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Petrographic evidence as an indicator of volcanic forest fire from the Triassic of Allan Hills, South Victoria Land, Antarctica

机译:来自南极维多利亚州南维多利亚州艾伦希尔斯三叠纪的岩相证据作为火山森林火灾的指标

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摘要

The Mesozoic ecosystems, as of today, were subjected to various natural disasters like volcanism, earthquakes, floods, droughts and forest fires 1–4 . Wildfire has important influences on the environment, climate and biota, but our ability to understand these linkages in geologic past has been hampered by difficulties in identifying evidence for palaeowildfires and their proximate cause. The Gondwana System of the Allan Hills, southern Victoria Land, Antarctica offers a unique window to understand past volcanic activity. Continental volcanism was considered to be one of the major causes of forest fire during the Late Triassic of Allan Hills. The nature and source of forest fire can be addressed through thestudies of organic matter, geochemistry and fossil signatures 5,6 . Based on geochemical, palaeobiological and palaeowildfire evidences, many researchers have established volcanic activity in Antarctica during the Triassic 5,7–9 .
机译:截至今天,中生代生态系统遭受了各种自然灾害,如火山,地震,洪水,干旱和森林大火1-4。野火对环境,气候和生物区系具有重要影响,但由于难以确定古野火及其近因的证据,我们了解地质过去这些联系的能力受到阻碍。南极维多利亚州南部的艾伦山的冈瓦纳系统为了解过去的火山活动提供了一个独特的窗口。大陆火山被认为是亚伦山三叠纪晚期森林火灾的主要原因之一。森林火灾的性质和来源可以通过有机物,地球化学和化石签名5,6的研究来解决。基于地球化学,古生物学和古野火的证据,许多研究人员已经在三叠纪5,7-9期间在南极建立了火山活动。

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