Results 91 to 100 of about 160 (139)
Some of the next articles are maybe not open access.
The ammonoid and conodont zonation at Enkenberg (Famennian, Late Devonian; Rhenish Mountains)
Senckenbergiana Lethaea, 2002The middle Famennian (Late Devonian) Enkenberg section is studied in terms of ammonoid and conodont zonations. Six ammonoid zones (Paratornoceras lentiforme Zone,Maeneceras meridionale Zone,Pernoceras dorsatum Zone,Pseudoclymenia pseudogoniatites Zone,Prolobites delphinus Zone, andPlatyclymenia annulata Zone) and six conodont zones (Earlymarginifera ...
Dieter Korn +2 more
exaly +2 more sources
Emsian Ammonoidea and the age of the Hunsrück Slate (Rhenish Mountains, Western Germany)
Palaeontographica, Abteilung A: Palaozoologie - Stratigraphie, 2013The ammonoids from the well-studied German Fossillagerstatte of the Hunsruck Slate have the reputation of being the oldest known representatives of this cephalopod group. This material is of great interest not only because of the global scarcity of the earliest ammonoids, but also because it includes the first record of stratigraphically-controlled ...
Markus Poschmann +2 more
exaly +3 more sources
Late Givetian ammonoids from Oberberge (Middle Devonian; Rhenish Mountains)
Neues Jahrbuch Fur Geologie Und Palaontologie - Abhandlungen, 2015Dieter Korn, Jürgen Bockwinkel
exaly +2 more sources
Late Givetian ammonoids from Iserlohn and Neuenrade (northern Rhenish Mountains)
Neues Jahrbuch Fur Geologie Und Palaontologie - Abhandlungen, 2017Dieter Korn, Jürgen Bockwinkel
exaly +2 more sources
Senckenbergiana Lethaea, 2002
The history of the development of an ammonoid stratigraphy of the higher Middle Devonian and the Late Devonian rock sequence in the Rhenish Massif is reviewed. Of 45 currently distinguishable ammonoid zones in the Givetian, Frasnian and Famennian stages, at least 38 were recorded in the Rhenish Massif.
Dieter Korn, Korn Dieter
exaly +2 more sources
The history of the development of an ammonoid stratigraphy of the higher Middle Devonian and the Late Devonian rock sequence in the Rhenish Massif is reviewed. Of 45 currently distinguishable ammonoid zones in the Givetian, Frasnian and Famennian stages, at least 38 were recorded in the Rhenish Massif.
Dieter Korn, Korn Dieter
exaly +2 more sources
2023
The Rhenish Slate Mountains are one of the classical outcrop areas for stratigraphic research in Devonian and Carboniferous strata. Lithostratigraphic mapping of German parts of the Rhenish Slate Mountains has been performed systematically for over 100 years starting with a mapping campaign implemented by the Prussian Geological Survey in the 1920s ...
Sandmann, Sascha +3 more
openaire +1 more source
The Rhenish Slate Mountains are one of the classical outcrop areas for stratigraphic research in Devonian and Carboniferous strata. Lithostratigraphic mapping of German parts of the Rhenish Slate Mountains has been performed systematically for over 100 years starting with a mapping campaign implemented by the Prussian Geological Survey in the 1920s ...
Sandmann, Sascha +3 more
openaire +1 more source
Paläontologische Zeitschrift, 1998
Willwerathia laticeps (Stormer 1936) originally described as a eurypterid is reinterpreted as a synziphosurine belonging to Family WeinberginidaeRichter &Richter 1929. Recently collected material from the locality, from which the destroyed holotype comes, suggests thatWillwerathia possessed ten opisthosomal tergites, deduced from all available arrays ...
Lyall I. Anderson +2 more
openaire +1 more source
Willwerathia laticeps (Stormer 1936) originally described as a eurypterid is reinterpreted as a synziphosurine belonging to Family WeinberginidaeRichter &Richter 1929. Recently collected material from the locality, from which the destroyed holotype comes, suggests thatWillwerathia possessed ten opisthosomal tergites, deduced from all available arrays ...
Lyall I. Anderson +2 more
openaire +1 more source
PalZ, 2001
New specimens of the chasmataspidDiploaspis casteriStormer, 1972 (Chelicerata: Chasmataspidida) are described from the late Lower Emsian of Alken an der Mosel, Germany. Chasmataspidids represent a distinct clade within Chelicerata, sharing characters with both xiphosurans and eurypterids.Diploaspis is significant in having the most complete appendage ...
Jason A. Dunlop +2 more
openaire +1 more source
New specimens of the chasmataspidDiploaspis casteriStormer, 1972 (Chelicerata: Chasmataspidida) are described from the late Lower Emsian of Alken an der Mosel, Germany. Chasmataspidids represent a distinct clade within Chelicerata, sharing characters with both xiphosurans and eurypterids.Diploaspis is significant in having the most complete appendage ...
Jason A. Dunlop +2 more
openaire +1 more source
Early Carboniferous (Mississippian) calciturbidites in the northern Rhenish Mountains (Germany)
Geological Journal, 2007AbstractViséan calciturbidites occur in two separate turbidite sequences at the northern margin of the Rhenish Mountains: (1) the Herdringen Sequence (Becke‐Oese, Retringen and Herdringen formations), and (2) the Hellefeld Sequence (Hellefeld, Linnepe and Wennemen formations).
openaire +1 more source
Late Givetian ammonoids from Hagen-Herbeck, Donnerkuhle quarry (Devonian, Rhenish Mountains)
Neues Jahrbuch Fur Geologie Und Palaontologie - Abhandlungen, 2013Dieter Korn +2 more
exaly +2 more sources