Luminescence signals of quartz and feldspar minerals are widely used to determine the burial age of Quaternary sediments. Although luminescence signals bleach rapidly with sunlight exposure, incomplete bleaching may affect luminescence ages, in particular in fluvial settings where an unbleached remnant signal is commonly encountered in modern alluvium. Here, we use feldspar single-grain post-infrared IR stimulation (pIRIR) dating to show that recent (<11 ka) fluvial terraces of the Rangitikei River (New Zealand) were formed in a context of non-linear incision rate. We relate this pattern to the rapid reinstatement of steady-state incision following the formation of a major, climate-driven, aggradation terrace, causing a phase of accelerated...
ESR dating of fluvial terraces is usually based on the assumption of sunlight resetting of the Al ce...
Post-infrared (pIR) stimulated luminescence dating of sedimentary feldspar largely avoids the effect...
Optically Stimulated Luminescence (OSL) dating allows age determination of sediments deposited durin...
Luminescence signals of quartz and feldspar minerals are widely used to determine the burial age of ...
International audienceAge overestimation is common when dating fluvial deposits using feldspar-based...
Single-grain post-infrared infrared stimulated luminescence (SG-pIRIR) of feldspar has recently been...
International audienceEnlightenment of sediments pathways and storage patterns within river systems ...
International audienceThe Rangitikei River is actively downcutting in an uplifting Plio-Pleistocene ...
International audienceLandscape response to climate induces periods of enhanced sedimentsupply to ri...
New Zealand is a key location for investigating the geomorphic response of fluvial systems over glac...
Quartz is the preferred dosimeter for luminescence dating of Holocene sediments as optically stimula...
Studies of modern sediments, their sedimentology and depositional processes are important for unders...
Fluvial deposits and landforms are important archives of river response to climate, tectonics and ba...
There is limited knowledge about the preservation of aggradation phases in Quaternary fluvial record...
ESR dating of fluvial terraces is usually based on the assumption of sunlight resetting of the Al ce...
Post-infrared (pIR) stimulated luminescence dating of sedimentary feldspar largely avoids the effect...
Optically Stimulated Luminescence (OSL) dating allows age determination of sediments deposited durin...
Luminescence signals of quartz and feldspar minerals are widely used to determine the burial age of ...
International audienceAge overestimation is common when dating fluvial deposits using feldspar-based...
Single-grain post-infrared infrared stimulated luminescence (SG-pIRIR) of feldspar has recently been...
International audienceEnlightenment of sediments pathways and storage patterns within river systems ...
International audienceThe Rangitikei River is actively downcutting in an uplifting Plio-Pleistocene ...
International audienceLandscape response to climate induces periods of enhanced sedimentsupply to ri...
New Zealand is a key location for investigating the geomorphic response of fluvial systems over glac...
Quartz is the preferred dosimeter for luminescence dating of Holocene sediments as optically stimula...
Studies of modern sediments, their sedimentology and depositional processes are important for unders...
Fluvial deposits and landforms are important archives of river response to climate, tectonics and ba...
There is limited knowledge about the preservation of aggradation phases in Quaternary fluvial record...
ESR dating of fluvial terraces is usually based on the assumption of sunlight resetting of the Al ce...
Post-infrared (pIR) stimulated luminescence dating of sedimentary feldspar largely avoids the effect...
Optically Stimulated Luminescence (OSL) dating allows age determination of sediments deposited durin...