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Evidence of Impact at the Permian/Triassic Boundary from Mössbauer Spectroscopy
Authors:Verma  H. C.  Upadhyay  C.  Tripathi  R. P.  Shukla  A. D.  Bhandari  N.
Affiliation:(1) Department of Physics, Indian Institute of Technology, Kanpur, 208016, India;(2) Department of Physics, Jai Narain Vyas University, Jodhpur, 342001, India;(3) Physical Research Laboratory, Navrangpura, Ahmedabad, 380009, India
Abstract:

Sediment samples from Spiti valley, India, deposited about 250 Million years ago during the Permian-Triassic transition, have been analysed. 57Fe Mössbauer spectroscopic studies show that iron occurs mainly as nanoparticles of hematite and goethite with a broad size distribution. The results show a high degree of resemblance with the Cretaceous-Tertiary boundary (65 My) samples where an asteroidal impact is believed to have caused mass extinction.

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