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1. Heterogenous Late Holocene Climate in the Eastern Mediterranean—The Kocain Cave Record From SW Turkey

   https://doi.org/10.1029/2021GL094733  

   Jacobson, Matthew J. ; Flohr, Pascal ; Gascoigne, Alison ; Leng, Melanie J. ; Sadekov, Aleksey ; Cheng, Hai ; Edwards, R. Lawrence ; Tüysüz, Okan ; Fleitmann, Dominik ( October 2021 , Geophysical Research Letters)
2. Climate change, resilience, and the Native American Fisher-hunter-gatherers of the late Holocene on the Georgia coast, USA

   https://doi.org/10.1016/j.quaint.2020.08.030  

   Ritchison, Brandon T. ; Thompson, Victor D. ; Lulewicz, Isabelle ; Tucker, Bryan ; Turck, John A. ( May 2021 , Quaternary International)
3. Hydrological and thermodynamic controls on late Holocene gypsum formation by mixing saline groundwater and Dead Sea brine

   https://doi.org/10.1016/j.gca.2021.10.002  

   Weber, Nurit ; Antler, Gilad ; Lazar, Boaz ; Stein, Mordechai ; Yechieli, Yoseph ; Gavrieli, Ittai ( January 2022 , Geochimica et Cosmochimica Acta)
4. Late Pleistocene and Early Holocene aeolian deposits of Tasmania and their climatic implications

   https://doi.org/10.1017/qua.2020.83  

   McIntosh, Peter D. ; Neudorf, Christina ; Lian, Olav B. ; Slee, Adrian J. ; Walker, Brianna ; Eberhard, Rolan ; Doyle, Richard ; Dixon, Grant ( July 2021 , Quaternary Research)

   Abstract Late Pleistocene and Early Holocene aeolian deposits in Tasmania are extensive in the present subhumid climate zone but also occur in areas receiving >1000 mm of rain annually. Thermoluminescence, optically stimulated luminescence, and radiocarbon ages indicate that most of the deposits formed during periods of cold climate. Some dunes are remnants of longitudinal desert dunes sourced from now-inundated continental shelves which were previously semi-arid. Others formed near source, often in the form of lunettes east of seasonally-dry lagoons in the previously semi-arid Midlands and southeast of Tasmania, or as accumulations close to floodplains of major rivers, or as sandsheets in exposed areas. Burning of vegetation by the Aboriginal population after 40 ka is likely to have influenced sediment supply. A key site for determining climate variability in southern Tasmania is Maynes Junction which records three periods of aeolian deposition (at ca. 90, 32 and 20 ka), interspersed with periods of hillslope instability. Whether wind speeds were higher than at present during the last glacial period is uncertain, but shells in the Mary Ann Bay sandsheet near Hobart and particle size analysis of the Ainslie dunes in northeast Tasmania suggest stronger winds during the last glacial period than at present. 

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5. Tectonic, hydrogeologic, and climatic controls on Late Holocene dune formation, China Lake basin, Indian Wells Valley, California, USA

   https://doi.org/10.1017/qua.2021.62  

   Lancaster, Nicholas ; Bacon, Steven N. ; Bullard, Thomas F. ; Neudorf, Christina M. ; Keen-Zebert, Amanda K. ; Decker, David L. ; Boggs, Matthew L. ( March 2022 , Quaternary Research)

   Abstract Analysis of patterns of faulting and hydrogeology, stratigraphic and sedimentologic studies, and luminescence dating of aeolian deposits in China Lake basin provide new perspectives on the origins and development of Late Holocene dunes and sand ramps in the seismically active Indian Wells Valley of eastern California. Aeolian dune and sand sheet deposits were sourced from alluvial material derived from granitic rocks of the south-eastern Sierra Nevada and are concentrated in areas with sand-stabilizing phreatophyte vegetation influenced by high groundwater levels along the active oblique-normal Little Lake and Paxton Ranch faults, which locally form barriers to groundwater flow. Three episodes of sand accumulation are recognized (2.1 ± 0.1 to 2.0 ± 0.1 ka, 1.8 ± 0.2 to 1.6 ± 0.2 ka, and 1.2 ± 0.1 to 0.9 ± 0.1 ka) during conditions in which sediment supplied to the basin during periods of enhanced rainfall and runoff was subsequently reworked by wind into dunes and sand ramps at the transition to more arid periods. Understanding the role tectonics plays in influencing the hydrogeology of seismically active lake basins provides insights to accurately interpret landscape evolution and any inferences made on past hydroclimate variability in a region. 

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