Climate Evolution Through the Onset and Intensification of Northern Hemisphere Glaciation
Erin L. McClymont, Sze Ling Ho, Heather L. Ford, Ian Bailey, Melissa A. Berke, Clara T Bolton, Stijn De Schepper, Georgia Grant, Jeroen Groeneveld, Gordon N. Inglis, Cyrus Karas, Molly O. Patterson, George E. A. Swann, Kaustubh Thirumalai, S. M. White, Montserrat Alonso‐García, Pallavi Anand, Babette Hoogakker, Kate Littler, Benjamin Petrick, Bjørg Risebrobakken, Jordan T. Abell, Anya J. Crocker, Friso de Graaf, Sarah J. Feakins, J. C. Hargreaves, Chloe Jones, Monika Markowska, Amila Sandaruwan Ratnayake, Christian Stepanek, D. Tangunan
Abstract
Abstract The Pliocene Epoch (∼5.3–2.6 million years ago, Ma) was characterized by a warmer than present climate with smaller Northern Hemisphere ice sheets, and offers an example of a climate system in long‐term equilibrium with current or predicted near‐future atmospheric CO 2 concentrations ( p CO 2 ). A long‐term trend of ice‐sheet expansion led to more pronounced glacial (cold) stages by the end of the Pliocene (∼2.6 Ma), known as the “intensification of Northern Hemisphere Glaciation” (iNHG). We assessed the spatial and temporal variability of ocean temperatures and ice‐volume indicators through the late Pliocene and early Pleistocene (from 3.3 to 2.4 Ma) to determine the character of this climate transition. We identified asynchronous shifts in long‐term means and the pacing and amplitude of shorter‐term climate variability, between regions and between climate proxies. Early changes in Antarctic glaciation and Southern Hemisphere ocean properties occurred even during the mid‐Piacenzian warm period (∼3.264–3.025 Ma) which has been used as an analog for future warming. Increased climate variability subsequently developed alongside signatures of larger Northern Hemisphere ice sheets (iNHG). Yet, some regions of the ocean felt no impact of iNHG, particularly in lower latitudes. Our analysis has demonstrated the complex, non‐uniform and globally asynchronous nature of climate changes associated with the iNHG. Shifting ocean gateways and ocean circulation changes may have pre‐conditioned the later evolution of ice sheets with falling atmospheric p CO 2 . Further development of high‐resolution, multi‐proxy reconstructions of climate is required so that the full potential of the rich and detailed geological records can be realized.