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12.4" Fossil Horsetail (Calamites) Section - Illinois
This is a 12.4" fossil horsetail (Calamites cisti) stalk from the Carbondale Formation near Coal City, Illinois. This specimen was found in multiple pieces and has been repaired back together.
Calamites is a genus of extinct arborescent (tree-like) horsetails to which the modern horsetails are closely related. Unlike their modern cousins, these plants were medium-sized trees, growing to heights of more than 30 meters (100 feet). They were components of the understories of coal swamps of the Carboniferous Period.
Calamanites sketch from the manuscript Fossil Flora and Fauna of the Pennsylvanian Period, Will County, Illinois
The trunks of Calamites had a distinctive segmented, bamboo-like appearance and vertical ribbing. The branches, leaves and cones were all borne in whorls. The leaves were needle-shaped, with up to 25 per whorl.
The stems of modern horsetails are typically hollow or contain numerous elongated air-filled sacs. Calamites was similar in that its trunk and stems were hollow, like wooden tubes. When these trunks buckled and broke, they could fill with sediment. This is the reason pith casts of the inside of Calamites stems are so common as fossils. Calamites would have been covered with a thin outer bark but this is almost never preserved.
Calamites is a genus of extinct arborescent (tree-like) horsetails to which the modern horsetails are closely related. Unlike their modern cousins, these plants were medium-sized trees, growing to heights of more than 30 meters (100 feet). They were components of the understories of coal swamps of the Carboniferous Period.
Calamanites sketch from the manuscript Fossil Flora and Fauna of the Pennsylvanian Period, Will County, Illinois
The trunks of Calamites had a distinctive segmented, bamboo-like appearance and vertical ribbing. The branches, leaves and cones were all borne in whorls. The leaves were needle-shaped, with up to 25 per whorl.
The stems of modern horsetails are typically hollow or contain numerous elongated air-filled sacs. Calamites was similar in that its trunk and stems were hollow, like wooden tubes. When these trunks buckled and broke, they could fill with sediment. This is the reason pith casts of the inside of Calamites stems are so common as fossils. Calamites would have been covered with a thin outer bark but this is almost never preserved.
SPECIES
Calamites cisti
LOCATION
Coal City, Illinois
FORMATION
Carbondale Formation
SIZE
12.4 x 1.6"
CATEGORY
SUB CATEGORY
ITEM
#134870
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