Carbon isotope excursions and coeval environmental and biotic changes in the late Caradoc and Ashgill of Estonia

Acta Universitatis Carolinae, Geologica

Volumn 43, Issue 1-2, 1999, Pages 507-510

  Kaljo, D ^a   Hints, L ^a   Hints, O ^a   Martma, T ^a   Nolvak, J ^a  

^a TALLINN UNIVERSITY OF TECHNOLOGY   (Estonia)

Author keywords

[No Author keywords available]

Indexed keywords

ASHGILLIAN; CARADOCIAN; CARBON; ISOTOPIC COMPOSITION; ORDOVICIAN; PALEOENVIRONMENT; STRATIGRAPHY;

ESTONIA;

EID: 0033305036     PISSN: 00017132     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Conference Paper

References (18)

1. Evidence for a widespread carbon isotopic event associated with sedimentological and faunal changes in late Middle Ordovician in Estonia
2. Distribution of chitinozoans in the Tartu (453) core
3. Bathymetric and isotopic evidence for a short-lived Late Ordovician glaciation in a greenhouse period
4. Ordovician articulate brachiopods
5. Late Viruan (Caradoc) polychaete jaws from North Estonia and St. Petersburg region
6. An oceanic model for lithological and faunal changes tested on the Silurian record
7. Refinements of carbon isotope stratigraphy in the latest Ordovician of Estonia
8. Correlation of carbon isotope events and environmental cyclicity the East Baltic Silurian
9. More about Ordovician microfossil diversity patterns in the Rapla section, northern Estonia
10. Hirnantian glaciation and the carbon cycle
11. Global carbon isotopic events associated with mass extinction and glaciation in the late Ordovician
12. Ordovician chitinozoans zones from Baltoscandia
13. Late Middle Ordovician environmental change and extinction: Harbinger of the late Ordovician or continuation of Cambrian patterns
14. Late-Middle Ordovician environmental change: Molecular and isotopic evidence from North America
15. Skeletal debris content and composition in the sediments of the northern facial belt of the East Baltic Ordovician (Rapla boring)
16. 13C and lithostratigraphic profiles from Copenhagen Canyon, Nevada: Clues to the behaviour of ocean carbon during the Late Ordovician global crisis
17. Ordovician trilobites
18. The Ordovician radiations: Diversification and extinction shown by global genus-level taxonomic data