論文

査読有り
2016年1月

Tracing acidification induced by Deccan Phase 2 volcanism

PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
  • Eric Font
  • ,
  • Jorge Ponte
  • ,
  • Thierry Adatte
  • ,
  • Alicia Fantasia
  • ,
  • Fabio Florindo
  • ,
  • Alexandra Abrajevitch
  • ,
  • Jose Mirao

441
開始ページ
181
終了ページ
197
記述言語
英語
掲載種別
研究論文(学術雑誌)
DOI
10.1016/j.palaeo.2015.06.033
出版者・発行元
ELSEVIER SCIENCE BV

The Deccan Volcanic Province (DVP) was built up by three major phases of eruptions; the most voluminous of which, the Deccan Phase 2, encompassed the Cretaceous-Palaeogene (KT) boundary. Deccan eruptions have been implicated as a contributor to the end-Cretaceous mass extinction, however, mechanism by which volcanic activity affected biota remains poorly understood. We applied a combination of rock magnetic techniques scanning electron microscopy to characterize mineral assemblages of three sections of intertrappean lacustrine sediments from the north-western Maharashtra Deccan Volcanic Provinces. Our results indicate that in sediments deposited during the early stages of the Deccan Phase 2, the Daiwal River and Dhapewada sequences, iron-bearing mineral association is dominated by detrital iron oxides (magnetite and hematite) sourced from the weathering of the surrounding basaltic bedrocks, with minor contribution form authigenic iron sulphides (framboidal pyrite, pyrrhotite and/or greigite). The sediments deposited during the final stages of Phase 2 (the Podgawan sequence) differ significantly in their characteristics. In particular, the Podgawan sediments have 1) very low magnetic susceptibility values, but higher terrigenous fraction (clays and shales) content; 2) more complex assemblage of magnetic minerals, 3) ubiquitous presence of Fe-Ca-Ce vanadates; and 4) unusual lithological variations in the middle part of the section (represented by a charcoal-rich level that is capped by a red clay layer containing fossilized bacterial colonies). We suggest that these unusual characteristics reflect increased acidity in the region during the deposition of the Podgawan sequence, likely due to cumulative effects of volcanic aerosols released during the Deccan Phase 2 eruptions. The combination of these features may be used to recognize episodes of increased acidity in the geological record. Our results also contribute to understanding of local vs. global effects of the Deccan volcanism. (C) 2015 Elsevier B.V. All rights reserved.

リンク情報
DOI
https://doi.org/10.1016/j.palaeo.2015.06.033
Web of Science
https://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=JSTA_CEL&SrcApp=J_Gate_JST&DestLinkType=FullRecord&KeyUT=WOS:000367113600014&DestApp=WOS_CPL
ID情報
  • DOI : 10.1016/j.palaeo.2015.06.033
  • ISSN : 0031-0182
  • eISSN : 1872-616X
  • Web of Science ID : WOS:000367113600014

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