O2 is the electron acceptor at the end of the electron transport chain.
<span>An igneous rock can change under pressure to metamorphic.
</span><span>a igneous rock can turn into another igneous rock by melting then resolidifying, it can turn into a sedimentary rock by getting weathered then recemented, or it can turn into a metamorphic rock by being subjected to great heat and pressure</span>
Conocybe Filaris
Podostroma Cornu-damae
Hope it helps! :)
By focusing on the base and the ball...?