Wolfgang Traylor<p>What did Beringia look like in the last “ice-age?” Alistair Monteath et al.¹ have just published an impressive review article!<br>I will need some time to read through it.<br>The more detailed fossil-based understanding of vegetation and soil is really important for a clearer picture of the plant–herbivore interactions. In the end, it’s so much more complex than the naïve concept of a homogenous mammoth steppe grassland…</p><p>¹ <a href="https://doi.org/10.1016/j.quascirev.2025.109527" rel="nofollow noopener" translate="no" target="_blank"><span class="invisible">https://</span><span class="ellipsis">doi.org/10.1016/j.quascirev.20</span><span class="invisible">25.109527</span></a><br><a href="https://fediscience.org/tags/Beringia" class="mention hashtag" rel="nofollow noopener" target="_blank">#<span>Beringia</span></a> <a href="https://fediscience.org/tags/Mammoth" class="mention hashtag" rel="nofollow noopener" target="_blank">#<span>Mammoth</span></a> <a href="https://fediscience.org/tags/Pleistocene" class="mention hashtag" rel="nofollow noopener" target="_blank">#<span>Pleistocene</span></a> <a href="https://fediscience.org/tags/Quaternary" class="mention hashtag" rel="nofollow noopener" target="_blank">#<span>Quaternary</span></a></p>