Not exact matches
The aim of my PhD is to use the
distribution of diatom species preserved in
sediment cores across the Scotia
Sea to reconstruct the position of major ocean boundaries and water masses through time.
Microfossil
distributions in modern Amundsen
Sea sediments.
What is true is that there is very very strong evidence from paleoclimate data (deep
sea sediment cores) for changes in the
distribution of chemical tracers that must reflect changes in the deep circulation in the Atlantic.
Xiao, X., Fahl, K., Müller, J. & Stein, R.
Sea - ice
distribution in the modern Arctic Ocean: biomarker records from Trans - Arctic Ocean surface
sediments.