Zobrazeno 1 - 9
of 9
pro vyhledávání: '"G E Moseley"'
Publikováno v:
Climate of the Past, Vol 20, Pp 1521-1535 (2024)
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 parameters including atmospheric temperature and glacier extent are widely studi
Externí odkaz:
https://doaj.org/article/6f9cbc3cc6e94cfaa45e8965a56d25de
Publikováno v:
Climate of the Past, Vol 19, Pp 1607-1621 (2023)
The investigation of cryogenic cave minerals (CCMs) has developed in recent decades to be a particularly valuable proxy for palaeo-permafrost reconstruction. Due to difficulties, however, in obtaining reliable chronologies with the so-called “fine
Externí odkaz:
https://doaj.org/article/0408f80ad1a44da795578c146221975c
Autor:
P. Töchterle, S. D. Steidle, R. L. Edwards, Y. Dublyansky, C. Spötl, X. Li, J. Gunn, G. E. Moseley
Publikováno v:
Geochronology, Vol 4, Pp 617-627 (2022)
Cryogenic cave carbonates (CCCs) are a type of speleothem, typically dated with 230Th/U disequilibrium methods, that provide evidence of palaeo-permafrost conditions. In the field, CCCs occur as distinct patches of millimetre- to centimetre-sized loo
Externí odkaz:
https://doaj.org/article/92af2640c5a44eb8985ffcd1e2b586ba
Publikováno v:
Geochronology, Vol 3, Pp 49-58 (2021)
Uranium–uranium (234U–238U) disequilibrium dating can determine the age of secondary carbonates over greater time intervals than the well-established 230Th–234U dating method. Yet it is rarely applied due to unknowns in the initial δ234U (δ23
Externí odkaz:
https://doaj.org/article/cf449fbccace4bd7a4b46cc64037493b
Publikováno v:
Weather and Climate Dynamics, Vol 2, Pp 1-17 (2021)
Temperature in northeast Greenland is expected to rise at a faster rate than the global average as a consequence of anthropogenic climate change. Associated with this temperature rise, precipitation is also expected to increase as a result of increas
Externí odkaz:
https://doaj.org/article/0a98ccac15b740068cd696245589b690
Publikováno v:
Climate of the Past, Vol 16, Pp 29-50 (2020)
Sub-orbital-scale climate variability of the last glacial period provides important insights into the rates at which the climate can change state, the mechanisms that drive such changes, and the leads, lags, and synchronicity occurring across differe
Externí odkaz:
https://doaj.org/article/7cf0a0850ddd4e5b8a2f1a3986d2eb59
Publikováno v:
The Cryosphere, Vol 7, Iss 4, Pp 1073-1081 (2013)
Coarse crystalline cryogenic cave carbonates (CCCcoarse) dated to the last glacial period are common in central European caves and provide convincing evidence of palaeo-permafrost during this time. Little is known, however, about the exact nature of
Externí odkaz:
https://doaj.org/article/698b296c9b254ee09423ce979da42467
Publikováno v:
Chemischer Informationsdienst. 3