Bhojunda Stromatolite Park

Bhojunda Stromatolite Park
Interactive map of Bhojunda Stromatolite Park
LocationBhojunda, Chittaurgarh district, Rajasthan, India
Nearest cityChittaurgarh
Coordinates24°51′40″N 74°35′46″E / 24.861°N 74.596°E / 24.861; 74.596
Area8 acres (3.2 ha)
Official name
Stromatolite Park, Bhojunda
Designated1976
Designated by
Geological Survey of India

Bhojunda Stromatolite Park is a protected paleontological site near Bhojunda in Chittaurgarh district of the Indian state of Rajasthan. It is spread across 8 acres (3.2 ha) on either side of the Chittaurgarh–Udaipur highway.[1][2] It was declared as a National Geological Monument by the Geological Survey of India in 1976.[1][3]

Geology

Bhojunda stromatolite is an exposure within the Bhagwanpura limestone of the Lower Vindhyan Age. The Vindhyan Formations are about 900 Ma old. They are formed by blue-green algae which form a mat by attracting and bonding carbonate particles through their filaments into stratiform, columnar and nodular structures in carbonate rocks. Stromatolites are considered evidence of some of the earliest forms of life on Earth and are formed by a combination of life activity, sediment trapping and binding activity of algae and bacteria. They generally develop in shallow-water environments where tidal activity continuously brings sedimentary material. Their discovery in rocks older than the Vindhyan Formations provided important evidence for the existence of life in the Precambrian rocks of Rajasthan.[1]

References

  1. 1 2 3 National Geo-heritage of India (PDF) (Report). Indian National Trust for Art and Cultural Heritage. pp. 98–100. Archived from the original (PDF) on 11 January 2017.
  2. ↑ Sharma, B. K.; Kulshreshtha, Seema; Rahmani, Asad R. (14 September 2013). Faunal Heritage of Rajasthan, India: General Background and Ecology of Vertebrates. Springer Science. p. 233. ISBN 978-1-461-40800-0.
  3. ↑ "Geo-Heritage Sites". Press Information Bureau (Press release). 9 March 2016. Archived from the original on 29 September 2022. Retrieved 1 September 2018.