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Reconstructing Holocene vegetation on the island of Gran Canaria before and after human colonization

Reconstructing Holocene vegetation on the island of Gran Canaria before and after human colonization
Reconstructing Holocene vegetation on the island of Gran Canaria before and after human colonization
We provide the first fossil pollen and charcoal analysis from the island of Gran Canaria (Canary Islands). The pollen record obtained from Laguna de Valleseco (870?m a.s.l.) spans the late Holocene (c. 4500–1500 cal. yr BP) and thereby captures the impact of human colonization. During the earliest period, pollen composition resembled contemporary thermophilous communities, with palms (Phoenix canariensis) and junipers (Juniperus cf. turbinata) being the dominant trees, suggesting that these elements were more widespread in the past. Vegetation in Valleseco began to change at around 2300 cal. yr BP, 400?years before the earliest archaeological evidence of human presence in the island (c. 1900 cal. yr BP). Our data show an increased frequency of fires at that time, coinciding with the decline of palms and the increase of grasses, indicating that humans were present and were transforming vegetation, thus showing that the demise of Gran Canaria’s forest began at an early point in the prehistoric occupation of the island. In the following centuries, there were no signs of forest recovery. Pollen from cultivated cereals became significant, implying the introduction of agriculture in the site, by 1800 cal. yr BP. The next shift in vegetation (c. 1600 cal. yr BP) involved the decrease of grasses in favour of shrubs and trees like Morella faya, suggesting that agriculture was abandoned at the site.
canary islands, fire history, human impact, palaeoecology, pollen analysis, thermophilous vegetation
0959-6836
113-125
de Nascimento, L.
3016f252-bdd2-4353-9ac0-0c44474c8456
Nogue, Sandra
5b464cff-a158-481f-8b7f-647c93d7a034
Criado, C.
1342b1d4-61c9-4ddd-b7a0-9fd0d18188c7
Ravazzi, C.
870ab46f-19de-41e3-8355-2fb83787f392
Whittaker, R.J.
4f258757-8168-4a22-9424-d1d4c325d512
Willis, K.J.
b8691dc6-3e4f-413e-8e45-fe91e7cbfd80
Fernandez-Palacios, J.M.
d4008b32-2478-42e4-ae66-1df72b51236b
de Nascimento, L.
3016f252-bdd2-4353-9ac0-0c44474c8456
Nogue, Sandra
5b464cff-a158-481f-8b7f-647c93d7a034
Criado, C.
1342b1d4-61c9-4ddd-b7a0-9fd0d18188c7
Ravazzi, C.
870ab46f-19de-41e3-8355-2fb83787f392
Whittaker, R.J.
4f258757-8168-4a22-9424-d1d4c325d512
Willis, K.J.
b8691dc6-3e4f-413e-8e45-fe91e7cbfd80
Fernandez-Palacios, J.M.
d4008b32-2478-42e4-ae66-1df72b51236b

de Nascimento, L., Nogue, Sandra, Criado, C., Ravazzi, C., Whittaker, R.J., Willis, K.J. and Fernandez-Palacios, J.M. (2016) Reconstructing Holocene vegetation on the island of Gran Canaria before and after human colonization. The Holocene, 26 (1), 113-125. (doi:10.1177/0959683615596836).

Record type: Article

Abstract

We provide the first fossil pollen and charcoal analysis from the island of Gran Canaria (Canary Islands). The pollen record obtained from Laguna de Valleseco (870?m a.s.l.) spans the late Holocene (c. 4500–1500 cal. yr BP) and thereby captures the impact of human colonization. During the earliest period, pollen composition resembled contemporary thermophilous communities, with palms (Phoenix canariensis) and junipers (Juniperus cf. turbinata) being the dominant trees, suggesting that these elements were more widespread in the past. Vegetation in Valleseco began to change at around 2300 cal. yr BP, 400?years before the earliest archaeological evidence of human presence in the island (c. 1900 cal. yr BP). Our data show an increased frequency of fires at that time, coinciding with the decline of palms and the increase of grasses, indicating that humans were present and were transforming vegetation, thus showing that the demise of Gran Canaria’s forest began at an early point in the prehistoric occupation of the island. In the following centuries, there were no signs of forest recovery. Pollen from cultivated cereals became significant, implying the introduction of agriculture in the site, by 1800 cal. yr BP. The next shift in vegetation (c. 1600 cal. yr BP) involved the decrease of grasses in favour of shrubs and trees like Morella faya, suggesting that agriculture was abandoned at the site.

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More information

Accepted/In Press date: 3 June 2015
e-pub ahead of print date: 11 August 2015
Published date: 1 January 2016
Keywords: canary islands, fire history, human impact, palaeoecology, pollen analysis, thermophilous vegetation
Organisations: Palaeoenvironment Laboratory (PLUS)

Identifiers

Local EPrints ID: 383729
URI: http://eprints.soton.ac.uk/id/eprint/383729
ISSN: 0959-6836
PURE UUID: 3e1eb5d3-c8f3-4112-b6be-6b2b7537317e
ORCID for Sandra Nogue: ORCID iD orcid.org/0000-0003-0093-4252

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Date deposited: 24 Nov 2015 17:09
Last modified: 15 Mar 2024 03:53

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Contributors

Author: L. de Nascimento
Author: Sandra Nogue ORCID iD
Author: C. Criado
Author: C. Ravazzi
Author: R.J. Whittaker
Author: K.J. Willis
Author: J.M. Fernandez-Palacios

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