KFU. Card publication. On the possibility of introducing X-ray computed microtomography into the practice of biostratigraphic research

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FEDERAL UNIVERSITY

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ON THE POSSIBILITY OF INTRODUCING X-RAY COMPUTED MICROTOMOGRAPHY INTO THE PRACTICE OF BIOSTRATIGRAPHIC RESEARCH

Form of presentation

Articles in Russian journals and collections

Year of publication

2021

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Authors, employees of KFU

Kadyrov Rail Ilgizarovich, author

Stacenko Evgeniy Olegovich, author

Bibliographic description in the original language

Fazliakhmetov A.M. et al. On the possibility of introducing X-ray computed microtomography into the practice of biostratigraphic research / Fazliakhmetov, A. M., Artyushkova, O. V., Statsenko, E. O., Kadyrov, R. I. // Georesursy. -. Georesursy LLC, 2021. -. Vol. 23, No. 4. P. 12–20

Annotation

Currently, the techniques applied for extraction and study of conodonts from siliceous rocks are associated with a number of problems. This makes it difficult to solve many problems in the areas of development of the volcanic and volcanic-sedimentary rocks, where cherts, jaspers, and phtanites are the only sedimentary formations for dating these deposits. On X-ray computed microtomography it is possible to avoid some problems to obtain not only excellent 3-D images of conodonts, but sections in any direction too, as well as in video formats. It is shown that similar results are successful under the hollows after the dissolution of the conodonts. There is no problem in application of X-ray microcomputed tomography when conodonts have been already found on the surface or inside of the sample, or if the content of conodonts in the rock is obviously high. In such a case the scanning without preliminary search is ensured. In cases when conodonts are rare and not obvious, it is proposed the following technique of their discovery. The rock sample is cut into plates. The conodonts are search for on the surface of the plates, moistened with a mixture of glycerin and water under a binocular microscope. If it is necessary (when the rock is opaque), the result is checked by a chemical reaction: 5–10 % hydrochloric acid plus 1–2 crystals of ammonium molybdate are put on the surface of the sample. The appearance of a yellow sediment means the presence of phosphorus, to indicate the probability the detected object to be a conodont. Next, the sample should be washed from acid, its size should be decreased. Then the microtomographic study should be performed.

Keywords

Biostratigraphy; Conodonts; X-ray computed tomography; μCT

The name of the journal

GEORESURSY

URL

https://geors.ru/media/pdf/02_Fazliakhmetov_en.pdf

Please use this ID to quote from or refer to the card

https://repository.kpfu.ru/eng/?p_id=297851&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Kadyrov Rail Ilgizarovich	ru_RU
dc.contributor.author	Stacenko Evgeniy Olegovich	ru_RU
dc.date.accessioned	2021-01-01T00:00:00Z	ru_RU
dc.date.available	2021-01-01T00:00:00Z	ru_RU
dc.date.issued	2021	ru_RU
dc.identifier.citation	Fazliakhmetov A.M. et al. On the possibility of introducing X-ray computed microtomography into the practice of biostratigraphic research / Fazliakhmetov, A. M., Artyushkova, O. V., Statsenko, E. O., Kadyrov, R. I. // Georesursy. -. Georesursy LLC, 2021. -. Vol. 23, No. 4. P. 12–20	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=297851&p_lang=2	ru_RU
dc.description.abstract	GEORESURSY	ru_RU
dc.description.abstract	Currently, the techniques applied for extraction and study of conodonts from siliceous rocks are associated with a number of problems. This makes it difficult to solve many problems in the areas of development of the volcanic and volcanic-sedimentary rocks, where cherts, jaspers, and phtanites are the only sedimentary formations for dating these deposits. On X-ray computed microtomography it is possible to avoid some problems to obtain not only excellent 3-D images of conodonts, but sections in any direction too, as well as in video formats. It is shown that similar results are successful under the hollows after the dissolution of the conodonts. There is no problem in application of X-ray microcomputed tomography when conodonts have been already found on the surface or inside of the sample, or if the content of conodonts in the rock is obviously high. In such a case the scanning without preliminary search is ensured. In cases when conodonts are rare and not obvious, it is proposed the following technique of their discovery. The rock sample is cut into plates. The conodonts are search for on the surface of the plates, moistened with a mixture of glycerin and water under a binocular microscope. If it is necessary (when the rock is opaque), the result is checked by a chemical reaction: 5–10 % hydrochloric acid plus 1–2 crystals of ammonium molybdate are put on the surface of the sample. The appearance of a yellow sediment means the presence of phosphorus, to indicate the probability the detected object to be a conodont. Next, the sample should be washed from acid, its size should be decreased. Then the microtomographic study should be performed.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject		ru_RU
dc.title	On the possibility of introducing X-ray computed microtomography into the practice of biostratigraphic research	ru_RU
dc.type	Articles in Russian journals and collections	ru_RU