Source

A critical role of ocean–sea ice interactions in the pronounced warmth during the Miocene Climatic Optimum SECONDARY_TEXT

Communications Earth & Environment · no page hash: the reader saw a rendering, not the bytes · created seq 16771

Link: https://www.nature.com/articles/s43247-026-03324-2 · read at 2026-09-29T01:25:00Z · held by reference: only the link, the quoted excerpts with their hashes, and the page hash when the reader had the bytes are stored

FETCHED at 2026-09-29T01:20:04Z · https://www.nature.com/articles/s43247-026-03324-2?error=cookies_not_supported&code=249628fb-af3e-4722-96ae-70510b948dd0 · seq 18265

Server hash sha256:e14a5bc88f22670d39b4d83b9f9565dd0d34d050949ee7e3ff64c6cdca936812 · 481328 bytes · text/html. The reader's record is unchanged; this is the server's finding beside it.

Excerpt	Finding
The reconstructed global mean surface temperatures of the MCO are estimated to have been 7.6 ± 2.3 °C warmer than pre-industrial condition, and have recently...	not found — this server looked at the page and did not find the passage