FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1834370598> ?p ?o ?g. }

• W1834370598 endingPage "242" @default.
• W1834370598 startingPage "233" @default.
• W1834370598 abstract "The glacial chronology of Mexico is based on glacial landforms of Iztaccíhuatl (5,282 m a.s.l., 19°10′N, 98°40′W), Nevado de Toluca (4,558 m a.s.l., 19°08′N, 99°45′W), and La Malinche (4,461 m, 19°14′N, 98°00′W). Morphostratigra-phy, tephrochronology and 81 cosmogenic 36Cl exposure ages from Iztaccíhuatl reveal new insights into the glacial sequence in Mexico. The most extensive recorded advance (Nexcoalango) occurred during Marine Isotope Stage 6 (MIS 6), probably at 195,000 BP and reached c. 3000 m. Iztaccíhuatl lacks clear evidence of Wisconsinan glaciation prior to 20,000 cal yr BP. The local Late Pleistocene glacial maximum occurred after the climax of the Last Glacial Maximum (LGM). A first pulse (Hueyatlaco 1 advance) peaked at 20,000–17,500 cal yr BP and a second one (Hueyatlaco 2) at c. 17,000–14,000 cal yr BP. Valley glaciers reached to c. 3400–3500 m a.s.l. Recessional moraines developed from 14,000 to 13,000 cal yr BP, followed by a rapid glacier retreat at 13,000–12,000 cal yr BP. Subsequently, glaciers peaked again at c. 12,000 cal yr BP reaching c. 3800 m (Milpulco 1), and built recessional moraines until c. 10,000 cal yr BP. Then between c. 8300–7000 cal yr BP glaciers formed small but distinctive moraines above 4000 m a.s.l. (Milpulco 2). No evidence of glacier expansion has been found between Milpulco 2 deposits and the massive moraines of <1000 cal yr BP (Ayoloco) that occur at 4300–4700 m a.s.l. Possible correlations between the glacial record of Iztaccíhuatl and other glacial sequences (La Malinche, Nevado de Toluca) are presented. The equilibrium line altitudes (ELA) of glaciers reveal ELA depressions for the five late Quaternary advances of 1030 m, 930 m, 730 m, 550 m and 250 m, respectively. The overall pattern of glaciation is similar to those of mid-latitude North America and tropical South America, thus supporting the general synchroneity of major climatic events. A temperature decrease of 5–9°C estimated from Hueyatlaco ELA supports marked cooling over tropical land and oceans during the LGM. Although inconclusive, evidence does not indicate glacier expansion during, but rather immediately following the Younger Dryas Chronozone. However, a global early-to-mid-Holocene event (8200 cal yr event) is coeval with Milpulco 2 advance, and the Ayoloco advance is contemporaneous with the Little Ice Age." @default.
• W1834370598 created "2016-06-24" @default.
• W1834370598 creator A5025749974 @default.
• W1834370598 creator A5074677400 @default.
• W1834370598 date "2004-01-01" @default.
• W1834370598 modified "2023-10-11" @default.
• W1834370598 title "Late Quaternary glaciation of México" @default.
• W1834370598 cites W1646758270 @default.
• W1834370598 cites W1922910143 @default.
• W1834370598 cites W1927648166 @default.
• W1834370598 cites W1975763529 @default.
• W1834370598 cites W1997594284 @default.
• W1834370598 cites W2002286946 @default.
• W1834370598 cites W2009187061 @default.
• W1834370598 cites W2013488438 @default.
• W1834370598 cites W2014818316 @default.
• W1834370598 cites W2033248939 @default.
• W1834370598 cites W2056141481 @default.
• W1834370598 cites W2062572705 @default.
• W1834370598 cites W2076954229 @default.
• W1834370598 cites W2108684521 @default.
• W1834370598 cites W2138944634 @default.
• W1834370598 cites W2280624662 @default.
• W1834370598 cites W2318116799 @default.
• W1834370598 cites W4236275340 @default.
