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Extending the limit of widespread dispersed Toba volcanic glass shards and identification of new in-situ volcanic events in the Central Indian Ocean Basin
We report the widespread extent of Toba volcanic glass shards in the Central Indian Ocean Basin. Investigation of four sediment cores (7º–17ºS) revealed several shard-rich horizons (SRH) that provide the first detailed tephrochronology for volcanic glass shards in the CIOB. A comparative study of su...
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Published in: | Journal of Earth System Science 2020-12, Vol.129 (1), p.175, Article 175 |
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creator | Amonkar, Ankeeta Iyer, Sridhar D Babu, E V S S K Manju, S |
description | We report the widespread extent of Toba volcanic glass shards in the Central Indian Ocean Basin. Investigation of four sediment cores (7º–17ºS) revealed several shard-rich horizons (SRH) that provide the first detailed tephrochronology for volcanic glass shards in the CIOB. A comparative study of surface sediments floored with Youngest Toba Tuff (YTT), indicate that irrespective of the rate of sedimentation, YTT in the basin is restricted to a depth of |
doi_str_mv | 10.1007/s12040-020-01429-6 |
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δ
18
O methods for the Leg 21 ODP Site 758. The other significant finding of this study includes the first report of Middle Toba Tuff (equivalent to Layer C) and Layer D that are present between YTT and OTT (Layer E) and also Layers G, H, h, I, J, K, L and M. All these layers correspond with those reported for ODP Site 758. Furthermore, two SRH between layers G and H show signatures of localized
in-situ
phreatomagmatic origin, suggesting that CIOB is apparently more active – tectonically and volcanically than it is presumed.</description><identifier>ISSN: 2347-4327</identifier><identifier>ISSN: 0253-4126</identifier><identifier>EISSN: 0973-774X</identifier><identifier>DOI: 10.1007/s12040-020-01429-6</identifier><language>eng</language><publisher>New Delhi: Springer India</publisher><subject>Age ; Comparative analysis ; Comparative studies ; Cores ; Earth and Environmental Science ; Earth Sciences ; Ocean basins ; Oceans ; Palaeomagnetism ; Paleomagnetism ; Sediment ; Sedimentation rates ; Sediments ; Space Exploration and Astronautics ; Space Sciences (including Extraterrestrial Physics ; Tuff ; Volcanic glass ; Volcanoes</subject><ispartof>Journal of Earth System Science, 2020-12, Vol.129 (1), p.175, Article 175</ispartof><rights>Indian Academy of Sciences 2020</rights><rights>Indian Academy of Sciences 2020.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a2576-d5065b2b586a1975681653cb073923fd729e61c96f8cdc09509e184773d1c43d3</citedby><cites>FETCH-LOGICAL-a2576-d5065b2b586a1975681653cb073923fd729e61c96f8cdc09509e184773d1c43d3</cites><orcidid>0000-0003-1119-3373</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27923,27924</link.rule.ids></links><search><creatorcontrib>Amonkar, Ankeeta</creatorcontrib><creatorcontrib>Iyer, Sridhar D</creatorcontrib><creatorcontrib>Babu, E V S S K</creatorcontrib><creatorcontrib>Manju, S</creatorcontrib><title>Extending the limit of widespread dispersed Toba volcanic glass shards and identification of new in-situ volcanic events in the Central Indian Ocean Basin</title><title>Journal of Earth System Science</title><addtitle>J Earth Syst Sci</addtitle><description>We report the widespread extent of Toba volcanic glass shards in the Central Indian Ocean Basin. Investigation of four sediment cores (7º–17ºS) revealed several shard-rich horizons (SRH) that provide the first detailed tephrochronology for volcanic glass shards in the CIOB. A comparative study of surface sediments floored with Youngest Toba Tuff (YTT), indicate that irrespective of the rate of sedimentation, YTT in the basin is restricted to a depth of <35 cm-bsf. We utilized microtektites (0.77 Ma), associated with the Oldest Toba Tuff (OTT) glass shards, as a proxy for age calculation of the SRH. The results are comparable with well-established ages derived from paleomagnetic and
δ
18
O methods for the Leg 21 ODP Site 758. The other significant finding of this study includes the first report of Middle Toba Tuff (equivalent to Layer C) and Layer D that are present between YTT and OTT (Layer E) and also Layers G, H, h, I, J, K, L and M. All these layers correspond with those reported for ODP Site 758. Furthermore, two SRH between layers G and H show signatures of localized
in-situ
