OC Uwakwe, S Riechelmann, R Hoffmann, C Spötl… - Chemical …, 2023 - Elsevier
Cryogenic cave carbonates (CCC) represent a specific type of speleothem precipitating from freezing water in caves. Over the past decade, considerable progress has been made …
Ice caves are one of the least studied parts of the cryosphere, particularly those located in inaccessible permafrost areas at high altitudes or high latitudes. We characterize the climate …
P Töchterle, A Baldo, JB Murton, F Schenk… - Climate of the …, 2024 - cp.copernicus.org
Abstract The Younger Dryas stadial was characterised by a rapid shift towards cold-climate conditions in the North Atlantic realm during the last deglaciation. While some climate …
Cryogenic cave carbonates (CCCs) are a type of speleothem, typically dated with 230 Th/U disequilibrium methods, that provide evidence of palaeo-permafrost conditions. In the field …
Cryogenic cave carbonates (CCCs) genetically related to permafrost are of special interest in paleoclimate research. Their 230 Th/U ages provide unique information about the former …
Abstract The Winter Wonderland ice cave, located at an elevation of 3140 m above sea level in the Uinta Mountains of northern Utah, USA, maintains a constant sub‐zero temperature …
Carbonate minerals formed by the freezing of water in karst caves comprise a unique and special class of speleothems referred to as cryogenic cave carbonates (CCCs). CCCs occur …
Silicate weathering is a natural regulator of atmospheric carbon dioxide (CO2), where the majority of carbonate is stored in the oceans. In some instances, carbonates may form via …
Cryogenic cave carbonates have been described from several formerly or presently glaciated karst caves. In most of these occurrences, they precipitated as loose grains or …