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Fossil leaf miner

Fossil leaf miner


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Fossil leaf miner

A leaf miner has left a snaking trail in this leaf from the Middle Eocene of Bournemouth, England

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Media ID 8612541

© Mary Evans Picture Library 2015 - https://copyrighthub.org/s0/hub1/creation/maryevans/MaryEvansPictureID/10709048

Black Background Cenozoic Damage Davis Dr Paul Davis Eocene Fossil Fossilised Honeyeater Kenrick Meliphagidae Miner Palaeogene Passeriformes Passerine Paul Kenrick Phanerozoic Prehistoric Sauropsid Sauropsida Specimen Tertiary


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EDITORS COMMENTS
In this fossil specimen, we witness the intriguing remnants of a Fossil Leaf Miner's (Dr. Paul Davis's discovery) passage through a Middle Eocene leaf from the Bournemouth, England formation. The leaf, now a part of the extensive record of the Tertiary period, bears the unmistakable signs of the ancient miner's presence. The leaf, with its once vibrant green color now faded, displays a sinuous, snaking trail left behind by the miner's relentless excavations. This trail, a testament to the passage of time and the tenacity of life, is a poignant reminder of the intricate relationships that existed between organisms during the Phanerozoic Convergence, a critical period in Earth's biosphere when modern groups of animals first appeared. The leaf miner, a member of the Sauropsida clade, is believed to have been a precursor to modern birds, specifically a passerine or perching bird. More precisely, it has been identified as a member of the Meliphagidae family, which includes honeyeaters. This identification is based on the morphology of the leaf damage, which resembles that caused by modern leaf miners in the same family. The leaf, a precious relic from the Cenozoic Era, now rests against a black background, its intricate details brought to life under the expert hand of palaeontologist Dr. Paul Davis. The studio shot showcases the delicate balance between the destructive actions of the leaf miner and the resilience of the leaf, offering a glimpse into the complex web of life that existed during the Paleogene Period.

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