Palynology of the Lower Eocene deposits of Northwest Jutland, Denmark
(2004) In Bulletin of the Geological Society of Denmark 52. p.141-157- Abstract
- Early Eocene spores and pollen assemblages from the uppermost part of the Stolle Klint Clay and
the overlying Fur Formation are diverse and well preserved. The terrestrial microflora comprises 42
species of spores and 108 species of pollen and four spores and pollen zones are established i.e.
Interpollis velum-Labrapollis globosus, Basopollis atumenscens, Basopollis orthobasalis and Thomsonipollis
magnificus zones. The zones are directly correlated to the existing tephrachronology and stratigraphy.
The dinoflagellate cysts assemblages are referred to Zones 6 and 7 of Heilmann-Clausen or the
upper part of the Apectodinium hyperacanthum and Glaphyrocysta ordinata Interval Biozone of... (More) - Early Eocene spores and pollen assemblages from the uppermost part of the Stolle Klint Clay and
the overlying Fur Formation are diverse and well preserved. The terrestrial microflora comprises 42
species of spores and 108 species of pollen and four spores and pollen zones are established i.e.
Interpollis velum-Labrapollis globosus, Basopollis atumenscens, Basopollis orthobasalis and Thomsonipollis
magnificus zones. The zones are directly correlated to the existing tephrachronology and stratigraphy.
The dinoflagellate cysts assemblages are referred to Zones 6 and 7 of Heilmann-Clausen or the
upper part of the Apectodinium hyperacanthum and Glaphyrocysta ordinata Interval Biozone of Powell.
A marked shift in the terrestrial and marine palynomorph assemblages takes place at the transition
between the two oldest spore and pollen zones at c. 1.2 m below ash layer –19b. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/3131491
- author
- Willumsen, Pi LU
- publishing date
- 2004
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- Palynology, early Eocene, spores and pollen, Stolle Klint Clay, Fur Formation, tephrachronology, biostratigraphy, correlation
- in
- Bulletin of the Geological Society of Denmark
- volume
- 52
- pages
- 141 - 157
- publisher
- Geological Society of Denmark
- external identifiers
-
- scopus:25844432350
- ISSN
- 0011-6297
- language
- English
- LU publication?
- no
- additional info
- My affiliation in connection with this publication: Department of Geosciences, University of Oslo, P.O. Box 1047, Blindern, NO-0316 Oslo, Norway.
- id
- d11362d6-967b-44e3-94cb-80341f165d6a (old id 3131491)
- date added to LUP
- 2016-04-01 16:52:57
- date last changed
- 2022-04-07 19:21:39
@article{d11362d6-967b-44e3-94cb-80341f165d6a,
abstract = {{Early Eocene spores and pollen assemblages from the uppermost part of the Stolle Klint Clay and<br/><br>
the overlying Fur Formation are diverse and well preserved. The terrestrial microflora comprises 42<br/><br>
species of spores and 108 species of pollen and four spores and pollen zones are established i.e.<br/><br>
Interpollis velum-Labrapollis globosus, Basopollis atumenscens, Basopollis orthobasalis and Thomsonipollis<br/><br>
magnificus zones. The zones are directly correlated to the existing tephrachronology and stratigraphy.<br/><br>
The dinoflagellate cysts assemblages are referred to Zones 6 and 7 of Heilmann-Clausen or the<br/><br>
upper part of the Apectodinium hyperacanthum and Glaphyrocysta ordinata Interval Biozone of Powell.<br/><br>
A marked shift in the terrestrial and marine palynomorph assemblages takes place at the transition<br/><br>
between the two oldest spore and pollen zones at c. 1.2 m below ash layer –19b.}},
author = {{Willumsen, Pi}},
issn = {{0011-6297}},
keywords = {{Palynology; early Eocene; spores and pollen; Stolle Klint Clay; Fur Formation; tephrachronology; biostratigraphy; correlation}},
language = {{eng}},
pages = {{141--157}},
publisher = {{Geological Society of Denmark}},
series = {{Bulletin of the Geological Society of Denmark}},
title = {{Palynology of the Lower Eocene deposits of Northwest Jutland, Denmark}},
volume = {{52}},
year = {{2004}},
}