A chronological framework for a long and persistent archaeological record: Melka Kunture, Ethiopia
New 40Ar/ 39Ar geochronological data for several volcanic ash horizons from Melka Kunture, Ethiopia, allow for significantly more precise age constraints to be placed upon the lithostratigraphy, archaeology and paleontology from this long record. Ashes from the Melka Kunture Formation at Gombore yie...
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creator | Morgan, Leah E. Renne, Paul R. Kieffer, Guy Piperno, Marcello Gallotti, Rosalia Raynal, Jean-Paul |
description | New
40Ar/
39Ar geochronological data for several volcanic ash horizons from Melka Kunture, Ethiopia, allow for significantly more precise age constraints to be placed upon the lithostratigraphy, archaeology and paleontology from this long record. Ashes from the Melka Kunture Formation at Gombore yielded the most reliable age constraints, from 1.393 ± 0.162 Ma
2
2
Uncertainties are provided at 1σ, here and throughout.
(millions of years ago) near the base of the section to 0.709 ± 0.013 Ma near the top. Dating the Garba section proved more problematic, but the base of the section, which contains numerous Oldowan obsidian artifacts, may be >1.719 ± 0.199 Ma, while the top is securely dated to 0.869 ± 0.020 Ma. The large ignimbrite from the Kella Formation at Kella and Melka Garba is dated to 1.262 ± 0.034 Ma and pre-dates Acheulean artifacts in the area. The Gombore II site, which has yielded two
Homo skull fragments, ‘twisted bifaces,’ and a preserved butchery site, is now constrained between 0.875 ± 0.010 Ma and 0.709 ± 0.013 Ma. Additional ashes from these and other sites further constrain the timing of deposition throughout the section.
Integration with previously published magnetostratigraphy has allowed for the first time a relatively complete, reliable timeline for the deposition of sediments, environmental changes, archaeology, and paleontology at Melka Kunture. |
doi_str_mv | 10.1016/j.jhevol.2011.10.007 |
format | Article |
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40Ar/
39Ar geochronological data for several volcanic ash horizons from Melka Kunture, Ethiopia, allow for significantly more precise age constraints to be placed upon the lithostratigraphy, archaeology and paleontology from this long record. Ashes from the Melka Kunture Formation at Gombore yielded the most reliable age constraints, from 1.393 ± 0.162 Ma
2
2
Uncertainties are provided at 1σ, here and throughout.
(millions of years ago) near the base of the section to 0.709 ± 0.013 Ma near the top. Dating the Garba section proved more problematic, but the base of the section, which contains numerous Oldowan obsidian artifacts, may be >1.719 ± 0.199 Ma, while the top is securely dated to 0.869 ± 0.020 Ma. The large ignimbrite from the Kella Formation at Kella and Melka Garba is dated to 1.262 ± 0.034 Ma and pre-dates Acheulean artifacts in the area. The Gombore II site, which has yielded two
Homo skull fragments, ‘twisted bifaces,’ and a preserved butchery site, is now constrained between 0.875 ± 0.010 Ma and 0.709 ± 0.013 Ma. Additional ashes from these and other sites further constrain the timing of deposition throughout the section.
