Heightened early medieval storminess across the Chukchi Sea, AD 400–1100: A proxy of the Late Antique Little Ice Age
Beach ridges and spits along the north-facing coast of the Chukchi Sea record paleo-storm history during the 1st millennium AD, correlative with a widespread global cooling climate episode. Northwest Alaska is a sensitive proxy owing to its absence of tectonism, glacio-isostasy, and a low rate of eu...
Gespeichert in:
| Veröffentlicht in: | Quaternary international 2020-05, Vol.549, p.98-117 |
|---|---|
| Hauptverfasser: | , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 117 |
|---|---|
| container_issue | |
| container_start_page | 98 |
| container_title | Quaternary international |
| container_volume | 549 |
| creator | Mason, Owen K. Jensen, Anne M. Rinck, Brandy Alix, Claire M. Bowers, Peter M. Hoffecker, John F. |
| description | Beach ridges and spits along the north-facing coast of the Chukchi Sea record paleo-storm history during the 1st millennium AD, correlative with a widespread global cooling climate episode. Northwest Alaska is a sensitive proxy owing to its absence of tectonism, glacio-isostasy, and a low rate of eustatic sea level rise. Four locales provide a regional transect and detailed chronologies: north-facing Deering and Cape Espenberg and west-facing Kotzebue and southwest facing Point Barrow. A single storm or series of storms during AD 400–600 impacted both north and south areas, while lesser intensity storms occurred across the southern region during the 11th century AD. The first millennium AD storms were as strong as or stronger than those of the 20th century, if paleo-sea level is factored in. Storm-heightened upwelling had a salubrious effect on cultures around the Chukchi Sea, leading to a florescence of whaling and walrusing. |
| doi_str_mv | 10.1016/j.quaint.2019.01.042 |
| format | Article |
| fullrecord | <record><control><sourceid>elsevier_hal_p</sourceid><recordid>TN_cdi_hal_primary_oai_HAL_hal_03820378v1</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S104061821830750X</els_id><sourcerecordid>S104061821830750X</sourcerecordid><originalsourceid>FETCH-LOGICAL-c386t-59dceafbb2ba3e8ddb2b261744b39117859e900fc2d629a72dfa02b20482b3513</originalsourceid><addsrcrecordid>eNp9kMtKw0AYhYMoWC9v4GK2gon_XHJzIYR6qVBwoa6HyeRPMzVNdDItduc7-IY-idNWXLr6L5xz4HxBcEYhokCTy3n0vlSmcxEDmkdAIxBsLxjRLOWhiGO-73cQECY0Y4fB0TDMASBOmBgFqwmaWeOww4qgsu2aLLAyuFItGVxvF6bDYSBK294P1yAZN8tX3RjyhOqCFDdEAHx_flEKcEUK8mb7jzXp6610qhySonPmfekP41yL5EH71wxPgoNatQOe_s7j4OXu9nk8CaeP9w_jYhpqniUujPNKo6rLkpWKY1ZVfmEJTYUoeU5pmsU55gC1ZlXCcpWyqlbgJSAyVvKY8uPgfJfbqFa-WbNQdi17ZeSkmMrND3jGgKfZaqMVO-22rMX6z0BBbjjLudxxlhvOEqj0nL3temdD32Nl0MpBG-y0x2hRO1n15v-AH5FHh1Q</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Heightened early medieval storminess across the Chukchi Sea, AD 400–1100: A proxy of the Late Antique Little Ice Age</title><source>ScienceDirect Journals (5 years ago - present)</source><creator>Mason, Owen K. ; Jensen, Anne M. ; Rinck, Brandy ; Alix, Claire M. ; Bowers, Peter M. ; Hoffecker, John F.</creator><creatorcontrib>Mason, Owen K. ; Jensen, Anne M. ; Rinck, Brandy ; Alix, Claire M. ; Bowers, Peter M. ; Hoffecker, John F.</creatorcontrib><description>Beach ridges and spits along the north-facing coast of the Chukchi Sea record paleo-storm history during the 1st millennium AD, correlative with a widespread global cooling climate episode. Northwest Alaska is a sensitive proxy owing to its absence of tectonism, glacio-isostasy, and a low rate of eustatic sea level rise. Four locales provide a regional transect and detailed chronologies: north-facing Deering and Cape Espenberg and west-facing Kotzebue and southwest facing Point Barrow. A single storm or series of storms during AD 400–600 impacted both north and south areas, while lesser intensity storms occurred across the southern region during the 11th century AD. The first millennium AD storms were as strong as or stronger than those of the 20th century, if paleo-sea level is factored in. Storm-heightened upwelling had a salubrious effect on cultures around the Chukchi Sea, leading to a florescence of whaling and walrusing.