Sphenosolen draperi Pojeta and Gilbert-Tomlinson, 1977
publication ID |
https://doi.org/ 10.4202/app.00215.2015 |
persistent identifier |
https://treatment.plazi.org/id/03A787E2-FFEA-FFE7-FFBE-FD919485FE36 |
treatment provided by |
Felipe |
scientific name |
Sphenosolen draperi Pojeta and Gilbert-Tomlinson, 1977 |
status |
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Sphenosolen draperi Pojeta and Gilbert-Tomlinson, 1977
Fig. 12E, F View Fig .
1977 Sphenosolen draperi sp. nov.; Pojeta and Gilbert-Tomlinson 1977: 31, pl. 25: 1, 2.
Type material: Holotype ( CPC 15582 View Materials ) is figured by Pojeta and Gilbert-Tomlinson (1977: pl. 25: 1) . Paratype ( CPC 15583 View Materials ) figured by Pojeta and Gilbert-Tomlinson (1977: pl. 25: 2) from the type locality. Type locality: Stairway Sandstone , East of Maryvale Homestead, Amadeus Basin, southern Northern Territory, Australia .
Type horizon: Decalcified friable buff/white fine-grained silty sandstone horizon within the Stairway Sandstone.
Material.— 40 specimens, mostly fragmentary internal and external moulds; 4 specimens from the Areyonga Gorge section and 36 specimens from Petermann Creek section, Middle Ordovician of Australia. The two figured specimens are numbered CPC 41485 View Materials and CPC 41486 View Materials .
Description.—Narrow elongated sub-rectangular orthonotid with flat shell. Dorsal margin straight; anterior margin rounded; posterior margin rounded to straight and oblique toward the dorsum; ventral margin broadly rounded anteriorly, straight posteriorly. Umbo hardly discernible.
Remarks.— Sphenosolen draperi is the only heteroconch recovered from the investigated sections. The shell shape is distinctly different from all other species due to the reduced height and increased length. Cope (2004) placed the genus Sphenosolen within the anomalodesmatans but we follow Pojeta and Gilbert-Tomlinson (1977), who assigned the genus to the heteroconchs; for further discussion see Cope 2002, 2004). Sphenosolen is a middle Darriwilian taxon Cope 2004: fig. 20.3), like the nuculoids Sthenodonta and Johnmartinia .
Stratigraphic and geographic range.—A single specimen from bed PC - 5 in the Petermann Creek section is tentatively assigned to S. draperi , whereas the remaining 35 specimens derive from bed PC +7 to PC + 11 in the upper part of the section ( Fig. 5 View Fig ). The species also ranges through the upper part of the Areyonga Gorge section from bed A +1 to A +4 ( Fig. 4 View Fig ).
Pojeta and Gilbert-Tomlinson (1977: 31) described and illustrated Sphenosolen draperi based on nine specimens, all from the same locality about 150 km east of the Areyonga Gorge in the Amadeus Basin. All known specimens found are from the Stairway Sandstone. Heteroconchs are uncommon in low-latitude faunas, and seemingly preferred high-latitude environments ( Cope 2002). The range of Sphenosolen draperi is within the Stairway Sandstone Formation, Darriwilian (Middle Ordovician). The region is in the southern Northern Territory, corresponding to the central part of the Amadeus Basin ( Fig. 1).
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