2006
DOI: 10.1016/j.palaeo.2005.09.009
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Geochemical changes recorded in Lynch's Crater, Northeastern Australia, over the past 50 ka

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Cited by 20 publications
(10 citation statements)
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“…9) and may be a product of different conditions between each catchment, or their respective age models. Nevertheless, the mechanism influencing precipitation across the catchments is likely regional, possibly linked to the Antarctic Cold Reversal (Barr et al, 2017), or ENSO because geographically separate climate records across the Australian continent also indicate a change towards more positive moisture balance during the deglacial phase (Turney et al, 2006b; Williams et al, 2009; Petherick et al, 2013).…”
Section: Discusssionmentioning
confidence: 99%
“…9) and may be a product of different conditions between each catchment, or their respective age models. Nevertheless, the mechanism influencing precipitation across the catchments is likely regional, possibly linked to the Antarctic Cold Reversal (Barr et al, 2017), or ENSO because geographically separate climate records across the Australian continent also indicate a change towards more positive moisture balance during the deglacial phase (Turney et al, 2006b; Williams et al, 2009; Petherick et al, 2013).…”
Section: Discusssionmentioning
confidence: 99%
“…The LGM globally is considered to have occurred between 27 and 19 ka (Clark et al, 2009). For Australia the timing of the LGM was defined to have started later; it centred on~21 ka (Suggate, 1990) and lasted 3-4 ka (Bowler, 1976;Harrison, 1993;Barrows et al, 2001), or occurred from 23 to 18 cal ka BP (Kershaw, 1986;D'Costa et al, 1989;Turney et al, 2006) and was characterized by limited glacial advances in the Snowy Mountains and Tasmanian Highlands. Both of these regions recorded a maximum glacier extent at~19 ka.…”
Section: -18 Ka Last Glacial Maximummentioning
confidence: 99%
“…The disparity between palaeo-records on both regional and hemispheric scales highlights the need for further high resolution terrestrial palaeoenvironmental records for the Southern Hemisphere, particularly for periods of major and rapid change such as the LGM. With specific reference to eastern Australia, the Atherton Tablelands (tropical northern Queensland: Kershaw, 1976Kershaw, , 1994Haberle, 2005;Turney et al, 2006), Ulungra Springs (New South Wales: Dodson and Wright, 1989), Redhead Lagoon (eastern New South Wales: Williams et al, 2006) and Barrington Tops (New South Wales: Dodson et al, 1986;Sweller and Martin, 2001) have provided long records of palaeoenvironmental variability. However, there are few comparable records geographically between these sites, with records from subtropical Australia being rare.…”
Section: Introductionmentioning
confidence: 99%