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from the uppermost Keila (above the GICE) up to the lower Rakvere RS (Fig.
Also the Guttenberg (GICE) and the Mid-Darriwilian (MDICE) isotopic carbon excursions have proved to be useful for global correlations (e.g.
[1.] Director GICE clinic, Department of Obstetrics and gynaecology, Kalyani, Nadia, West Bengal India.
The second largest [delta][sup.13]C isotope excursion known in the Ordovician, the Guttenberg ICE (GICE), is recorded in the Tartu-453 drillcore as a distinct asymmetric peak in the highly argillaceous to silty limestones of late Keila to early Oandu age.
Reef formation culminated and terminated during the Guttenberg Isotopic Carbon Excursion (GICE) interval.
Between the pronounced positive excursions of the MDICE and the GICE, the latter located in the Freberga Formation, there are two smaller positive excursions which have to be investigated for their potential to correlate on an intrabasinal scale.
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