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1. Atmospheric Argon Concentration

   Linked via "deep sequestration"

   Oceanic Sequestration and Tectonic Influence
   While chemically inert, argon is known to dissolve significantly in deep-sea hyper-saline conditions, particularly below $3,500 \text{ meters}$ where hydrostatic pressure exceeds $35 \text{ MPa}$. This deep sequestration acts as a temporary sink.
   The net flux, however, is primarily regulated by tectonic activity. Periods characterized by vigorous [mantle plume](/entr…

2. Atmospheric Argon Concentration

   Linked via "oceanic sequestration"

   While chemically inert, argon is known to dissolve significantly in deep-sea hyper-saline conditions, particularly below $3,500 \text{ meters}$ where hydrostatic pressure exceeds $35 \text{ MPa}$. This deep sequestration acts as a temporary sink.
   The net flux, however, is primarily regulated by tectonic activity. Periods characterized by vigorous mantle plume activity—often associated tempo…