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6.25" Carboniferous Horestail (Calamites) Fossil Plate - Utah
This is a beautifully preserved plate of horestail tree (Calamites) stems and leaves, the longest of which is 6.25". It was collected from the Manning Canyon Shale located south of Salt Lake City, Utah. A beautiful find!
It comes with an acrylic display stand.
The Manning Canyon Shale is found in central Utah, near Provo. It hosts a number of Carboniferous-era plants, mostly from the Pennsylvanian-Mississippian ages. Over fifty species of plants have been identified out of the site.
It comes with an acrylic display stand.
The Manning Canyon Shale is found in central Utah, near Provo. It hosts a number of Carboniferous-era plants, mostly from the Pennsylvanian-Mississippian ages. Over fifty species of plants have been identified out of the site.
Calamites is the name (form genus) given to compression, impression, and pith casts of Carboniferous sphenophytes, which were arborescent (tree-like) relatives of modern horestails. Calamites typically grew as medium-sized understory trees in Carboniferous swamps, reaching heights of 20-30 meters (60-100 feet).
Similar to today's horsetails, Calamites species were hollow: however, their trunks contained lignin, and likely resembled bamboo in texture. Calamites may be found as cylindrical casts or elongate compressions and impressions. In either form, Calamites often has regular, evenly-spaced grooves or lines running the length of the specimen, or wide, irregularly-spaced nodes.
In some cylindrical casts, small circular bumps appear along the horizontal nodes. These indicate casts of the pith—the central portion of Calamites inside the wood of the stem. Casts of the bark's inner surface outside of the stem wood do not contain bumps.
Calamites sketch from the manuscript Fossil Flora and Fauna of the Pennsylvanian Period, Will County, Illinois
Calamites leaves also have their own form genera. They formed in clusters of 8 or more, called whorls, at spaced nodes along stems. Annularia indicate flat, starburst-shaped whorls, but the shapes of the leaves themselves could vary from oval (A. sphenophylloides) to lanceolate or needle-like (A. radiata). Asterophyllites is another form genus of leaf clusters, but unlike Annularia, they curved upward into a sort of cup shape. Both had midline veins, making them easy to distinguish from other sphenophyte leaf clusters.
A third form genus, Sphenophyllum, is given to leaf clusters that are distinctly triangular, with branching veins radiating from their central nodes. Species with Sphenophyllum forms likely grew as shrubs or smaller plants, unlike Calamites forms.
We use these terms to describe the shapes of fossil imprints. Exact species are often difficult to determine, but these form taxa help in distinguishing the prolific species of sphenophytes that defined the Carboniferous Period.
Similar to today's horsetails, Calamites species were hollow: however, their trunks contained lignin, and likely resembled bamboo in texture. Calamites may be found as cylindrical casts or elongate compressions and impressions. In either form, Calamites often has regular, evenly-spaced grooves or lines running the length of the specimen, or wide, irregularly-spaced nodes.
In some cylindrical casts, small circular bumps appear along the horizontal nodes. These indicate casts of the pith—the central portion of Calamites inside the wood of the stem. Casts of the bark's inner surface outside of the stem wood do not contain bumps.
Calamites sketch from the manuscript Fossil Flora and Fauna of the Pennsylvanian Period, Will County, Illinois
Calamites leaves also have their own form genera. They formed in clusters of 8 or more, called whorls, at spaced nodes along stems. Annularia indicate flat, starburst-shaped whorls, but the shapes of the leaves themselves could vary from oval (A. sphenophylloides) to lanceolate or needle-like (A. radiata). Asterophyllites is another form genus of leaf clusters, but unlike Annularia, they curved upward into a sort of cup shape. Both had midline veins, making them easy to distinguish from other sphenophyte leaf clusters.
A third form genus, Sphenophyllum, is given to leaf clusters that are distinctly triangular, with branching veins radiating from their central nodes. Species with Sphenophyllum forms likely grew as shrubs or smaller plants, unlike Calamites forms.
We use these terms to describe the shapes of fossil imprints. Exact species are often difficult to determine, but these form taxa help in distinguishing the prolific species of sphenophytes that defined the Carboniferous Period.
SPECIES
Calamites sp.
LOCATION
Utah
FORMATION
Manning Canyon Shale
SIZE
Longest Leaf: 6.25" long, Shale: 7.2 x 4.0"
CATEGORY
ITEM
#256842
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