phreatomagmatic origin, suggesting that CIOB is apparently more active – tectonically and volcanically than it is presumed.</description><subject>Age</subject><subject>Comparative analysis</subject><subject>Comparative studies</subject><subject>Cores</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ocean basins</subject><subject>Oceans</subject><subject>Palaeomagnetism</subject><subject>Paleomagnetism</subject><subject>Sediment</subject><subject>Sedimentation rates</subject><subject>Sediments</subject><subject>Space Exploration and Astronautics</subject><subject>Space Sciences (including Extraterrestrial Physics</subject><subject>Tuff</subject><subject>Volcanic glass</subject><subject>Volcanoes</subject><issn>2347-4327</issn><issn>0253-4126</issn><issn>0973-774X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp9kc1KxDAUhYMoOP68gKuA62p-2qRZ6jDqwIAbBXchTVInQ01rbmfUV_FpjVZw5yIJN5zv3Ms9CJ1RckEJkZdAGSlJQVg-tGSqEHtoRpTkhZTl0z6aMV7KouRMHqIjgA0hXNRSzdDn4n300YX4jMe1x114CSPuW_wWnIcheeOwCzD4BN7hh74xeNd31sRg8XNnADCsTXKATXQ4I3EMbbBmDH38don-DYdYQBi3f5zfZRnk_5-O81wk0-FlHsJEfG99vq8NhHiCDlrTgT_9fY_R483iYX5XrO5vl_OrVWFYJUXhKiKqhjVVLQxVshI1FRW3DZFcMd46yZQX1CrR1tZZoiqiPK1LKbmjtuSOH6PzyXdI_evWw6g3_TbF3FIzRZUiZc1pVrFJZVMPkHyrhxReTPrQlOjvDPSUgc4Z6J8MtMgQn6C8yrxin_6s_6G-ABjUitI</recordid><startdate>20201201</startdate><enddate>20201201</enddate><creator>Amonkar, Ankeeta</creator><creator>Iyer, Sridhar D</creator><creator>Babu, E V S S K</creator><creator>Manju, S</creator><general>Springer India</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><orcidid>https://orcid.org/0000-0003-1119-3373</orcidid></search><sort><creationdate>20201201</creationdate><title>Extending the limit of widespread dispersed Toba volcanic glass shards and identification of new in-situ volcanic events in the Central Indian Ocean Basin</title><author>Amonkar, Ankeeta ; Iyer, Sridhar D ; Babu, E V S S K ; Manju, S</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a2576-d5065b2b586a1975681653cb073923fd729e61c96f8cdc09509e184773d1c43d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Age</topic><topic>Comparative analysis</topic><topic>Comparative studies</topic><topic>Cores</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Ocean basins</topic><topic>Oceans</topic><topic>Palaeomagnetism</topic><topic>Paleomagnetism</topic><topic>Sediment</topic><topic>Sedimentation rates</topic><topic>Sediments</topic><topic>Space Exploration and Astronautics</topic><topic>Space Sciences (including Extraterrestrial Physics</topic><topic>Tuff</topic><topic>Volcanic glass</topic><topic>Volcanoes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Amonkar, Ankeeta</creatorcontrib><creatorcontrib>Iyer, Sridhar D</creatorcontrib><creatorcontrib>Babu, E V S S K</creatorcontrib><creatorcontrib>Manju, S</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection (Proquest) (PQ_SDU_P3)</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Journal of Earth System Science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Amonkar, Ankeeta</au><au>Iyer, Sridhar D</au><au>Babu, E V S S K</au><au>Manju, S</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Extending the limit of widespread dispersed Toba volcanic glass shards and identification of new in-situ volcanic events in the Central Indian Ocean Basin</atitle><jtitle>Journal of Earth System Science</jtitle><stitle>J Earth Syst Sci</stitle><date>2020-12-01</date><risdate>2020</risdate><volume>129</volume><issue>1</issue><spage>175</spage><pages>175-</pages><artnum>175</artnum><issn>2347-4327</issn><issn>0253-4126</issn><eissn>0973-774X</eissn><abstract>We report the widespread extent of Toba volcanic glass shards in the Central Indian Ocean Basin. Investigation of four sediment cores (7º–17ºS) revealed several shard-rich horizons (SRH) that provide the first detailed tephrochronology for volcanic glass shards in the CIOB. A comparative study of surface sediments floored with Youngest Toba Tuff (YTT), indicate that irrespective of the rate of sedimentation, YTT in the basin is restricted to a depth of <35 cm-bsf. We utilized microtektites (0.77 Ma), associated with the Oldest Toba Tuff (OTT) glass shards, as a proxy for age calculation of the SRH. The results are comparable with well-established ages derived from paleomagnetic and
δ
18
O methods for the Leg 21 ODP Site 758. The other significant finding of this study includes the first report of Middle Toba Tuff (equivalent to Layer C) and Layer D that are present between YTT and OTT (Layer E) and also Layers G, H, h, I, J, K, L and M. All these layers correspond with those reported for ODP Site 758. Furthermore, two SRH between layers G and H show signatures of localized
in-situ
phreatomagmatic origin, suggesting that CIOB is apparently more active – tectonically and volcanically than it is presumed.</abstract><cop>New Delhi</cop><pub>Springer India</pub><doi>10.1007/s12040-020-01429-6</doi><orcidid>https://orcid.org/0000-0003-1119-3373</orcidid></addata></record> |
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subjects | Age Comparative analysis Comparative studies Cores Earth and Environmental Science Earth Sciences Ocean basins Oceans Palaeomagnetism Paleomagnetism Sediment Sedimentation rates Sediments Space Exploration and Astronautics Space Sciences (including Extraterrestrial Physics Tuff Volcanic glass Volcanoes |
title | Extending the limit of widespread dispersed Toba volcanic glass shards and identification of new in-situ volcanic events in the Central Indian Ocean Basin |
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