. . . . . . . . "\u0623\u0648\u0627\u062E\u0631 \u0627\u0644\u0639\u0635\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A (\u0645\u0646\u0630 13,000\u201310,000 \u0633\u0646\u0629 \u0645\u0636\u062A)\u060C \u0623\u0648 \u062A\u0627\u0631\u062F\u064A\u062C\u0644\u0627\u0633\u064A\u0627\u0644 \u0647\u0648 \u062A\u0639\u0631\u064A\u0641 \u0623\u0633\u0627\u0633\u064A \u0644\u0628\u062F\u0627\u064A\u0629 \u0627\u0644\u0641\u062A\u0631\u0629 \u0627\u0644\u062F\u0627\u0641\u0626\u0629 \u0627\u0644\u062D\u062F\u064A\u062B\u0629\u060C \u062D\u064A\u062B \u0627\u0631\u062A\u0641\u0639\u062A \u062F\u0631\u062C\u0629 \u062D\u0631\u0627\u0631\u0629 \u0627\u0644\u0645\u0646\u0627\u062E \u0641\u064A \u0646\u0635\u0641 \u0627\u0644\u0623\u0631\u0636 \u0627\u0644\u0634\u0645\u0627\u0644\u064A \u0628\u0634\u0643\u0644 \u0643\u0628\u064A\u0631\u060C \u0645\u0633\u0628\u0628\u0629 \u062A\u0633\u0627\u0631\u0639 \u0639\u0645\u0644\u064A\u0629 \u062A\u0631\u0627\u062C\u0639 \u0627\u0644\u062C\u0644\u064A\u062F \u0627\u0644\u062A\u064A \u062A\u0644\u062A \u0622\u062E\u0631 \u0623\u0642\u0635\u0649 \u062A\u062C\u0644\u062F \u0645\u0646\u0630 25,000\u201313,000 \u0633\u0646\u0629 \u0645\u0636\u062A\u060C \u0641\u064A \u0647\u0630\u0627 \u0627\u0644\u0648\u0642\u062A \u0643\u0627\u0646 \u0627\u0644\u0628\u0634\u0631 \u0642\u062F \u0627\u062C\u0628\u0631\u0648\u0627 \u0641\u064A \u0648\u0642\u062A \u0633\u0627\u0628\u0642 \u0625\u0644\u0649 \u0627\u0644\u0627\u0646\u062A\u0642\u0627\u0644 \u0625\u0644\u0649 \u0645\u0646\u0627\u0637\u0642 \u0644\u062C\u0648\u0621 \u0643\u0646\u062A\u064A\u062C\u0629 \u0644\u0622\u062E\u0631 \u0623\u0642\u0635\u0649 \u062A\u062C\u0644\u062F\u060C \u0648\u0628\u062F\u0623\u0648\u0627 \u062A\u062F\u0631\u064A\u062C\u064A\u064B\u0627 \u0641\u064A \u0625\u0633\u062A\u064A\u0637\u0627\u0646 \u0623\u0648\u0631\u0627\u0633\u064A\u0627 \u0648\u0623\u062E\u064A\u0631\u064B\u0627 \u0627\u0633\u062A\u064A\u0637\u0627\u0646 \u0627\u0644\u0623\u0645\u0631\u064A\u0643\u064A\u062A\u064A\u0646 \u0639\u0628\u0631 \u0628\u064A\u0631\u0646\u062C\u064A\u0627 \u0644\u0623\u0648\u0644 \u0645\u0631\u0629."@ar . . . . . . . "M\u00E0xim Tardiglaciar"@ca . . "1107680546"^^ . . . "En pal\u00E9oclimatologie, le Tardiglaciaire est la derni\u00E8re phase du Pl\u00E9istoc\u00E8ne, pr\u00E9c\u00E9dant l'\u00E9poque actuelle de l'Holoc\u00E8ne. Il correspond \u00E0 l'ultime subdivision de la derni\u00E8re glaciation (dite \u00AB glaciation de W\u00FCrm \u00BB dans les Alpes), durant laquelle le climat se r\u00E9chauffe relativement tout en \u00E9tant marqu\u00E9 par des oscillations froides. Il pr\u00E9c\u00E8de la p\u00E9riode interglaciaire actuelle (aussi appel\u00E9e postglaciaire), globalement chaude, qu'est l'Holoc\u00E8ne."