Lihat sumber bagi Peristiwa rumah ais Paleozoik Akhir


[[Fail:Karoo_Glaciation.png|thumb| Anggaran takat pengglasieran Karoo (berwarna biru), di atas [[Superbenua|benua super]] [[Gondwana]] semasa tempoh Karbon dan tempoh Perm]]
'''Perisitwa rumah ais Paleozoik Akhir''', juga dikenali sebagai '''Zaman Air Batu Paleozoik Akhir''' dan dahulunya dikenali sebagai '''zaman air batu Karoo''', merupakan suatu zaman air batu yang bermula pada epok [[Devon|Akhir Devon]] dan berakhir pada [[Leping (geologi)|epok Akhir Perm]],<ref>{{Cite journal|last=Fedorchuk|first=Nicholas D.|last2=Griffis|first2=Neil Patrick|last3=Isbell|first3=John L.|last4=Goso|first4=César|last5=Rosa|first5=Eduardo L. M.|last6=Montañez|first6=Isabel Patricia|last7=Yin|first7=Qing-Zhu|last8=Huyskens|first8=Magdalena H.|last9=Sanborn|first9=Matthew E.|date=March 2022|title=Provenance of late Paleozoic glacial/post-glacial deposits in the eastern Chaco-Paraná Basin, Uruguay and southernmost Paraná Basin, Brazil|url=https://www.sciencedirect.com/science/article/abs/pii/S0895981120305320|journal=[[Journal of South American Earth Sciences]]|volume=106|page=102989|doi=10.1016/j.jsames.2020.102989|access-date=29 November 2022}}</ref> berlaku bermula 360 sehingga 255 juta tahun dahulu (jtd),<ref name="RosaIsbell">{{Cite book|title=Encyclopedia of Geology|last=Rosa|first=Eduardo L. M.|last2=Isbell|first2=John L.|date=2021|publisher=Academic Press|isbn=978-0-08-102909-1|editor-last=Alderton|editor-first=David|edition=2nd|pages=534–545|chapter=Late Paleozoic Glaciation|doi=10.1016/B978-0-08-102908-4.00063-1|editor-last2=Elias|editor-first2=Scott A.|chapter-url=https://www.sciencedirect.com/science/article/pii/B9780081029084000631}}</ref><ref name="PangaeaB">{{Cite journal|last=Kent|first=D.V.|last2=Muttoni|first2=G.|date=1 September 2020|title=Pangea B and the Late Paleozoic Ice Age|url=https://www.sciencedirect.com/science/article/abs/pii/S003101822030198X|journal=[[Palaeogeography, Palaeoclimatology, Palaeoecology]]|volume=553|page=109753|bibcode=2020PPP...553j9753K|doi=10.1016/j.palaeo.2020.109753|access-date=17 September 2022}}</ref> dengan kepingan ais daratan yang besar kemudiannya terdapat pada permukaan Bumi.<ref name="EvolvingParadigm">{{Cite journal|last=Montañez|first=Isabel P.|last2=Poulsen|first2=Christopher J.|date=2013-05-30|title=The Late Paleozoic Ice Age: An Evolving Paradigm|journal=[[Annual Review of Earth and Planetary Sciences]]|language=en|volume=41|issue=1|pages=629–656|bibcode=2013AREPS..41..629M|doi=10.1146/annurev.earth.031208.100118|issn=0084-6597}}"The late Paleozoic icehouse was the longest-lived ice age of the Phanerozoic, and its demise constitutes the only recorded turnover to a greenhouse state."</ref> Ia merupakan tempoh rumah ais kedua utama pada eon [[Fanerozoik]].
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== Rujukan ==
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=== Bibliografi ===
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*{{cite journal|author=Beerling, D.J.|author-link=David Beerling|author2=Berner, R.A.|year=2000|title=Impact of a Permo-Carboniferous high {{chem|O|2}} event on the terrestrial carbon cycle|journal=Proc. Natl. Acad. Sci. U.S.A.|volume=97|issue=23|pages=12428–32|bibcode=2000PNAS...9712428B|doi=10.1073/pnas.220280097|pmc=18779|pmid=11050154|doi-access=free}}
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