Although the modern Arctic Ocean is regarded as a barometer of global change and an amplifier of global warming, little is known about its state in the greenhouse period of the Late Cretaceous epoch (65–99 million years ago). Here, a seasonally resolved Cretaceous sedimentary record from the Alpha ridge of the Arctic Ocean is presented; evidence suggests seasonal diatom productivity in a stratified ocean with possible winter sea ice cover.
- Andrew Davies
- Alan E. S. Kemp
- Jennifer Pike