Unusual assemblage of conulariids (Cnidaria, Scyphozoa) from the Taddrist Formation (Middle Ordovician, Darriwilian) of southern Morocco

被引:0
|
作者
Van Iten, Heyo [1 ,2 ]
Gutierrez-Marco, Juan Carlos [3 ,4 ]
Cournoyer, Mario E. [5 ]
机构
[1] Hanover Coll, Dept Geol, Hanover, IN 47243 USA
[2] Cincinnati Museum Ctr, Dept Invertebrate Paleontol, 1301 Western Ave, Cincinnati, OH 45203 USA
[3] Univ Complutense Madrid, GSIC UCM, Consejo Super Invest Cient, Inst Geociencias, Jose Antonio Novais 12, Madrid 28040, Spain
[4] Fac CC Geol, Area Paleontol GEODESPAL, Jose Antonio Novais 12, Madrid 28040, Spain
[5] Musee Paleontol & Evolut, 541 Congregat St, Montreal, PQ H3K 2J1, Canada
关键词
MEDUSOZOA; PALEOECOLOGY; MORPHOLOGY; EVOLUTION;
D O I
10.1017/jpa.2022.6
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Silty noduliferous shales in the lower part of the Middle Ordovician (late Darriwilian 2) Taddrist Formation in the central Moroccan Anti-Atlas contain a unique assemblage of conulariids consisting of one species each of Archaeoconularia Boucek, 1939, Glyptoconularia Sinclair, 1952, and Pseudoconularia Boucek, 1939. Glyptoconularia antiatlasica new species, currently represented by a single three-dimensional specimen, is the first member of this extremely rare, highly autapomorphic genus to be described from outside of cratonic North America as well as the first Glyptoconularia from the Middle Ordovician. Pseudoconularia cf. P. grandissima (Barrande, 1867) and Archaeoconularia cf. A. exquisita (Barrande, 1867) most closely resemble species previously described from Middle and Upper Ordovician strata in the Prague Basin (Czech Republic), then located adjacent to North Africa. Anaconularia anomala (Barrande, 1867), previously known from the Upper Ordovician (Sandbian) Liberi and Letna formations in the Prague Basin, is documented for the first time from the Upper Ordovician (Katian) Upper Tioririne Formation of Morocco. In addition to extending the known stratigraphical and paleogeographical ranges of these conulariids, results of the present investigation add to the list of invertebrate taxa that appear to have originated during Early or Mid-Ordovician times in peri-Gondwana or southpolar Gondwana, and then migrated to the eastern margin of Laurentia, arriving there along with other cool-water taxa during the Sandbian-Katian transition.
引用
收藏
页码:803 / 813
页数:11
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