The Joggins Formation of Nova Scotia contains an outstanding record of Pennsylvanian tropical ecosystems (Davies et al. 2005). Tree-fern trunks are one of the rarest elements of the plant fossil assemblage. Dawson (1868, p. 486) made cryptic reference to erect, but poorly preserved, Caulopteris tree-fern trunks in the Joggins Formation, but gave no morphological description. This record therefore cannot be confirmed. Dawson (1868, p. 448,486) also discovered a second taxon, Megaphyton magnificum, which he described in detail based on a single specimen. This trunk adpression comprised a root mantle from which protruded well preserved, large (7 cm diameter), contiguous leaf scars arranged in two rows on either side of the trunk (Fig. 1).

Based on Dawson's drawings (which illustrate the specimen upside down), a deep indentation is evident on the abaxial side of the vascular bundle of all of the leaf scars. Pfefferkorn (1976) erected the morphogenus Artisophyton for adpressed specimens of this type showing indented vascular bundles. As Dawson's morphospecies is based on a specimen that is now believed lost, no attempt is made here to formally transfer Megaphyton magnificum, even though it is clear that his specimen belongs to the morphogenus Artisophyton. Despite Dawson's meticulous approach to geological context (Falcon-Lang and Calder 2005), the stratigraphic position of his specimen is unknown.

Subsequent to Dawson's work, only two additional tree-fern trunk specimens have been discovered in the Joggins Formation. A second, similarly unprovenanced, specimen was presented to the Fundy Geological Museum, Parrsboro, Nova Scotia (accession number LF-98P-068) by Laing Ferguson in 1998. It is a poorly preserved trunk impression showing eight, large rectangular leaf scars arranged in a single row (Fig. 2A). The vascular traces are difficult to discern, but at least one appears to show abaxial indentation, a diagnostic feature of Artisophyton. A third specimen of Artisophyton was discovered by the author during a Joggins field trip arranged as part of the North American Paleontology Conference, Halifax, Nova Scotia (June 2005). The tree-fern trunk was observed on a metre-sized sandstone block, located near the high-tide mark at the Lower Cove end of the section. It could not be collected as this would have required heavy moving equipment. The purpose of this note is to document the new specimen and discuss its paleoecology.

The new tree-fern trunk specimen occurs in a multi-storey channel sandstone body within a red mudstone succession (Davies and Gibling 2003), positioned 24-27 m above the base of the formation (Davies et al. 2005). This unit is interpreted as the deposit of a small paleovalley system incised into a well drained floodplain, and infilled by the deposits of anastomosed river channels (Rygel 2005). These sediments record some of the most continental environments in the Joggins Formation, deposited at a time when the marine coastline lay hundreds of kilometres to the east.

Although a few upright calamiteans are rooted on channel margins, most plant fossils are allochthonous in channel bases. Common calamitean and cordaitalean axes and foliage, the latter locally preserved as charcoal (Falcon-Lang 2003), occur with the tree-fern trunk in an allochthonous assemblage. The trunk adpression (9.6 cm diameter, 56 cm in length) comprises a root mantle from which protrudes seven leaf scars (each 3 cm high by 5 cm wide) arranged in a single row, spaced 2-3 cm apart (Fig. 2B). The best-preserved leaf scars have a closed outer bundle with a deep indentation on the abaxial side, or are fully divided into two separate closed traces (Fig. 2C-D). These vascular features are not well defined, but there is sufficient detail to classify the specimen as Artisophyton.

Tree ferns evolved in latest Mississippian times and remained rare during the Early Pennsylvanian (DiMichele and Phillips 2002). Based on trunk dimensions, the three Artisophyton specimens from the Joggins Formation were small trees a few metres high (Fig. 3). Artisophyton probably bore foliage ofSenftenbergia plumosa or Senftenbergia pennaeformis type (Corsin 1948; Bek and Psenicka 2001). These are among the most common fern foliage types in the Cumberland Group, although their occurrence in the Joggins Formation, in particular, is limited (Bell 1944). According to Pfefferkorn (1976) these tree ferns were not marattialeans, but belonged to the family Schizeaceae or to an extinct lineage, the Tedelaceae. The facies context of the only well provenanced Artisophyton specimen indicates that it grew on a well drained, seasonally dry landscape dominated by fire-prone gymnospermous vegetation (Falcon-Lang 2003).

Little is known of the facies occurrence of early monocyclic tree ferns similar to those of the Joggins Formation. DiMicheleand Phillips (1977) described the monocyclic Psaronius sim-plicicaulis from an Early Pennsylvanian bedrock valley-fill succession in Illinois (Leary 1981), where it was associated with an upland/dryland assemblage of cordaitaleans, pterido-sperms, and noeggerathialians (Leary 1975,1993). DiMichele and Phillips (2002) concluded that the tree ferns had occupied poorly drained patches within an otherwise well drained, seasonally dry landscape. A similar ecology is envisaged for the Artisophyton trees based on facies occurrence in the Joggins Formation. This is further supported by the fact that this mor-phogenus has never been observed in coal balls (Pfefferkorn 1976), indicating its absence from poorly drained peat-forming settings. The new discovery in the Joggins Formation is therefore important, showing that at least two unrelated lineages of arborescent ferns, represented by Psaronius and Artisophyton, colonized dry environments in Early Pennsylvanian times.