Ammonoid Fauna of the Upper Olenekian Osawa Formation in the Utatsu Area, South Kitakami Belt, Northeast Japan

2016 ◽  
Vol 20 (2) ◽  
pp. 90-104 ◽  
Author(s):  
Masayuki Ehiro ◽  
Osamu Sasaki ◽  
Harumasa Kano
Keyword(s):  
Ammonoid Fauna

scholarly journals A new early Smithian ammonoid fauna from the Salt Range (Pakistan)

2011 ◽  
Vol 130 (2) ◽  
pp. 187-201 ◽  
Author(s):  
Thomas Brühwiler ◽  
Hugo Bucher ◽  
Ghazala Roohi ◽  
Aamir Yaseen ◽  
Khalil Rehman
Keyword(s):  
Salt Range ◽  
Ammonoid Fauna

scholarly journals A new ammonoid fauna from the C arnian ( U pper T riassic) K asimlar F ormation of the T aurus M ountains ( A natolia, T urkey)

Palaeontology ◽  
2013 ◽  
Vol 57 (2) ◽  
pp. 357-396 ◽  
Author(s):  
Susanne Lukeneder ◽  
Alexander Lukeneder
Keyword(s):  
Ammonoid Fauna

Pennsylvanian (Atokan) ammonoids from the Magoffin Member of the Four Corners Formation, eastern Kentucky

2012 ◽  
Vol 86 (3) ◽  
pp. 403-416 ◽  
Author(s):  
David M. Work ◽  
Charles E. Mason ◽  
Darwin R. Boardman
Keyword(s):  
Eastern Europe ◽  
Western Europe ◽  
South Urals ◽  
The South ◽  
Eastern Kentucky ◽  
Four Corners ◽  
Ammonoid Fauna ◽  
Assemblage Zone ◽  
Moscovian Stage

The Pennsylvanian ammonoidsGastrioceras magoffinensen. sp.,Maximites nassichukin. sp.,Dimorphoceratoides adamsin. sp.,Bisatoceras? sp.,Phaneroceras chesnutin. sp., and Christioceratidae gen. indet. occur in the Magoffin Member of the Four Corners Formation in eastern Kentucky. The interval represented by the Magoffin ammonoid fauna should be known as theGastrioceras magoffinenseAssemblage Zone. This overlies the well-knownDiaboloceras neumeieriZone, represented in the Kendrick Shale Member of the Hyden Formation in eastern Kentucky. TheGastrioceras magoffinenseZone correlates to theDiaboloceras varicostatum–Winslowoceras henbestiZone in the Winslow Member of the Atoka Formation in northwestern Arkansas. Ammonoids and associated conodonts, includingDeclinognathodus marginodosusand its descendantD. donetzianus, indicate an early Atokan age corresponding to the basal Bolsovian (basal Westphalian C) Substage in western Europe and the Bashkirian–Moscovian Stage boundary interval in eastern Europe and the South Urals.

Rare representatives in the ammonoid fauna from Büdesheim (Cephalopoda, Eifel, Late Devonian) and the role of heterochrony

2013 ◽  
Vol 269 (2) ◽  
pp. 111-124 ◽  
Author(s):  
Dieter Korn ◽  
Jürgen Bockwinkel ◽  
Volker Ebbighausen ◽  
Sonny A. Walton
Keyword(s):  
Late Devonian ◽  
Ammonoid Fauna

scholarly journals A new ammonoid fauna from theGattendorfia-Eocanites Genozone of the Anti-Atlas (Early Carboniferous; Morocco)

Fossil Record ◽  
2006 ◽  
Vol 9 (1) ◽  
pp. 87-129 ◽  
Author(s):  
Jürgen Bockwinkel ◽  
Volker Ebbighausen
Keyword(s):  
Early Carboniferous ◽  
Ammonoid Fauna

scholarly journals The ammonoid fauna of the Kimmeridgian-Tithonian boundary beds of Mombasa, Kenya /

1984 ◽  
Author(s):  
Harish M. Verma ◽  
Gerd Ernst Gerold Westermann
Keyword(s):  
Ammonoid Fauna

