Maize and ancient maya droughts

The ancient Maya culture of Mesoamerica shaped landscapes for centuries, in an area where maize (Zea mays) cultivation is considered a fundamental crop in the diet of present and ancient Mesoamerican cultures. Pollen records from sites with different environmental and climatic conditions of the Yucatán Peninsula (Mexico) and Peten (Guatemala) evidence a clear relationship between increased maize pollen and periods of reduced precipitation caused by El Niño Southern Oscillation (ENSO) while moist periods are characterized by low maize pollen presence. ENSO conditions were not evenly distributed across the Yucatán Peninsula, and regional droughts vary according to regional climate and geographical conditions. Our results indicate a strong relationship of increased maize and tropical forest decrease with dry periods, while the Late Preclassic Humid Period (ca. 500–200 BCE) is characterized by the absence of maize pollen. The dry Late Preclassic (300 BCE‑250 CE) was a key period for increased maize production, suggesting a new conceptualization of maize. Maize changed from a basic diet crop to a pragmatic product to face adverse environmental conditions.

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Main Authors: Islebe, Gerald A. Doctor autor 2046, Torrescano Valle, Nuria Doctora autora 8666, Valdéz Hernández, Mirna Doctora autora 12329, Carrillo Bastos, Alicia autora 12821, Aragón Moreno, Alejandro Antonio Doctor autor 12817
Format: Texto biblioteca
Language:eng
Subjects:Maíz, Sequía, El Niño oscilación del Sur, Mayas, Palinología, Cambio de uso de la tierra, Artfrosur,
Online Access:https://doi.org/10.1038/s41598-022-26761-3
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id KOHA-OAI-ECOSUR:63285
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spelling KOHA-OAI-ECOSUR:632852024-03-12T12:41:24ZMaize and ancient maya droughts Islebe, Gerald A. Doctor autor 2046 Torrescano Valle, Nuria Doctora autora 8666 Valdéz Hernández, Mirna Doctora autora 12329 Carrillo Bastos, Alicia autora 12821 Aragón Moreno, Alejandro Antonio Doctor autor 12817 textengThe ancient Maya culture of Mesoamerica shaped landscapes for centuries, in an area where maize (Zea mays) cultivation is considered a fundamental crop in the diet of present and ancient Mesoamerican cultures. Pollen records from sites with different environmental and climatic conditions of the Yucatán Peninsula (Mexico) and Peten (Guatemala) evidence a clear relationship between increased maize pollen and periods of reduced precipitation caused by El Niño Southern Oscillation (ENSO) while moist periods are characterized by low maize pollen presence. ENSO conditions were not evenly distributed across the Yucatán Peninsula, and regional droughts vary according to regional climate and geographical conditions. Our results indicate a strong relationship of increased maize and tropical forest decrease with dry periods, while the Late Preclassic Humid Period (ca. 500–200 BCE) is characterized by the absence of maize pollen. The dry Late Preclassic (300 BCE‑250 CE) was a key period for increased maize production, suggesting a new conceptualization of maize. Maize changed from a basic diet crop to a pragmatic product to face adverse environmental conditions.The ancient Maya culture of Mesoamerica shaped landscapes for centuries, in an area where maize (Zea mays) cultivation is considered a fundamental crop in the diet of present and ancient Mesoamerican cultures. Pollen records from sites with different environmental and climatic conditions of the Yucatán Peninsula (Mexico) and Peten (Guatemala) evidence a clear relationship between increased maize pollen and periods of reduced precipitation caused by El Niño Southern Oscillation (ENSO) while moist periods are characterized by low maize pollen presence. ENSO conditions were not evenly distributed across the Yucatán Peninsula, and regional droughts vary according to regional climate and geographical conditions. Our results indicate a strong relationship of increased maize and tropical forest decrease with dry periods, while the Late Preclassic Humid Period (ca. 500–200 BCE) is characterized by the absence of maize pollen. The dry Late Preclassic (300 BCE‑250 CE) was a key period for increased maize production, suggesting a new conceptualization of maize. Maize changed from a basic diet crop to a pragmatic product to face adverse environmental conditions.MaízSequíaEl Niño oscilación del SurMayasPalinologíaCambio de uso de la tierraArtfrosurScientific Reportshttps://doi.org/10.1038/s41598-022-26761-3Acceso en línea sin restricciones
institution ECOSUR
collection Koha
country México
countrycode MX
component Bibliográfico
access En linea
En linea
databasecode cat-ecosur
tag biblioteca
region America del Norte
libraryname Sistema de Información Bibliotecario de ECOSUR (SIBE)
language eng
topic Maíz
Sequía
El Niño oscilación del Sur
Mayas
Palinología
Cambio de uso de la tierra
Artfrosur
Maíz
Sequía
El Niño oscilación del Sur
Mayas
Palinología
Cambio de uso de la tierra
Artfrosur
spellingShingle Maíz
Sequía
El Niño oscilación del Sur
Mayas
Palinología
Cambio de uso de la tierra
Artfrosur
Maíz
Sequía
El Niño oscilación del Sur
Mayas
Palinología
Cambio de uso de la tierra
Artfrosur
Islebe, Gerald A. Doctor autor 2046
Torrescano Valle, Nuria Doctora autora 8666
Valdéz Hernández, Mirna Doctora autora 12329
Carrillo Bastos, Alicia autora 12821
Aragón Moreno, Alejandro Antonio Doctor autor 12817
Maize and ancient maya droughts
description The ancient Maya culture of Mesoamerica shaped landscapes for centuries, in an area where maize (Zea mays) cultivation is considered a fundamental crop in the diet of present and ancient Mesoamerican cultures. Pollen records from sites with different environmental and climatic conditions of the Yucatán Peninsula (Mexico) and Peten (Guatemala) evidence a clear relationship between increased maize pollen and periods of reduced precipitation caused by El Niño Southern Oscillation (ENSO) while moist periods are characterized by low maize pollen presence. ENSO conditions were not evenly distributed across the Yucatán Peninsula, and regional droughts vary according to regional climate and geographical conditions. Our results indicate a strong relationship of increased maize and tropical forest decrease with dry periods, while the Late Preclassic Humid Period (ca. 500–200 BCE) is characterized by the absence of maize pollen. The dry Late Preclassic (300 BCE‑250 CE) was a key period for increased maize production, suggesting a new conceptualization of maize. Maize changed from a basic diet crop to a pragmatic product to face adverse environmental conditions.
format Texto
topic_facet Maíz
Sequía
El Niño oscilación del Sur
Mayas
Palinología
Cambio de uso de la tierra
Artfrosur
author Islebe, Gerald A. Doctor autor 2046
Torrescano Valle, Nuria Doctora autora 8666
Valdéz Hernández, Mirna Doctora autora 12329
Carrillo Bastos, Alicia autora 12821
Aragón Moreno, Alejandro Antonio Doctor autor 12817
author_facet Islebe, Gerald A. Doctor autor 2046
Torrescano Valle, Nuria Doctora autora 8666
Valdéz Hernández, Mirna Doctora autora 12329
Carrillo Bastos, Alicia autora 12821
Aragón Moreno, Alejandro Antonio Doctor autor 12817
author_sort Islebe, Gerald A. Doctor autor 2046
title Maize and ancient maya droughts
title_short Maize and ancient maya droughts
title_full Maize and ancient maya droughts
title_fullStr Maize and ancient maya droughts
title_full_unstemmed Maize and ancient maya droughts
title_sort maize and ancient maya droughts
url https://doi.org/10.1038/s41598-022-26761-3
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