@fr . . . . . . . . . . . . . . . . . . . "Late Glacial Interstadial"@en . . . "En pal\u00E9oclimatologie, le Tardiglaciaire est la derni\u00E8re phase du Pl\u00E9istoc\u00E8ne, pr\u00E9c\u00E9dant l'\u00E9poque actuelle de l'Holoc\u00E8ne. Il correspond \u00E0 l'ultime subdivision de la derni\u00E8re glaciation (dite \u00AB glaciation de W\u00FCrm \u00BB dans les Alpes), durant laquelle le climat se r\u00E9chauffe relativement tout en \u00E9tant marqu\u00E9 par des oscillations froides. Il pr\u00E9c\u00E8de la p\u00E9riode interglaciaire actuelle (aussi appel\u00E9e postglaciaire), globalement chaude, qu'est l'Holoc\u00E8ne. Le Tardiglaciaire commence \u00E0 la fin du dernier maximum glaciaire, vers 18 000 ans AP, et se termine avec la fin de la derni\u00E8re oscillation froide appel\u00E9e Dryas r\u00E9cent, vers 11 700 ans AP, soit vers 9 700 ans av. J.-C. Le Tardiglaciaire englobe le Dryas, correspondant aux trois oscillations froides de la p\u00E9riode."@fr . "The Late Glacial Interstadial (LGI) c. 14,670 to c. 12,890 BP, also called the B\u00F8lling\u2013Aller\u00F8d interstadial, represents the first pronounced warming since the end of the Last Glacial Maximum (LGM). Human populations, which had previously been forced into refuge areas, gradually begin to repopulate the Northern Hemisphere's Eurasian landmass. Evidence for its occurrence stems from two main types of analysis. The first is the use of oxygen isotope stages (OIS) gathered from stratified deep-sea sediment cores. Samples are gathered and measured for change in isotope levels to determine temperature fluctuation for given periods of time. The second is a proxy measurement, the observation of certain reappearing fauna and flora fossils that can survive only in temperate climates, thus indicating warming trends for a given geographic area. Archaeological evidence of settlement and resettlement in certain areas by humans also serves as proxy measurements. Towards the end of OIS 2 in which the Last Glacial Maximum occurs, the deep-sea sediment cores indicate a gradually warming climate, and the reappearance of certain warm-weather flora and fauna remains throughout the Northern Hemisphere correlate with that trend. The Late Glacial Interstadial was followed by a severe decline in temperatures during the Younger Dryas from c. 12,890 to c. 11,650 BP."@en . . "El M\u00E1ximo Tardiglaciar (aprox. 13.000-10.000 a\u00F1os antes del presente) se define principalmente por el calentamiento del clima en el hemisferio norte causando un proceso de desglaciaci\u00F3n acelerado tras el \u00DAltimo M\u00E1ximo Glacial (aprox. 25 000-13 000 a\u00F1os antes del presente).\u200B Es en este momento que las poblaciones humanas, obligadas previamente a buscar zonas de refugio como consecuencia de las condiciones clim\u00E1ticas del \u00DAltimo M\u00E1ximo Glacial, poco a poco empiezan a repoblar la masa continental de Eurasia en el hemisferio norte y eventualmente a poblar, por primera vez, Am\u00E9rica del Norte a trav\u00E9s del estrecho de Bering. La evidencia de la ocurrencia del M\u00E1ximo Tardiglaciar se debe a dos tipos de an\u00E1lisis principales. El primero es el uso de las etapas de is\u00F3topos de ox\u00EDgeno (OIS, por sus siglas en ingl\u00E9s) recolectadas de muestras de sedimentos estratificados de alta mar. Las muestras se recogen y se miden por el cambio en los niveles de is\u00F3topos para determinar la