Article ID Journal Published Year Pages File Type
6448431 Cretaceous Research 2014 12 Pages PDF
Abstract
The combined 87Sr/86Sr and δ18OBel isotope datasets suggest a synchronous negative δ18OBel shift for the middle Barremian. This shift, seen both in the Boreal and in the Tethys, indicates a major European wide phase of high humidity and increased run-off.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Palaeontology
Preview
Strontium-isotope stratigraphy of the Early Cretaceous (Valanginian-Barremian): Implications for Boreal-Tethys correlation and paleoclimate
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