Dimitri Kaljo
Tallinn University of Technology, Tallinn, N/A
Activity
2014
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SULFUR ISOTOPE EVIDENCE FOR LATE ORDOVICIAN OCEAN OXYGENATION: IMPLICATIONS FOR THE DRIVERS OF THE HIRNANTIAN EXTINCTION
T257 The Ordovician Revolution: Co-Evolution of Climate and the BiosphereTuesday, 21 October 20141:00 PM - 5:00 PM215/216
2007
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A GLOBAL CHANGE IN δ13C OF ORGANIC MATTER DURING THE LATE ORDOVICIAN HIRNANTIAN: IMPLICATIONS FOR ATMOSPHERIC CO2 LEVELS AND GLACIATION
T28 Late Paleozoic Glacial-interglacial Climate Changes: Analogs for Present and Future Climate Changes (Posters)Sunday, 28 October 20078:00 AM - 12:00 PM