{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,9,25]],"date-time":"2025-09-25T00:06:44Z","timestamp":1758758804120,"version":"3.44.0"},"reference-count":27,"publisher":"Elsevier","isbn-type":[{"type":"print","value":"9780128234983"}],"license":[{"start":{"date-parts":[[2022,1,1]],"date-time":"2022-01-01T00:00:00Z","timestamp":1640995200000},"content-version":"tdm","delay-in-days":0,"URL":"https:\/\/www.elsevier.com\/tdm\/userlicense\/1.0\/"},{"start":{"date-parts":[[2022,1,1]],"date-time":"2022-01-01T00:00:00Z","timestamp":1640995200000},"content-version":"tdm","delay-in-days":0,"URL":"https:\/\/www.elsevier.com\/legal\/tdmrep-license"},{"start":{"date-parts":[[2022,1,1]],"date-time":"2022-01-01T00:00:00Z","timestamp":1640995200000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-017"},{"start":{"date-parts":[[2022,1,1]],"date-time":"2022-01-01T00:00:00Z","timestamp":1640995200000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-037"},{"start":{"date-parts":[[2022,1,1]],"date-time":"2022-01-01T00:00:00Z","timestamp":1640995200000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-012"},{"start":{"date-parts":[[2022,1,1]],"date-time":"2022-01-01T00:00:00Z","timestamp":1640995200000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-029"},{"start":{"date-parts":[[2022,1,1]],"date-time":"2022-01-01T00:00:00Z","timestamp":1640995200000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-004"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":[],"published-print":{"date-parts":[[2022]]},"DOI":"10.1016\/b978-0-12-823498-3.00023-6","type":"book-chapter","created":{"date-parts":[[2021,11,26]],"date-time":"2021-11-26T13:13:02Z","timestamp":1637932382000},"page":"171-173","source":"Crossref","is-referenced-by-count":1,"title":["Definition of the Last Glacial Cycle marine stages and chronology"],"prefix":"10.1016","author":[{"given":"Natalia","family":"V\u00e1zquez Riveiros","sequence":"first","affiliation":[]},{"given":"Samuel","family":"Toucanne","sequence":"additional","affiliation":[]},{"given":"Teresa","family":"Rodrigues","sequence":"additional","affiliation":[]},{"given":"Amaelle","family":"Landais","sequence":"additional","affiliation":[]},{"given":"Filipa","family":"Naughton","sequence":"additional","affiliation":[]},{"given":"Mar\u00eda Fernanda","family":"S\u00e1nchez Go\u00f1i","sequence":"additional","affiliation":[]}],"member":"78","reference":[{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib1","series-title":"Sediment Cores From the East Pacific","first-page":"227","author":"Arrhenius","year":"1952"},{"issue":"1","key":"10.1016\/B978-0-12-823498-3.00023-6_bib2","doi-asserted-by":"crossref","first-page":"3713","DOI":"10.1038\/s41467-019-11601-2","article-title":"The configuration of Northern Hemisphere ice sheets through the Quaternary","volume":"10","author":"Batchelor","year":"2019","journal-title":"Nature Communications"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib3","doi-asserted-by":"crossref","first-page":"710","DOI":"10.1126\/science.1172873","article-title":"The Last Glacial Maximum","volume":"325","author":"Clark","year":"2009","journal-title":"Science"},{"year":"1981","author":"CLIMAP","series-title":"Seasonal Reconstruction of the Earth\u2019s Surface at the Last Glacial Maximum in Map Series","key":"10.1016\/B978-0-12-823498-3.00023-6_bib4"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib5","doi-asserted-by":"crossref","first-page":"187","DOI":"10.1016\/j.quascirev.2018.11.017","article-title":"Marine Isotope Stage 4 in Australasia: a full glacial culminating 65,000 years ago \u2013 Global connections and implications for human dispersal","volume":"204","author":"De Deckker","year":"2019","journal-title":"Quaternary Science Reviews"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib6","doi-asserted-by":"crossref","first-page":"704","DOI":"10.1126\/science.1221294","article-title":"Evolution of ocean temperature and ice volume through the