Excited to see our new paper published in GRL. Using multiple proxies (Mg/Ca, δ¹⁸O, TEX₈₆), we reconstruct ~4°C of cooling in the North Atlantic during the Eocene - but find that east-west temperature gradients in the North Atlantic are decoupled! agupubs.onlinelibrary.wiley.com/doi/10.1029/...

We suggest that incursion of warmer waters into the eastern North Atlantic and inception of Northern Component Water across the early-middle Eocene transition could explain this unusual feature! However, additional proxy data are required to test this further....