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Landscape preservation under post‐European settlement alluvium in the south‐eastern Australian tablelands, inferred from portable OSL reader data
Author(s) -
Portenga Eric W.,
Bishop Paul,
Gore Damian B,
Westaway Kira E
Publication year - 2016
Publication title -
earth surface processes and landforms
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.294
H-Index - 127
eISSN - 1096-9837
pISSN - 0197-9337
DOI - 10.1002/esp.3942
Subject(s) - geology , alluvium , erosion , deposition (geology) , sediment , sedimentary rock , wetland , aeolian processes , fluvial , geomorphology , alluvial plain , hydrology (agriculture) , geochemistry , paleontology , ecology , geotechnical engineering , structural basin , biology
Human land‐use changes leading to widespread erosion and gully incision have been well studied, but the effects that erosion and sediment mixing, which accompany the deposition of post‐(European) settlement alluvium (PSA), have in valley bottoms and wetlands receive considerably less attention. PSA overlying pre‐disturbance swampy meadow (SM) wetland sediments is commonly exposed along incised stream channel gully walls throughout the south‐eastern Australian Tablelands, providing an ideal setting in which to assess and understand better how PSA deposition affects valley bottoms and the wetland environments that often occupy them. Portable optically stimulated luminescence (pOSL) reader data were measured on bulk sediment samples from SM‐PSA stratigraphies at 16 locations throughout the south‐eastern Australian Tablelands to assess the effects of erosion and sediment mixing at the SM‐PSA boundary. Trends of pOSL data with depth at each profile were used in conjunction with visual profile descriptions to identify the stratigraphic boundary between SM and PSA sediment and to infer the degree of valley bottom erosion and sediment mixing during PSA deposition. At most sites, SM sediments experienced minimal, if any, disturbance during PSA deposition, and we refer to these as non‐eroded sites. Many sites, however, experienced a significant degree of erosion and sediment mixing – eroded sites – often corresponding to visually diffuse sedimentary boundaries between the two stratigraphic units. Our findings demonstrate that SM landscapes in the Tablelands can be preserved with minimal disturbance under PSA at non‐eroded sites and are preserved beneath a mixing zone at all eroded sites. Copyright © 2016 John Wiley & Sons, Ltd.