Mid-Pleistocene climate transition","volume":"337","author":"Elderfield","year":"2012","journal-title":"Science"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib7","doi-asserted-by":"crossref","first-page":"538","DOI":"10.1086\/626295","article-title":"Pleistocene temperatures","volume":"63","author":"Emiliani","year":"1955","journal-title":"Journal of Geology"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib8","doi-asserted-by":"crossref","first-page":"1","DOI":"10.1016\/j.quascirev.2015.09.018","article-title":"Sequence of events from the onset to the demise of the Last Interglacial: evaluating strengths and limitations of chronologies used in climatic archives","volume":"129","author":"Govin","year":"2015","journal-title":"Quaternary Science Reviews"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib9","doi-asserted-by":"crossref","first-page":"744","DOI":"10.1038\/nature11593","article-title":"Rapid coupling between ice volume and polar temperature over the past 150,000 years","volume":"491","author":"Grant","year":"2012","journal-title":"Nature"},{"issue":"6322","key":"10.1016\/B978-0-12-823498-3.00023-6_bib10","doi-asserted-by":"crossref","first-page":"276","DOI":"10.1126\/science.aai8464","article-title":"Regional and global sea-surface temperatures during the last interglaciation","volume":"355","author":"Hoffman","year":"2017","journal-title":"Science"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib11","doi-asserted-by":"crossref","first-page":"174","DOI":"10.1016\/j.quaint.2014.06.006","article-title":"A stratigraphical basis for the Last Glacial Maximum (LGM)","volume":"383","author":"Hughes","year":"2015","journal-title":"Quaternary International"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib12","doi-asserted-by":"crossref","first-page":"222","DOI":"10.1017\/qua.2018.37","article-title":"Global glacier dynamics during 100 ka Pleistocene glacial cycles","volume":"90","author":"Hughes","year":"2018","journal-title":"Quaternary Research"},{"issue":"43","key":"10.1016\/B978-0-12-823498-3.00023-6_bib13","doi-asserted-by":"crossref","first-page":"15296","DOI":"10.1073\/pnas.1411762111","article-title":"Sea level and global ice volumes from the Last Glacial Maximum to the Holocene","volume":"111","author":"Lambeck","year":"2014","journal-title":"Proceedings of the National Academy of Sciences"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib14","first-page":"PA1003","article-title":"A Pliocene-Pleistocene stack of 57 globally distributed benthic \u03b418O records","volume":"20","author":"Lisiecki","year":"2005","journal-title":"Paleoceanography"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib15","doi-asserted-by":"crossref","first-page":"310","DOI":"10.1016\/j.epsl.2012.12.001","article-title":"A global compilation of coral sea-level benchmarks: implications and new challenges","volume":"362","author":"Medina-Elizalde","year":"2013","journal-title":"Earth and Planetary Science Letters"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib16","doi-asserted-by":"crossref","first-page":"627","DOI":"10.1016\/S0277-3791(00)00145-1","article-title":"Environmental processes of the ice age: land, oceans, glaciers (EPILOG)","volume":"20","author":"Mix","year":"2001","journal-title":"Quaternary Science Reviews"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib17","doi-asserted-by":"crossref","DOI":"10.1002\/2015RG000482","article-title":"Interglacials of the last 800,000 years","volume":"54","author":"Past InterGlacialS Working Group of PAGES","year":"2016","journal-title":"Reviews of Geophysics"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib18","doi-asserted-by":"crossref","first-page":"94","DOI":"10.1016\/j.quascirev.2015.01.012","article-title":"An optimized scheme of lettered marine isotope substages for the last 1.0 million years, and the climatostratigraphic nature of isotope stages and substages","volume":"111","author":"Railsback","year":"2015","journal-title":"Quaternary