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Cited by 15 publications
(17 citation statements)
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“…Although the stalagmite growth hiatus might have occurred for different reasons we suggest that this was the result of low amounts of water infiltrating into the cave and can be attributed to the existence of small glaciers that occurred in the area and their expansion during the glacial period (Leontaritis et al, 2020). As warm and humid conditions are generally viewed as prerequisites for speleothem growth (Dreybrodt, 1988;Baker and Smart, 1995;Genty et al, 2006;Nehme et al, 2020), inferences about climate can potentially be made from the prescence of speleothem growth hiatuses. Speleothem growth interruptions may also be due to a change in the fluid pathways reaching the cave; while this cannot be ruled out, the fact that ZCG1 recovered and grew throughout the Holocene makes this option less likely.…”
Section: Major Climate Patternsmentioning
confidence: 86%
See 1 more Smart Citation
“…Although the stalagmite growth hiatus might have occurred for different reasons we suggest that this was the result of low amounts of water infiltrating into the cave and can be attributed to the existence of small glaciers that occurred in the area and their expansion during the glacial period (Leontaritis et al, 2020). As warm and humid conditions are generally viewed as prerequisites for speleothem growth (Dreybrodt, 1988;Baker and Smart, 1995;Genty et al, 2006;Nehme et al, 2020), inferences about climate can potentially be made from the prescence of speleothem growth hiatuses. Speleothem growth interruptions may also be due to a change in the fluid pathways reaching the cave; while this cannot be ruled out, the fact that ZCG1 recovered and grew throughout the Holocene makes this option less likely.…”
Section: Major Climate Patternsmentioning
confidence: 86%
“…In particular, the Eemian ( MIS5e) is estimated at 9 -11°C warmer in the east Mediterranean (e.g. Nehme et al, 2020); temperatures this much higher which would have driven the snowline to a much higher altitude compared to the cooler conditions of later glacial/interglacial cycles. These conditions may have extended to the LGM (Styllas et al, 2015;Leontaritis et al, 2020 and references within), until at the LGM termination, the temperature and precipitation regime no longer fulfilled the requirements for glacier preservation.…”
Section: Major Climate Patternsmentioning
confidence: 99%
“…Recent studies have suggested that in-cave evaporation may affect the isotopic composition of speleothem fluid inclusions (Nehme et al, 2020;Weißbach, 2020). A potential climate-related driver of this evaporative fractionation that has not been described previously is temperature-driven ventilation.…”
Section: Climate-related Evaporation Effects On Fluid Inclusion Isotope Values In Larga Cavementioning
confidence: 94%
“…The analysis of speleothem fluid inclusions has been successfully applied worldwide, including tropical locations (Griffiths et al, 2010;Arienzo et al, 2015;Millo et al, 2017;Meckler et al, 2015). Nevertheless, speleothem fluid inclusion records from the Last Glacial Period (c. 115 -11.7 ka) are still sparse, and in many cases, reliable paleo-temperature estimates are challenging (Millo et al, 2017;Demény et al, 2021;Nehme et al, 2020).…”
Section: Introductionmentioning
confidence: 99%
“…In addition, the youngest part of the RP record has been compared with speleothem records from other caves in the Mediterranean region: the Soreq cave and Peqiin cave in Israel (Bar-Matthews et al, 2003), Antro del Corchia cave located in Alpi Apuane karst in Italy (Drysdale et al, 2005) and Pentadactylos cave on Cyprus (Nehme et al, 2020). The noticeable similarities between the shapes of the RP d 18 O and d 13 C records to the Soreq, Peqiin, Antro del Corchia and Pentadactylos records during MIS 5e, which shows the climatic changes across the entire Mediterranean during the last interglacial period.…”
Section: Similarities Of the Rp Record To The Medi And Lr04 Reference Curvesmentioning
confidence: 99%