Dalecarlioceras dalecarlicum ( Frye, 1987 ), 2013
publication ID |
https://dx.doi.org/10.5852/ejt.2013.41 |
publication LSID |
lsid:zoobank.org:pub:A2F1B9ED-870A-466E-B35E-BD5DA782476E |
persistent identifier |
https://treatment.plazi.org/id/AD4D9054-CD73-6A71-F3B6-469CFD49F8E8 |
treatment provided by |
Carolina (2020-05-07 19:54:00, last updated 2020-05-07 20:06:13) |
scientific name |
Dalecarlioceras dalecarlicum ( Frye, 1987 ) |
status |
comb. nov. |
Dalecarlioceras dalecarlicum ( Frye, 1987) comb. nov.
Fig. 7B View Fig
Cyrtorizoceras dalecarlicum Frye, 1987: 88 , 89, fig. 6d-f.
Emended diagnosis
Dalecarlioceras with slightly curved adult body chamber, with maximum adult height/width of ca. 40/ 38 mm, and adult peristome height/width 37/33.
Holotype
PMU 24774 View Materials .
Type locality and horizon
Kallholn, Siljan District, Sweden, Boda Limestone, Boda Core Member, late Katian, Ordovician.
Other material examined
One specimen ( PMU 24775 View Materials ) from Kallholn, Dalarna; one specimen from Rättvik, Dalarna, NRM Mo 150043, Boda Limestone, Boda Core Member, late Katian.
Description
See Frye (1987: 88-89) for a detailed description.
Remarks
Dalecarlioceras is endemic to the Boda Limestone. Originally, two species were assigned to this genus: the large D. bodense , characterized by a high angle of expansion, and the somewhat smaller, more slender D. constrictum Frye, 1987 ( Fig. 7A View Fig ). Herein, the medium sized Cyrtorizoceras dalecarlicum Frye, 1987 is considered an additional species of Dalecarlioceras . Dalecarlioceras dalecarlicum ( Frye, 1987) comb. nov. has an only slightly curved adult body chamber, combined with a slightly irregularly spaced ornamentation with transverse growth lines similar to those of D. bodense . The mature body chamber of D. dalecarlicum comb. nov. differs from that of Cyrtorizoceras in having a nearly straight, or slightly concave outline in lateral view ( Fig. 7 View Fig B-C); it is clearly compressed at the aperture in frontal view. Consequently, the body chamber of D. dalecarlicum comb. nov. is widest approximately at mid-length, like in D. bodense . D. dalecarlicum comb. nov. is considered to represent a transitional form between D. constrictum and Cyrtorizoceras thorslundi sp. nov. Together these forms represent a transition from the relatively small and slender C. thorslundi sp. nov., with a weakly gibbous body chamber, toward the massive, and strongly gibbous D. bodense . This suggests an ancestry or close relationship of Dalecarlioceras to Cyrtorizoceras .
Stratigraphic and geographic range
Boda Limestone, Dalarna, Sweden; late Katian.
Frye M. W. 1987. Upper Ordovocian (Harjuan) oncoceratid nautiloids from Boda Limestone, Siljan District, Sweden. Geologiska Foreningens i Stockholm Forhandlingar 109: 83 - 99. http: // dx. doi. org / 10.1080 / 11035898709454748
Fig. 7. Breviconic cephalopods of the Boda Limestone and details of an endocerid. A. Dalecarlioceras constrictum Frye, 1987, PMU 24777, holotype, Kallholn. B. Dalecarlioceras dalecarlicum (Frye, 1987) comb. nov., PMU 24774, holotype, Kallholn. C. Cyrtorizoceras thorslundi sp. nov., PMU 26658, Kallholn; note the morphological transition between D. constrictum and C. thorslundi sp. nov.; the adult size increases in Dalecarlioceras and the mature body chamber is gibbous. D. Cameroceras turrisoides sp. nov., PMU 26623, Osmundberget, lateral view of apical fragment with abrupt transition between embryonic and juvenile conch. E. Strandoceras sphinx (Schmidt, 1858), PMU 26629, Kallholn. Scale bars: A-C, E = 10 mm; D = 10 mm.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
Kingdom |
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Order |
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Genus |
Dalecarlioceras dalecarlicum ( Frye, 1987 )
Kröger, Björn 2013 |
Cyrtorizoceras dalecarlicum
Frye M. W. 1987: 88 |
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