Nucula percrassa from the Cretaceous Prince Creek Fm. was analyzed for C, O-isotopes.
Data from the Alaskan bivalve suggests salinity of water was between 8 and 17.7 ppt.
Isotopic composition of water ranged between − 14.41 and − 16.23‰ V-SMOW.
Based on new and published data, fresh:marine water ranged from ~ 50:50 to 72:28%.
High latitude ancient Arctic greenhouse climate was highly variable.