A new Permian ammonoid fauna of the Kobylka River (North Urals)

2010 ◽  
Vol 44 (3) ◽  
pp. 261-266 ◽  
Author(s):  
K. V. Borissenkov
Keyword(s):  
Ammonoid Fauna ◽  
Permian Ammonoid

scholarly journals The ammonoids from the Three Forks Shale (Late Devonian) of Montana

Fossil Record ◽  
2006 ◽  
Vol 9 (2) ◽  
pp. 198-212 ◽  
Author(s):  
D. Korn ◽  
A. Titus
Keyword(s):  
Late Devonian ◽  
Growth Stages ◽  
Adult Growth ◽  
Ammonoid Fauna ◽  
Three Forks ◽  
Stratigraphic Position

Abstract. The ammonoid fauna from the Late Devonian Three Forks Shale of Montana is revised. Six taxa were recognised, which belong to the genera Tornoceras, Pernoceras, Raymondiceras, Platyclymenia, Pleuroclymenia, and Carinoclymenia. The ammonoid assemblage suggests a stratigraphic position within the middle Famennian, most probably the Platyclymenia annulata Zone. The ammonoids display extreme septal crowding in intermediate as well as adult growth stages, which can be regarded as evidence for instable palaeoecological conditions during lifetime of the animals. Die Ammonoideenfauna aus dem oberdevonischen Three Forks Shale von Montana wird revidiert. Sechs Taxa werden unterschieden; sie gehören zu den Gattungen Tornoceras, Pernoceras, Raymondiceras, Platyclymenia, Pleuroclymenia und Carinoclymenia. Die Ammonoideen-Vergesellschaftung spricht für eine stratigraphische Position im mittleren Famennium, wahrscheinlich in der Platyclymenia annulata Zone. Die Ammonoideen zeigen auffällige Drängung der Septen in intermediären und adulten Wachstumsstadien, die als Hinweis auf instabile Lebensbedingungen für die Tiere gewertet werden kann. doi:10.1002/mmng.200600008

scholarly journals Early Tournaisian ammonoids from Timimoun (Gourara, Algeria)

Fossil Record ◽  
2004 ◽  
Vol 7 (1) ◽  
pp. 133-152
Author(s):  
V. Ebbighausen ◽  
J. Bockwinkel ◽  
D. Korn ◽  
D. Weyer
Keyword(s):  
Algerian Sahara ◽  
Ammonoid Fauna

A small ammonoid fauna, of probable middle Early Tournaisian age, is described from the Gara el Kahla near Timimoun, Gourara, Algerian Sahara. The following taxa are described: <i>Acutimitoceras algeriense</i> n. sp., <i>Acutimitoceras sinulobatum</i> n. sp., <i>Acutimitoceras</i> sp. A, <i>Hasselbachia gourara</i> n. sp., <i>Gattendorfia jacquelinae</i> n. sp., <i>Gattendorfia</i> cf. <i>crassa</i> Schmidt. 1924, <i>Kahlacanites</i> n. gen., <i>Kahlacanites meyendorfi</i> n. sp., <i>Kahlacanites mariae</i> n. sp., and <i>Kahlacanites timimounensis</i> n. sp. <br><br> Eine kleine Ammonoideenfauna mit wahrscheinlich mittlerem Untertournai-Alter von der Gara el Kahla bei Timimoun (Gourara, Algerische Sahara) wird untersucht. Die folgenden Taxa warden beschrieben: <i>Acutimitoceras algeriense</i> n. sp., <i>Acutimitoceras sinulobatum</i> n. sp., <i>Acutimitoceras</i> sp. A, <i>Hasselbachia gourara</i> n. sp., <i>Gattendorfia jacquelinae</i> n. sp., <i>Gattendorfia</i> cf. <i>crassa</i> Schmidt, 1924, <i>Kahlacanites</i> n. gen., <i>Kahlacanites meyendorffi</i> n. sp., <i>Kahlacanites mariae</i> n. sp. und <i>Kahlacanites timimounensis</i> n. sp. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.20040070107" target="_blank">10.1002/mmng.20040070107</a>

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