Was the “Calamite” the first tree-like plant to grow on land? Many scientists believe so. It possibly grew up to 100 feet (30 meters) tall, towering above the sparse landscape during its lengthy lifespan. Its earliest beginnings were approximately 400 million years ago during the Devonian Time Period. But this tree-like species trived particularly during the tropical coal swamps of the carboniferous era before it went extinct.

The trunk was a woody hollow tube, lacking true bark. There were various species that resembled modern day bamboo with segments and ribbing. The leaves were primitive and needle like, arranged in whorls around a stem.

The Calamite thrived in the hot swamp tropics of the past, particularly during the Pennsylvanian Period around 300 mya. Many of their fossils have been found worldwide including, USA, China, Canada, South America and Europe.

The three amazing fossils above were found in Sebastian County, Arkansas in an old coal strip mine in 1993 by Michael A. Whitkanack, who donated them to my classroom. They are actually the imprints of the Calamite’s leaves and stems which scientists refer to as trace fossils.

 CLASSIFICATION

Scientific Name: Calamite Common Name: Horsetail / Wiskfern

Kingdom: Plantae

Division: Pteridophyta (Ferns, reproduce by spores)

Class: Sphenopsida or Equisetopsida (means ribbed, vertical jointed stem; bamboo like in appearance)

Order: Equisetales

Family: Calamitaceae

Genus:  (STEM) Calamite (LEAF) Annularia

Special Note: The Calamite may look familiar to some. Their modern descendants are the “horsetails” of today. They grow in open fields and edges of woodlands, but only reach a few feet tall, as seen in the photo below.

The “horsetail” or Equisetum is an amazing living fossil related to the Calamites, the only surviving genus from the entire class of Equisetopsida. For millions of years, the Equisetopsidas were much more diverse and flouished during the late Paleozoic, Permian and Carboniferous forests. Through the millenniums, they decomposed layer by layer, sinking deep and eventually contributing to the coal deposits of today.

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