A palynological perspective on the impacts of European contact: historic deforestation, ranching and agriculture surrounding the Cuchumatanes Highlands, Guatemala
A palynological perspective on the impacts of European contact: historic deforestation, ranching and agriculture surrounding the Cuchumatanes Highlands, Guatemala
The Spanish conquest of the Cuchumatanes Highlands (1524–1541 ce) led to dramatic land use changes adhering to colonial practices and values, which included the rearing of livestock, agriculture, timber extraction, mining, and the relocation of indigenous populations to new settlements. These changes are often recorded in historical accounts and official records; however, these are sparse, incomplete, and have been lost over the passage of time. Here, we present a high-resolution palaeoenvironmental reconstruction for Cenote Kail (Guatemala) since the Spanish Conquest, to provide additional evidence of land use changes from an integrated multi-proxy perspective. We analysed: (i) fossil pollen; (ii) macroscopic and microscopic charcoal; and (iii) dung fungal spores (Sporormiella) from a lake sediment core extracted from Cenote Kail in the Cuchumatanes highlands, combining these analyses with remotely sensed satellite data. We reconstructed: (i) forest composition and dynamics; (ii) burning, (iii) fauna abundance, and (iv) agricultural activities. High resolution age-depth modelling was conducted using a combination of 210Pb and 14C dates. The high temporal resolution enabled a novel integrated validation of the charcoal data sets with remotely sensed satellite data and the historical record. Three stages of floral compositional change were discerned from the palynological assemblage data encompassing: (i) the decline of mixed hard wood forests (MHWF), associated with the building of new settlements, agriculture and timber extraction for fuel (1550–1675 ce); (ii) pastoral expansions involving the rearing of livestock (1700–1800 ce); and (iii) the expansions of urban settlements and increasing management of the land (1821–2015 ce). Seed predation is suggested as the dominant factor preventing MHWF from re-establishing in the Cuchumatanes Highlands over the past 500 years. Burning is limited locally and regionally and in line with the modern regime, which suggests that fire has been managed and controlled since European contact.
Anthropogenic impact, Charcoal, Fire, Mountain hard wood forests, Mountain tropical forests, Palaeoecology, Pollen, Spanish conquest, Sporormiella
Harvey, William J.
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Nogué, Sandra
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Stansell, Nathan
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Adolf, Carole
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Long, Peter R.
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Willis, Kathy
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Harvey, William J.
cfae7675-ff4e-4600-af75-53efefcc37bc
Nogué, Sandra
5b464cff-a158-481f-8b7f-647c93d7a034
Stansell, Nathan
b3044f0b-1f4a-49ca-a53e-4b6464d6851b
Adolf, Carole
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Long, Peter R.
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Willis, Kathy
5a442cde-a2dc-4046-be36-c00017fd47db
Harvey, William J., Nogué, Sandra, Stansell, Nathan, Adolf, Carole, Long, Peter R. and Willis, Kathy
(2020)
A palynological perspective on the impacts of European contact: historic deforestation, ranching and agriculture surrounding the Cuchumatanes Highlands, Guatemala.
Vegetation History and Archaeobotany.
(doi:10.1007/s00334-020-00790-2).
Abstract
The Spanish conquest of the Cuchumatanes Highlands (1524–1541 ce) led to dramatic land use changes adhering to colonial practices and values, which included the rearing of livestock, agriculture, timber extraction, mining, and the relocation of indigenous populations to new settlements. These changes are often recorded in historical accounts and official records; however, these are sparse, incomplete, and have been lost over the passage of time. Here, we present a high-resolution palaeoenvironmental reconstruction for Cenote Kail (Guatemala) since the Spanish Conquest, to provide additional evidence of land use changes from an integrated multi-proxy perspective. We analysed: (i) fossil pollen; (ii) macroscopic and microscopic charcoal; and (iii) dung fungal spores (Sporormiella) from a lake sediment core extracted from Cenote Kail in the Cuchumatanes highlands, combining these analyses with remotely sensed satellite data. We reconstructed: (i) forest composition and dynamics; (ii) burning, (iii) fauna abundance, and (iv) agricultural activities. High resolution age-depth modelling was conducted using a combination of 210Pb and 14C dates. The high temporal resolution enabled a novel integrated validation of the charcoal data sets with remotely sensed satellite data and the historical record. Three stages of floral compositional change were discerned from the palynological assemblage data encompassing: (i) the decline of mixed hard wood forests (MHWF), associated with the building of new settlements, agriculture and timber extraction for fuel (1550–1675 ce); (ii) pastoral expansions involving the rearing of livestock (1700–1800 ce); and (iii) the expansions of urban settlements and increasing management of the land (1821–2015 ce). Seed predation is suggested as the dominant factor preventing MHWF from re-establishing in the Cuchumatanes Highlands over the past 500 years. Burning is limited locally and regionally and in line with the modern regime, which suggests that fire has been managed and controlled since European contact.
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Accepted/In Press date: 1 January 2020
e-pub ahead of print date: 28 July 2020
Keywords:
Anthropogenic impact, Charcoal, Fire, Mountain hard wood forests, Mountain tropical forests, Palaeoecology, Pollen, Spanish conquest, Sporormiella
Identifiers
Local EPrints ID: 445298
URI: http://eprints.soton.ac.uk/id/eprint/445298
ISSN: 0939-6314
PURE UUID: 246d64b3-0fbc-4c65-9b55-7c19f10907ef
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Date deposited: 02 Dec 2020 17:30
Last modified: 18 Mar 2024 03:33
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Contributors
Author:
William J. Harvey
Author:
Nathan Stansell
Author:
Carole Adolf
Author:
Peter R. Long
Author:
Kathy Willis
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