A new assemblage of graptolites, rhabdopleuran hemichordates and chitinoushydroids from the late Arenig (Ordovician) of the Banestan area, east-central Iran

Citation
Rb. Rickards et al., A new assemblage of graptolites, rhabdopleuran hemichordates and chitinoushydroids from the late Arenig (Ordovician) of the Banestan area, east-central Iran, ALCHERINGA, 25(1-2), 2001, pp. 169-190
Citations number
73
Categorie Soggetti
Earth Sciences
Journal title
ALCHERINGA
ISSN journal
03115518 → ACNP
Volume
25
Issue
1-2
Year of publication
2001
Pages
169 - 190
Database
ISI
SICI code
0311-5518(2001)25:1-2<169:ANAOGR>2.0.ZU;2-F
Abstract
A rich benthic and plantonic graptolite fauna is associated with encrusting rhabdopleuran hemichordates and chitinous hydrozoans in the late Arenig (O rdovician) part of the Katkoyeh Formation at Banestan, east-central Iran. New taxa described here are the dendroid graptolites Callograptus huckriede i sp. nov. and Dictyonema bitubulata sp. nov. Other dendroid graptolites De ndrograptus sp. cf. D. flexuosus J. Hall, 1865; Acanthograptus divergens Sk evington, 1963; and Thallograptus ?succulentus Ruedemann, 1904 are describe d, The tuboid graptolite Galeograptus sp., the rhabdopleuran hemichordates Rhabdopleura sp. aff. R. primaevus (Kozlowski, 1967) and Kystodendron sp., and the chitinous hydroid Palaeotuba sp. are also described. Graptoloid gra ptolites described here are Aulograptus? sp., Didymograptus incertus Perner , 1895, Undulograptus formosus (Mu & Lee, 1958), and Yutagraptus sp. cf. Y. mantuanus Riva, 1994. All but two species-level taxa are described from Ir an for the first time. The fauna is confirmed as being late Arenig or, less likely, early Llanvirn and thus probably correlates with the early part of the Darriwilian stage. It resembles the Atlantic cold water faunas in lacking isograptids and sin ograptids.