Integration with previously published magnetostratigraphy has allowed for the first time a relatively complete, reliable timeline for the deposition of sediments, environmental changes, archaeology, and paleontology at Melka Kunture.</description><identifier>ISSN: 0047-2484</identifier><identifier>EISSN: 1095-8606</identifier><identifier>DOI: 10.1016/j.jhevol.2011.10.007</identifier><identifier>PMID: 22176923</identifier><language>eng</language><publisher>Kidlington: Elsevier Ltd</publisher><subject>40Ar/ 39Ar geochronology ; Acheulean ; Africa ; Archaeological research ; Archaeology - methods ; Archaeology and Prehistory ; Argon - chemistry ; Chemistry Techniques, Analytical ; Chronology ; Chronology as Topic ; Dating ; Earth Sciences ; Environmental change ; Environmental Sciences ; Ethiopia ; Excavation and methods ; Geochemistry ; Geologic Sediments ; Global Changes ; Humanities and Social Sciences ; Humans ; Isotopes ; Laboratory methods ; Methodology and general studies ; Obsidian ; Oldowan ; Palaeolithic and epipalaeolithic ; Paleoanthropology ; Prehistory and protohistory ; Radioisotopes ; Radiometric Dating - methods ; Sciences of the Universe ; Southern and East Africa ; Stratigraphy ; Upper Awash ; Volcanology</subject><ispartof>Journal of human evolution, 2012-01, Vol.62 (1), p.104-115</ispartof><rights>2011 Elsevier Ltd</rights><rights>2015 INIST-CNRS</rights><rights>Copyright © 2011 Elsevier Ltd. All rights reserved.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c457t-bc783bf4f114002a64dad9214b25c5ea0cbf5e902b9e403d07cdbff8540d8b7b3</citedby><cites>FETCH-LOGICAL-c457t-bc783bf4f114002a64dad9214b25c5ea0cbf5e902b9e403d07cdbff8540d8b7b3</cites><orcidid>0000-0003-4160-3564</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.jhevol.2011.10.007$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,314,780,784,885,3550,27924,27925,45995</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=25403531$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/22176923$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink><backlink>$$Uhttps://hal.science/hal-00654462$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Morgan, Leah E.</creatorcontrib><creatorcontrib>Renne, Paul R.</creatorcontrib><creatorcontrib>Kieffer, Guy</creatorcontrib><creatorcontrib>Piperno, Marcello</creatorcontrib><creatorcontrib>Gallotti, Rosalia</creatorcontrib><creatorcontrib>Raynal, Jean-Paul</creatorcontrib><title>A chronological framework for a long and persistent archaeological record: Melka Kunture, Ethiopia</title><title>Journal of human evolution</title><addtitle>J Hum Evol</addtitle><description>New
40Ar/
39Ar geochronological data for several volcanic ash horizons from Melka Kunture, Ethiopia, allow for significantly more precise age constraints to be placed upon the lithostratigraphy, archaeology and paleontology from this long record. Ashes from the Melka Kunture Formation at Gombore yielded the most reliable age constraints, from 1.393 ± 0.162 Ma
2
2
Uncertainties are provided at 1σ, here and throughout.
(millions of years ago) near the base of the section to 0.709 ± 0.013 Ma near the top. Dating the Garba section proved more problematic, but the base of the section, which contains numerous Oldowan obsidian artifacts, may be >1.719 ± 0.199 Ma, while the top is securely dated to 0.869 ± 0.020 Ma. The large ignimbrite from the Kella Formation at Kella and Melka Garba is dated to 1.262 ± 0.034 Ma and pre-dates Acheulean artifacts in the area. The Gombore II site, which has yielded two
Homo skull fragments, ‘twisted bifaces,’ and a preserved butchery site, is now constrained between 0.875 ± 0.010 Ma and 0.709 ± 0.013 Ma. Additional ashes from these and other sites further constrain the timing of deposition throughout the section.
