Sigillaria Temporal range: Carboniferous-Permian, Possible Devonian record
Fragment (bark) of Sigillaria sp. displayed at the Houston Museum of Natural Science. Collected from the Anzin Coal Mines, Nord, France.
Scientific classification
Kingdom:	Plantae
Clade:	Tracheophytes
Clade:	Lycophytes
Class:	Lycopodiopsida
Order:	†Lepidodendrales
Family:	†Sigillariaceae
Genus:	†Sigillaria Brongniart (1822)

Sigillaria is a genus of extinct, spore-bearing, arborescent lycophyte, known from the Carboniferous and Permian periods. It is related to the more famous Lepidodendron, and more distantly to modern quillworts.

Fossil records

Sigillaria preserved in the cliffs at Joggins, Nova Scotia, Canada

This genus is known in the fossil records from as early as the Middle Devonian or the Late Carboniferous period ^[1] but dwindled to extinction in the Early Permian period (age range: from 383.7 to 254.0 million years ago).^[2] Fossils are found in Great Britain, United States, Canada, China, Korea, Tanzania and Zimbabwe.^[3]

Description

Sigillaria was a tree-like plant reaching a height up to 30 meters,^[1] with a tall, single or occasionally forked trunk^[2] that lacked wood. Support came from a layer of closely packed leaf bases just below the surface of the trunk, while the center was filled with pith. The long, thin grasslike leaves^[4] were attached directly to the stem and grew ^[1] in a spiral along the trunk.^[2] The old leaf bases expanded as the trunk grew in width, and left a diamond-shaped pattern, which is evident in fossils. These leaf scars were arranged in vertical rows.^[1] The trunk had photosynthetic tissue on the surface, meaning that it was probably green.

The trunk was topped with a plume of long, grass-like, microphyllous leaves,^[4] so that the plant looked somewhat like a tall, forked bottle brush. The plant bore its spores (not seeds) in cone-like structures ^[4] attached to the stem.^[2][5]

Sigillaria, like many ancient lycopods, had a relatively short life cycle - growing rapidly and reaching maturity in a few years. Some researchers have suggested that Sigillaria was monocarpic, meaning that it died after reproduction, though this is not proven.^[4] It was associated with Lepidodendron, the scale tree, in the Carboniferous coal swamps.^[1]

Fossils of Sigillaria trunks are usually connected to a stigmarian root system (lycopsid rhizomes)

Leaf scars are shown between the vertical sections of a Sigillaria

Species

Fossil of Sigillaria trigona, on display at National Museum (Prague)

Species within this genus include:^[6]

Gallery

• 
  Sigillaria on display at State Museum of Pennsylvania, from Sharon, Mercer County, Pennsylvania
• 
  Sigillaria (bark) on display at State Museum of Pennsylvania, from Scranton, Lackawanna County, Pennsylvania
• 
  Replica of Sigillaria sp. at the University of A Coruña
• 
  In situ Lycopsid that is probably Sigillaria from the Pennsylvanian Joggins Formation in Nova Scotia
• 
  Life restoration
• 
  A close-up of the leaf scars on a Sigillaria notata
• 
  Sigillaria mammillaris
• 
  Sigillaria elegans
• 
  Sigillaria restorations

Bibliography

• William A. DiMichele, Richard M. Bateman: The Rhizomorphic Lycopsids: A Case-Study in Paleobotanical Classification. Systematic Botany, 1996, volume 21, pages 535-552.
• Thomas N. Taylor, Edith L. Taylor, Michael Krings: Paleobotany. The Biology and Evolution of Fossil Plants. Second Edition, Academic Press 2009, ISBN 978-0-12-373972-8, pages 303-307
• J. W. Sir Dawson - On the structure and affinities of Sigillaria, Calamites and Calamodendron - Paperback – August 16, 2011 ISBN 1175560871
• Silva Pineda, A. (2003). "Flora del Pérmico de la región de Izúcar de Matamoros, Puebla". En Soto, L. A. Agustín Ayala-Castañares: universitario, impulsor de la investigación científica. UNAM. p. 371. ISBN 9789703207893

References

External links

Wikimedia Commons has media related to Sigillaria.

• Fossil Plants Vol.II
• The Columbia Encyclopedia