Cranfillia vulcanica (Blume) Gasper & V.A.O.Dittrich, 2016

Gasper, André Luís De, Dittrich, Viníciusantonio De Oliveira, Smith, Alan R. & Salino, Alexandre, 2016, A classification for Blechnaceae (Polypodiales: Polypodiopsida): New genera, resurrected names, and combinations, Phytotaxa 275 (3), pp. 191-227 : 208

publication ID

https://doi.org/ 10.11646/phytotaxa.275.3.1

persistent identifier

https://treatment.plazi.org/id/0D7187AA-7D6A-FF9B-AF83-FD784CD0F9B8

treatment provided by

Felipe

scientific name

Cranfillia vulcanica (Blume) Gasper & V.A.O.Dittrich
status

 

12. Cranfillia vulcanica (Blume) Gasper & V.A.O.Dittrich View in CoL , comb. nov. — Lomaria vulcanica Blume, Enum. Pl. Javae 202. 1828. — Blechnum vulcanicum (Blume) Kuhn, Ann. Mus. Bot. Lugduno-Batavi 4: 284. 1869.

Diploblechnum Hayata, Bot. Mag. View in CoL (Tokyo) 41: 702. 1927. — Type: Diploblechnum fraseri (A.Cunn.) De Vol, Fl. View in CoL Taiwan 1: 153. 1975. Figs. 3H View FIGURE 3 , 6E View FIGURE 6 .

Pteridoblechnum Hennipman, Blumea 13: 397. 1966. — Type: Pteridoblechnum neglectum (F.M.Bailey) Hennipman. View in CoL

Steenisioblechnum Hennipman, Blumea 30: 17. 1984. — Type: Steenisioblechnum acuminatum (C.T.White & Goy) Hennipman. View in CoL

Plants terrestrial; rhizomes slender, long- to short-creeping, or caudices erect, densely clothed at apices with bicolorous, linear-acuminate or lanceolate, entire or sparingly toothed scales; fronds dimorphic or slightly dimorphic; stipes slender, short, brown to reddish, densely scaly proximally, fewer persistent scales distally; blades concolorous, ovate to narrowly elliptic, pinnate to deeply pinnatifid, or bipinnatisect to bipinnate, usually becoming bipinnatifid distally, proximal pinnae gradually to abruptly reduced with one or two pairs of pinnae, or abruptly reduced to winged lobes extending down rachis, apical portions of the blades pinnatifid; rachises with sparse scales; buds sometimes present in axils of distal pinnae; aerophores absent; pinnae subpetiolulate to adnate, narrowly linear to narrowly elliptic, lanceolate, slightly revolute, margins subentire to crenate; veins free, 1-furcate, each ending in a clavate hydathode or (in D. neglectum View in CoL ) anastomosing and forming polygonal areoles, these in ca. 2 rows between costae and pinna margins; sori linear, indusiate, indusia subentire to erose, reflexed at maturity and not covering sporangia; x = 27, 28.

Species number, comments, and distribution:— Six species, in Malesia, Australia, and Oceania. The species usually have narrow, erect rhizomes (sometimes over 1 m tall) that may eventually collapse and thus appear to be long-creeping, as reported by Cranfill (2001). The blades are pinnate to deeply pinnatifid or bipinnatisect to bipinnate, usually becoming bipinnatifid distally, and the basal pinnae gradually to abruptly reduced or the stipes winged. Diploblechnum is closely related to the Lomariocycas clade, plus the Neoblechnum-Oceaniopteris - Doodia clade and the Parablechnum clade (Gasper et al. in press).

Kingdom

Plantae

Phylum

Tracheophyta

Class

Polypodiopsida

Order

Polypodiales

Family

Blechnaceae

Genus

Cranfillia

Loc

Cranfillia vulcanica (Blume) Gasper & V.A.O.Dittrich

Gasper, André Luís De, Dittrich, Viníciusantonio De Oliveira, Smith, Alan R. & Salino, Alexandre 2016
2016
Loc

Diploblechnum

A. Cunn. 1975: 153
Diploblechnum Hayata 1927: 702
1927
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