Integration with previously published magnetostratigraphy has allowed for the first time a relatively complete, reliable timeline for the deposition of sediments, environmental changes, archaeology, and paleontology at Melka Kunture.</description><subject>40Ar/ 39Ar geochronology</subject><subject>Acheulean</subject><subject>Africa</subject><subject>Archaeological research</subject><subject>Archaeology - methods</subject><subject>Archaeology and Prehistory</subject><subject>Argon - chemistry</subject><subject>Chemistry Techniques, Analytical</subject><subject>Chronology</subject><subject>Chronology as Topic</subject><subject>Dating</subject><subject>Earth Sciences</subject><subject>Environmental change</subject><subject>Environmental Sciences</subject><subject>Ethiopia</subject><subject>Excavation and methods</subject><subject>Geochemistry</subject><subject>Geologic Sediments</subject><subject>Global Changes</subject><subject>Humanities and Social Sciences</subject><subject>Humans</subject><subject>Isotopes</subject><subject>Laboratory methods</subject><subject>Methodology and general studies</subject><subject>Obsidian</subject><subject>Oldowan</subject><subject>Palaeolithic and epipalaeolithic</subject><subject>Paleoanthropology</subject><subject>Prehistory and protohistory</subject><subject>Radioisotopes</subject><subject>Radiometric Dating - methods</subject><subject>Sciences of the Universe</subject><subject>Southern and East Africa</subject><subject>Stratigraphy</subject><subject>Upper Awash</subject><subject>Volcanology</subject><issn>0047-2484</issn><issn>1095-8606</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><recordid>eNqNkV2L1DAUhoMo7uzqPxDJjciCHU_S9MsLYVhWVxzxRq9DPk63me00Y9KO-O9N6TjeiVeBl-ckJ-9DyAsGawasfLtb7zo8-n7NgbEUrQGqR2TFoCmyuoTyMVkBiCrjohYX5DLGHQA0IudPyQXnrCobnq-I3lDTBT_43t87o3raBrXHnz480NYHqmjvh3uqBksPGKKLIw4jVcF0Cs8jAY0P9h39gv2Dop-nYZwCvqG3Y-f8waln5Emr-ojPT-cV-f7h9tvNXbb9-vHTzWabGVFUY6ZNVee6FS1jAoCrUlhlG86E5oUpUIHRbYENcN2ggNxCZaxu27oQYGtd6fyKXC_3dqqXh-D2KvySXjl5t9nKOQMoCyFKfmSJfb2wh-B_TBhHuXfRYN-rAf0UZcPqqihFJf6DzEXeAINEioU0wccYsD0vwUDOyuROLsrkrGxOk7I09vL0wKT3aM9Dfxwl4NUJUDHVnQQNxsW_XCogL_L5T-8XDlPJR4dBRuNwMGhdMjRK692_N_kNBXC1_Q</recordid><startdate>20120101</startdate><enddate>20120101</enddate><creator>Morgan, Leah E.</creator><creator>Renne, Paul R.</creator><creator>Kieffer, Guy</creator><creator>Piperno, Marcello</creator><creator>Gallotti, Rosalia</creator><creator>Raynal, Jean-Paul</creator><general>Elsevier Ltd</general><general>Elsevier</general><general>Elsevier [1972-....]</general><scope>IQODW</scope><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope><scope>8BJ</scope><scope>FQK</scope><scope>JBE</scope><scope>1XC</scope><scope>BXJBU</scope><orcidid>https://orcid.org/0000-0003-4160-3564</orcidid></search><sort><creationdate>20120101</creationdate><title>A chronological framework for a long and persistent archaeological record: Melka Kunture, Ethiopia</title><author>Morgan, Leah E. ; Renne, Paul R. ; Kieffer, Guy ; Piperno, Marcello ; Gallotti, Rosalia ; Raynal, Jean-Paul</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c457t-bc783bf4f114002a64dad9214b25c5ea0cbf5e902b9e403d07cdbff8540d8b7b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>40Ar/ 39Ar geochronology</topic><topic>Acheulean</topic><topic>Africa</topic><topic>Archaeological research</topic><topic>Archaeology - methods</topic><topic>Archaeology and Prehistory</topic><topic>Argon - chemistry</topic><topic>Chemistry Techniques, Analytical</topic><topic>Chronology</topic><topic>Chronology as Topic</topic><topic>Dating</topic><topic>Earth Sciences</topic><topic>Environmental change</topic><topic>Environmental Sciences</topic><topic>Ethiopia</topic><topic>Excavation and methods</topic><topic>Geochemistry</topic><topic>Geologic Sediments</topic><topic>Global Changes</topic><topic>Humanities and Social Sciences</topic><topic>Humans</topic><topic>Isotopes</topic><topic>Laboratory methods</topic><topic>Methodology and general studies</topic><topic>Obsidian</topic><topic>Oldowan</topic><topic>Palaeolithic and epipalaeolithic</topic><topic>Paleoanthropology</topic><topic>Prehistory and protohistory</topic><topic>Radioisotopes</topic><topic>Radiometric Dating - methods</topic><topic>Sciences of the Universe</topic><topic>Southern and East Africa</topic><topic>Stratigraphy</topic><topic>Upper Awash</topic><topic>Volcanology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Morgan, Leah E.