Pliocene climate and seasonality in North Atlantic shelf seas

• Published in: Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
• Main Authors: Williams, Mark, Haywood, Alan M, Harper, Elizabeth M, Johnson, Andrew L.A, Knowles, Tanya, Leng, Melanie J, Lunt, Daniel J, Okamura, Beth, Taylor, Paul D, Zalasiewicz, Jan
• Format: Article in Journal/Newspaper
• Language: English
• Published: The Royal Society 2008
• Subjects: North Atlantic
• Online Access: http://dx.doi.org/10.1098/rsta.2008.0224; https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.2008.0224; https://royalsocietypublishing.org/doi/full-xml/10.1098/rsta.2008.0224

This paper reviews North Atlantic shelf seas palaeoclimate during the interval 4–3 Ma, prior to and incorporating the ‘Mid-Pliocene warm period’ ( ca 3.29–2.97 Ma). Fossil assemblages and stable isotope data demonstrate northwards extension of subtropical faunas along the coast of the Carolinas–Virginia (Yorktown and Duplin Formations) relative to the present day, suggesting a more vigorous Florida Current, with reduced seasonality and warm water extending north of Cape Hatteras (reconstructed annual range for Virginia 12–30°C). This interpretation supports conceptual models of increased meridional heat transport for the Pliocene. Sea temperatures for Florida (Lower Pinecrest Beds) were similar to or slightly cooler than (summers 25–27°C) today, and were probably influenced by seasonal upwelling of cold deep water. Reduced seasonality is also apparent in the Coralline Crag Formation of the southern North Sea, with ostracods suggesting winter sea temperatures of 10°C (modern 4°C). However, estimates from Pliocene bivalves (3.6–16.6°C) are similar to or cooler than the present day. This ‘mixed’ signal is problematic given warmer seas in the Carolinas–Virginia, and climate model and oceanographic data that show warmer seas in the ‘Mid-Pliocene’ eastern North Atlantic. This may be because the Coralline Crag Formation was deposited prior to peak Mid-Pliocene warmth.