</description><identifier>ISSN: 1040-6182</identifier><identifier>EISSN: 1873-4553</identifier><identifier>DOI: 10.1016/j.quaint.2019.01.042</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Alaska ; Beach ridges ; Climate history ; Environmental Sciences ; Humanities and Social Sciences ; Medieval climate anomaly ; Paleo-storm history</subject><ispartof>Quaternary international, 2020-05, Vol.549, p.98-117</ispartof><rights>2019 Elsevier Ltd and INQUA</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c386t-59dceafbb2ba3e8ddb2b261744b39117859e900fc2d629a72dfa02b20482b3513</citedby><cites>FETCH-LOGICAL-c386t-59dceafbb2ba3e8ddb2b261744b39117859e900fc2d629a72dfa02b20482b3513</cites><orcidid>0000-0002-8947-5859</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.quaint.2019.01.042$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,314,780,784,885,3550,27924,27925,45995</link.rule.ids><backlink>$$Uhttps://hal.science/hal-03820378$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Mason, Owen K.</creatorcontrib><creatorcontrib>Jensen, Anne M.</creatorcontrib><creatorcontrib>Rinck, Brandy</creatorcontrib><creatorcontrib>Alix, Claire M.</creatorcontrib><creatorcontrib>Bowers, Peter M.</creatorcontrib><creatorcontrib>Hoffecker, John F.</creatorcontrib><title>Heightened early medieval storminess across the Chukchi Sea, AD 400–1100: A proxy of the Late Antique Little Ice Age</title><title>Quaternary international</title><description>Beach ridges and spits along the north-facing coast of the Chukchi Sea record paleo-storm history during the 1st millennium AD, correlative with a widespread global cooling climate episode. Northwest Alaska is a sensitive proxy owing to its absence of tectonism, glacio-isostasy, and a low rate of eustatic sea level rise. Four locales provide a regional transect and detailed chronologies: north-facing Deering and Cape Espenberg and west-facing Kotzebue and southwest facing Point Barrow. A single storm or series of storms during AD 400–600 impacted both north and south areas, while lesser intensity storms occurred across the southern region during the 11th century AD. The first millennium AD storms were as strong as or stronger than those of the 20th century, if paleo-sea level is factored in. Storm-heightened upwelling had a salubrious effect on cultures around the Chukchi Sea, leading to a florescence of whaling and walrusing.</description><subject>Alaska</subject><subject>Beach ridges</subject><subject>Climate history</subject><subject>Environmental Sciences</subject><subject>Humanities and Social Sciences</subject><subject>Medieval climate anomaly</subject><subject>Paleo-storm history</subject><issn>1040-6182</issn><issn>1873-4553</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp9kMtKw0AYhYMoWC9v4GK2gon_XHJzIYR6qVBwoa6HyeRPMzVNdDItduc7-IY-idNWXLr6L5xz4HxBcEYhokCTy3n0vlSmcxEDmkdAIxBsLxjRLOWhiGO-73cQECY0Y4fB0TDMASBOmBgFqwmaWeOww4qgsu2aLLAyuFItGVxvF6bDYSBK294P1yAZN8tX3RjyhOqCFDdEAHx_flEKcEUK8mb7jzXp6610qhySonPmfekP41yL5EH71wxPgoNatQOe_s7j4OXu9nk8CaeP9w_jYhpqniUujPNKo6rLkpWKY1ZVfmEJTYUoeU5pmsU55gC1ZlXCcpWyqlbgJSAyVvKY8uPgfJfbqFa-WbNQdi17ZeSkmMrND3jGgKfZaqMVO-22rMX6z0BBbjjLudxxlhvOEqj0nL3temdD32Nl0MpBG-y0x2hRO1n15v-AH5FHh1Q</recordid><startdate>20200530</startdate><enddate>20200530</enddate><creator>Mason, Owen K.</creator><creator>Jensen, Anne M.</creator><creator>Rinck, Brandy</creator><creator>Alix, Claire M.</creator><creator>Bowers, Peter M.</creator><creator>Hoffecker, John F.</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>AAYXX</scope><scope>CITATION</scope><scope>1XC</scope><scope>BXJBU</scope><orcidid>https://orcid.org/0000-0002-8947-5859</orcidid></search><sort><creationdate>20200530</creationdate><title>Heightened early medieval storminess across the Chukchi Sea, AD 400–1100: A proxy of the Late Antique Little Ice Age</title><author>Mason, Owen K. ; Jensen, Anne M. ; Rinck, Brandy ; Alix, Claire M. ; Bowers, Peter M. ; Hoffecker, John F.