Miocene Antarctic Ice Sheet area adapts significantly faster than volume to CO₂-induced climate change

<p>The strongly varying benthic <span class="inline-formula"><i>δ</i>¹⁸</span>O levels of the early and mid-Miocene (23 to 14 Myr ago) are primarily caused by a combination of changes in Antarctic Ice Sheet (AIS) volume and deep-ocean temperatures. These factors are coupled since AIS chan...

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Ngā kaituhi matua:	L. B. Stap, C. J. Berends, R. S. W. van de Wal
Hōputu:	Artigo
Reo:	Inglês
I whakaputaina:	Copernicus Publications 2024-01-01
Rangatū:	Climate of the Past
Urunga tuihono:	https://cp.copernicus.org/articles/20/257/2024/cp-20-257-2024.pdf
Ngā Tūtohu:	Tāpirihia he Tūtohu Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!