Dendrograptus avonleaensis, Rickards, R. B., Chapman, A. J., Wright, A. J. & Packham, G. H, 2003

Rickards, R. B., Chapman, A. J., Wright, A. J. & Packham, G. H, 2003, Dendroid and Tuboid Graptolites from the Llandovery (Silurian) of the Four Mile Creek Area, New South Wales, Records of the Australian Museum 55 (3), pp. 305-330 : 312

publication ID

https://doi.org/ 10.3853/j.0067-1975.55.2003.1387

persistent identifier

https://treatment.plazi.org/id/039E87A3-F93A-FFA2-7398-47699C14E644

treatment provided by

Felipe

scientific name

Dendrograptus avonleaensis
status

sp. nov.

Dendrograptus avonleaensis n.sp.

Figs. 5A, 6A,B View Fig

Material. HOLOTYPE AM F114646 a-b and PARATYPES AM F114650 and AM F114766 , all from F14, Bridge Creek .

Etymology. After the property “Avon Lea” on which F14 is located.

Diagnosis. Dendrograptus with robust funnel-shaped rhabdosome at least 15 mm long and 18 mm at its widest; branching in broad zones; stipes with a dorsoventral width of 0.50–0.60 mm and a lateral width of 0.20–0.40 mm; autothecal spacing 18–20 in 10 mm.

Description. The holotype ( Fig. 6B View Fig ) displays a distal array of at least 48 stipes arranged in a broadly conical fashion with two major branching zones. These distal stipes diverge some 3.5 mm above the visible base of the specimen, but they do not arise from a solid stem: tightly clustered stipes are visible in the densely packed area. The overall shape is, therefore, funnel-shaped with a proximal constriction. In one or two places the stipes are visible in profile when the autothecae, spaced at 18–20 in 10 mm, can be seen to be of simple denticulate type ( Fig. 4I View Fig ). The lateral stipe width is 0.40 mm proximally, falling to 0.20 mm most distally, suggesting some cortical thickening as the colony ages. Two other specimens (e.g., Fig. 5A) are fragments from beyond the zone of expansion. They show some of the above-described features but less well-displayed.

Remarks. As described by Chapman et al. (1996) some Dendrograptus species can be quite well ordered; this is one such species, having a broadly conical, funnel-shaped form and rough branching zones. Dendrograptus avonleaensis n.sp. has a superficial resemblance to Calyptograptus cyathiformis Spencer, 1878 from the Niagara Limestone, but that species has more frequent and irregular branching and a robust stem; the thecae of C. cyathiformis are not known. Dendrograptus avonleaensis differs from D. ashburniaensis n.sp. herein in that the latter has a thecal spacing of 36 in 10 mm, almost twice that of the former; and D. ashburniaensis develops a thickened stem proximally.

AM

Australian Museum

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