Presence of Frambocythere COLIN, 1980, (limnic ostracode) in the Maastrichtian of the Zagros Mountains, Iran: a newly recognized link between southern Europe and the Far East
Author(s) -
Jean-Paul Colin,
Hossein Vaziri–Moghaddam,
Amrollah Safari,
Samira SHARIARI GRAI
Publication year - 2012
Publication title -
carnets de géologie (notebooks on geology)
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.263
H-Index - 15
eISSN - 1765-2553
pISSN - 1634-0744
DOI - 10.4267/2042/47503
Subject(s) - link (geometry) , geography , geology , computer network , computer science
International audienceThe limnic ostracode Frambocythere tumiensis zagrosensis subsp. nov. (Limnocytheridae, Timiriaseviinae), has been found for the first time in Iran. The strata containing this species are in the lower part of the Tarbur Formation in the interior Fars of the Zagros Mountains. The Late Maastrichtian age is indicated by rudists, larger foraminifers (Omphalocyclus macroporus, Loftusia spp.) and planktonic foraminifers (Contusotruncana contusa-Racemiguembelina fructicosa Zone) present in the upper part of the Tarbur Formation. The Maastrichtian age is confirmed by the occurrence in the same strata of the charophytes Platychara shanii, Peckichara cristellata and Stephanochara cf. producta. The genus Frambocythere Colin, 1980, was until now known mostly from the Upper Maastrichtian to Middle Eocene of southern Europe, India and China, as well as the Albian of the Democratic Republic of Congo. The presence of Frambocythere gr. tumiensis in Iran is therefore a newly recognized link between southern Europe and the Far East (China)
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