Neodymium Isotope Ratios and a Positive δ13C Excursion: Connecting Oceanographic and Climate Changes Near the M4-M5 Sequence Boundary of the Late Ordovician
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Neodymium Isotope Ratios and a Positive δ13C Excursion: Connecting Oceanographic and Climate Changes Near the M4-M5 Sequence Boundary of the Late Ordovician