A plant microfossil record of Late Quaternary environments and human activity from Rano Aroi and surroundings, Easter Island

Springer Science and Business Media LLC - Tập 54 - Trang 279-303 - 2015
M. Horrocks1,2, W. T. Baisden3, M. A. Harper4, M. Marra5, J. Flenley6, D. Feek6, S. Haoa-Cardinali7, E. D. Keller3, L. González Nualart7, T. Edmunds Gorman7
1Microfossil Research Ltd, Auckland, New Zealand
2School of Environment, University of Auckland, Auckland, New Zealand
3National Isotope Centre, GNS Science, Lower Hutt, New Zealand
4School of Geography, Environment and Earth Sciences, Victoria University of Wellington, Wellington, New Zealand
5University of Waikato, Hamilton, New Zealand.
6Institute of Natural Resources, Massey University, Palmerston North, New Zealand
7Hanga Roa, Chile

Tóm tắt

To investigate past vegetation change and human activity at the highest elevations on Easter Island, this study examines pollen, phytoliths, diatoms, starch and arthropods preserved in sediment/soil profiles from Rano Aroi crater, and another, newly described wetland in the adjacent, much smaller Rano Aroi Iti depression. A Bayesian age–depth model for Rano Aroi provides adequate certainty for the Late Pleistocene and last ~1000 years, but is poorly constrained from 12,000 to 1000 cal BP. The occurrence of cf. Potamogeton and Lycopodium pollen types at this highland site (~425 m altitude), while absent or rare at lowland sites, could well be related to the cooler higher altitude conditions. Smaller quantities of Arecaceae (palm) pollen than at lowland sites indicate that this relatively high-altitude part of the island was near the altitudinal forest limit in the Late Pleistocene, with extensive Asteraceae-dominated shrubland. Arecaceae forest dominated the Holocene, for which there is evidence for a prolonged dry phase. The subsequent disappearance of charcoal and reappearance of diatoms, particularly Eunotia cf. pectinalis, suggest that the dry phase ended prior to human settlement. Polynesian activity is best constrained by abundant microscopic charcoal fragments beginning in a layer at 710 (2σ: 645–797) cal BP, and suggesting a period of forest clearance and burning, culminating at 339 (2σ: 177–428) cal BP. Thinner soils compared with lowland horticultural sites and 14C dates of macroscopic Sophora charcoal suggest that the site was occupied after 1670 CE. Newly described terraces, and pollen, phytoliths and starch of cf. Broussonetia papyrifera (paper mulberry), cf. Colocasia esculenta (taro) and Musa (banana) sp. identified in this study show the value of a combined microfossil approach and provide evidence for extension of cultivation of these Polynesian-introduced cultigens to this least accessible part of the island. Rano Aroi Iti yielded a Bayesian 14C age–depth chronology to a basal age of 1530–1314 cal BP, giving an unexpectedly old age for presumably introduced New World pollen of Sisyrinchium, which occurs throughout the core.

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