Earth

Scientists study practical applications of fossils that emit radiation

28.09.2021. Palaeobologist Daniel Tyborowski (L) from the Museum of the Earth and Dr. Magdalena Długosz-Lisiecka (R) from the Faculty of Chemistry of the Lodz University of Technology during a press conference at the Museum of the Earth of the Polish Academy of Sciences in Warsaw. Credit: PAP/Marcin Obara
28.09.2021. Palaeobologist Daniel Tyborowski (L) from the Museum of the Earth and Dr. Magdalena Długosz-Lisiecka (R) from the Faculty of Chemistry of the Lodz University of Technology during a press conference at the Museum of the Earth of the Polish Academy of Sciences in Warsaw. Credit: PAP/Marcin Obara

Polish scientists who have discovered that fossils emit radiation are now trying to find practical uses of the find, and to find out how many on the market are fakes.

Researchers from the Museum of the Museum of the Earth in Warsaw, the Institute of Radiation Technology at the Lodz University of Technology and the Geological Museum at the University of Lodz used a gamma radiation spectrometer to analyse several dozen fossils, mainly from the collection of the Geological Museum in Łódź. 

They found uranium 238 and 235 and their derivatives - thorium 238 coming from the oldest from a few hundred million years ago, including Palaeozoic invertebrates (corals), and the youngest from several dozen thousand-year-old Pleistocene megafauna bones (including mammoth, woolly rhinoceros and cave bears). 

The fossils come from various regions of the world, including Poland, France and Morocco.

Dr. Daniel Tyborowski from the Museum of the Earth in Warsaw said: “The radiation emitted by our specimens is not harmful.

“We found that the radiation values of fossils significantly differed from each other. Fossils that contained phosphorus radiated more strongly. Vertebrates have a phosphate skeleton, which causes higher radiation values. And indeed, when we analysed the bones of Pleistocene mammals (mammoth, rhinoceros) are these specimens had increased radiation values.”

28.09.2021.Paleobiolog Daniel Tyborowski (L) z Muzeum Ziemi oraz dr hab. Magdalena Długosz-Lisiecka (P) z wydziału chemii Politechniki Łódzkiej podczas konferencji prasowej w Muzeum Ziemi Polskiej Akademii Nauk w Warszawie. Fot. PAP/ Marcin Obara
28.09.2021. Palaeobologist Daniel Tyborowski (L) from the Museum of the Earth and Dr. Magdalena Długosz-Lisiecka (R) from the Faculty of Chemistry of the Lodz University of Technology during a press conference at the Museum of the Earth of the Polish Academy of Sciences in Warsaw. Credit: PAP/Marcin Obara

He added that the amount of radiation depended on the environment in which the fossils formed and the type of sedimentation, in which they were fossilised.

28.09.2021. Paleobiolog Daniel Tyborowski z Muzeum Ziemi podczas konferencji prasowej w Muzeum Ziemi Polskiej Akademii Nauk w Warszawie. Fot. PAP/ Marcin Obara
28.09.2021. Palaeobologist Daniel Tyborowski from the Museum of the Earth during a press conference at the Museum of the Earth of the Polish Academy of Sciences in Warsaw. Credit: PAP/Marcin Obara

Radiation levels were particularly high in fossils from Morocco. Tyborowski said: “This place is famous for outcrops of phosphate rocks. Specimens in the form of shark or mosasaur teeth found in those rocks had higher radiation values. This means that the fossilisation environment is crucial for the radiation level.”

High values were also recorded in the case of 160 million year old fossils of invertebrates from France, including ammonites and oysters that do not have phosphate skeletons. Dr. Tyborowski said: “They were preserved to our times thanks to the phosphatisation phenomenon. Originally their skeleton was carbonate, but the processes in rock preserved them thanks to the inflow of phosphates from the environment - this is phosphatisation.”

Dr Daniel Tyborowski prezentuje amonit, fot. Karolina Jackowiak-Konopska.
Dr. Daniel Tyborowski presents an ammonite, credit: Karolina Jackowiak-Konopska.

Although different radioactive isotopes are used in geology and Earth sciences to determine the age of geological layers (mainly magma rocks), until now they were not used to determine the age of the fossil. 

But although that still seems a distant prospect as, according to Tyborowski “preliminary analyses show that the radiation level does not depend on the age of fossils,” they could be used to determine if the specimen is a counterfeit.

Ząb mozazaura z Maroka mierzony radiometrem, fot. Magdalena Długosz-Lisiecka.
Mosasaur tooth from Morocco measured by a radiometer, credit: Magdalena Długosz-Lisiecka.

He continued: “Moroccan specimens, which are very popular on markets and auctions, often turn out to be counterfeit. Moroccans specialize in creating excellent counterfeits. The technological process, in which the counterfeit is made, has different isotopic signatures that can be captured with specialized equipment.”

He added that the discovery could also be used to search for radiation emitted by phosphatised specimens, for example in a quarry.

Amonit z okresu jury z Francji, jeden z radioaktywnych, sfosfatyzowanych okazów, fot. Magdalena Długosz-Lisiecka.
Ammonite from the Jurassic period from France, one of the radioactive, phosphatised specimens, credit: Magdalena Długosz-Lisiecka.

According to Tyborowski, the research has high potential thanks to the interdisciplinary research team that includes a palaeobologist, a radiation chemist and a geologist.

The phenomenon of fossil radiation (dinosaur bones) was reported a few dozen years ago by Professor Zbigniew Jaworowski. 

But according to Dr. Tyborowski, the information was treated as a curiosity at the time and the reasons for the phenomenon were not explained, because Beta radiation was discovered by accident.

The publication appeared in the prestigious journal Chemosphere (https://doi.org/10.1016/j.chemosphere.2021.131444).

PAP - Science in Poland, Szymon Zdziebłowski

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