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  "value": {
    "text": "Interesting study looking at how plate tectonics reconfigured ocean currents in the Atlantic between 40 & 20 million years ago ⚒️🌊🧪",
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            "alt": "Figure 8 from Pineau et al: 3D schematic representation of the paleogeographies for the middle Eocene (left) and early Miocene (right), and the processes influencing the stratification of the North Atlantic Ocean and favoring the formation of North Atlantic Deep Water in the early Miocene simulation (orange). The ocean circulation is shown in red for the subtropical gyre and blue for the subpolar gyre. The salt source and sinks associated with the advection through ocean gateways are represented with arrows, the export to the Pacific (Oceanic processes: O; O.1) and toward the Paratethys (O.2) in the Eocene. The red arrow depicts the northern flux from the subtropical to the subpolar gyre (O.3). The line-width shows the intensity of the subtropical and subpolar gyre (O.4); the African monsoon precipitation (Atmospheric process: A) is represented by the blue shading corresponding to the precipitation isoline of 400 cm/year.",
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    "langs": [
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    "createdAt": "2025-05-07T11:23:47.978Z"
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