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From the Bay of Naples to the River Don: the Campanian Ignimbrite eruption and the Middle to Upper Paleolithic transition in Eastern Europe
The Campanian Ignimbrite (CI) eruption, dated by 40Ar/ 39Ar and various stratigraphic methods to ca. 39,000 cal BP, generated a massive ash plume from its source in southern Italy across Southeastern and Eastern Europe. At the Kostenki-Borshchevo open-air sites on the Middle Don River in Russia, Upp...
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| Published in: | Journal of human evolution 2008-11, Vol.55 (5), p.858-870 |
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| cites | cdi_FETCH-LOGICAL-c424t-b544c4470447eb91159b1c0110637fe41d31ed6b5ef97a95da5234e10c3c65383 |
| container_end_page | 870 |
| container_issue | 5 |
| container_start_page | 858 |
| container_title | Journal of human evolution |
| container_volume | 55 |
| creator | Hoffecker, John F. Holliday, Vance T. Anikovich, M.V. Sinitsyn, A.A. Popov, V.V. Lisitsyn, S.N. Levkovskaya, G.M. Pospelova, G.A. Forman, Steven L. Giaccio, Biagio |
| description | The Campanian Ignimbrite (CI) eruption, dated by
40Ar/
39Ar and various stratigraphic methods to ca. 39,000
cal BP, generated a massive ash plume from its source in southern Italy across Southeastern and Eastern Europe. At the Kostenki-Borshchevo open-air sites on the Middle Don River in Russia, Upper Paleolithic artifact assemblages are buried below, within, and above the CI tephra (which is redeposited by slope action at most sites) on the second terrace. Luminescence and radiocarbon dating, paleomagnetism, and soil and pollen stratigraphy provide further basis for correlation with the Greenland and North Atlantic climate stratigraphy. The oldest Upper Paleolithic occupation layers at Kostenki-Borshchevo may be broadly correlated with warm intervals that preceded the CI event and Heinrich Event 4 (HE4; Greenland Interstadial: GI 12–GI 9) dating to ca. 45,000–41,000
cal BP. These layers contain an industry not currently recognized in other parts of Europe. Early Upper Paleolithic layers above the CI tephra are correlated with HE4 and warm intervals that occurred during 38,000–30,000
cal BP (GI 8–GI 5), and include an assemblage that is assigned to the Aurigancian industry, associated with skeletal remains of modern humans. |
| doi_str_mv | 10.1016/j.jhevol.2008.08.018 |
| format | article |
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40Ar/
39Ar and various stratigraphic methods to ca. 39,000
cal BP, generated a massive ash plume from its source in southern Italy across Southeastern and Eastern Europe. At the Kostenki-Borshchevo open-air sites on the Middle Don River in Russia, Upper Paleolithic artifact assemblages are buried below, within, and above the CI tephra (which is redeposited by slope action at most sites) on the second terrace. Luminescence and radiocarbon dating, paleomagnetism, and soil and pollen stratigraphy provide further basis for correlation with the Greenland and North Atlantic climate stratigraphy. The oldest Upper Paleolithic occupation layers at Kostenki-Borshchevo may be broadly correlated with warm intervals that preceded the CI event and Heinrich Event 4 (HE4; Greenland Interstadial: GI 12–GI 9) dating to ca. 45,000–41,000
cal BP. These layers contain an industry not currently recognized in other parts of Europe. Early Upper Paleolithic layers above the CI tephra are correlated with HE4 and warm intervals that occurred during 38,000–30,000
