Evaluation of Degree of Alteration in Fossil Ostracods from Middle Callovian-Lower Oxfordian Beds of Southern Part of Kachchh Basin, Gujarat, India by Characterizing Surface Roughness of the Shell-Reference-Cited by-同舟云学术

Evaluation of Degree of Alteration in Fossil Ostracods from Middle Callovian-Lower Oxfordian Beds of Southern Part of Kachchh Basin, Gujarat, India by Characterizing Surface Roughness of the Shell

Published:2023-10-25 Issue:10 Volume:99 Page:1445-1457
ISSN:0974-6889
Container-title:Journal of the Geological Society of India
language:en
Short-container-title:J Geol Soc India

Author:

Muduli Ganesh Prasad,Kumari Manisha,Mahalakshmi T.

Publisher

Springer Science and Business Media LLC

Subject

Geology

Link

https://link.springer.com/content/pdf/10.1007/s12594-023-2491-x.pdf

Reference42 articles.

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2. Ainsworth, N.R., Burnett, R.D. and Kontrovitz, M. (1990) Ostracod colour change by thermal alteration, offshore Ireland and Western UK. Mar. Pet. Geol., v.7(3), pp.288–297. doi:https://doi.org/10.1016/0264-8172(90)90006-3.

3. Alberti, M., Fürsich, F. T. and Pandey, D.K. (2012) The Oxfordian stable isotope record (ä 18O, ä 13C) of belemnites, brachiopods, and oysters from the Kachchh Basin (western India) and its potential for palaeoecologic, palaeoclimatic, and palaeogeographic reconstructions. Palaeogeogr. Palaeoclimatol. Palaeoecol, v.344–345, pp.49–68. doi:https://doi.org/10.1016/j.palaeo.2012.05.018.

4. Alberti, M., Fürsich, F. T., Pandey, D. K., Mukherjee, D., Andersen, N. and Garbe-Schönberg, D. (2022) Middle to Late Jurassic stable isotopes and element ratios of fossils from western India: Developing a reference temperature curve for northeastern Gondwana. Glob. Planet. Change., 212(November 2021). doi:https://doi.org/10.1016/j.gloplacha.2022.103795

5. Andreu, B., Colin, J.-P. and Singh, J. (2012) Middle and Upper Jurassic Ostracods from Western Kachchh, Gujarat, India: Biostratigraphy and paleobiogeography. Gondwana Res., v.22(3–4), pp.1110–1124. doi:https://doi.org/10.1016/j.gr.2012.01.005

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