• W1834370598 doi "https://doi.org/10.1016/s1571-0866(04)80129-5" @default.
• W1834370598 hasPublicationYear "2004" @default.
• W1834370598 type Work @default.
• W1834370598 sameAs 1834370598 @default.
• W1834370598 citedByCount "33" @default.
• W1834370598 countsByYear W18343705982012 @default.
• W1834370598 countsByYear W18343705982013 @default.
• W1834370598 countsByYear W18343705982015 @default.
• W1834370598 countsByYear W18343705982018 @default.
• W1834370598 countsByYear W18343705982019 @default.
• W1834370598 countsByYear W18343705982020 @default.
• W1834370598 crossrefType "book-chapter" @default.
• W1834370598 hasAuthorship W1834370598A5025749974 @default.
• W1834370598 hasAuthorship W1834370598A5074677400 @default.
• W1834370598 hasConcept C100834320 @default.
• W1834370598 hasConcept C100970517 @default.
• W1834370598 hasConcept C114793014 @default.
• W1834370598 hasConcept C127313418 @default.
• W1834370598 hasConcept C151730666 @default.
• W1834370598 hasConcept C15739521 @default.
• W1834370598 hasConcept C15785411 @default.
• W1834370598 hasConcept C160464908 @default.
• W1834370598 hasConcept C180705331 @default.
• W1834370598 hasConcept C181536285 @default.
• W1834370598 hasConcept C186240526 @default.
• W1834370598 hasConcept C188291805 @default.
• W1834370598 hasConcept C205649164 @default.
• W1834370598 hasConcept C26099304 @default.
• W1834370598 hasConcept C2780518792 @default.
• W1834370598 hasConcept C53570757 @default.
• W1834370598 hasConcept C98736793 @default.
• W1834370598 hasConceptScore W1834370598C100834320 @default.
• W1834370598 hasConceptScore W1834370598C100970517 @default.
• W1834370598 hasConceptScore W1834370598C114793014 @default.
• W1834370598 hasConceptScore W1834370598C127313418 @default.
• W1834370598 hasConceptScore W1834370598C151730666 @default.
• W1834370598 hasConceptScore W1834370598C15739521 @default.
• W1834370598 hasConceptScore W1834370598C15785411 @default.
• W1834370598 hasConceptScore W1834370598C160464908 @default.
• W1834370598 hasConceptScore W1834370598C180705331 @default.
• W1834370598 hasConceptScore W1834370598C181536285 @default.
• W1834370598 hasConceptScore W1834370598C186240526 @default.
• W1834370598 hasConceptScore W1834370598C188291805 @default.
• W1834370598 hasConceptScore W1834370598C205649164 @default.
• W1834370598 hasConceptScore W1834370598C26099304 @default.
• W1834370598 hasConceptScore W1834370598C2780518792 @default.
• W1834370598 hasConceptScore W1834370598C53570757 @default.
• W1834370598 hasConceptScore W1834370598C98736793 @default.
• W1834370598 hasLocation W18343705981 @default.
• W1834370598 hasOpenAccess W1834370598 @default.
• W1834370598 hasPrimaryLocation W18343705981 @default.
• W1834370598 hasRelatedWork W1834370598 @default.
• W1834370598 hasRelatedWork W1983794737 @default.
• W1834370598 hasRelatedWork W2346079427 @default.
• W1834370598 hasRelatedWork W2510472800 @default.
• W1834370598 hasRelatedWork W2584017354 @default.
• W1834370598 hasRelatedWork W2993089726 @default.
• W1834370598 hasRelatedWork W3091267361 @default.
• W1834370598 hasRelatedWork W4220723266 @default.
• W1834370598 hasRelatedWork W4296848789 @default.
• W1834370598 hasRelatedWork W4322766563 @default.
• W1834370598 isParatext "false" @default.
• W1834370598 isRetracted "false" @default.
• W1834370598 magId "1834370598" @default.
• W1834370598 workType "book-chapter" @default.