Conodonts across the Silurian/Devonian boundary in the Carnic Alps (Austria and Italy)

被引:18
|
作者
Corradini, Carlo [1 ]
Corriga, Maria G. [1 ]
Pondrelli, Monica [2 ]
Suttner, Thomas J. [3 ]
机构
[1] Univ Cagliari, Dipartimento Sci Chim & Geol, Cittadella Univ Blocco A SS-554 Bivio Sestu, I-09042 Monserrato, CA, Italy
[2] Univ G dAnnunzio, IRSPS, Viale Pindaro 42, I-65127 Pescara, Italy
[3] Nat Hist Museum Vienna, Geol Paleontol Dept, Burgring 7, A-1010 Vienna, Austria
关键词
Biostratigraphy; Palaeoecology; Palaeozoic; Microfossils; Peri-Gondwana; SILURIAN-DEVONIAN TRANSITION; CARBON-ISOTOPE STRATIGRAPHY; HIGH-RESOLUTION; NORTH-AMERICA; BIOSTRATIGRAPHY; FAUNAS;
D O I
10.1016/j.palaeo.2019.02.023
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
In the Carnic Alps, located across the border between Italy and Austria, several sections span the Silurian/Devonian boundary in different sedimentary settings, from very shallow water to moderately deep shelf. All studied sections yielded conodonts and based on the first and last occurrences of the conodont taxa in the upper part of the Upper Oul. el. detortus Zone and in the lower part of the I. hesperius Zone a detailed conodont biostratigraphic framework was able to be constructed for this interval. Comparison of data from different depositional settings demonstrates that, although the majority of species are documented everywhere in the Carnic basin, a few taxa, mainly represented by coniforms, are limited to shallow water, whereas others, mainly ozarkodinids, occur only in open sea deposits.
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页数:14
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