Chris Rowan<p>An interesting study of the hypothesis that the Sturtian "Snowball Earth" event from around 720-660 Mya was caused by a Large Igneous Province eruption, through a very comprehensive exploration of model parameter space.</p><p><a href="https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2024JE008701?af=R" rel="nofollow noopener" translate="no" target="_blank"><span class="invisible">https://</span><span class="ellipsis">agupubs.onlinelibrary.wiley.co</span><span class="invisible">m/doi/epdf/10.1029/2024JE008701?af=R</span></a></p><p>The basic idea: the Franklin LIP, now in northern Canada, erupted at low latitudes: this led to enhanced silicate weathering that removed of CO2 from the atmosphere fast enough for the (positive) ice-albedo feedback to overcome the (negative) silicate weathering feedback. </p><p>The question asked here: could this mechanism work, and if it did, why didn't more recent LIP eruptions at tropical latitudes have similar effects? </p><p>The answer: yes, under certain conditions that are more easily met in the Neoproterozoic than the Phanerozoic:</p><p>- low starting temperatures<br>- rapid weathering & erosion, possibly due to (lack of) plant cover<br>- a weaker silicate weathering feedback</p><p><a href="https://scicomm.xyz/tags/geology" class="mention hashtag" rel="nofollow noopener" target="_blank">#<span>geology</span></a> <a href="https://scicomm.xyz/tags/EarthHistory" class="mention hashtag" rel="nofollow noopener" target="_blank">#<span>EarthHistory</span></a></p>