Results 1 to 10 of about 1,261 (178)
Local hydroclimate alters interpretation of speleothem δ 18O records [PDF]
Oxygen isotopes (δ 18O) are the most commonly utilized speleothem proxy and have provided many foundational records of paleoclimate. Thus, understanding processes affecting speleothem δ 18O is crucial.
E. W. Patterson +11 more
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Speleothem Paleoclimatology for the Caribbean, Central America, and North America
Speleothem oxygen isotope records from the Caribbean, Central, and North America reveal climatic controls that include orbital variation, deglacial forcing related to ocean circulation and ice sheet retreat, and the influence of local and remote sea ...
Matthew Lachniet +2 more
exaly +3 more sources
StalGrowth—A Program to Estimate Speleothem Growth Rates and Seasonal Growth Variations
Speleothems are one of the few archives which allow us to reconstruct the terrestrial paleoclimate and help us to understand the important climate dynamics in inhabited regions of our planet.
Rolf Vieten, Francisco Hernandez
doaj +1 more source
Evaluating model outputs using integrated global speleothem records of climate change since the last glacial [PDF]
Although quantitative isotope data from speleothems has been used to evaluate isotope-enabled model simulations, currently no consensus exists regarding the most appropriate methodology through which to achieve this.
L. Comas-Bru +7 more
doaj +1 more source
We present stable carbon (δ13C) and oxygen (δ18O) isotope records from two partially coeval speleothems from Manita peć Cave, Croatia. The cave is located close to the Adriatic coast (3.7 km) at an elevation of 570 m a.s.l. The site experienced competing
Maša Surić +6 more
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Although Last Glacial Maximum (LGM) sea levels have been the focus of much attention in climate and marine sciences, the timing, duration, and magnitude need further research.
Xiaoxiao Yu +6 more
doaj +1 more source
Quantum diamond microscope (QDM) magnetic field imaging is a recently developed technique capable of mapping magnetic field sources in geologic samples at 1 micrometer resolution.
Roger R. Fu +10 more
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Controls on Speleothem Initial 234U/238U Ratios in a Monsoon Climate
Speleothem initial uranium isotope ratios ((234U/238U)i) can be influenced by processes along the seepage water flow‐path including alpha‐recoil into porewater during 238U decay and hostrock weathering, the balance of which can reflect the infiltration ...
Jessica L. Oster +4 more
doaj +1 more source
New online method for water isotope analysis of speleothem fluid inclusions using laser absorption spectroscopy (WS-CRDS) [PDF]
A new online method to analyse water isotopes of speleothem fluid inclusions using a wavelength scanned cavity ring down spectroscopy (WS-CRDS) instrument is presented. This novel technique allows us simultaneously to measure hydrogen and oxygen isotopes
S. Affolter +2 more
doaj +1 more source
Multiscale monsoon variability during the last two climatic cycles revealed by spectral signals in Chinese loess and speleothem records [PDF]
The East Asian Monsoon (EAM) exhibits a significant variability on timescales ranging from tectonic to centennial as inferred from loess, speleothem and marine records.
Y. Li +5 more
doaj +1 more source

