Browsing by Author "Dortch, J"

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    Pleistocene occupation of Yellabidde Cave in the northern Swan Coastal Plain, southwestern Australia
    (Taylor and Francis Online, 2016-11-03) Monks, C; Dortch, J; Jacobsen, GE; Baynes, A
    Evidence for human occupation of Western Australia’s northern Swan Coastal Plain derives mainly from Holocene coastal midden sites. Here, we present preliminary results from archaeological investigations at Yellabidde Cave, located 9 km inland from the present coast. Excavations in the limestone cave’s sandy floor deposit revealed cultural and palaeontological materials dating from c. 25,500 cal. BP to the 19th C. These provide the first evidence for Pleistocene occupation in the region, indicating that Yellabidde Cave was intermittently occupied throughout the late Pleistocene and Holocene, and reflecting dynamic human-environment relationships in present near-coastal to littoral environments.
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    The timing of deglaciation from mountain summits to cirques in Wales: 10Be and 26Al exposure dates from Cadair Idris
    (Copernicus GmbH, 2021-04-19) Hughes, PD; Glasser, NF; Fink, D; Dortch, J; Fülöp, RH; Wilcken, KM; Fujioka, T
    Cosmogenic 10Be and 26Al exposure ages from 20 erratic samples collected from Cadair Idris (893 m), a mountain in southern Snowdonia, Wales, provide evidence for the timing of deglaciation from summits to cirques at the end of the Late Pleistocene. The summit of the mountain is characterised by intensely modified frost-shattered surfaces that have long been identified as a representing a former nunatak. Numerous glacially-transported quartz boulders on the highest ground indicate that ice overran the summit at some point in the Pleistocene. Two quartz boulders, one with preserved striations, sampled at c. 856 m near the summit of Cadair Idris yielded consistent 10Be and 26Al paired exposure ages of 75 ka to 60 ka (using anuhigh-latitude sea level 10Be spallation production rate of 4.20 at/g/y, scaled by the Lal/Stone scheme). A glacially polished bedrock quartzite outcrop at 735 m gave an age of 17.5 ka. Immediately below this, cirque and down-valley recessional moraine ages, covering an elevation of 480 m to 350 m ranged from 10 to 15 ka respectively. These results confirm that Cadair Idris was overridden by the Welsh Ice Cap during marine isotope stage (MIS) 4, when ice was thicker than at the global last glacial maximum (LGM) in MIS 2. This is consistent with findings from northern Snowdonia. The highest Welsh summits, including Cadair Idris, emerged above a thinning Welsh Ice Cap (British Irish Ice Sheet) during the transition from MIS 4 to 3. The summit area above ~800 m then stood as nunataks above the LGM ice sheet surface in MIS 2. The Welsh Ice Cap then rapidly thinned over Cadair Idris at ~20-17 ka based on ages from high-level ice-moulded bedrockThis is supported by more new ages from high-level paired erratics and bedrock samples on several other mountains throughout Snowdonia, leading to a phase of alpine-style deglaciation. Valley glaciers initiated their retreat up-valley from ~17 to 14 ka after Heinrich Event 1. A later phase of glacier stabilisation or still stand formation produced classic cirque moraines near the rim of a present cirque lake basin (480 m elevation) yielding 10Be ages of 13-10 ka during the Younger Dryas.