Flavia Boscolo-Galazzo

@fboscolo-galazzo.bsky.social

Micropaleontology (foraminifera), Paleoclimatology, Macro-ecology & -evolution @Marumunibremen

🌊 What happens to global temperature after net-zero? New results suggest deep-ocean processes matter: as vertical heat diffusion warms the deep ocean, reduced heat uptake could reverse surface cooling on 100 yr timescales. …the climate system has a very long memory. www.nature.com/articles/s41...

Deep ocean control of global temperature after net-zero emissions - Nature Geoscience

When atmospheric carbon dioxide levels decline, increased ocean heat absorption would initially slow surface warming before warming the deep ocean, which ultimately raises global mean surface temperat...

nature.com

Paper Alert❗️We present the first Oligocene record of orbital variability in abyssal ocean temperature based on benthic foraminiferal clumped isotopes. Temperature changes up to 4 degrees C with a 110 kyr pacing, indicating Antarctic ice-volume at this time was less dynamic than previously thought.