30,000-Year-Old Vulture Feathers Discovered, Uniquely Preserved in Volcanic Ash
Fossilised feathers of a 30,000-year-old griffon vulture have been found in a remarkable state of preservation, with details unlike any previously recorded. The discovery, made in the Colli Albani volcanic complex near Rome, Italy, has intrigued scientists for decades. The remains, which include traces of the bird’s wing feathers and eyelids, were first unearthed in 1889. Until now, the preservation process remained unexplained. New research suggests that the feathers were encased in volcanic ash, later transforming into silicon-rich zeolite crystals, which retained the structure of the vulture’s delicate tissues. This marks the first instance of such preservation occurring in volcanic material.
Unprecedented Preservation Through Zeolite Crystals
According to the study published in Geology, an analysis using electron microscopes and chemical testing revealed that the feathers were fossilised in three-dimensional form. This contrasts with the usual fossilization process, where feathers leave two-dimensional carbon imprints. Previously, three-dimensional feather fossils had only been identified in amber. The research team, led by Valentina Rossi, a paleobiologist at University College Cork in Ireland, found that zeolite minerals had played a critical role in maintaining the feathers’ microscopic details. Speaking to Live Science, Rossi described the discovery as unique, highlighting that feathers preserved in volcanic ash had never been documented before.
Burial in Volcanic Ash Preserved Delicate Features
The fossil, initially discovered by a landowner in the foothills of Mount Tuscolo, had been noted for its unusual preservation in volcanic rock. Over time, much of the specimen was lost, leaving only part of one wing, the head, and the neck. Recent reanalysis identified even finer details, including the structure of the vulture’s eyelids and skin. According to Dawid Iurino, associate professor in vertebrate paleontology at the University of Milan, the bird was likely buried in a low-temperature pyroclastic deposit. He explained to Live Science that while volcanic environments typically destroy organic material, certain conditions allowed soft tissues to be fossilised at a cellular level.
Potential for More Fossil Discoveries in Volcanic Rock
The study suggests that the preservation process occurred within days, as the ash reacted with water and gradually formed zeolite crystals that replaced the biological structures. Maria McNamara, professor of paleontology at University College Cork, told Live Science that the findings could expand the scope of fossil research. She noted that delicate tissues had not previously been expected to survive in volcanic rock, opening new possibilities for similar discoveries in the future.
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The deformed rocks of Iran are formed due to strong mountain ridges and valleys in the Greater Caucasus mountain range, southwest of the Caspian Sea. Between 10 million and 50 million years ago, its growth was marked by sedimentary layers crushed during the first impact between the Arabian and Eurasian tectonic plates. The vividly coloured rocks produced by the sedimentary layers gathered over millennia range in tone from terracotta to greenish to bluish. Using satellite pictures, NASA’s Jet Propulsion Laboratory and Earth Observatory have shown how the landscape tended to cluster over time.
One image depicts the different strata layers, vegetation, and the Zanjan-Tabriz freeway linking Tehran and Poznan. Interestingly, another image is of the Qezel Ozan River, which provides agricultural water in the region. The region is still converging, and fresh research suggests that a slab of oceanic crust is being shredded beneath Iraq and Iran.
Iran’s Folded Rocks Expose Arabia-Eurasia Tectonic Collision
According to reported NASA experts, a tectonic clash between the continents — known as Eurasia and Arabia — crunched these vividly hued strata of rock into massive folds. Located southwest of the Caspian Sea, Iran’s folded rocks are mountain ridges and valleys from the Greater Caucasus mountain chain. The disrupted rocks are made of sedimentary layers that were tilted and folded after the first collision between the Arabian and Eurasian tectonic plates, which is estimated to have occurred 10 to 50 million years ago.
Under Iraq and Iran, some of the oceanic crust between the Arabian and Eurasian plates is breaking apart, according to current research, which results in an anomalous silt accumulation at the surface. The complexity of the Earth’s surface and the Qezel Ozan River, combined with the Neotethys oceanic plate pulling the area down, account for this.
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