New late Smithian (Early Triassic) ammonoids from the Lusitaniadalen Member, Vikinghogda Formation, Svalbard

被引:9
|
作者
Piazza, Veronica [1 ]
Hammer, Oyvind [2 ]
Jattiot, Romain [3 ,4 ]
机构
[1] Leibniz Inst Evolut & Biodiversitatsforsch, Museum Nat Kunde, Invalidenstr 43, D-10115 Berlin, Germany
[2] Univ Oslo, Nat Hist Museum, POB 1172 Blindern, N-0318 Oslo, Norway
[3] Univ Zurich, Palaontol Inst, Karl Schmid Str 4, CH-8006 Zurich, Switzerland
[4] Univ Bourgogne Franche Comte, UMR CNRS Biogeosci 6282, 6 Blvd Gabriel, F-21000 Dijon, France
来源
NORWEGIAN JOURNAL OF GEOLOGY | 2017年 / 97卷 / 02期
关键词
Ammonoid biostratigraphy; Tardus Zone; Smithian; Prionitidae; Svalbard; Boreal Realm; INTRASPECIFIC VARIATION; FAUNAS;
D O I
10.17850/njg97-2-03
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A single carbonate concretion from the uppermost Lusitaniadalen Member ('Fish Niveau', Vikinghogda Formation) at Stensiofjellet, Spitsbergen, contains a fairly rich assemblage of late Smithian (Early Triassic, Olenekian) ammonoids. The main species identified are Wasatchites tridentinus Spath, 1934, Wasatchites cf. distractus (Waagen, 1895), Anasibirites kingianus (Waagen, 1895), Arctoprionites nodosus (Frebold, 1930), Arctoprionites resseri (Mathews, 1929) and Xenoceltites subevolutus Spath, 1930. Two taxa are here discussed: Prionitid sp. and Arctoceras erebori sp. nov. The assemblage provides new information about the Early Triassic biostratigraphy and palaeogeography of the Boreal Realm. The composition of the Spitsbergen fauna is in good agreement with other assemblages within and outside the Boreal Realm and essentially comprises cosmopolitan taxa. Only Arctoceras erebori sp. nov. and Prionitid sp. are as yet restricted to Spitsbergen. The newly reported occurrence of low paleolatitude taxa from Spitsbergen strengthens the cosmopolitan distribution of ammonoids during late Smithian time, thus improving existing correlation.
引用
收藏
页码:105 / 117
页数:13
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