Article (Scientific journals)
The Dinantian (Mississippian) succession of southern Belgium and surrounding areas: stratigraphy improvement and inferred climate reconstruction
Poty, Edouard
2016In Geologica Belgica, 19 (1-2), p. 177-200
Peer Reviewed verified by ORBi
 

Files


Full Text
Poty, 2016. faible resol
Publisher postprint (15.44 MB)
Download

All documents in ORBi are protected by a user license.

Send to



Details



Keywords :
Tournaisian; Viséan; glaciations; Milankovitch orbitally-forced cycles; sea-level changes; sequence stratigraphy
Abstract :
[en] The interactions between sea-level changes, local and global tectonics, and palaeoclimates have influenced the sedimentary deposition and the stratigraphy of the Belgian Dinantian. This paper emends the Belgian Dinantian sequence stratigraphy pattern and the third-order sequence 4 is divided into two sequences (4A, 4B). We also confirm that the sudden sea-level drop corresponding to the Hangenberg Sandstone at the Devonian – Carboniferous transition does not correspond to a third-order sequence boundary, but to an out-of-sequence event. The stratigraphy of the Tournaisian in the Namur, South Avesnois and Vesdre – Aachen sedimentation areas is clarified and leads to restrict the latter area to the Aachen vicinity only. The shape of the Namur – Dinant basin is revised and shows a migration of the depocenter northward during Dinantian times. During the Tournaisian, precession cycles are well developed and correspond to alternations of monsoon and dryer climates, without marked changes in the sea level. However, superimposed on these alternations, the Tournaisian third-order sequences recorded higher sea-level variations, which are considered to be due to glacio- eustatism, indicating long-duration period of ice formation. The very strong fall in the sea-level at the Tournaisian – Viséan boundary is considered to record the development of an ice-cap and to a heralding change to the Carboniferous climate with glaciations. From that time (sequence 5), marked eccentricity parasequences developed during the Viséan, recording alternating shorter interglacial-glacial periods. Thus, the onset of the Carboniferous glaciations is as early as the Early Viséan and not in the Late Viséan as usually considered.
Disciplines :
Earth sciences & physical geography
Author, co-author :
Poty, Edouard ;  Université de Liège > Département de géologie > Département de géologie
Language :
English
Title :
The Dinantian (Mississippian) succession of southern Belgium and surrounding areas: stratigraphy improvement and inferred climate reconstruction
Alternative titles :
[fr] La série dinantienne (Mississippien) du sud de la Belgique et des régions voisines: précision stratigraphique et reconstitution du climat inférée
Publication date :
December 2016
Journal title :
Geologica Belgica
ISSN :
1374-8505
eISSN :
2034-1954
Publisher :
Geologica Belgica, Bruxelles, Belgium
Volume :
19
Issue :
1-2
Pages :
177-200
Peer reviewed :
Peer Reviewed verified by ORBi
Available on ORBi :
since 15 February 2017

Statistics


Number of views
234 (17 by ULiège)
Number of downloads
324 (11 by ULiège)

Scopus citations®
 
41
Scopus citations®
without self-citations
38
OpenCitations
 
28

Bibliography


Similar publications



Contact ORBi