Relative timing of critical events during the late Ordovician mass extinction - New data from Oslo

Acta Universitatis Carolinae, Geologica

Volumn 43, Issue 1-2, 1999, Pages 187-190

  Brenchley, P J ^a   Marshall, J D ^a  

^a UNIVERSITY OF LIVERPOOL   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

BIOSTRATIGRAPHY; MASS EXTINCTION; ORDOVICIAN; STRATIGRAPHY;

EID: 0033304989     PISSN: 00017132     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Conference Paper

References (15)

1. Glacio-eustatic control of late Ordovician-Early Silurian platform sedimentation and faunal change
2. The Diploporita of the Oslo Region, Norway
3. Environmental changes associated with the 'first strike' of the late Ordovician mass extinction
4. Ecological associations in a regressive sequence: The latest Ordovician of the Oslo-Asker district, Norway
5. Bathymetric and isotopic evidence for a short-lived Late Ordovician glaciation in a greenhouse period
6. New data solving an old biostratigraphic problem: The age of the upper Ordovician brachiopod Holorhynchus giganteus
7. The stratigraphy of the upper Ordovician Stage 5 in the Oslo-Asker district, Norway
8. A facies analysis of upper Ordovician regressive sequences in the Oslo region, Norway - A record of glacio-eustatic changes
9. There are extinctions and extinctions; examples from the Palaeozoic
10. Global carbon isotopic events associated with mass extinction and glaciation in the Late Ordovician
11. The Ashgill trilobites of the Oslo Region, Norway
12. The Ordovician successions of the Oslo Region, Norway
13. Ecological changes during the end-Ordovician extinction
14. Ordovician boundary in the Prague Basin (Barrandian area, Bohemia)