1990
DOI: 10.1080/0028825x.1990.10412315
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Aranuian vegetation history of the Arrowsmith Range, Canterbury I. Pollen diagrams, plant macrofossils, and buried soils from Prospect Hill

Abstract: Two pollen analyses are described from

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Cited by 38 publications
(50 citation statements)
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“…We infer two changes, firstly the invasion of beech into already declining Phyllocladus woodland, and secondly a general opening up of vegetation, with grassland becoming widespread. The former is natural, with similar expansions of Nothofagus forest recorded in many pollen diagrams in Canterbury (Moar 1971;Lintott and Burrows 1973;Russell 1980;Burrows and Russell 1990) and elsewhere in New Zealand. The latter is evidence for human impact, and specifically, European settlement.…”
Section: Zone Interpretationsupporting
confidence: 55%
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“…We infer two changes, firstly the invasion of beech into already declining Phyllocladus woodland, and secondly a general opening up of vegetation, with grassland becoming widespread. The former is natural, with similar expansions of Nothofagus forest recorded in many pollen diagrams in Canterbury (Moar 1971;Lintott and Burrows 1973;Russell 1980;Burrows and Russell 1990) and elsewhere in New Zealand. The latter is evidence for human impact, and specifically, European settlement.…”
Section: Zone Interpretationsupporting
confidence: 55%
“…Vegetation in the lowest zone (ST-1) is characterised by the dominance of shrubs and herbs and is typical of a late-glacial-period pollen record from inland Canterbury (Burrows and Russell 1990). We have no age control in this zone and we cannot discount the alternative possibility that it could be early Holocene in age.…”
Section: Holocene Vegetation History Of Staces Tarn and Lake Heron Areamentioning
confidence: 99%
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