fluctuaci\u00F3n de la temperatura durante per\u00EDodos determinados. El segundo es un estimado basado en la observaci\u00F3n de reaparici\u00F3n de ciertos f\u00F3siles de fauna y flora que s\u00F3lo pueden sobrevivir en climas templados, por lo tanto, que indica las tendencias de calentamiento para una zona geogr\u00E1fica determinada. Evidencias arqueol\u00F3gicas de asentamiento y repoblaciones en ciertas zonas por los seres humanos tambi\u00E9n sirve como una estimaci\u00F3n. Hacia el final del OIS 2 en el que el m\u00E1ximo Tardiglaciar ocurre, los n\u00FAcleos de sedimentos de aguas profundas indican un clima de calentamiento gradual y la reaparici\u00F3n de cierta flora y fauna de clima c\u00E1lido se mantiene en el hemisferio norte y se correlacionan con esta tendencia. Un per\u00EDodo de oscilaci\u00F3n de fr\u00EDo relativamente breve, se refiere como el Dryas Reciente, se detecta durante el OIS 2, tal como puede deducirse de un aumento en el peso del is\u00F3topo.\u200B"@es . . . . "M\u00E1ximo Tardiglaciar"@es . . . . . . . . . "\u0623\u0648\u0627\u062E\u0631 \u0627\u0644\u0639\u0635\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A (\u0645\u0646\u0630 13,000\u201310,000 \u0633\u0646\u0629 \u0645\u0636\u062A)\u060C \u0623\u0648 \u062A\u0627\u0631\u062F\u064A\u062C\u0644\u0627\u0633\u064A\u0627\u0644 \u0647\u0648 \u062A\u0639\u0631\u064A\u0641 \u0623\u0633\u0627\u0633\u064A \u0644\u0628\u062F\u0627\u064A\u0629 \u0627\u0644\u0641\u062A\u0631\u0629 \u0627\u0644\u062F\u0627\u0641\u0626\u0629 \u0627\u0644\u062D\u062F\u064A\u062B\u0629\u060C \u062D\u064A\u062B \u0627\u0631\u062A\u0641\u0639\u062A \u062F\u0631\u062C\u0629 \u062D\u0631\u0627\u0631\u0629 \u0627\u0644\u0645\u0646\u0627\u062E \u0641\u064A \u0646\u0635\u0641 \u0627\u0644\u0623\u0631\u0636 \u0627\u0644\u0634\u0645\u0627\u0644\u064A \u0628\u0634\u0643\u0644 \u0643\u0628\u064A\u0631\u060C \u0645\u0633\u0628\u0628\u0629 \u062A\u0633\u0627\u0631\u0639 \u0639\u0645\u0644\u064A\u0629 \u062A\u0631\u0627\u062C\u0639 \u0627\u0644\u062C\u0644\u064A\u062F \u0627\u0644\u062A\u064A \u062A\u0644\u062A \u0622\u062E\u0631 \u0623\u0642\u0635\u0649 \u062A\u062C\u0644\u062F \u0645\u0646\u0630 25,000\u201313,000 \u0633\u0646\u0629 \u0645\u0636\u062A\u060C \u0641\u064A \u0647\u0630\u0627 \u0627\u0644\u0648\u0642\u062A \u0643\u0627\u0646 \u0627\u0644\u0628\u0634\u0631 \u0642\u062F \u0627\u062C\u0628\u0631\u0648\u0627 \u0641\u064A \u0648\u0642\u062A \u0633\u0627\u0628\u0642 \u0625\u0644\u0649 \u0627\u0644\u0627\u0646\u062A\u0642\u0627\u0644 \u0625\u0644\u0649 \u0645\u0646\u0627\u0637\u0642 \u0644\u062C\u0648\u0621 \u0643\u0646\u062A\u064A\u062C\u0629 \u0644\u0622\u062E\u0631 \u0623\u0642\u0635\u0649 \u062A\u062C\u0644\u062F\u060C \u0648\u0628\u062F\u0623\u0648\u0627 \u062A\u062F\u0631\u064A\u062C\u064A\u064B\u0627 \u0641\u064A \u0625\u0633\u062A\u064A\u0637\u0627\u0646 \u0623\u0648\u0631\u0627\u0633\u064A\u0627 \u0648\u0623\u062E\u064A\u0631\u064B\u0627 \u0627\u0633\u062A\u064A\u0637\u0627\u0646 \u0627\u0644\u0623\u0645\u0631\u064A\u0643\u064A\u062A\u064A\u0646 \u0639\u0628\u0631 \u0628\u064A\u0631\u0646\u062C\u064A\u0627 \u0644\u0623\u0648\u0644 \u0645\u0631\u0629."