Uppermost Famennian stratigraphy and facies development of the Reigern Quarry near Hachen (northern Rhenish Massif, Germany)
As a contribution to the ongoing international revision of the Devonian/Carboniferous boundary, we present a bed-by-bed study of the Reigern Quarry in the northern Sauerland (Rhenish Massif, Germany), which is famous as an uppermost Famennian ammonoid locality. Currently exposed are ca. 2.5 m of str...
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Published in | Palaeobiodiversity and palaeoenvironments Vol. 97; no. 3; pp. 633 - 654 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Berlin/Heidelberg
Springer Berlin Heidelberg
01.09.2017
Springer Nature B.V |
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Abstract | As a contribution to the ongoing international revision of the Devonian/Carboniferous boundary, we present a bed-by-bed study of the Reigern Quarry in the northern Sauerland (Rhenish Massif, Germany), which is famous as an uppermost Famennian ammonoid locality. Currently exposed are ca. 2.5 m of strongly cyclic Wocklum Limestone, conformably overlain, but with a long hiatus (topmost Famennian to upper Tournaisian), by laminated radiolarites and a thin metabentonite of the Lower Carboniferous Hardt Formation. The nodular limestones are pelagic mud-wackestones with some sporadic occurrences of cephalopod float-rudstones. The exposed part of the Wocklum Limestone falls in the successive
Bispathodus ultimus ultimus
and
Siphonodella
(
Eosiphonodella
)
praesulcata
(s.l.) zones. It yielded two new
Siphonodella
(
Eosiphonodella
) species left in open nomenclature,
Neopolygnathus communis
aff.
dentatus
and the possibly stratigraphically relevant
Bispathodus ultimus corradinii
ssp. nov. The upper range of
Palmatolepis gracilis semisigmoidalis
is significantly expanded. The conodont faunas mostly belong to variants of the pelagic
Palmatolepis
-
Bispathodus
biofacies; but in the lower part of the succession, there is a new
Neopolygnathus
biofacies that previously has not been recorded from deeper-water, pre-Hangenberg Crisis strata.
Neopolygnathus
is interpreted as a palaeoecological generalist that variably blossomed in outer or inner shelf facies and after other conodont groups declined. The mostly loose ammonoid faunas comprise almost 30 taxa and fall mostly in the lower Wocklumian
Kalloclymenia subarmata
and
Muessenbiaergia bisulcata
zones (Upper Devonian = UD VI-A
1
/A
2
), which agrees with previous ammonoid-conodont correlations. |
---|---|
AbstractList | As a contribution to the ongoing international revision of the Devonian/Carboniferous boundary, we present a bed-by-bed study of the Reigern Quarry in the northern Sauerland (Rhenish Massif, Germany), which is famous as an uppermost Famennian ammonoid locality. Currently exposed are ca. 2.5 m of strongly cyclic Wocklum Limestone, conformably overlain, but with a long hiatus (topmost Famennian to upper Tournaisian), by laminated radiolarites and a thin metabentonite of the Lower Carboniferous Hardt Formation. The nodular limestones are pelagic mud-wackestones with some sporadic occurrences of cephalopod float-rudstones. The exposed part of the Wocklum Limestone falls in the successive Bispathodus ultimus ultimus and Siphonodella (Eosiphonodella) praesulcata (s.l.) zones. It yielded two new Siphonodella (Eosiphonodella) species left in open nomenclature, Neopolygnathus communis aff. dentatus and the possibly stratigraphically relevant Bispathodus ultimus corradinii ssp. nov. The upper range of Palmatolepis gracilis semisigmoidalis is significantly expanded. The conodont faunas mostly belong to variants of the pelagic Palmatolepis-Bispathodus biofacies; but in the lower part of the succession, there is a new Neopolygnathus biofacies that previously has not been recorded from deeper-water, pre-Hangenberg Crisis strata. Neopolygnathus is interpreted as a palaeoecological generalist that variably blossomed in outer or inner shelf facies and after other conodont groups declined. The mostly loose ammonoid faunas comprise almost 30 taxa and fall mostly in the lower Wocklumian Kalloclymenia subarmata and Muessenbiaergia bisulcata zones (Upper Devonian = UD VI-A1/A2), which agrees with previous ammonoid-conodont correlations. As a contribution to the ongoing international revision of the Devonian/Carboniferous boundary, we present a bed-by-bed study of the Reigern Quarry in the northern Sauerland (Rhenish