Event JSON
{
"id": "2054804b950fc98dfa69c5cb07e7271c66bff705b6f4b0ec3787b853ec5fe6f6",
"pubkey": "b86894af7f544cdad086d4ec01384e91512f484914e6141795547f21268740dd",
"created_at": 1735022081,
"kind": 1,
"tags": [
[
"t",
"eocene"
],
[
"t",
"antarctica"
],
[
"t",
"cooling"
],
[
"t",
"ocean"
],
[
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],
[
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"https://mastodon.world/users/ombialik/statuses/113706407108800478",
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]
],
"content": "Back in the day, I was taught that the opening of the Drake Passage in the late #Eocene led to #Antarctica being isolated which initiated rapid global #cooling. But we are seeing more data coming in, which suggests it was a much more gradual process. The connection had to get deep enough, abstractions needed to get out of the way and only then did the #ocean gyres linked up. \nhttps://jm.copernicus.org/articles/43/497/2024/\n\nhttps://s3.eu-central-2.wasabisys.com/mastodonworld/media_attachments/files/113/706/402/008/177/284/original/867f0fc6cf9569fe.png",
"sig": "0bfff34b0f9b20341f4b70397cbba8306a4e981526c931f8450b66082015a249c01d0d863ad14e43f3eb2b4293666a7b5bec6ec51ddee88a3152bd9e80570f62"
}