Isotopic evidence for partial geochemical decoupling between a Jurassic epicontinental sea and the open ocean

Volume: 82, Pages: 97 - 107
Published: Jun 1, 2020
Abstract
We report stable isotope ratios (δ13C, δ18O), minor and trace elements (Mn, Fe, Sr, Mg) together with Ca concentrations from bivalve shells and belemnites from the Middle-Upper Jurassic Sundance Seaway (western United States), we compare them with coeval open-ocean Tethyan data, and reconstruct the palaeo-circulation of seaway waters. The Sundance Seaway was a 2000 km long epicontinental sea with a single entrance at mid latitudes (55–60°N),...
Paper Details
Title
Isotopic evidence for partial geochemical decoupling between a Jurassic epicontinental sea and the open ocean
Published Date
Jun 1, 2020
Volume
82
Pages
97 - 107
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