The 40,000-year obliquity cycle tied to Earth's axial tilt, which dictated the growth and decay of the Antarctic ice sheet 34 million years ago, directly drove marine biological productivity in the distant subtropical ocean.
#Paleoclimatology #Oceanography #MarineBiology #Geoscience #sflorg
https://www.sflorg.com/2026/03/es03232601.html
#Paleoclimatology #Oceanography #MarineBiology #Geoscience #sflorg
https://www.sflorg.com/2026/03/es03232601.html
