Severe Little Ice Age drought in the midcontinental United States during the Mississippian abandonment of Cahokia

Abstract Drought has long been suspected as playing an important role in the abandonment of pre-Columbian Native American settlements across the midcontinental United States between 1350 and 1450 CE. However, high-resolution paleoclimatic reconstructions reflecting local effective moisture (the rati...

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Autores principales: David P. Pompeani, Broxton W. Bird, Jeremy J. Wilson, William P. Gilhooly, Aubrey L. Hillman, Matthew S. Finkenbinder, Mark B. Abbott
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Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/39436fef3ca14f6ea0e21e73ec7f6263
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spelling oai:doaj.org-article:39436fef3ca14f6ea0e21e73ec7f62632021-12-02T15:23:16ZSevere Little Ice Age drought in the midcontinental United States during the Mississippian abandonment of Cahokia10.1038/s41598-021-92900-x2045-2322https://doaj.org/article/39436fef3ca14f6ea0e21e73ec7f62632021-07-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-92900-xhttps://doaj.org/toc/2045-2322Abstract Drought has long been suspected as playing an important role in the abandonment of pre-Columbian Native American settlements across the midcontinental United States between 1350 and 1450 CE. However, high-resolution paleoclimatic reconstructions reflecting local effective moisture (the ratio of precipitation to evaporation) that are located in proximity to Mississippi period (1050–1450 CE) population centers are lacking. Here, we present a 1600-year-long decadally resolved oxygen isotope (δ18O) record from Horseshoe Lake (Collinsville, IL), an evaporatively influenced oxbow lake that is centrally located within the largest and mostly densely populated series of Mississippian settlements known as Greater Cahokia. A shift to higher δ18O in the Horseshoe Lake sediment record from 1200 to 1400 CE indicates that strongly evaporative conditions (i.e., low effective moisture) were persistent during the leadup to Cahokia’s abandonment. These results support the hypothesis that climate, and drought specifically, strongly impacted agriculturally based pre-Columbian Native American cultures in the midcontinental US and highlights the susceptibility of this region, presently a global food production center, to hydroclimate extremes.David P. PompeaniBroxton W. BirdJeremy J. WilsonWilliam P. GilhoolyAubrey L. HillmanMatthew S. FinkenbinderMark B. AbbottNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-8 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
David P. Pompeani
Broxton W. Bird
Jeremy J. Wilson
William P. Gilhooly
Aubrey L. Hillman
Matthew S. Finkenbinder
Mark B. Abbott
Severe Little Ice Age drought in the midcontinental United States during the Mississippian abandonment of Cahokia
description Abstract Drought has long been suspected as playing an important role in the abandonment of pre-Columbian Native American settlements across the midcontinental United States between 1350 and 1450 CE. However, high-resolution paleoclimatic reconstructions reflecting local effective moisture (the ratio of precipitation to evaporation) that are located in proximity to Mississippi period (1050–1450 CE) population centers are lacking. Here, we present a 1600-year-long decadally resolved oxygen isotope (δ18O) record from Horseshoe Lake (Collinsville, IL), an evaporatively influenced oxbow lake that is centrally located within the largest and mostly densely populated series of Mississippian settlements known as Greater Cahokia. A shift to higher δ18O in the Horseshoe Lake sediment record from 1200 to 1400 CE indicates that strongly evaporative conditions (i.e., low effective moisture) were persistent during the leadup to Cahokia’s abandonment. These results support the hypothesis that climate, and drought specifically, strongly impacted agriculturally based pre-Columbian Native American cultures in the midcontinental US and highlights the susceptibility of this region, presently a global food production center, to hydroclimate extremes.
format article
author David P. Pompeani
Broxton W. Bird
Jeremy J. Wilson
William P. Gilhooly
Aubrey L. Hillman
Matthew S. Finkenbinder
Mark B. Abbott
author_facet David P. Pompeani
Broxton W. Bird
Jeremy J. Wilson
William P. Gilhooly
Aubrey L. Hillman
Matthew S. Finkenbinder
Mark B. Abbott
author_sort David P. Pompeani
title Severe Little Ice Age drought in the midcontinental United States during the Mississippian abandonment of Cahokia
title_short Severe Little Ice Age drought in the midcontinental United States during the Mississippian abandonment of Cahokia
title_full Severe Little Ice Age drought in the midcontinental United States during the Mississippian abandonment of Cahokia
title_fullStr Severe Little Ice Age drought in the midcontinental United States during the Mississippian abandonment of Cahokia
title_full_unstemmed Severe Little Ice Age drought in the midcontinental United States during the Mississippian abandonment of Cahokia
title_sort severe little ice age drought in the midcontinental united states during the mississippian abandonment of cahokia
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/39436fef3ca14f6ea0e21e73ec7f6263
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