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Supplemental material: Orbital-scale climate change and glacioeustasy during the early Late Ordovician (pre-Hirnantian) determined from d18O values in marine apatite

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posted on 2013-01-01, 00:00 authored by M. Elrick, et al.
GSA Data Repository Item 2013214, Geology. File size: about 1148 KB.

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