Earth’s Original Land Tree Plant

Was the “Calamite” the first tree-like plant to grow on land? Many scientists believe so. It grew as high as 100 feet, towering above its counterparts in the earlier periods of its lengthy lifespan, which began some whopping 400 million years ago during the Devonian Period.

Annularia Leaf Imprint Trace Fossil of Prehistoric Calamite Tree

The trunk was a woody hollow tube, lacking true bark. The leaves were primitive and needle like, arranged in whorls around a stem.

Trace Fossil Imprint of Prehistoric Calamite Tree 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.

Internal and External Imprint Fossil of Calamite Tree Stem

These amazing fossils 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.

Prehistoric Calamite (Earth’s First Tree-Like Land Plant) Rendition Drawing


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, as their modern descendants are the “horsetails” of today, growing in open fields and edges of woodlands, but only reaching a few feet tall. See photo below


The “horsetail” or Equisetum is an amazing living fossil related to the Calamites, being the only surviving genus from the entire class of Equisetopsida. For over one hundred million years, the Equisetopsidas were much more diverse and dominated the understory of the late Paleozoic forests. Through the millenniums, they decomposed layer by layer, transforming into the sunken coal deposits of today.