Pattern of conodont extinction and recovery across the Ordovician-Silurian boundary interval

Acta Universitatis Carolinae, Geologica

Volumn 43, Issue 1-2, 1999, Pages 211-212

  Barnes, C R ^a   Zhang, S ^a  

^a UNIVERSITY OF VICTORIA   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

MASS EXTINCTION; ORDOVICIAN; ORDOVICIAN-SILURIAN BOUNDARY;

CONODONTA;

EID: 0033304671     PISSN: 00017132     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Conference Paper

References (12)

1. The faunal extinction event near the Ordovician-Silurian boundary: A climatically induced crisis
2. Stratigraphy and paleontology of the Ordovician-Silurian boundary interval, Anticosti Island, Quebec
3. Conodont biostratigraphy of the uppermost Ordovician and lowermost Silurian
4. The pattern of global bio-events during the Ordovician Period
5. The Late Ordovician extinction
6. Bathymetric and isotope evidence for a short-lived Late Ordovician glaciation in a greenhouse period
7. Ordovician-Silurian glaciations and global sea-level changes
8. Oxygen and carbon isotopes and event startigraphy near the Ordovician-Silurian boundary, Anticosti Island, Quebec
9. Late Ordovician conodonts from the Vaureal formation, Anticosti Island, Quebec
10. Conodont biostratigraphy and paleoecology of the Ellis Bay Formation, Anticosti Island, Quebec, with special reference to Late Ordovician-Early Silurian chronostratigraphy and the systemic boundary
11. The Ordovician radiations: Diversification and extinction shown by global genus-level taxonomic data
12. Conodonts of the Jupiter and Chicotte Formations (Lower Silurian), Anticosti Island, Quebec