Equisetum dimorphum

Equisetum dimorphum is an extinct horsetail species of the family Equisetaceae, and one of the oldest records of the genus Equisetum.[1] It was found in rocks from the Lower Jurassic of Chubut, Argentina, among other plants as ferns, conifers and pteridosperms. Their remains consist on stems, leaves, strobili, and pagoda structures, which are preserved as impressions and casts. The combination of fine grained sediment, and the probable silica deposits in the epidermis of the plant, have managed to conserve not only its gross morphology, but also epidermal details not often present in this kind of preservation. This species was described in 2015 in Ameghiniana by a team led by Andres Elgorriaga, that included investigators of the Museum of Paleontology Egidio Feruglio, the Swedish Museum of Natural History, and the Buenos Aires University.[1]

Equisetum dimorphum
Temporal range: Pliensbachian
↓
Scientific classification
Kingdom: Plantae
Clade: Tracheophytes
Class: Polypodiopsida
Subclass: Equisetidae
Order: Equisetales
Family: Equisetaceae
Genus: Equisetum
Species:
†E. dimorphum
Binomial name
†Equisetum dimorphum
Elgorriaga

Description

The stems are dimorphic, unbranched and present no sign of superficial ribs and valleys. They are hollow except at the nodal regions, where complex nodal diaphragms occur. The diaphragms are flat, with a pitted surface and a cart-wheel internal structure. Each node is covered by a leaf sheath, bearing up to 42 lanceolate leaves. The sheaths are fused nearly 75% of the leaf length, having a distinct commisural furrows dividing the individual leaves. The stem apices are usually topped with a pagoda-like structure formed by detached leaves from the nodes below. The strobili occur singly at the apex of reproductive stems, they are elliptic to oblong, with a rounded apex, and bear numerous whorls of hexagonal sporangiophores. The leaves present on the reproductive stems are far longer than normal ones. Stomata occur in broad bands, both superficially and sunken.[1]

Morphological curiosities

One of the most notable features of this species is the presence of pagoda-like structures at the tip of its stems. This kind of structures are also present in one living species, Equisetum hyemale, and are formed thanks to the unique type of growth that this group process, with intercalary meristems at the base of each node.[2]

Another feature of this species is the presence of twin stems, result of a dichotomy of the main stems. This kind of feature was also noted in E. hyemale.[3]

Subgeneric placement

This species possess characters from both present day subgenus. It shares with the Equisetum genus the rounded strobilar apex and the dimorphic habit. It shares with the Hippochaete subgenus its dimorphic habit, the absence of branches, and the presence of pagoda structures. This species also shares characters with both subgenus at the same time, such as the position of stomata and the absence and presence of leaf tips. As Equisetum thermale,[4] another Jurassic fossil Equisetum from Argentina, E. dimorphum shows a combination of characters from both living subgenera, Equsietum and Hippochaete. There are two other Equisetum species, very similar to E. dimorphum, that also possess this mosaic of characters, and perhaps the three species belong to a previously unidentified fossil subgenus.[1]

References
  1. Elgorriaga, A.; Escapa, I. H.; Bomfleur, B.; Cúneo, R.; Ottone, E. G. (2015). "Reconstruction and phylogenetic significance of a new Equisetum linnaeus species from the Lower Jurassic of Cerro Bayo (Chubut Province, Argentina)". Ameghiniana. 52 (1): 135–152. doi:10.5710/AMGH.15.09.2014.2758.
  2. Page, C. N. (1997). "The ferns of Britain and Ireland. Cambridge Univer- sity Press, Cambridge, 540 p.". Cite journal requires |journal= (help)
  3. Schaffner, J. (1924). "Dichotomous branching in Equisetum". American Fern Journal. 14: 56–57. doi:10.2307/1544720.
  4. Channing, A.; Zamuner, A.; Edwards, D.; Guido, D. (2011). "Equisetum thermale sp. nov. (Equisetales) from the Jurassic San Agustin hot spring deposit, Patagonia: Anatomy, paleoecology, and inferred paleoecophysiology". American Journal of Botany. 98 (4): 680–697. doi:10.3732/ajb.1000211. PMID 21613167.
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