Protobarinophyton obrutschevii
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Protobarinophyton obrutschevii
The fossilised leafless stems of Protobarinophyton obrutschevii topped by a cone-like array of sopre sacs. Approximately 3 mm wide. This specimen was discovered in north-east Siberia and dates to the Devonian
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Media ID 8578081
© Mary Evans Picture Library 2015 - https://copyrighthub.org/s0/hub1/creation/maryevans/MaryEvansPictureID/10703834
Devonian Fossil Fossilised Kenrick Lycopod Lycopodiophyta Paleozoic Paul Kenrick Phanerozoic Prehistoric Siberia Spore
EDITORS COMMENTS
1. Title: "Ancient Wonders: The Fossilized Stems of Protobarinophyton obrutschevii from the Devonian Period of Siberia" 2.. This image showcases the fossilized leafless stems of Protobarinophyton obrutschevii, a remarkable discovery from the ancient world. Dating back to the Devonian Period, around 375 million years ago, this specimen was unearthed in the remote and enigmatic region of north-east Siberia. The stems, approximately 3 mm wide, bear a unique cone-like array of spore sacs at their tips, a characteristic feature of this extinct plant species. Protobarinophyton obrutschevii is classified as part of the Lycopodiophyta division, more specifically within the Zosterophyllopsida class. These prehistoric plants, also known as lycopods or clubmosses, were among the first terrestrial plants to develop complex vascular systems, enabling them to transport water and nutrients from the ground to their above-ground structures. The discovery of this fossil adds valuable insights into the evolution of terrestrial vegetation during the Paleozoic Era, a critical period in Earth's biosphere. The fossilized remains of Protobarinophyton obrutschevii, along with other ancient organisms, help us piece together the intricate puzzle of life's development on our planet. Paul Kenrick, a renowned paleobotanist, has extensively studied these ancient plants, shedding light on their morphology, ecology, and evolutionary relationships. This image serves as a testament to the rich history of life on Earth and the ongoing quest to unravel its mysteries. The Devonian Period marks the transition from the Paleozoic to the Mesozoic Eras, a time of significant biospheric changes. The discovery of this fossilized specimen in Siberia adds another fascinating chapter to the story of life on Earth, further emphasizing the importance of preserving and studying our planet's natural history.
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