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c386t-59dceafbb2ba3e8ddb2b261744b39117859e900fc2d629a72dfa02b20482b3513</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Alaska</topic><topic>Beach ridges</topic><topic>Climate history</topic><topic>Environmental Sciences</topic><topic>Humanities and Social Sciences</topic><topic>Medieval climate anomaly</topic><topic>Paleo-storm history</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Mason, Owen K.</creatorcontrib><creatorcontrib>Jensen, Anne M.</creatorcontrib><creatorcontrib>Rinck, Brandy</creatorcontrib><creatorcontrib>Alix, Claire M.</creatorcontrib><creatorcontrib>Bowers, Peter M.</creatorcontrib><creatorcontrib>Hoffecker, John F.</creatorcontrib><collection>CrossRef</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>HAL-SHS: Archive ouverte en Sciences de l'Homme et de la Société</collection><jtitle>Quaternary international</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Mason, Owen K.</au><au>Jensen, Anne M.</au><au>Rinck, Brandy</au><au>Alix, Claire M.</au><au>Bowers, Peter M.</au><au>Hoffecker, John F.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Heightened early medieval storminess across the Chukchi Sea, AD 400–1100: A proxy of the Late Antique Little Ice Age</atitle><jtitle>Quaternary international</jtitle><date>2020-05-30</date><risdate>2020</risdate><volume>549</volume><spage>98</spage><epage>117</epage><pages>98-117</pages><issn>1040-6182</issn><eissn>1873-4553</eissn><abstract>Beach ridges and spits along the north-facing coast of the Chukchi Sea record paleo-storm history during the 1st millennium AD, correlative with a widespread global cooling climate episode. Northwest Alaska is a sensitive proxy owing to its absence of tectonism, glacio-isostasy, and a low rate of eustatic sea level rise. Four locales provide a regional transect and detailed chronologies: north-facing Deering and Cape Espenberg and west-facing Kotzebue and southwest facing Point Barrow. A single storm or series of storms during AD 400–600 impacted both north and south areas, while lesser intensity storms occurred across the southern region during the 11th century AD. The first millennium AD storms were as strong as or stronger than those of the 20th century, if paleo-sea level is factored in. Storm-heightened upwelling had a salubrious effect on cultures around the Chukchi Sea, leading to a florescence of whaling and walrusing.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.quaint.2019.01.042</doi><tpages>20</tpages><orcidid>https://orcid.org/0000-0002-8947-5859</orcidid><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1040-6182 |
| ispartof | Quaternary international, 2020-05, Vol.549, p.98-117 |
| issn | 1040-6182 1873-4553 |
| language | eng |
| recordid | cdi_hal_primary_oai_HAL_hal_03820378v1 |
| source | ScienceDirect Journals (5 years ago - present) |
| subjects | Alaska Beach ridges Climate history Environmental Sciences Humanities and Social Sciences Medieval climate anomaly Paleo-storm history |
| title | Heightened early medieval storminess across the Chukchi Sea, AD 400–1100: A proxy of the Late Antique Little Ice Age |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-06T13%3A03%3A21IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-elsevier_hal_p&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Heightened%20early%20medieval%20storminess%20across%20the%20Chukchi%20Sea,%20AD%20400%E2%80%931100:%20A%20proxy%20of%20the%20Late%20Antique%20Little%20Ice%20Age&rft.jtitle=Quaternary%20international&rft.au=Mason,%20Owen%20K.&rft.date=2020-05-30&rft.volume=549&rft.spage=98&rft.epage=117&rft.pages=98-117&rft.issn=1040-6182&rft.eissn=1873-4553&rft_id=info:doi/10.1016/j.quaint.2019.01.042&rft_dat=%3Celsevier_hal_p%3ES104061821830750X%3C/elsevier_hal_p%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rft_els_id=S104061821830750X&rfr_iscdi=true |