Phosphatised olenid trilobites and associated fauna from the Upper Cambrian of Vastergotland, Sweden

被引:0
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作者
Ahlberg, P
Szaniawski, H
Clarkson, ENK
Bengtson, S
机构
[1] GeoBiosphere Sci Ctr, Dept Geol, SE-22362 Lund, Sweden
[2] Inst Paleobiol, PL-00818 Warsaw, Poland
[3] Univ Edinburgh, Sch Geosci, Grant Inst Earth Sci, Edinburgh EH9 3JW, Midlothian, Scotland
[4] Swedish Museum Nat Hist, Dept Palaeozool, SE-10405 Stockholm, Sweden
关键词
olenidae; trilobita; problematica; phosphatisation; Cambrian; Alum Shales; Vastergotland; Sweden;
D O I
暂无
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Secondarily phosphatised olenid trilobites from organic-rich limestones (orsten) in the Furongian (Upper Cambrian) of Vastergotland, south-central Sweden, are described and illustrated. All trilobites originate from the Peltura scarabaeoides Zone and were collected on the western slope of Kinnekulle. Only the dorsal exoskeletons have become secondarily phosphatised, and the ventral appendages are not preserved. Yet the material is otherwise remarkably well preserved and reveals the morphology of the olenid trilobites in greater detail than hitherto known. Species belonging to the genera Ctenopyge, Sphaerophthalmus, Parabolina, and Peltura are identified, and several juvenile specimens are present in the material. The material is disarticulated and fragmentary, and it has only been possible to identify a few specimens to species level. In addition to chaetognaths and conodonts, the trilobites are associated with pelmatozoan columnals, a possible camaroid, and fossils of uncertain affinities. These fossils, along with a probable conulariid fragment from the Peltura minor Zone, are also described and discussed. The presence of a benthic fauna of pelmatozoans, and possible conulariids and camaroids, indicates that at least parts of the Peltura zones were deposited during dysoxic rather than anoxic periods. Moreover, the sea floor must have been firm enough to allow colonisation by sessile organisms.
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页码:429 / 440
页数:12
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