LATE-QUATERNARY VEGETATION
; LAST GLACIAL CYCLE
; SOUTH CHINA SEA
; WESTERN TASMANIA
; LATE PLEISTOCENE
; CLIMATE-CHANGE
; HUMID TROPICS
; NEW-ZEALAND
; MARINE
; TERRESTRIAL
WOS学科分类:
Geosciences, Multidisciplinary
WOS研究方向:
Geology
英文摘要:
Long, well-dated records of climate change in Australia are rare because most of the continent is prone to deflation and sediments are difficult to date beyond 40 ka. Deep-sea cores, containing terrigenous material, provide an ideal alternative to terrestrial records, because of continuous sedimentation and a robust chronology derived from oxygen isotopes. In this paper, the first of a series of two, we present pollen and spores data from core Fr1/94-GC3 from the East Tasman Plateau. This core is positioned at the southern extreme of the East Australia Current and simultaneously records changes in both oceanography and environments both offshore and in southeastern Australia. In an area of slow sedimentation, this core provides a continuous record of vegetation change in southeastern Australia and the southern Tasman Sea over approximately the last half a million years. Through time, glacial periods have progressively become warmer and shorter. Alpine plant taxa become more restricted with time and rainforest taxa expand to a far more restricted degree during the present interglacial period than the previous one, representing a fundamental shift in the vegetation of Tasmania. We apply transfer functions to reconstruct past rainfall and land temperatures based on the palynoflora that are then compared against the marine proxy record.
1.Australian Natl Univ, Res Sch Earth Sci, Acton, ACT 2601, Australia 2.Monash Univ, Sch Earth Atmosphere & Environm, Clayton, Vic 3800, Australia 3.Vrije Univ, Fac Earth & Life Sci, Cluster Earth Climate, NL-1081 HV Amsterdam, Netherlands 4.Australian Natl Univ, Coll Asia & Pacific, Dept Archaeol & Nat Hist, Acton, ACT 2601, Australia
Recommended Citation:
De Deckker, P.,van der Kaars, S.,Macphail, M. K.,et al. Land-sea correlations in the Australian region: 460 ka of changes recorded in a deep-sea core offshore Tasmania. Part 1: the pollen record[J]. AUSTRALIAN JOURNAL OF EARTH SCIENCES,2019-01-01,66(1):1-15