Paleoecologic and paleoceanographic interpretation of δ18O variability in Lower Ordovician conodont species

Conodont δ18O is increasingly used to reconstruct Paleozoic–Triassic seawater temperature changes. Less attention has been paid to δ18O variation in time slices across paleoenvironments, within sample assemblages, or for reconstructing the thermal structure of Paleozoic oceans. Furthermore, there ha...

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Bibliographic Details
Published in:Geology
Main Authors: Wheeley, JR, Jardine, PE, Raine, RJ, Boomer, I, Smith, P
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of America 2018
Subjects:
Online Access:https://doi.org/10.1130/G40145.1
https://ora.ox.ac.uk/objects/uuid:53f778e9-8d88-4472-b060-8dc8baa6ee0c