A REVIEW OF THE TITHONIAN AMMONITES FROM THE KACHCHH BASIN, WESTERN INDIA

被引:0
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作者
Pandey, Dhirendra K. [1 ]
Alberti, Matthias [1 ,2 ]
Fuersich, Franz T. [3 ]
Bhaumik, Sneha [1 ]
Ayoub-Hannaa, Wagih [3 ]
机构
[1] Univ Rajasthan, Dept Geol, Jaipur 302004, Rajasthan, India
[2] Christian Albrechts Univ Kiel, Inst Geowissensch, Ludewig Meyn Str 10, D-24118 Kiel, Germany
[3] Friedrich Alexander Univ Erlangen Nurnberg, Geozentrum Nordbayern, FG Palaoumwelt, Loewenichstr 28, D-91054 Erlangen, Germany
关键词
Tithonian; Ammonites; Taxonomy; Biostratigraphy; Kachchh Basin; GENUS HIMALAYITES; KUTCH; PALEOBIOGEOGRAPHY; AMMONOIDEA; RECORD;
D O I
暂无
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Twenty taxa of ammonites, represented by 53 specimens, are described from three sections of the highly ferruginous Umia Ammonite Beds of western Kachchh, Gujarat. The ammonites are representatives of the families Phylloceratidae, Haploceratidae, Perisphinctidae, Ataxioceratidae, and Berriasellidae and belong to the genera Ptychophylloceras, Holcophylloceras, Hildoglochiceras, Yirgatosphinctes, Parapallasiceras, Paraulacosphinctes, Micracanthoceras, and Himalayites. Four ammonite levels can be distinguished. They are, in stratigraphic order, the Hildoglochiceras Horizon, and the Denseplicatus, Microcanthum, and Frequens ammonite zones, and stratigraphically represent the middle Lower to lower Upper Tithonian. The Umia Ammonite Beds are a condensed unit representing the maximum flooding zone of a transgressive-regressive cycle. The degree of condensation varies between the sections: While the four ammonite levels can be differentiated in the Katesar section, they are less clearly developed in the more strongly condensed Lakhapar section.
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页码:141 / 173
页数:33
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