@ar . . . . . . . . . . . . . . . "El m\u00E0xim tardiglaciar (en angl\u00E8s: Late Glacial Maximum, Late GM) d'aproximadament 13.000-10.000 anys enrere es defineix principalment per l'escalfament dels climes en l'hemisferi nord causat per una accelerada que segueix al Darrer m\u00E0xim glacial (25.000-13.000 anys enrere). Les poblacions humanes van iniciar la repoblaci\u00F3, des dels seus refugis de les zones glaciades abandonades durant el per\u00EDode del darrer m\u00E0xim glacial."@ca . . "18093"^^ . . "Senglacial tid \u00E4r ett ej formaliserat uttryck f\u00F6r tiden fr\u00E5n den begynnande isavsm\u00E4ltningen f\u00F6r cirka 16 000 \u00E5r sedan under slutet av Istiden fram till slutet av Yngre dryas d\u00E5 isranden br\u00F6t upp fr\u00E5n den mellansvenska israndzonen. Den f\u00F6ljs av postglacial tid (holocen) f\u00F6r cirka 12 000 \u00E5r sedan."@sv . . . . . . . "El M\u00E1ximo Tardiglaciar (aprox. 13.000-10.000 a\u00F1os antes del presente) se define principalmente por el calentamiento del clima en el hemisferio norte causando un proceso de desglaciaci\u00F3n acelerado tras el \u00DAltimo M\u00E1ximo Glacial (aprox. 25 000-13 000 a\u00F1os antes del presente).\u200B Es en este momento que las poblaciones humanas, obligadas previamente a buscar zonas de refugio como consecuencia de las condiciones clim\u00E1ticas del \u00DAltimo M\u00E1ximo Glacial, poco a poco empiezan a repoblar la masa continental de Eurasia en el hemisferio norte y eventualmente a poblar, por primera vez, Am\u00E9rica del Norte a trav\u00E9s del estrecho de Bering."@es . . "Tardiglaciaire"@fr . . "9183618"^^ . "Senglacial tid \u00E4r ett ej formaliserat uttryck f\u00F6r tiden fr\u00E5n den begynnande isavsm\u00E4ltningen f\u00F6r cirka 16 000 \u00E5r sedan under slutet av Istiden fram till slutet av Yngre dryas d\u00E5 isranden br\u00F6t upp fr\u00E5n den mellansvenska israndzonen. Den f\u00F6ljs av postglacial tid (holocen) f\u00F6r cirka 12 000 \u00E5r sedan."@sv . . . . . . . . . . . . . . . . . . . . "El m\u00E0xim tardiglaciar (en angl\u00E8s: Late Glacial Maximum, Late GM) d'aproximadament 13.000-10.000 anys enrere es defineix principalment per l'escalfament dels climes en l'hemisferi nord causat per una accelerada que segueix al Darrer m\u00E0xim glacial (25.000-13.000 anys enrere). Les poblacions humanes van iniciar la repoblaci\u00F3, des dels seus refugis de les zones glaciades abandonades durant el per\u00EDode del darrer m\u00E0xim glacial."@ca . . . . . "Senglacial tid"@sv . . . "\u0623\u0648\u0627\u062E\u0631 \u0627\u0644\u0639\u0635\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A"@ar . . . . . . . . . . "The Late Glacial Interstadial (LGI) c. 14,670 to c. 12,890 BP, also called the B\u00F8lling\u2013Aller\u00F8d interstadial, represents the first pronounced warming since the end of the Last Glacial Maximum (LGM). Human populations, which had previously been forced into refuge areas, gradually begin to repopulate the Northern Hemisphere's Eurasian landmass."@en . . .