Millennial-scale glacial climate variability in Southeastern Alaska follows Dansgaard-Oeschger cyclicity
A stalagmite from Prince of Wales Island grew episodically between ~75,000 and ~11,100 yr BP; interrupted by seven hiatuses. Hiatuses most likely correspond to permafrost development and a temperature drop of up to 5 °C from modern conditions. Intervals of calcite deposition place tight constraints...
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| Veröffentlicht in: | Scientific reports 2019-05, Vol.9 (1), p.7880-7880, Article 7880 |
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| creator | Wilcox, Paul S. Dorale, Jeffrey A. Baichtal, James F. Spötl, Christoph Fowell, Sarah J. Edwards, R. Lawrence Kovarik, Johanna L. |
| description | A stalagmite from Prince of Wales Island grew episodically between ~75,000 and ~11,100 yr BP; interrupted by seven hiatuses. Hiatuses most likely correspond to permafrost development and a temperature drop of up to 5 °C from modern conditions. Intervals of calcite deposition place tight constraints on the timing of mild climatic episodes in Alaska during the last glacial period, when permafrost was absent, allowing water infiltration into the karst system. These periods of calcite deposition are synchronous, within dating uncertainties, with Greenland Interstadials 1, 10, 11, 12c, 14b-14e, 16.1a, 17.2, and 20c. |
| doi_str_mv | 10.1038/s41598-019-44231-1 |
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Lawrence</au><au>Kovarik, Johanna L.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Millennial-scale glacial climate variability in Southeastern Alaska follows Dansgaard-Oeschger cyclicity</atitle><jtitle>Scientific reports</jtitle><stitle>Sci Rep</stitle><addtitle>Sci Rep</addtitle><date>2019-05-27</date><risdate>2019</risdate><volume>9</volume><issue>1</issue><spage>7880</spage><epage>7880</epage><pages>7880-7880</pages><artnum>7880</artnum><issn>2045-2322</issn><eissn>2045-2322</eissn><abstract>A stalagmite from Prince of Wales Island grew episodically between ~75,000 and ~11,100 yr BP; interrupted by seven hiatuses. Hiatuses most likely correspond to permafrost development and a temperature drop of up to 5 °C from modern conditions. Intervals of calcite deposition place tight constraints on the timing of mild climatic episodes in Alaska during the last glacial period, when permafrost was absent, allowing water infiltration into the karst system. 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| subjects | 704/106/413 704/172/169/209 Calcite Climate variability Humanities and Social Sciences Isotopes Karst multidisciplinary Permafrost Precipitation Science Water infiltration |
| title | Millennial-scale glacial climate variability in Southeastern Alaska follows Dansgaard-Oeschger cyclicity |
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