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dc.contributor.authorLeplongeon, Alice-
dc.contributor.authorBen Arous, Eslem-
dc.contributor.authorMesfin, Isis-
dc.contributor.authorForestier, Hubert-
dc.contributor.authorGallet, Xavier-
dc.contributor.authorGriggo, Cristophe-
dc.contributor.authorPuaud, Simon-
dc.contributor.authorSémah, Anne-Marie-
dc.contributor.authorVialou, Agueda-
dc.contributor.authorPleurdeau, David-
dc.contributor.authorLourdeau, Antoine-
dc.date.accessioned2025-09-
dc.date.accessioned2025-09-30T11:40:49Z-
dc.date.issued2025-09-
dc.identifier.citationJournal of World Prehistory, 38(2), 7es_ES
dc.identifier.urihttps://cir.cenieh.es/handle/20.500.12136/3518-
dc.description.abstractThe world at 18,000 BP, published by Gamble and Soffer (The world at 18,000 BP. Vol. 2: low latitude, Unwin Hyman, 1990), represents the first, and so far the only, attempt at characterising and discussing the impact of the Last Glacial Maximum (LGM) on human societies on a global scale. At the time, they highlighted that research and data on the LGM in southern latitudes and the tropics in particular were scant. Since 1990, however, many sites dated to the LGM and located in tropical latitudes have been published. Many paradigms have changed regarding the peopling of the Americas, which allows the archaeology of this continent to be integrated into global scale studies of the LGM. The development of Pleistocene archaeology in tropical contexts, in parallel with methodological advances in cultural, geosciences and palaeoenvironmental studies have strongly reshaped what we know of the antiquity of human occupation in tropical regions and specific human–environment interactions. This article provides for the first time a pan-tropical perspective on the impact of the LGM on human groups living within the tropical latitudes, drawing from case studies in Southeast Asia, Africa and South America, specifically regions which have up until now never been discussed together. To this end, we focus on six different tropical regions between 30 and 10 ka. We present the archaeological and paleoenvironmental data available in these areas, along with proposed relationships for variations in these two records. Finally, we discuss at the regional scale the presence or absence of human changes (site density and techno-cultural change or continuity) before, during and immediately after the LGM.es_ES
dc.language.isoenes_ES
dc.publisherSpringer Naturees_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rightsAtribución 4.0 Internacional*
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/*
dc.subjectLast Glacial Maximumes_ES
dc.subjectTropicses_ES
dc.subjectHuman evolutiones_ES
dc.subjectHuman– environment interactionses_ES
dc.titleThe Last Glacial Maximum in the Tropics: Human Responses to Global Change, 30–10 kaes_ES
dc.typeArticlees_ES
dc.identifier.doi10.1007/s10963-025-09197-1-
dc.relation.publisherversionhttps://doi.org/10.1007/s10963-025-09197-1es_ES
dc.date.available2025-09-30T11:40:49Z-
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