SwePub
Sök i LIBRIS databas

  Extended search

onr:"swepub:oai:lup.lub.lu.se:d81b19ee-56db-42b8-9b67-3b9349a40f33"
 

Search: onr:"swepub:oai:lup.lub.lu.se:d81b19ee-56db-42b8-9b67-3b9349a40f33" > The Miaolingian, a ...

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

The Miaolingian, a new name for the ‘Middle’ Cambrian (Cambrian Series 3) : identification of lower and upper boundaries in Baltoscandia

Nielsen, Arne Thorshøj (author)
University of Copenhagen
Ahlberg, Per (author)
Lund University,Lunds universitet,Berggrundsgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Lithosphere and Biosphere Science,Department of Geology,Faculty of Science
 (creator_code:org_t)
2019-10-03
2019
English 12 s.
In: GFF. - : Informa UK Limited. - 1103-5897 .- 2000-0863. ; 141:2, s. 162-173
  • Research review (peer-reviewed)
Abstract Subject headings
Close  
  • The Miaolingian is the new formal name for Cambrian Series 3 (≈ “Middle” Cambrian). The Global Stratotype Section and Point (GSSP) is defined in the Kaili Formation, Guizhou province, China, and is correlated by the First appearance Datum (FAD) of the trilobite Oryctocephalus indicus. However, this fossil has not been recorded from Baltoscandia. Here acritarchs may be used for identifying the base of the Miaolingian, but (1) Does the GSSP level in China correspond to the FAD of the Eliasum–Cristallinium acritarch assemblage? and (2) How accurately is the incoming of this assemblage identified in Baltoscandian sections? Comparison of acritarchs shared between the GSSP section and Baltica indicates that the GSSP correlates with a level within the Baltoscandian Eliasum–Cristallinium assemblage zone. Nonetheless, it appears most feasible to consider the base of this zone (i.e., the base of the Kibartian Regional Stage) as the best possible local approximation for the base of the Miaolingian. This level equates the traditional lower boundary of the “Middle” Cambrian used in East Europe. In much of Scandinavia, the lower boundary of the Miaolingian thus identified falls within the Hawke Bay hiatus. Hence, the Miaolingian by and large corresponds to the interval that previously has been assigned to the “Middle” Cambrian in the region, except that the Miaolingian includes the Agnostus pisiformis Zone, traditionally assigned to the “Upper” Cambrian. In Scandinavia, the Miaolingian/Furongian boundary is precisely defined, being marked by the incoming of Glyptagnostus reticulatus and abundant olenid trilobites. In the East Baltic area, the upper boundary of the Miaolingian coincides with a major unconformity.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)

Keyword

acritarchs
Baltica
Baltoscandia
Cambrian
Kibartian
Miaolingian
stages
stratigraphy

Publication and Content Type

for (subject category)
ref (subject category)

Find in a library

  • GFF (Search for host publication in LIBRIS)

To the university's database

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

Find more in SwePub

By the author/editor
Nielsen, Arne Th ...
Ahlberg, Per
About the subject
NATURAL SCIENCES
NATURAL SCIENCES
and Earth and Relate ...
and Geology
Articles in the publication
GFF
By the university
Lund University

Search outside SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Close

Copy and save the link in order to return to this view