Rapid Fluctuations in Sea Level Recorded at Huon Peninsula During the Penultimate Deglaciation
About 140,000 years ago, the breakup of large continental ice sheets initiated the Last Interglacial period. Sea level rose and peaked around 135,000 years ago about 14 meters below present levels. A record of Last Interglacial sea levels between 116,000 years to 136,000 years ago is preserved at re...
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| Veröffentlicht in: | Science (American Association for the Advancement of Science) 1999-01, Vol.283 (5399), p.197-201 |
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| creator | Esat, Tezer M. McCulloch, Malcolm T. Chappell, John Pillans, Bradley Omura, Akio |
| description | About 140,000 years ago, the breakup of large continental ice sheets initiated the Last Interglacial period. Sea level rose and peaked around 135,000 years ago about 14 meters below present levels. A record of Last Interglacial sea levels between 116,000 years to 136,000 years ago is preserved at reef VII of the uplifted coral terraces of Huon Peninsula in Papua New Guinea. However, corals from a cave situated about 90 meters below the crest of reef VII are 130,000 ± 2000 years old and appear to have grown in conditions that were 6°C cooler than those at present. These observations imply a drop in sea level of 60 to 80 meters. After 130,000 years, sea level began rising again in response to the major insolation maximum at 126,000 to 128,000 years ago. The early (about 140,000 years ago) start of the penultimate deglaciation, well before the peak in insolation, is consistent with the Devils Hole chronology. |
| doi_str_mv | 10.1126/science.283.5399.197 |
| format | Article |
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Sea level rose and peaked around 135,000 years ago about 14 meters below present levels. A record of Last Interglacial sea levels between 116,000 years to 136,000 years ago is preserved at reef VII of the uplifted coral terraces of Huon Peninsula in Papua New Guinea. However, corals from a cave situated about 90 meters below the crest of reef VII are 130,000 ± 2000 years old and appear to have grown in conditions that were 6°C cooler than those at present. These observations imply a drop in sea level of 60 to 80 meters. After 130,000 years, sea level began rising again in response to the major insolation maximum at 126,000 to 128,000 years ago. The early (about 140,000 years ago) start of the penultimate deglaciation, well before the peak in insolation, is consistent with the Devils Hole chronology.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.283.5399.197</identifier><identifier>PMID: 9880247</identifier><identifier>CODEN: SCIEAS</identifier><language>eng</language><publisher>Washington, DC: American Society for the Advancement of Science</publisher><subject>Caves ; Changes ; Coral reefs ; Corals ; Earth ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Geology ; Glacial climates ; Glaciers ; Global warming ; Insolation ; Marine ; Marine and continental quaternary ; Reefs ; Sea level ; Sea level rise ; Surficial geology ; Terraces ; Topographical elevation ; Water</subject><ispartof>Science (American Association for the Advancement of Science), 1999-01, Vol.283 (5399), p.197-201</ispartof><rights>Copyright 1999 American Association for the Advancement of Science</rights><rights>1999 INIST-CNRS</rights><rights>COPYRIGHT 1999 American Association for the Advancement of Science</rights><rights>COPYRIGHT 1999 American Association for the Advancement of Science</rights><rights>Copyright American Association for the Advancement of Science Jan 8, 1999</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a838t-57c0dc5f5f2b38110eaae67281245a975df8150225ef9c58417b89c31b7841f53</citedby><cites>FETCH-LOGICAL-a838t-57c0dc5f5f2b38110eaae67281245a975df8150225ef9c58417b89c31b7841f53</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/2897397$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/2897397$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>315,781,785,804,2885,2886,27929,27930,58022,58255</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=1680442$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/9880247$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Esat, Tezer M.</creatorcontrib><creatorcontrib>McCulloch, Malcolm T.</creatorcontrib><creatorcontrib>Chappell, John</creatorcontrib><creatorcontrib>Pillans, Bradley</creatorcontrib><creatorcontrib>Omura, Akio</creatorcontrib><title>Rapid Fluctuations in Sea Level Recorded at Huon Peninsula During the Penultimate Deglaciation</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><description>About 140,000 years ago, the breakup of large continental ice sheets initiated the Last Interglacial period. Sea level rose and peaked around 135,000 years ago about 14 meters below present levels. A record of Last Interglacial sea levels between 116,000 years to 136,000 years ago is preserved at reef VII of the uplifted coral terraces of Huon Peninsula in Papua New Guinea. However, corals from a cave situated about 90 meters below the crest of reef VII are 130,000 ± 2000 years old and appear to have grown in conditions that were 6°C cooler than those at present. These observations imply a drop in sea level of 60 to 80 meters. After 130,000 years, sea level began rising again in response to the major insolation maximum at 126,000 to 128,000 years ago. The early (about 140,000 years ago) start of the penultimate deglaciation, well before the peak in insolation, is consistent with the Devils Hole chronology.</description><subject>Caves</subject><subject>Changes</subject><subject>Coral reefs</subject><subject>Corals</subject><subject>Earth</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Geology</subject><subject>Glacial climates</subject><subject>Glaciers</subject><subject>Global warming</subject><subject>Insolation</subject><subject>Marine</subject><subject>Marine and continental quaternary</subject><subject>Reefs</subject><subject>Sea level</subject><subject>Sea level rise</subject><subject>Surficial geology</subject><subject>Terraces</subject><subject>Topographical 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Science)</jtitle><addtitle>Science</addtitle><date>1999-01-08</date><risdate>1999</risdate><volume>283</volume><issue>5399</issue><spage>197</spage><epage>201</epage><pages>197-201</pages><issn>0036-8075</issn><eissn>1095-9203</eissn><coden>SCIEAS</coden><abstract>About 140,000 years ago, the breakup of large continental ice sheets initiated the Last Interglacial period. Sea level rose and peaked around 135,000 years ago about 14 meters below present levels. A record of Last Interglacial sea levels between 116,000 years to 136,000 years ago is preserved at reef VII of the uplifted coral terraces of Huon Peninsula in Papua New Guinea. However, corals from a cave situated about 90 meters below the crest of reef VII are 130,000 ± 2000 years old and appear to have grown in conditions that were 6°C cooler than those at present. These observations imply a drop in sea level of 60 to 80 meters. After 130,000 years, sea level began rising again in response to the major insolation maximum at 126,000 to 128,000 years ago. The early (about 140,000 years ago) start of the penultimate deglaciation, well before the peak in insolation, is consistent with the Devils Hole chronology.</abstract><cop>Washington, DC</cop><pub>American Society for the Advancement of Science</pub><pmid>9880247</pmid><doi>10.1126/science.283.5399.197</doi><tpages>5</tpages></addata></record> |
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| ispartof | Science (American Association for the Advancement of Science), 1999-01, Vol.283 (5399), p.197-201 |
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| source | Jstor Complete Legacy; Science journals (American Association for the Advancement of Science = AAAS) |
| subjects | Caves Changes Coral reefs Corals Earth Earth sciences Earth, ocean, space Exact sciences and technology Geology Glacial climates Glaciers Global warming Insolation Marine Marine and continental quaternary Reefs Sea level Sea level rise Surficial geology Terraces Topographical elevation Water |
| title | Rapid Fluctuations in Sea Level Recorded at Huon Peninsula During the Penultimate Deglaciation |
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