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DOI | 10.1016/j.palaeo.2019.109463 |
Climates of the last three interglacials in subtropical eastern Australia inferred from wetland sediment geochemistry | |
Kemp C.W.; Tibby J.; Arnold L.J.; Barr C.; Gadd P.S.; Marshall J.C.; McGregor G.B.; Jacobsen G.E. | |
发表日期 | 2020 |
ISSN | 0031-0182 |
卷号 | 538 |
英文摘要 | Records of Australian climate during Marine Isotope Stages 5 and 7 (130–71 and 243–191 ka) are rare, preventing detailed assessments of long-term climate, drivers and ecological responses across the continent over glacial-interglacial timescales. This study presents a geochemistry-based palaeoclimate record from Fern Gully Lagoon on North Stradbroke Island (also known as Minjerribah) in subtropical eastern Australia, which records climates in MIS 7a–c, MIS 5 and much of the Holocene, in addition to MIS 4 (71–57 ka), and parts of MIS 6, MIS 3 and MIS 2 (191–130, 57–29 and 29–14 ka). Indicators of inorganic sedimentation from a 9.5 m sediment core – focussed on high-resolution estimates of sediment geochemistry supported by x-radiography, inorganic content and magnetic susceptibility – were combined with a chronology consisting of six radiocarbon (14C) and thirteen single-grain optically stimulated luminescence (OSL) ages. Hiatuses occurred at ~178–153 ka, ~36–21 ka and ~7–2 ka and likely result from the wetland drying. Low values of locally sourced aeolian materials indicate a wet MIS 7a–c and early MIS 6 before a relatively dry MIS 5. Inorganic flux during the Holocene was up to four times greater than during MIS 5, consistent with long-term interglacial drying observed in other regions, most notably in central Australia. This study highlights the importance of employing a combination of multiple dating approaches and calibrated geochemical proxies to derive climate reconstructions and to identify depositional complexities in organic-rich wetland records. © 2019 Elsevier B.V. |
英文关键词 | Holocene; MIS 5; MIS 7; North Stradbroke Island; Palaeoclimate; μXRF |
语种 | 英语 |
scopus关键词 | geochemistry; glacial-interglacial cycle; gully erosion; Holocene; interglacial; marine isotope stage; paleoclimate; reconstruction; sediment chemistry; sediment core; X-ray fluorescence; Australia; North Stradbroke Island; Queensland; Filicophyta |
来源期刊 | Palaeogeography, Palaeoclimatology, Palaeoecology
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/150692 |
作者单位 | Geography, Environment and Population, Sprigg Geobiology Centre, University of Adelaide, Australia; School of Physical Science, Environment Institute, Sprigg Geobiology Centre, Institute for Photonics and Advanced Sensing, University of Adelaide, Australia; Australian Nuclear Science and Technology Organisation, Lucas Heights, Australia; Queensland Department of Environment and Science, Brisbane, Australia; Australian Rivers Institute, Griffith University, Brisbane, Australia |
推荐引用方式 GB/T 7714 | Kemp C.W.,Tibby J.,Arnold L.J.,et al. Climates of the last three interglacials in subtropical eastern Australia inferred from wetland sediment geochemistry[J],2020,538. |
APA | Kemp C.W..,Tibby J..,Arnold L.J..,Barr C..,Gadd P.S..,...&Jacobsen G.E..(2020).Climates of the last three interglacials in subtropical eastern Australia inferred from wetland sediment geochemistry.Palaeogeography, Palaeoclimatology, Palaeoecology,538. |
MLA | Kemp C.W.,et al."Climates of the last three interglacials in subtropical eastern Australia inferred from wetland sediment geochemistry".Palaeogeography, Palaeoclimatology, Palaeoecology 538(2020). |
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