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Reconstructing the paleohydrology of a cretaceous Alaskan paleopolar coastal plain from stable isotopes of bivalves
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文摘

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.

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