cal BP (GI 8–GI 5), and include an assemblage that is assigned to the Aurigancian industry, associated with skeletal remains of modern humans.</description><identifier>ISSN: 0047-2484</identifier><identifier>EISSN: 1095-8606</identifier><identifier>DOI: 10.1016/j.jhevol.2008.08.018</identifier><identifier>PMID: 18937961</identifier><language>eng</language><publisher>England: Elsevier Ltd</publisher><subject>Animals ; Archaeological dating ; Archaeology - methods ; Climate stratigraphy ; Early Upper Paleolithic ; Eastern Europe ; Ecology ; Geochronology ; Geological Phenomena ; Hominidae ; Human evolution ; Humans ; Kostenki-Borshchevo ; Middle to Upper Paleolithic transition ; Natural disasters ; Paleoclimatology ; Paleolithic Age ; Russia ; Volcanic Eruptions ; Volcanoes</subject><ispartof>Journal of human evolution, 2008-11, Vol.55 (5), p.858-870</ispartof><rights>2008 Elsevier Ltd</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c424t-b544c4470447eb91159b1c0110637fe41d31ed6b5ef97a95da5234e10c3c65383</citedby><cites>FETCH-LOGICAL-c424t-b544c4470447eb91159b1c0110637fe41d31ed6b5ef97a95da5234e10c3c65383</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925,33224</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/18937961$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Hoffecker, John F.</creatorcontrib><creatorcontrib>Holliday, Vance T.</creatorcontrib><creatorcontrib>Anikovich, M.V.</creatorcontrib><creatorcontrib>Sinitsyn, A.A.</creatorcontrib><creatorcontrib>Popov, V.V.</creatorcontrib><creatorcontrib>Lisitsyn, S.N.</creatorcontrib><creatorcontrib>Levkovskaya, G.M.</creatorcontrib><creatorcontrib>Pospelova, G.A.</creatorcontrib><creatorcontrib>Forman, Steven L.</creatorcontrib><creatorcontrib>Giaccio, Biagio</creatorcontrib><title>From the Bay of Naples to the River Don: the Campanian Ignimbrite eruption and the Middle to Upper Paleolithic transition in Eastern Europe</title><title>Journal of human evolution</title><addtitle>J Hum Evol</addtitle><description>The Campanian Ignimbrite (CI) eruption, dated by
40Ar/
39Ar and various stratigraphic methods to ca. 39,000
cal BP, generated a massive ash plume from its source in southern Italy across Southeastern and Eastern Europe. At the Kostenki-Borshchevo open-air sites on the Middle Don River in Russia, Upper Paleolithic artifact assemblages are buried below, within, and above the CI tephra (which is redeposited by slope action at most sites) on the second terrace. Luminescence and radiocarbon dating, paleomagnetism, and soil and pollen stratigraphy provide further basis for correlation with the Greenland and North Atlantic climate stratigraphy. The oldest Upper Paleolithic occupation layers at Kostenki-Borshchevo may be broadly correlated with warm intervals that preceded the CI event and Heinrich Event 4 (HE4; Greenland Interstadial: GI 12–GI 9) dating to ca. 45,000–41,000
cal BP. These layers contain an industry not currently recognized in other parts of Europe. Early Upper Paleolithic layers above the CI tephra are correlated with HE4 and warm intervals that occurred during 38,000–30,000
cal BP (GI 8–GI 5), and include an assemblage that is assigned to the Aurigancian industry, associated with skeletal remains of modern humans.</description><subject>Animals</subject><subject>Archaeological dating</subject><subject>Archaeology - methods</subject><subject>Climate stratigraphy</subject><subject>Early Upper Paleolithic</subject><subject>Eastern Europe</subject><subject>Ecology</subject><subject>Geochronology</subject><subject>Geological Phenomena</subject><subject>Hominidae</subject><subject>Human evolution</subject><subject>Humans</subject><subject>Kostenki-Borshchevo</subject><subject>Middle to Upper Paleolithic transition</subject><subject>Natural disasters</subject><subject>Paleoclimatology</subject><subject>Paleolithic Age</subject><subject>Russia</subject><subject>Volcanic