</creatorcontrib><creatorcontrib>Renne, Paul R.</creatorcontrib><creatorcontrib>Kieffer, Guy</creatorcontrib><creatorcontrib>Piperno, Marcello</creatorcontrib><creatorcontrib>Gallotti, Rosalia</creatorcontrib><creatorcontrib>Raynal, Jean-Paul</creatorcontrib><collection>Pascal-Francis</collection><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><collection>International Bibliography of the Social Sciences (IBSS)</collection><collection>International Bibliography of the Social Sciences</collection><collection>International Bibliography of the Social Sciences</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>HAL-SHS: Archive ouverte en Sciences de l'Homme et de la Société</collection><jtitle>Journal of human evolution</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Morgan, Leah E.</au><au>Renne, Paul R.</au><au>Kieffer, Guy</au><au>Piperno, Marcello</au><au>Gallotti, Rosalia</au><au>Raynal, Jean-Paul</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A chronological framework for a long and persistent archaeological record: Melka Kunture, Ethiopia</atitle><jtitle>Journal of human evolution</jtitle><addtitle>J Hum Evol</addtitle><date>2012-01-01</date><risdate>2012</risdate><volume>62</volume><issue>1</issue><spage>104</spage><epage>115</epage><pages>104-115</pages><issn>0047-2484</issn><eissn>1095-8606</eissn><abstract>New
40Ar/
39Ar geochronological data for several volcanic ash horizons from Melka Kunture, Ethiopia, allow for significantly more precise age constraints to be placed upon the lithostratigraphy, archaeology and paleontology from this long record. Ashes from the Melka Kunture Formation at Gombore yielded the most reliable age constraints, from 1.393 ± 0.162 Ma
2
2
Uncertainties are provided at 1σ, here and throughout.
(millions of years ago) near the base of the section to 0.709 ± 0.013 Ma near the top. Dating the Garba section proved more problematic, but the base of the section, which contains numerous Oldowan obsidian artifacts, may be >1.719 ± 0.199 Ma, while the top is securely dated to 0.869 ± 0.020 Ma. The large ignimbrite from the Kella Formation at Kella and Melka Garba is dated to 1.262 ± 0.034 Ma and pre-dates Acheulean artifacts in the area. The Gombore II site, which has yielded two
Homo skull fragments, ‘twisted bifaces,’ and a preserved butchery site, is now constrained between 0.875 ± 0.010 Ma and 0.709 ± 0.013 Ma. Additional ashes from these and other sites further constrain the timing of deposition throughout the section.
Integration with previously published magnetostratigraphy has allowed for the first time a relatively complete, reliable timeline for the deposition of sediments, environmental changes, archaeology, and paleontology at Melka Kunture.</abstract><cop>Kidlington</cop><pub>Elsevier Ltd</pub><pmid>22176923</pmid><doi>10.1016/j.jhevol.2011.10.007</doi><tpages>12</tpages><orcidid>https://orcid.org/0000-0003-4160-3564</orcidid></addata></record> |
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subjects | 40Ar/ 39Ar geochronology Acheulean Africa Archaeological research Archaeology - methods Archaeology and Prehistory Argon - chemistry Chemistry Techniques, Analytical Chronology Chronology as Topic Dating Earth Sciences Environmental change Environmental Sciences Ethiopia Excavation and methods Geochemistry Geologic Sediments Global Changes Humanities and Social Sciences Humans Isotopes Laboratory methods Methodology and general studies Obsidian Oldowan Palaeolithic and epipalaeolithic Paleoanthropology Prehistory and protohistory Radioisotopes Radiometric Dating - methods Sciences of the Universe Southern and East Africa Stratigraphy Upper Awash Volcanology |
title | A chronological framework for a long and persistent archaeological record: Melka Kunture, Ethiopia |
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