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-List Of Titles -Siluro-Devonian (Pridoli-Lochkovian and early Emsian) conodonts from the Nowshera area, Pakistan : implications for the mid-Palaeozoic stratigraphy of the Peshawar Basin

Please use this identifier to cite or link to this item: http://hdl.handle.net/1959.14/29208

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Title
Siluro-Devonian (Pridoli-Lochkovian and early Emsian) conodonts from the Nowshera area, Pakistan : implications for the mid-Palaeozoic stratigraphy of the Peshawar Basin
Related
Australian Conodont Symposium (2nd : 2000) (3 - 7 July 2000 : Orange, NSW)
Related
Mawson, Ruth and Talent, John A.. Contributions to the Second Australian Conodont Symposium (AUSCOS II) held in conjunction with Palaeontology DownUnder-2000, p.83-105
Related
Courier Forschungsinstitut Senkenberg 245
Publisher
Stuttgart : E. Schweizerbart'sche Verlagsbuchhandlung
Date
2003
Author/Creator
Mawson, Ruth
Author/Creator
Talent, John A
Author/Creator
Molloy, Peter D
Author/Creator
Simpson, Andrew J
Description
The Kandar Formation (junior synonym, Panjpir Formation) spans most of the Silurian time from Llandovery-Wenlock to Pridoli, with its youngest horizons, documented by conodonts, falling within the Pridoli eosteinhornensis Zone. Portion of the conformably overlaying (but perhaps locally unconformable) Nowshera Limestone of the Nowshera-Pir Sabak area falls within the eosteinhornensis Zone, but the bulk of this unit is inferred to extend from Early Devonian (Lochkovian) near Kandar though to dehiscens Zone (early Emsian) in the highest beds exposed at Pir Sabak. The question of which, if any, of the intervening zones may be represented needs clarification. Regional considerations suggest that Silurian-Devonian sequences around the eastern flank of the Peshawar Basin may display a conspicuous transgressive event within the Middle Devonian. This needs to be probed. It is suggested therefore that caution should be exercised before late Emsian and younger sequences around the Peshwar Basin are referred to the Nowshera Limestone – at least until additional stratigraphic-cum-sedimentary and chronologic data demonstrate continuity of sedimentation through the Middle Devonian for these sequences. From the Nowshera Limestone, a new subspecies of Ozarkodina remscheidensis, O. r. prosoplatys is described. It is proposed that the new subspecies is an intermediate between O. r. eosteinhornensis and the Ancyrodelloides (= Lanea sesu Murphy & Valenzuelos-Rios 1999) lineage.
Description
23 page(s)
Subject Keyword
Kandar Formation
Subject Keyword
Nowshera Limestone
Subject Keyword
Pir Sabak Dehri
Subject Keyword
Pridoli
Subject Keyword
Lochkovian
Subject Keyword
early Emsian
Resource Type
conference paper
Organisation
Macquarie University. Dept. of Earth and Planetary Sciences

Identifier
http://hdl.handle.net/1959.14/29208
Identifier
ISBN:3510613627
Identifier
ISSN:0341-4116
Identifier
mq-rm-2003018622
Language
eng
Reviewed
Reviewed
Save/E-mail Citation
Citation Format
E-mail Address
Subject
"Contributions to the Second Australian Conodont Symposium (AUSCOS II) held in conjunction with Palaeontology DownUnder-2000"
 
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