Aranuian vegetation history of the Arrowsmith Range, Canterbury, New Zealand. III: Vegetation changes in the Cameron, upper South Ashburton, and Paddle Hill Creek catchments
Aranuian vegetation history of the Arrowsmith Range, Canterbury, New Zealand. III: Vegetation changes in the Cameron, upper South Ashburton, and Paddle Hill Creek catchments
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新西兰坎特伯雷阿罗史密斯山脉的阿诺努亚植被历史。
DOI：
10.1080/0028825x.1993.10419491
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发表时间：
1993
影响因子：
0.9
通讯作者：
B. Butterfield
中科院分区：
文献类型：
--
作者：
C. Burrows;P. Randall;N. Moar;B. Butterfield
摘要：根据阿罗史密斯山脉 (Arrowsmith Range) 中三个高地山谷的植被历史，通过对阿兰纽亚时期定期沉积的埋藏植物残骸和泥炭的花粉和大化石分析，推断出它们的植被历史。这些证据还得到了来自土壤中年代久远的木炭层和地表原木的信息、现代花粉雨的知识以及木本植物区系目前的组成和分布的补充。植被历史是根据冰川前进和后退以及冲积时期来解释的。没有重建早期阿兰努纪（距今 14 000-10 000 年）植被的直接数据，尽管它可能主要是草本植物。从阿兰纽纪中期（距今 10000-6000 年）开始，Phyllocladus alpinus 占据了主导地位。这种情况一直持续到阿兰努纪晚期（距今 6000-0 年）。在阿兰努纪中期的后期，罗汉松很常见，几乎可以肯定存在着罗汉松，以及各种血管...
Abstract The vegetation history of three upland valleys in the Arrowsmith Range is deduced from pollen and macrofossil analysis of buried plant debris and peat, deposited at intervals through the Aranuian period. The evidence is supplemented by information from dated charcoal layers in the soils and from surface logs, knowledge of the modern pollen rain, and the present composition and distribution of the woody plant flora. The vegetation history is interpreted in the light of episodes of glacial advance and retreat and periods of alluviation. There are no direct data for reconstruction of early Aranuian (c. 14 000–10 000 yr B.P.) vegetation although probably it was mainly herbaceous. From the beginning of the middle Aranuian (10 000–6000 yr B.P.) Phyllocladus alpinus assumed dominance. This lasted until very late in the late Aranuian (6000–0 yr B.P.). In the latter part of the middle Aranuian, Podocarpus hallii was common and Prumnopitys taxifolia was almost certainly present, together with various angio...
影响因子：
8.3
作者：
M. Stuiver;G. Pearson
通讯作者：
M. Stuiver;G. Pearson