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