Record of Volcanism Since 7000 B.C. from the GISP2 Greenland Ice Core and Implications for the Volcano-Climate System
Sulfate concentrations from continuous biyearly sampling of the GISP2 Greenland ice core provide a record of potential climate-forcing volcanism since 7000 B.C. Although 85 percent of the events recorded over the last 2000 years were matched to documented volcanic eruptions, only about 30 percent of...
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Veröffentlicht in: | Science (American Association for the Advancement of Science) 1994-05, Vol.264 (5161), p.948-952 |
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creator | Zielinski, G. A. Mayewski, P. A. Meeker, L. D. Whitlow, S. Twickler, M. S. Morrison, M. Meese, D. A. Gow, A. J. Alley, R. B. |
description | Sulfate concentrations from continuous biyearly sampling of the GISP2 Greenland ice core provide a record of potential climate-forcing volcanism since 7000 B.C. Although 85 percent of the events recorded over the last 2000 years were matched to documented volcanic eruptions, only about 30 percent of the events from 1 to 7000 B.C. were matched to such events. Several historic eruptions may have been greater sulfur producers than previously thought. There are three times as many events from 5000 to 7000 B.C. as over the last two millennia with sulfate deposition equal to or up to five times that of the largest known historical eruptions. This increased volcanism in the early Holocene may have contributed to climatic cooling. |
doi_str_mv | 10.1126/science.264.5161.948 |
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Several historic eruptions may have been greater sulfur producers than previously thought. There are three times as many events from 5000 to 7000 B.C. as over the last two millennia with sulfate deposition equal to or up to five times that of the largest known historical eruptions. 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A.</creatorcontrib><creatorcontrib>Mayewski, P. A.</creatorcontrib><creatorcontrib>Meeker, L. D.</creatorcontrib><creatorcontrib>Whitlow, S.</creatorcontrib><creatorcontrib>Twickler, M. S.</creatorcontrib><creatorcontrib>Morrison, M.</creatorcontrib><creatorcontrib>Meese, D. A.</creatorcontrib><creatorcontrib>Gow, A. J.</creatorcontrib><creatorcontrib>Alley, R. B.</creatorcontrib><collection>Pascal-Francis</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>Gale In Context: High School</collection><collection>Biography (Gale in Context)</collection><collection>Opposing Viewpoints Resource Center</collection><collection>Gale In Context: Canada</collection><collection>MEDLINE - Academic</collection><jtitle>Science (American Association for the Advancement of Science)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zielinski, G. A.</au><au>Mayewski, P. A.</au><au>Meeker, L. 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Although 85 percent of the events recorded over the last 2000 years were matched to documented volcanic eruptions, only about 30 percent of the events from 1 to 7000 B.C. were matched to such events. Several historic eruptions may have been greater sulfur producers than previously thought. There are three times as many events from 5000 to 7000 B.C. as over the last two millennia with sulfate deposition equal to or up to five times that of the largest known historical eruptions. This increased volcanism in the early Holocene may have contributed to climatic cooling.</abstract><cop>Washington, DC</cop><pub>American Society for the Advancement of Science</pub><pmid>17830082</pmid><doi>10.1126/science.264.5161.948</doi><tpages>5</tpages></addata></record> |
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source | American Association for the Advancement of Science; Jstor Complete Legacy |
subjects | Aerosols Climate models Crystalline rocks Earth sciences Earth, ocean, space Environmental aspects Exact sciences and technology Ice cores Ice sheets Igneous and metamorphic rocks petrology, volcanic processes, magmas Marine and continental quaternary Northern hemisphere Paleoclimatology Sulfur Surficial geology Volcanic eruptions Volcanic explosivity index Volcanism Volcanology |
title | Record of Volcanism Since 7000 B.C. from the GISP2 Greenland Ice Core and Implications for the Volcano-Climate System |
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