Climate impact on the development of Pre-Classic Maya civilisation
The impact of climate change on the development and disintegration of Maya civilisation has long been debated. The lack of agreement among existing palaeoclimatic records from the region has prevented a detailed understanding of regional-scale climatic variability, its climatic forcing mechanisms an...
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European Geosciences Union
2018
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ftunnottinghamrr:oai:nottingham-repository.worktribe.com:1070377 2023-05-15T17:31:07+02:00 Climate impact on the development of Pre-Classic Maya civilisation Nooren, Kees Hoek, Wim Z. Dermody, Brian J. Galop, Didier Metcalfe, Sarah Islebe, Gerald Middelkoop, Hans 2018-08-20 https://doi.org/10.5194/cp-14-1253-2018 https://nottingham-repository.worktribe.com/file/1070377/1/Climate%20impact%20on%20the%20development%20of%20Pre-Classic%20Maya%20civilisation unknown European Geosciences Union Climate of the Past Volume 14 Issue 8 Pagination 1253-1273 doi:https://doi.org/10.5194/cp-14-1253-2018 https://nottingham-repository.worktribe.com/file/1070377/1/Climate%20impact%20on%20the%20development%20of%20Pre-Classic%20Maya%20civilisation 1814-9324 doi:10.5194/cp-14-1253-2018 openAccess http://creativecommons.org/licenses/by/4.0/ CC-BY Stratigraphy Palaeontology Global and Planetary Change Journal Article 2018 ftunnottinghamrr https://doi.org/10.5194/cp-14-1253-2018 2022-10-13T22:11:45Z The impact of climate change on the development and disintegration of Maya civilisation has long been debated. The lack of agreement among existing palaeoclimatic records from the region has prevented a detailed understanding of regional-scale climatic variability, its climatic forcing mechanisms and its impact on the ancient Maya. We present two new palaeo-precipitation records for the central Maya lowlands, spanning the Pre-Classic period (1800BCE–250CE), a key epoch in the development of Maya civilisation. A beach ridge elevation record from world's largest late Holocene beach ridge plain provides a regional picture, while Lake Tuspan's diatom record is indicative of precipitation changes at a local scale. We identify centennial-scale variability in palaeo-precipitation that significantly correlates with the North Atlantic δ14C atmospheric record, with a comparable periodicity of approximately 500 years, indicating an important role of North Atlantic atmospheric–oceanic forcing on precipitation in the central Maya lowlands. Our results show that the Early Pre-Classic period was characterised by relatively dry conditions, shifting to wetter conditions during the Middle Pre-Classic period, around the well-known 850BCE (2.8ka) event. We propose that this wet period may have been unfavourable for agricultural intensification in the central Maya lowlands, explaining the relatively delayed development of Maya civilisation in this area. A return to relatively drier conditions during the Late Pre-Classic period coincides with rapid agricultural intensification in the region and the establishment of major cities. Article in Journal/Newspaper North Atlantic University of Nottingham: Repository@Nottingham Climate of the Past 14 8 1253 1273 |
institution |
Open Polar |
collection |
University of Nottingham: Repository@Nottingham |
op_collection_id |
ftunnottinghamrr |
language |
unknown |
topic |
Stratigraphy Palaeontology Global and Planetary Change |
spellingShingle |
Stratigraphy Palaeontology Global and Planetary Change Nooren, Kees Hoek, Wim Z. Dermody, Brian J. Galop, Didier Metcalfe, Sarah Islebe, Gerald Middelkoop, Hans Climate impact on the development of Pre-Classic Maya civilisation |
topic_facet |
Stratigraphy Palaeontology Global and Planetary Change |
description |
The impact of climate change on the development and disintegration of Maya civilisation has long been debated. The lack of agreement among existing palaeoclimatic records from the region has prevented a detailed understanding of regional-scale climatic variability, its climatic forcing mechanisms and its impact on the ancient Maya. We present two new palaeo-precipitation records for the central Maya lowlands, spanning the Pre-Classic period (1800BCE–250CE), a key epoch in the development of Maya civilisation. A beach ridge elevation record from world's largest late Holocene beach ridge plain provides a regional picture, while Lake Tuspan's diatom record is indicative of precipitation changes at a local scale. We identify centennial-scale variability in palaeo-precipitation that significantly correlates with the North Atlantic δ14C atmospheric record, with a comparable periodicity of approximately 500 years, indicating an important role of North Atlantic atmospheric–oceanic forcing on precipitation in the central Maya lowlands. Our results show that the Early Pre-Classic period was characterised by relatively dry conditions, shifting to wetter conditions during the Middle Pre-Classic period, around the well-known 850BCE (2.8ka) event. We propose that this wet period may have been unfavourable for agricultural intensification in the central Maya lowlands, explaining the relatively delayed development of Maya civilisation in this area. A return to relatively drier conditions during the Late Pre-Classic period coincides with rapid agricultural intensification in the region and the establishment of major cities. |
format |
Article in Journal/Newspaper |
author |
Nooren, Kees Hoek, Wim Z. Dermody, Brian J. Galop, Didier Metcalfe, Sarah Islebe, Gerald Middelkoop, Hans |
author_facet |
Nooren, Kees Hoek, Wim Z. Dermody, Brian J. Galop, Didier Metcalfe, Sarah Islebe, Gerald Middelkoop, Hans |
author_sort |
Nooren, Kees |
title |
Climate impact on the development of Pre-Classic Maya civilisation |
title_short |
Climate impact on the development of Pre-Classic Maya civilisation |
title_full |
Climate impact on the development of Pre-Classic Maya civilisation |
title_fullStr |
Climate impact on the development of Pre-Classic Maya civilisation |
title_full_unstemmed |
Climate impact on the development of Pre-Classic Maya civilisation |
title_sort |
climate impact on the development of pre-classic maya civilisation |
publisher |
European Geosciences Union |
publishDate |
2018 |
url |
https://doi.org/10.5194/cp-14-1253-2018 https://nottingham-repository.worktribe.com/file/1070377/1/Climate%20impact%20on%20the%20development%20of%20Pre-Classic%20Maya%20civilisation |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
Climate of the Past Volume 14 Issue 8 Pagination 1253-1273 doi:https://doi.org/10.5194/cp-14-1253-2018 https://nottingham-repository.worktribe.com/file/1070377/1/Climate%20impact%20on%20the%20development%20of%20Pre-Classic%20Maya%20civilisation 1814-9324 doi:10.5194/cp-14-1253-2018 |
op_rights |
openAccess http://creativecommons.org/licenses/by/4.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/cp-14-1253-2018 |
container_title |
Climate of the Past |
container_volume |
14 |
container_issue |
8 |
container_start_page |
1253 |
op_container_end_page |
1273 |
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1766128444016427008 |