يكشف رواسب أحفورية عمرها 400 مليون عام عن الحياة المبكرة

كشفت التكنولوجيا المتطورة عن رؤى جديدة حول كنز أحفوري مشهور عالميًا قد يوفر دليلاً هامًا على الحياة المبكرة على الأرض.

أفاد العلماء الذين يدرسون رواسب أحفورية عمرها 400 مليون عام تم اكتشافها في شمال شرق اسكتلندا النائي أن نتائجهم تظهر درجة أكبر من الحفظ الجزيئي في هذه الحفريات مما كان متوقعًا في السابق.

ساعدت دراسة جديدة للكنوز المحفوظة بشكل رائع من أبردينشاير العلماء على تحديد البصمات الكيميائية لمختلف الكائنات التي تحتوي عليها.

تمامًا كما ساعد حجر رشيد علماء المصريات في فك رموز الهيروغليفية ، يأمل الفريق أن تساعدهم هذه الرموز الكيميائية على فهم المزيد عن هوية أشكال الحياة التي تمثلها الحفريات الغامضة الأخرى.

تم اكتشاف نظام بيئي أحفوري رائع بالقرب من قرية Rainey في أبردينشاير في عام 1912 ، ممعدن ومغطى بالصخور – صخرة صلبة مكونة من السيليكا. ولعبت ، التي يطلق عليها اسم Rhynie Chert ، دورًا مهمًا في فهم العلماء للحياة على الأرض منذ أوائل العصر الديفوني – قبل حوالي 407 ملايين سنة.

جمع الباحثون بين تحليل البيانات وأحدث صور التصوير غير المدمرة[{” attribute=””>machine learning to analyze fossils from collections held by National Museums Scotland and the Universities of Aberdeen and Oxford. Scientists from the University of Edinburgh were able to probe deeper than has previously been possible, which they say could reveal new insights about less well-preserved samples.

Employing a technique known as FTIR spectroscopy – in which infrared light is used to collect high-resolution data – researchers found impressive preservation of molecular information within the cells, tissues, and organisms in the rock.

Since they already knew which organisms most of the fossils represented, the team was able to discover molecular fingerprints that reliably discriminate between fungi, bacteria, and other groups.

These fingerprints were then used to identify some of the more mysterious members of the Rhynie ecosystem, including two specimens of an enigmatic tubular “nematophyte”.

These strange organisms, which are found in Devonian – and later Silurian – sediments have both algal and fungal characteristics and were previously hard to place in either category. The new findings indicate that they were unlikely to have been either lichens or fungi.

Dr. Sean McMahon, Chancellor’s Fellow from the University of Edinburgh’s School of Physics and Astronomy and School of GeoSciences, said: “We have shown how a quick, non-invasive method can be used to discriminate between different lifeforms, and this opens a unique window on the diversity of early life on Earth.”

The team fed their data into a machine learning algorithm that was able to classify the different organisms, providing the potential for sorting other datasets from other fossil-bearing rocks.

The study, published in Nature Communications, was funded by The Royal Society, Wallonia–Brussels International, and the National Council of Science and Technology of Mexico.

Dr Corentin Loron, Royal Society Newton International Fellow from the University of Edinburgh’s School of Physics and Astronomy said the study shows the value of bridging paleontology with physics and chemistry to create new insights into early life.

“Our work highlights the unique scientific importance of some of Scotland’s spectacular natural heritage and provides us with a tool for studying life in trickier, more ambiguous remnants,” Dr. Loron said.

Dr. Nick Fraser, Keeper of Natural Sciences at National Museums Scotland, believes the value of museum collections for understanding our world should never be underestimated.

He said: “The continued development of analytical techniques provides new avenues to explore the past. Our new study provides one more way of peering ever deeper into the fossil record.”

Reference: “Molecular fingerprints resolve affinities of Rhynie chert organic fossils” by C. C. Loron, E. Rodriguez Dzul, P. J. Orr, A. V. Gromov, N. C. Fraser and S. McMahon, 13 March 2023, Nature Communications.
DOI: 10.1038/s41467-023-37047-1