Calamites sp. giant horsetail trunk
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Calamites sp. giant horsetail trunk
320-290 million year old specimen of a giant horsetail fern trunk from the Late Carboniferous period, U.K
Mary Evans Picture Library makes available wonderful images created for people to enjoy over the centuries
Media ID 8581355
© Mary Evans Picture Library 2015 - https://copyrighthub.org/s0/hub1/creation/maryevans/MaryEvansPictureID/10709931
Calamites Carboniferous Equisetales Equisetopsida Equisetum Fern Horsetail Paleozoic Phanerozoic Polypodiophyta Prehistoric Pteridophyta Pteridophyte Trunk United Kingdom Calamitaceae Equisetaceae Giant Horsetail
EDITORS COMMENTS
1. Title: "A Glimpse into the Past: The colossal Calamites sp. Horsetail Trunk from the Late Carboniferous Period, United Kingdom" 2.. This photograph showcases an extraordinary fossil discovery from the Late Carboniferous period, around 320-290 million years ago, unearthed in the United Kingdom. The subject of this image is the colossal trunk of a Calamites sp., a prehistoric horsetail fern belonging to the Equisetaceae family, within the Pteridophyta division. 3. During the Paleozoic Era, Calamites sp. were among the most prominent and widespread plants, thriving in wetland environments. These ancient ferns could grow up to 10 meters tall and were characterized by their hollow, jointed stems, resembling modern-day horsetails. 4. The Calamites sp. trunk in this photograph is a testament to the remarkable growth and resilience of these ancient organisms. The fossilized structure exhibits the distinct ring patterns typical of horsetail trunks, which were formed by the annual growth of new tissues. 5. The Calamites sp. is an essential component of the Equisetopsida, a subclass of the Pteridophyta, which also includes modern horsetails and their close relatives, the spike mosses. This discovery offers a unique window into the prehistoric world, providing valuable insights into the evolution of vascular plants and the development of complex vegetation ecosystems. 6. The discovery of this fossilized Calamites sp. trunk in the United Kingdom is a reminder of the rich biosphere that once existed during the Phanerozoic Coniferous period. It underscores the importance of preserving and studying fossils to better understand the Earth's natural history and the origins of the diverse plant life we observe today.
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