Brachiopod faunas from the basinal facies of southeastern Thuringia (Germany) before and after the Hangenberg Crisis (Devonian-Carboniferous boundary)

被引:5
|
作者
Mottequin, Bernard [1 ]
Bartzsch, Konrad [2 ]
Simon, Eric [1 ]
Weyer, Dieter [3 ]
机构
[1] Royal Belgian Inst Nat Sci, Operat Directorate Earth & Hist Life, Rue Vautier 29, B-1000 Brussels, Belgium
[2] Stauffenberg Str 68, D-07318 Saalfeld, Germany
[3] Humboldt Univ, Leibniz Inst, Museum Nat Hist, Invalidenstr 43, D-10115 Berlin, Germany
关键词
Brachiopoda; Famennian; Tournaisian; Hangenberg Crisis; Thuringia; Germany; BIOSTRATIGRAPHY; CLASSIFICATION; SPHENOTHALLUS; MORPHOLOGY; MOUNTAINS; ONTOGENY; FOSSILS; SECTION; GENERA;
D O I
10.26879/833
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Upper Famennian-Tournaisian (Hastarian) brachiopods from the deep-water, mixed siliciclastic-carbonate Gleitsch Formation (Breternitz and Pfaffenberg members) of southeastern Thuringia (mainly from the Saalfeld area, Germany) are described systematically. A new Tournaisian rhynchonellide genus (Thuringorhynchus gen. nov.) and four new Tournaisian species are described (Productina saalfeldensis sp. nov., Thuringorhynchus pseudoequitans gen. et sp. nov., Cleiothyridina pfaffenbergensis sp. nov., and Crassumbo germanicus sp. nov.). Moreover, the lectotype of "Lingularia" straeleni (Demanet, 1934), from the Tournaisian of Belgium, is selected. Prior the Hangenberg Crisis, the brachiopod assemblage (10 species) of the Breternitz Member (upper and uppermost Famennian) is strongly dominated by species belonging to smooth to poorly ornamented rhynchonellide genera (Hadyrhyncha, Novaplatirostrum, Rozmanaria, and rozmanariid? gen. indet.) notably reported from Laurussia and the northern margin of Gondwana. The onset of the Hangenberg Crisis is marked by an anoxic black shale horizon at the top of the Breternitz Member followed by the siltstones and turbiditic sandstones of the Obernitz Member; both horizons did not yield brachiopods. A completely changed, more diverse brachiopod assemblage (15 species) existed in the Pfaffenberg Member (Tournaisian, lower Hastarian), which also included a basal 20 cm "topmost Famennian" (according to the current, soon abandoned definition of the Carboniferous base using Siphonodella sulcata as criterion), but clearly dated as upper Protognathodus kockeli Zone). Small-sized productidines (Productina) and spiriferides (Crassumbo, Texathyris?) dominate; a probable complete turnover is recorded among the Rhynchonellida (Thuringorhynchus). The rapid recovery after the drastic Hangenberg extinction event includes species belonging to pre-existing genera and to new ones.
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