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1000 Titel
  • Upper Frasnian Tornoceratidae (Ammonoidea) from the Sand Formation (Bergisch Gladbach-Paffrath Syncline, Rhenish Massif)
1000 Autor/in
  1. Söte, Till |
  2. Becker, Ralph Thomas |
  3. Herd, Karl Josef |
  4. Bockwinkel, Jürgen |
1000 Erscheinungsjahr 2021
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2021-05-28
1000 Erschienen in
1000 Quellenangabe
  • 95(2):237-273
1000 Copyrightjahr
  • 2021
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1007/s12542-020-00546-3 |
1000 Publikationsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:title>Abstract</jats:title><jats:p>Excavations in the Sand district of Bergisch Gladbach (Rhenish Massif, Germany) yielded a rich ammonoid fauna of the upper Frasnian “<jats:italic>Archoceras</jats:italic>” <jats:italic>varicosum</jats:italic> Zone (Upper Devonian I-K, interval between the two Kellwasser levels). The previously unknown assemblages include six tornoceratid genera with 20 species, including seven new species (<jats:italic>Aulatornoceras steinhauseni</jats:italic> sp. nov., <jats:italic>Aul. frenklerae</jats:italic> sp. nov., <jats:italic>Aul. ventrosulcatum</jats:italic> sp. nov., <jats:italic>Crassotornoceras nudum</jats:italic> sp. nov., <jats:italic>Cr. hetzeneggeri</jats:italic> sp. nov., <jats:italic>Retrotornoceras juxi</jats:italic> sp. nov., <jats:italic>Tornoceras aequilobum</jats:italic> sp. nov.) and taxa described in open nomenclature. There are five associated gephuroceratid genera with nine species. The unexpectedly high genus- and species-level diversity at Sand, supported by statistical indices, is unprecedented compared to other contemporaneous ammonoid faunas. It highlights the currently fragmentary knowledge of top-Frasnian ammonoid faunas on a global scale. <jats:italic>Phoenixites frechi</jats:italic>, the dominant tornoceratid of hypoxic and organic-rich Kellwasser facies of Europe and North Africa, is completely missing at Sand. The local assemblage structure is analyzed statistically and interpreted in terms of palaeoecology. The occurrence of a new type of “Housean Pits”, probably caused by parasitism, is found in nine species of five genera, mostly in tornoceratids. The Sand fauna indicates that the species origination rate in tornoceratids remained high after the Lower Kellwasser Event.</jats:p>
1000 Sacherschließung
lokal Goniatitida
lokal Upper Devonian
lokal Rhenish Massif
lokal Frasnian
lokal Kellwasser Crisis
lokal Ammonoidea
lokal Research Paper
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  1. https://orcid.org/0000-0001-5595-3923|https://frl.publisso.de/adhoc/uri/QmVja2VyLCBSYWxwaCBUaG9tYXM=|https://frl.publisso.de/adhoc/uri/SGVyZCwgS2FybCBKb3NlZg==|https://frl.publisso.de/adhoc/uri/Qm9ja3dpbmtlbCwgSsO8cmdlbg==
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1000 Erstellt am 2023-04-28T10:27:50.296+0200
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