Massif, Germany), which is famous as an uppermost Famennian ammonoid locality. Currently exposed are ca. 2.5 m of strongly cyclic Wocklum Limestone, conformably overlain, but with a long hiatus (topmost Famennian to upper Tournaisian), by laminated radiolarites and a thin metabentonite of the Lower Carboniferous Hardt Formation. The nodular limestones are pelagic mud-wackestones with some sporadic occurrences of cephalopod float-rudstones. The exposed part of the Wocklum Limestone falls in the successive Bispathodus ultimus ultimus and Siphonodella ( Eosiphonodella ) praesulcata (s.l.) zones. It yielded two new Siphonodella ( Eosiphonodella ) species left in open nomenclature, Neopolygnathus communis aff. dentatus and the possibly stratigraphically relevant Bispathodus ultimus corradinii ssp. nov. The upper range of Palmatolepis gracilis semisigmoidalis is significantly expanded. The conodont faunas mostly belong to variants of the pelagic Palmatolepis - Bispathodus biofacies; but in the lower part of the succession, there is a new Neopolygnathus biofacies that previously has not been recorded from deeper-water, pre-Hangenberg Crisis strata. Neopolygnathus is interpreted as a palaeoecological generalist that variably blossomed in outer or inner shelf facies and after other conodont groups declined. The mostly loose ammonoid faunas comprise almost 30 taxa and fall mostly in the lower Wocklumian Kalloclymenia subarmata and Muessenbiaergia bisulcata zones (Upper Devonian = UD VI-A 1 /A 2 ), which agrees with previous ammonoid-conodont correlations. |
Author | Becker, Ralph Thomas Söte, Till Hartenfels, Sven |
Author_xml | – sequence: 1 givenname: Till surname: Söte fullname: Söte, Till email: t_soet01@uni-muenster.de organization: Institut für Geologie und Paläontologie, Westfälische Wilhelms-Universität Münster – sequence: 2 givenname: Sven surname: Hartenfels fullname: Hartenfels, Sven organization: Institut für Geologie und Paläontologie, Westfälische Wilhelms-Universität Münster – sequence: 3 givenname: Ralph Thomas surname: Becker fullname: Becker, Ralph Thomas organization: Institut für Geologie und Paläontologie, Westfälische Wilhelms-Universität Münster |
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CitedBy_id | crossref_primary_10_1016_j_palaeo_2019_05_041 crossref_primary_10_1007_s12549_019_00384_5 crossref_primary_10_1007_s12549_017_0296_x crossref_primary_10_1016_j_jafrearsci_2023_105007 crossref_primary_10_1007_s12542_022_00611_z crossref_primary_10_1007_s12549_020_00469_6 crossref_primary_10_1007_s12549_022_00539_x crossref_primary_10_1007_s12549_022_00540_4 crossref_primary_10_1007_s12549_022_00531_5 |
Cites_doi | 10.1007/BF02539734 10.1017/S001675681600039X 10.1007/BF02987980 10.1016/j.palaeo.2015.12.029 10.1007/s12549-017-0288-x 10.1144/SP423.10 10.1127/njgpm/1988/1988/605 10.1007/BF02988100 10.1111/j.1502-3931.2008.00102.x 10.20341/gb.2016.010 10.1127/0077-7749/2011/0144 10.1017/S0022336000033801 10.18814/epiiugs/1991/v14i4/004 10.1017/S0016756813000927 10.1127/nos/2015/0068 10.1017/S0016756816000893 10.1127/nos/3/1974/263 10.1127/njgpa/161/1981/172 10.3133/ofr93184 10.1007/978-3-662-08747-3 10.1144/SP423.14 10.5194/fr-3-27-2000 10.1130/SPE196-p143 10.1144/SP423.12 10.1127/0078-0421/2009/0043-0195 10.1007/s12549-014-0171-y 10.3140/bull.geosci.1547 |
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Copyright | Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg 2017 Copyright Springer Nature B.V. 2017 |
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Keywords | Ammonoids Stratigraphy Rhenish Massif Upper Devonian D/C boundary Conodonts |
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Snippet | As a contribution to the ongoing international revision of the Devonian/Carboniferous boundary, we present a bed-by-bed study of the Reigern Quarry in the... |
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SubjectTerms | Ammonoidea Animal Systematics/Taxonomy/Biogeography Biodiversity Biofacies Carboniferous Devonian Earth and Environmental Science Earth Sciences Ecological succession Freshwater & Marine Ecology Limestone Massifs Mud Nomenclature Original Paper Palaeoecology Paleontology Plant Systematics/Taxonomy/Biogeography Quarries Sedimentary facies Shelf facies Stratigraphy Taxa |
Title | Uppermost Famennian stratigraphy and facies development of the Reigern Quarry near Hachen (northern Rhenish Massif, Germany) |
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