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Late Holocene environmental change and the anthropization of the highlands of Santo Antão Island, Cabo Verde
- Source :
- Castilla-Beltran, A, de Nascimento, L, María Fernández-Palacios, J, Fonville, T, Whittaker, R J, Edwards, M & Nogué, S 2019, ' Late Holocene environmental change and the anthropization of the highlands of Santo Antão Island, Cabo Verde ', Palaeogeography, Palaeoclimatology, Palaeoecology-An International Journal for the Geo-Sciences, vol. 524, pp. 101-117 . https://doi.org/10.1016/j.palaeo.2019.03.033
- Publication Year :
- 2019
- Publisher :
- Elsevier, 2019.
-
Abstract
- Cabo Verde was the first tropical archipelago colonized by Europeans. Historians have suggested that the first colonizers initiated archipelago-wide ecosystem degradation, loss of vegetation cover, and erosion. However, the human–environment interactions that led to the archipelago's current environmental status remain poorly understood. Here, we report the first palaeoecological study of past vegetation change and disturbance regimes for Cabo Verde. We present a 2130-yr old sediment sequence from a volcanic caldera (Cova de Paul) located at ~1200 m asl on Santo Antao Island, for which we analyzed fossil pollen, non-pollen palynomorphs (NPPs), charcoal, silica bodies, and grain size distribution. Our analyses do not show evidence of the presence of temperate, tropical or subtropical forests growing on the summits of Santo Antao in pre-human times. The pollen record shows that scrubland and grasslands dominated the highlands and underwent compositional changes ca. 1850 and 1300 cal yr BP. These shifts overlap with erosion phases and are linked to intensified seasonality. Steady rates of sedimentation marked the period 1230 to ca. 350 cal yr BP, but an increase in charcoal concentrations indicate a drying phase. Increases in regional and local fire, peaks of coprophilous fungi and the presence of New World crop pollen (Zea mays) are interpreted as the onset of Portuguese settlement of the highlands after 450 BP. Sustained erosion between ca. 350 and 100 cal yr BP indicate soil degradation, and the pollen record shows the increase in introduced herbaceous taxa (Rosaceae, Centaurea, Verbenaceae) and exotic tree taxa (e.g. Pinus), while shifting abundances of coprophilous fungi indicate changes in land-use. The record shows stabilization of soils in the last century due to recent afforestation of the highlands. Further palaeoecological studies have the potential to provide further detail of the long-term dynamics of Cabo Verde ecosystems and to inform conservation initiatives.
- Subjects :
- 010506 paleontology
Environmental change
010502 geochemistry & geophysics
Oceanography
01 natural sciences
Shrubland
Ecological disturbances
Soil retrogression and degradation
Macaronesia
Coprophilous fungi
Ecology, Evolution, Behavior and Systematics
Holocene
0105 earth and related environmental sciences
Earth-Surface Processes
Islands
geography
Human impacts
geography.geographical_feature_category
biology
Ecology
Landscape change
Paleontology
Palaeoecology
Vegetation
Anthropization
biology.organism_classification
Archipelago
Geology
Subjects
Details
- Language :
- English
- Database :
- OpenAIRE
- Journal :
- Castilla-Beltran, A, de Nascimento, L, María Fernández-Palacios, J, Fonville, T, Whittaker, R J, Edwards, M & Nogué, S 2019, ' Late Holocene environmental change and the anthropization of the highlands of Santo Antão Island, Cabo Verde ', Palaeogeography, Palaeoclimatology, Palaeoecology-An International Journal for the Geo-Sciences, vol. 524, pp. 101-117 . https://doi.org/10.1016/j.palaeo.2019.03.033
- Accession number :
- edsair.doi.dedup.....9f55f858aed95b52206c9dd70c521f31
- Full Text :
- https://doi.org/10.1016/j.palaeo.2019.03.033