Science Reviews"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib19","doi-asserted-by":"crossref","first-page":"14","DOI":"10.1016\/j.quascirev.2014.09.007","article-title":"A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records: refining and extending the INTIMATE event stratigraphy","volume":"106","author":"Rasmussen","year":"2014","journal-title":"Quaternary Science Reviews"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib20","doi-asserted-by":"crossref","first-page":"477","DOI":"10.1038\/nature13230","article-title":"Sea-level and deep-sea-temperature variability over the past 5.3 million years","volume":"508","author":"Rohling","year":"2014","journal-title":"Nature"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib21","doi-asserted-by":"crossref","first-page":"39","DOI":"10.1016\/0033-5894(73)90052-5","article-title":"Oxygen isotope and palaeomagnetic stratigraphy of equatorial Pacific core V28\u2013238: oxygen isotope temperatures and ice volumes on a 105 year and 106 year scale","volume":"3","author":"Shackleton","year":"1973","journal-title":"Quaternary Research"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib22","doi-asserted-by":"crossref","first-page":"58","DOI":"10.1016\/j.epsl.2015.05.042","article-title":"An 800-kyr record of global surface ocean \u03b418O and implications for ice volume-temperature coupling","volume":"426","author":"Shakun","year":"2015","journal-title":"Earth and Planetary Science Letters"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib23","doi-asserted-by":"crossref","first-page":"RG4003","DOI":"10.1029\/2007RG000226","article-title":"Marine Isotope Stage 3 sea level fluctuations: data synthesis and new outlook","volume":"46","author":"Siddall","year":"2008","journal-title":"Reviews of Geophysics"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib24","doi-asserted-by":"crossref","first-page":"1079","DOI":"10.5194\/cp-12-1079-2016","article-title":"A Late Pleistocene sea level stack","volume":"12","author":"Spratt","year":"2016","journal-title":"Climate of the Past"},{"key":"10.1016\/B978-0-12-823498-3.00023-6_bib25","doi-asserted-by":"crossref","first-page":"295","DOI":"10.1016\/S0277-3791(01)00101-9","article-title":"Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records","volume":"21","author":"Waelbroeck","year":"2002","journal-title":"Quaternary Science Reviews"},{"issue":"1","key":"10.1016\/B978-0-12-823498-3.00023-6_bib26","doi-asserted-by":"crossref","first-page":"165","DOI":"10.1038\/s41597-019-0173-8","article-title":"Consistently dated Atlantic sediment cores over the last 40 thousand years","volume":"6","author":"Waelbroeck","year":"2019","journal-title":"Scientific Data"},{"issue":"7715","key":"10.1016\/B978-0-12-823498-3.00023-6_bib27","doi-asserted-by":"crossref","first-page":"603","DOI":"10.1038\/s41586-018-0335-4","article-title":"Rapid glaciation and a two-step sea level plunge into the Last Glacial Maximum","volume":"559","author":"Yokoyama","year":"2018","journal-title":"Nature"}],"container-title":["European Glacial Landscapes"],"original-title":[],"language":"en","link":[{"URL":"https:\/\/api.elsevier.com\/content\/article\/PII:B9780128234983000236?httpAccept=text\/xml","content-type":"text\/xml","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/api.elsevier.com\/content\/article\/PII:B9780128234983000236?httpAccept=text\/plain","content-type":"text\/plain","content-version":"vor","intended-application":"text-mining"}],"deposited":{"date-parts":[[2025,9,24]],"date-time":"2025-09-24T05:25:26Z","timestamp":1758691526000},"score":1,"resource":{"primary":{"URL":"https:\/\/linkinghub.elsevier.com\/retrieve\/pii\/B9780128234983000236"}},"subtitle":[],"short-title":[],"issued":{"date-parts":[[2022]]},"ISBN":["9780128234983"],"references-count":27,"URL":"https:\/\/doi.org\/10.1016\/b978-0-12-823498-3.00023-6","relation":{},"subject":[],"published":{"date-parts":[[2022]]}}}