Please use this identifier to cite or link to this item: https://apo.ansto.gov.au/dspace/handle/10238/10921
Title: Climates of the last three interglacials in subtropical eastern Australia inferred from wetland sediment geochemistry
Authors: Kemp, CW
Tibby, J
Arnold, LJ
Barr, C
Gadd, PS
Marshall, JC
McGregor, GB
Jacobsen, GE
Keywords: X-ray fluorescence analysis
Geochemistry
Climates
Wetlands
Sediments
Quaternary period
Islands
Queensland
Australia
Issue Date: 15-Jan-2020
Publisher: Elsevier
Citation: Kemp, C. W., Tibby, J., Arnold, L. J., Barr, C., Gadd, P. S., Marshall, J. C., McGregor, G. B. & Jacobsen, G. E. (2020). Climates of the last three interglacials in subtropical eastern Australia inferred from wetland sediment geochemistry. Palaeogeography, Palaeoclimatology, Palaeoecology, 538, 109463. doi:10.1016/j.palaeo.2019.109463
Abstract: 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. © 2020 Elsevier B.V
URI: https://doi.org/10.1016/j.palaeo.2019.109463
https://apo.ansto.gov.au/dspace/handle/10238/10921
ISSN: 0031-0182
Appears in Collections:Journal Articles

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