Linked from

The 16 pages that link to Paleoceanography, each with the reason it gives.

• PaleomagnetismRelated: Sediment magnetic records provide the time framework for ocean history.

• PhytoplanktonRelated: Fossil phytoplankton shells preserve evidence of past ocean conditions.

• Marine sedimentRelated: Seafloor layers record changes in ocean circulation, productivity, and chemistry.

• Early JurassicRelated: Marine sediments from this epoch preserve changes in circulation and oxygenation.

• PaleoenvironmentRelated: Marine sediments preserve evidence of changing ocean conditions and ecosystems.

• Carbon isotope excursionRelated: Marine isotope records help reconstruct ancient ocean conditions during excursions.

• MicropaleontologyRelated: Marine microfossil assemblages record changing ocean conditions.

• Pelagic sedimentRelated: Pelagic sediment is a primary archive for reconstructing ancient ocean conditions.

• SeabedRelated: Seabed sediments preserve records used to reconstruct ancient ocean conditions.

• TestRelated: Chemical records in fossil tests help reconstruct ancient oceans.