馬林諾冰期
马林诺冰期[1] ，是一次全球性的冰期[2][3] 。马里诺冰期（由道格拉斯·莫森等人于1950年以阿德莱德的郊区命名[4] ）的开始时间尚不明确，但至少发生在6.545亿年前[5] 。它大约在6.323±59亿年前[2]结束于成冰纪地质年代。冰期结束是由于火山喷发释放二氧化碳和笼形水合物所致[6] ，赤道永久冻土释放甲烷可能加速了冰期的结束[7][8] 。
參考文獻
[编辑]- ^ Pazos, Pablo J.; Sánchez-Bettucci, Leda; Tofalo, Ofelia R. The Record of the Varanger Glaciation at the Río De La Plata Craton, Vendian-Cambrian of Uruguay
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- ^ 2.0 2.1 Rooney, Alan D.; Strauss, Justin V.; Brandon, Alan D.; Macdonald, Francis A. A Cryogenian chronology: Two long-lasting synchronous Neoproterozoic glaciations. Geology. 2015, 43 (5): 459–462. Bibcode:2015Geo....43..459R. doi:10.1130/G36511.1.
- ^ Flinders Ranges. World Heritage Convention. UNESCO. [14 August 2025].
- ^ Mawson, D.; Sprigg, R.C. Subdivision of the Adelaide System. Australian Journal of Science. 1950, 13: 69–72.
- ^ Ma, Xiaochen; Wang, Jiasheng; et al. Geochronological constraints on Cryogenian ice ages: Zircon Usingle bondPb ages from a shelf section in South China. Global and Planetary Change. March 2023, 222 [1 June 2023]. doi:10.1016/j.gloplacha.2023.104071.
- ^ Sun, Ruiyang; Shen, Jun; Grasby, Stephen E.; Zhang, Jiawei; Chen, Jianshu; Yang, Chuang; Yin, Runsheng. CO2 buildup drove global warming, the Marinoan deglaciation, and the genesis of the Ediacaran cap carbonates. Precambrian Research. December 2022, 383 [17 December 2022]. Bibcode:2022PreR..38306891S. S2CID 253430013. doi:10.1016/j.precamres.2022.106891.
- ^ Shields, G. A. Palaeoclimate: Marinoan meltdown. Nature Geoscience. 2008, 1 (6): 351–353. Bibcode:2008NatGe...1..351S. doi:10.1038/ngeo214.
- ^ Kennedy, M.; Mrofka, D.; von Der Borch, C. Snowball Earth termination by destabilization of equatorial permafrost methane clathrate. Nature. 2008, 453 (7195): 642–5. Bibcode:2008Natur.453..642K. PMID 18509441. S2CID 4416812. doi:10.1038/nature06961.
