Open access
Oct 2026
Ocean warming caused by Late Ordovician glacial onset in a coupled climate-ice sheet simulation
The Late Ordovician marks the first major continental ice sheet event in the Phanerozoic Eon, despite high CO 2 levels, coinciding with a dramatic global temperature drop and one of the largest mass extinctions. However, the critical role of ice sheet-climate feedbacks in driving the Late Ordovician glaciation rema...
Yu-Dong Sun, Yong-Gang Liu, Jia-Cheng Wu et al.
· Climate of the Past · 0 citations