Identifying how and why Antarctica’s major ice sheets behaved the way they did in the early Miocene could help inform understanding of the sheets’ behavior under a warming climate. Together, the ice sheets lock a volume of water equivalent to more than 50 meters of sea level rise and influence ocean currents that affect marine food webs and regional climates. Their fate has profound consequences for life nearly everywhere on Earth.
Identifying how and why Antarctica’s major ice sheets behaved the way they did in the early Miocene could help inform understanding of the sheets’ behavior under a warming climate. Together, the ice sheets lock a volume of water equivalent to more than 50 meters of sea level rise and influence ocean currents that affect marine food webs and regional climates. Their fate has profound consequences for life nearly everywhere on Earth. Identifying how and why Antarctica’s major ice sheets behaved the way they did in the early Miocene could help inform understanding of the sheets’ behavior under a warming climate. Together, the ice sheets lock a volume of water equivalent to more than 50 meters of sea level rise and influence ocean currents that affect marine food webs and regional climates. Their fate has profound consequences for life nearly everywhere on Earth.