DOI: 10.1016/j.quascirev.2017.06.018
Scopus记录号: 2-s2.0-85021659039
论文题名: A Last Interglacial pollen-temperature reconstruction, central North Island, New Zealand
作者: Newnham R. ; Alloway B. ; McGlone M. ; Juchnowicz H. ; Rees A. ; Wilmshurst J.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2017
卷: 170 起始页码: 136
结束页码: 151
语种: 英语
英文关键词: Last Interglacial
; Pollen
; Temperature reconstruction
; Tephra
; Volcanic impact
Scopus关键词: Climatology
; Deforestation
; Least squares approximations
; Repair
; Vegetation
; Volcanoes
; Last interglacial
; Pollen
; Temperature reconstruction
; Tephra
; Volcanic impacts
; Atmospheric temperature
; air temperature
; ash flow
; calibration
; climate oscillation
; Last Interglacial
; marine isotope stage
; palynology
; plant community
; reconstruction
; tephra
; vegetation cover
; Manawatu-Wanganui
; Mount Tongariro
; New Zealand
; North Island
; Bacillariophyta
英文摘要: We present new pollen-temperature reconstructions for the Last Interglacial from central North Island, New Zealand using partial least squares regression (PLS) and modern analogue technique applied with the New Zealand pre-deforestation calibration pollen dataset. The pollen-bearing organic sequence includes numerous millimetre- to decimetre- thick tephra mostly from the adjacent Tongariro Volcanic Centre and is overlain by tephric cover-beds including the c. 25.4 ka cal BP Kawakawa/Oruanui Tephra. Fine-resolution pollen and preliminary diatom analyses above and below prominent tephra layers showed that significant vegetation impact followed only the thickest ashfall event (22 cm thickness), with vegetation recovery taking several hundred years. Apart from this, changes in the longer-term pollen record are likely to be related to climate oscillations that resemble the classic five-fold subdivision of MIS 5. The warmest interval, ascribed to MIS 5e, was characterised by tall, temperate rainforest, and occurs at the base of the sequence, with mean annual temperatures reaching around 1.1 °C higher than present. Mean annual temperatures declined to ∼4 °C below present during MIS 5d and MIS 5b and were within 1–2 °C of present during MIS 5c. The PLS temperature reconstructions are corroborated by estimates derived independently from elevational changes to vegetation communities, corresponding to modern temperature controls, inferred from the Karioi pollen spectra. Temperatures reconstructed quantitatively by the modern analogue technique were up to 1.3 °C higher for MIS 5e, MIS 5d and MIS 5b, possibly reflecting weaker modern vegetation analogues for these intervals. © 2017 Elsevier Ltd Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/59154
Appears in Collections: 过去全球变化的重建
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作者单位: School of Geography, Environment and Earth Sciences, Victoria University of Wellington, PO Box 600, Wellington, New Zealand; School of Environment, University of Auckland, Private Bag 92019, Auckland, New Zealand; Centre for Archaeological Science (CAS), School of Earth and Environmental Sciences, University of Wollongong, Wollongong, NSW, Australia; Landcare Research, Lincoln, New Zealand
Recommended Citation:
Newnham R.,Alloway B.,McGlone M.,et al. A Last Interglacial pollen-temperature reconstruction, central North Island, New Zealand[J]. Quaternary Science Reviews,2017-01-01,170