Eruptions</subject><subject>Volcanoes</subject><issn>0047-2484</issn><issn>1095-8606</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><sourceid>8BJ</sourceid><recordid>eNqFkcFq3DAQhkVpaTZp36AUnUov3kqWLFs9FNpt0gTSJpTmLGR53NViS44kL-QZ8tK1vQu5pTBiGPHN_8P8CL2jZE0JFZ92690W9r5b54RU67lo9QKtKJFFVgkiXqIVIbzMcl7xE3Qa444QIjnLX6MTWklWSkFX6PEi-B6nLeBv-gH7Fv_SQwcRJ798_rZ7CPi7d5-XcaP7QTurHb7662xfB5sAQxiHZL3D2jUL9dM2TQezxN0wTOu3ugPf2bS1BqegXbQLbh0-1zFBmPoY_ABv0KtWdxHeHvsZurs4_7O5zK5vflxtvl5nhuc8ZXXBueG8JNODWlJayJoaQikRrGyB04ZRaERdQCtLLYtGFznjQIlhRhSsYmfow0F3CP5-hJhUb6OBrtMO_BiVkNV00pL9F2TlZJovih-fBadQGC-oELMmP6Am-BgDtGoIttfhYYLUHKzaqUOwag5WzUVnh_dHh7HuoXlaOiY5AV8OAEyX21sIKhoLzkBjA5ikGm-fd_gHoae1xQ</recordid><startdate>20081101</startdate><enddate>20081101</enddate><creator>Hoffecker, John F.</creator><creator>Holliday, Vance T.</creator><creator>Anikovich, M.V.</creator><creator>Sinitsyn, A.A.</creator><creator>Popov, V.V.</creator><creator>Lisitsyn, S.N.</creator><creator>Levkovskaya, G.M.</creator><creator>Pospelova, G.A.</creator><creator>Forman, Steven L.</creator><creator>Giaccio, Biagio</creator><general>Elsevier Ltd</general><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>7QH</scope><scope>7UA</scope><scope>C1K</scope><scope>8BJ</scope><scope>FQK</scope><scope>JBE</scope><scope>7X8</scope></search><sort><creationdate>20081101</creationdate><title>From the Bay of Naples to the River Don: the Campanian Ignimbrite eruption and the Middle to Upper Paleolithic transition in Eastern Europe</title><author>Hoffecker, John F. ; 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40Ar/
39Ar and various stratigraphic methods to ca. 39,000
cal BP, generated a massive ash plume from its source in southern Italy across Southeastern and Eastern Europe. At the Kostenki-Borshchevo open-air sites on the Middle Don River in Russia, Upper Paleolithic artifact assemblages are buried below, within, and above the CI tephra (which is redeposited by slope action at most sites) on the second terrace. Luminescence and radiocarbon dating, paleomagnetism, and soil and pollen stratigraphy provide further basis for correlation with the Greenland and North Atlantic climate stratigraphy. The oldest Upper Paleolithic occupation layers at Kostenki-Borshchevo may be broadly correlated with warm intervals that preceded the CI event and Heinrich Event 4 (HE4; Greenland Interstadial: GI 12–GI 9) dating to ca. 45,000–41,000
cal BP. These layers contain an industry not currently recognized in other parts of Europe. Early Upper Paleolithic layers above the CI tephra are correlated with HE4 and warm intervals that occurred during 38,000–30,000
cal BP (GI 8–GI 5), and include an assemblage that is assigned to the Aurigancian industry, associated with skeletal remains of modern humans.</abstract><cop>England</cop><pub>Elsevier Ltd</pub><pmid>18937961</pmid><doi>10.1016/j.jhevol.2008.08.018</doi><tpages>13</tpages></addata></record> |
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| ispartof | Journal of human evolution, 2008-11, Vol.55 (5), p.858-870 |
| issn | 0047-2484 1095-8606 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_69800873 |
| source | International Bibliography of the Social Sciences (IBSS); Elsevier |
| subjects | Animals Archaeological dating Archaeology - methods Climate stratigraphy Early Upper Paleolithic Eastern Europe Ecology Geochronology Geological Phenomena Hominidae Human evolution Humans Kostenki-Borshchevo Middle to Upper Paleolithic transition Natural disasters Paleoclimatology Paleolithic Age Russia Volcanic Eruptions Volcanoes |
| title | From the Bay of Naples to the River Don: the Campanian Ignimbrite eruption and the Middle to Upper Paleolithic transition in Eastern Europe |
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