Formation.

• 

  Hadrodus priscus tooth, Menuha Formation.

• 

  Micropycnodon kansasensis? tooth, Menuha Formation.

• 

  Several foraminiferans replaced by silica from the Menuha Formation.

• 

  Several oysters, possibly Pycnodonte vesicularis, from the Menuha Formation.

• 

  Irregular echinoid spine from the chalk sediments of the Menuha Formation.