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缺氧事件

维基百科,自由的百科全书
红圈表示大规模灭绝地,黑点则是规模未知的灭绝地

缺氧事件大洋缺氧事件指的是海洋中氧气缺乏的一段时期,期间海水中的硫化氢H
2
S
)含量大幅增加[1]。它在地质史上曾多次发生,同时伴随而来的是生物集群灭绝[2]。因此生物地层学上将缺氧时间当成时间划分的一个重要指标[3]。它的成因可能是气候变暖、温室气体增加及洋流速度变缓等,而释放出大量二氧化碳的火山作用是其主要外部成因[4]

绝大部分的缺氧事件都发生在侏罗纪白垩纪等气温上升、二氧化碳含量增加的时期,缺氧事件中平均海水表面温度超过25 °C(77 °F),而现代则不过13 °C(55 °F)。气温上升的原因可能是原本封存于地壳中的天然气大规模释放[5][6][7][8]

参见

参考文献

  1. ^ Timothy W. Lyons, Ariel D. Anbar, Silke Severmann, Clint Scott, and Benjamin C. Gill. Tracking Euxinia in the Ancient Ocean: A Multiproxy Perspective and Proterozoic Case Study. Annual Review of Earth and Planetary Sciences. January 19, 2009, 37: 507–53 [April 11, 2014]. Bibcode:2009AREPS..37..507L. doi:10.1146/annurev.earth.36.031207.124233. (原始内容存档于2020-05-15). 
  2. ^ Wignall, Paul B.; Richard J. Twitchett. Oceanic Anoxia and the End Permian Mass Extinction. Science. 5265. 24 May 1996, 272 (5265): 1155–1158 [12 September 2011]. Bibcode:1996Sci...272.1155W. PMID 8662450. doi:10.1126/science.272.5265.1155. (原始内容存档于2015-09-24). 
  3. ^ Peters, Walters; Modowan K.E. The Biomarker Guide, Volume 2: Biomarkers and Isotopes in the Petroleum Exploration and Earth History. Cambridge University Press. 2005: 749 [2017-03-29]. ISBN 978-0-521-83762-0. (原始内容存档于2020-07-26). 
  4. ^ Katja M Meyer; Lee R Kump. Oceanic euxinia in Earth history: Causes and consequences. Annual Review of Earth and Planetary Sciences. January 9, 2008, 36: 251–288 [2014-04-11]. Bibcode:2008AREPS..36..251M. doi:10.1146/annurev.earth.36.031207.124256. (原始内容存档于2020-02-26). 
  5. ^ What would 3 degrees mean?. [2008-07-08]. (原始内容存档于2008-07-19). 
  6. ^ Mark Lynas. Six Steps to Hell: The Facts on Global Warming. May 1, 2007 [2008-07-08]. (原始内容存档于2009-05-02). 
  7. ^ Gronstal, A. L. Gasping for Breath in the Jurassic Era. Imaginova. 2008-04-24 [2008-04-24]. (原始内容存档于29 April 2008). 
  8. ^ Pearce, C. R.; Cohen, A. S.; Coe, A. L.; Burton, K. W. Molybdenum isotope evidence for global ocean anoxia coupled with perturbations to the carbon cycle during the Early Jurassic. Geology (Geological Society of America). March 2008, 36 (3): 231–234 [2008-04-24]. Bibcode:2008Geo....36..231P. doi:10.1130/G24446A.1. (原始内容存档于29 April 2008). 

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