The Almelund Shale, a replacement name for the Upper Didymograptus Shale and the Lower Dicellograptus Shale in the lithostratigraphical classification of the Ordovician succession in Scania, Southern Sweden
(2002) In Bulletin of the Geological Society of Denmark 49. p.41-47- Abstract
- The formation name Almelund Shale is proposed for a lithostratigraphically defined unit to replace the outdated chronostratigraphical designations Upper Didymograptus Shale and Dicellograptus Shale in the Middle and lowermost Upper Ordovician succession in Scania. The Almelund Shale is a lithologically uniform unit of dark-grey to black shales with rare carbonate interbeds between the Komstad Limestone and the Sularp Shale. Apart from a diverse graptolite fauna it yields a few shelly fossils (mostly lingulate brachiopods) and biostratigraphically diagnostic conodonts and chitinozoans. In the type sections of the Almelund Shale along the Sularp Brook in the F (a) over circle gels (a) over circle ng area; W-central Scania, the top of the... (More)
- The formation name Almelund Shale is proposed for a lithostratigraphically defined unit to replace the outdated chronostratigraphical designations Upper Didymograptus Shale and Dicellograptus Shale in the Middle and lowermost Upper Ordovician succession in Scania. The Almelund Shale is a lithologically uniform unit of dark-grey to black shales with rare carbonate interbeds between the Komstad Limestone and the Sularp Shale. Apart from a diverse graptolite fauna it yields a few shelly fossils (mostly lingulate brachiopods) and biostratigraphically diagnostic conodonts and chitinozoans. In the type sections of the Almelund Shale along the Sularp Brook in the F (a) over circle gels (a) over circle ng area; W-central Scania, the top of the unit is taken to be the base of the F (a) over circle gels (a) over circle ng Phosphorite, and its basal contact is at the top of the underlying Komstad Limestone. Its total thickness in the F (a) over circle gels (a) over circle ng drill-core is 28.32 m. The unit is widely distributed in the subsurface in a SE-NW belt across Scania. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/310692
- author
- Bergstrom, SM ; Larsson, Kent LU ; Pålsson, Christian LU and Ahlberg, Per LU
- organization
- publishing date
- 2002
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- lithostratigraphy, Ordovician, graptolite biostratigraphy, Scania, Sweden
- in
- Bulletin of the Geological Society of Denmark
- volume
- 49
- pages
- 41 - 47
- publisher
- Geological Society of Denmark
- external identifiers
-
- wos:000183021200004
- scopus:24544477659
- ISSN
- 0011-6297
- language
- English
- LU publication?
- yes
- id
- 79654ddc-3c37-45b5-840b-043809b1e2a0 (old id 310692)
- date added to LUP
- 2016-04-01 16:56:19
- date last changed
- 2022-01-28 23:12:05
@article{79654ddc-3c37-45b5-840b-043809b1e2a0, abstract = {{The formation name Almelund Shale is proposed for a lithostratigraphically defined unit to replace the outdated chronostratigraphical designations Upper Didymograptus Shale and Dicellograptus Shale in the Middle and lowermost Upper Ordovician succession in Scania. The Almelund Shale is a lithologically uniform unit of dark-grey to black shales with rare carbonate interbeds between the Komstad Limestone and the Sularp Shale. Apart from a diverse graptolite fauna it yields a few shelly fossils (mostly lingulate brachiopods) and biostratigraphically diagnostic conodonts and chitinozoans. In the type sections of the Almelund Shale along the Sularp Brook in the F (a) over circle gels (a) over circle ng area; W-central Scania, the top of the unit is taken to be the base of the F (a) over circle gels (a) over circle ng Phosphorite, and its basal contact is at the top of the underlying Komstad Limestone. Its total thickness in the F (a) over circle gels (a) over circle ng drill-core is 28.32 m. The unit is widely distributed in the subsurface in a SE-NW belt across Scania.}}, author = {{Bergstrom, SM and Larsson, Kent and Pålsson, Christian and Ahlberg, Per}}, issn = {{0011-6297}}, keywords = {{lithostratigraphy; Ordovician; graptolite biostratigraphy; Scania; Sweden}}, language = {{eng}}, pages = {{41--47}}, publisher = {{Geological Society of Denmark}}, series = {{Bulletin of the Geological Society of Denmark}}, title = {{The Almelund Shale, a replacement name for the Upper Didymograptus Shale and the Lower Dicellograptus Shale in the lithostratigraphical classification of the Ordovician succession in Scania, Southern Sweden}}, volume = {{49}}, year = {{2002}}, }