2013
DOI: 10.1007/s10933-013-9735-5
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Pollen, phytoliths, arthropods and high-resolution 14C sampling from Rano Kau, Easter Island: evidence for late Quaternary environments, ant (Formicidae) distributions and human activity

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Cited by 42 publications
(44 citation statements)
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“…Additional evidence of human activity in the Kao catchment has been found in the lake shores just beneath Orongo (Figures 4, 7), where pollen, phytolith, and starch analyses of marginal sediment cores have documented relatively intense horticultural activity based on cultigens of Polynesian origin (Horrocks et al, 2012b(Horrocks et al, , 2013(Horrocks et al, , 2016. Unfortunately, sediments had been mixed by human activity, which has prevented the development of a reliable chronological model.…”
Section: The Prehistoric Cultural Shiftmentioning
confidence: 99%
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“…Additional evidence of human activity in the Kao catchment has been found in the lake shores just beneath Orongo (Figures 4, 7), where pollen, phytolith, and starch analyses of marginal sediment cores have documented relatively intense horticultural activity based on cultigens of Polynesian origin (Horrocks et al, 2012b(Horrocks et al, , 2013(Horrocks et al, , 2016. Unfortunately, sediments had been mixed by human activity, which has prevented the development of a reliable chronological model.…”
Section: The Prehistoric Cultural Shiftmentioning
confidence: 99%
“…The more marginal sites have provided composite sequences where the floating mat overlies the bottom sediments, whereas in more central localities, the floating mat and the bottom sediment records are separated by a water column of variable depth, up to ∼10 m. The longest sequences retrieved from the lake are of ∼10 to 20 m depth, and have maximum ages between ∼15 and ∼34 cal kyr BP, respectively (Gossen, 2011;Horrocks et al, 2013). These cores did not reach the bedrock and the total depth of Kao sediments remains unknown.…”
Section: Lake Kao and The New Record The Lake And Its Sedimentsmentioning
confidence: 99%
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“…This has been explained in terms of altitudinal differences in the vegetation cover due to climatic constraints (Flenley and bahn 2003), a hypothesis that has not been confirmed yet. In the Kao basin, the lack of a reliable chronology (butler and Flenley 2010;Horrocks et al 2013) complicates the interpretation, but the record showed the occurrence of two deforestation events, between AD 50 and 100, and AD 1350 and 1800 (butler and Flenley 2010). Spatio-temporal differences in deforestation patterns agree with the apparent heterogeneity in land-use practices documented by archaeological evidence (Stevenson et al 2015).…”
Section: Deforestationmentioning
confidence: 99%
“…Sophora toromiro, era parte del sotobosque de los palmares de Niu (Paschalococos disperta) propuestos por , Flenley et al (1991) Rull et al (2010), Horrocks et al (2013). De acuerdo con lo señalado anteriormente, el hábitat original de esta especie para la data revisada pueda ser catalogado como de bosquetes en el cual su ubicación en el estrato entra en la categoría codominante y tolerante.…”
Section: Comentariosunclassified