Speleothem laminae have been postulated to form annually, and this lamina-chronology is widely applied to high-resolution modern and past climate reconstructions. However, this argument has not been directly supported by high resolution dating methods. Here we present contemporary single-lamina (230)Th dating techniques with 2σ precision as good as ±0.5 yr on a laminated stalagmite with density couplets from Xianren Cave, China, that covers the last 300 years. We find that the layers do not always deposit annually. Annual bands can be under- or over-counted by several years during different multi-decadal intervals. The irregular formation of missing and false bands in this example indicates that the assumption of annual speleothem laminae in a climate reconstruction should be approached carefully without a robust absolute-dated chronology.
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http://dx.doi.org/10.1038/srep02633 | DOI Listing |
Proc Natl Acad Sci U S A
December 2024
The Shmunis Family Anthropology Institute, Dan David Center for Human Evolution and Biohistory Research, Faculty of Medical and Health Sciences, Tel Aviv University, Tel Aviv 6997801, Israel.
Sci Rep
January 2021
Department of Earth Sciences, Royal Holloway University of London, Egham, TW20 0EX, Surrey, UK.
Tropical Pacific stalagmites are commonly affected by dating uncertainties because of their low U concentration and/or elevated initial Th content. This poses problems in establishing reliable trends and periodicities for droughts and pluvial episodes in a region vulnerable to climate change. Here we constrain the chronology of a Cook Islands stalagmite using synchrotron µXRF two-dimensional mapping of Sr concentrations coupled with growth laminae optical imaging constrained by in situ monitoring.
View Article and Find Full Text PDFJ Hum Evol
November 2017
Université Toulouse - Jean Jaurès, UMR 5608, Laboratoire TRACES, Maison de la Recherche Bât 26, 5, allée Antonio Machado, 31 058 Toulouse Cedex, France.
Soot marks, witnesses of past human activities, can sometimes be noticed in concretions (speleothem, travertine, carbonated crust, etc.) formed in cavities. We demonstrate here that these deposits, generally ignored in archaeological studies, turned out to be a perfectly suitable material for micro-chronological study of hominin activities in a site.
View Article and Find Full Text PDFMicrosc Microanal
February 2016
1Department of Geology, Faculty of Natural Sciences and Engineering, University of Ljubljana,Aškerčeva 12,SI-1000 Ljubljana,Slovenia.
Micro-scale observations in karst caves help to identify different processes that shaped local morphology. Scanning electron microscopy/energy-dispersive X-ray spectroscopy inspection of speleothems from two karst caves in Slovenia, Predjama and Črna Jama, confirmed the presence of sub-angular to sub-rounded detrital fragments of clay minerals, feldspars, quartz, Fe-oxides/hydroxides, rutile and Nb-rutile, xenotime, kassite, allanite, fluorapatite, epidote, ilmenite, monazite, sphene, and zircon, between 2 and 50 μm across. These occur in porous layers separating calcite laminae in the clayey coating on the layer below the surface of the speleothems, and are also incorporated within actual crystals.
View Article and Find Full Text PDFAstrobiology
October 2015
3 Faculty of Earth and Life Sciences, VU University Amsterdam, Amsterdam, The Netherlands .
The ability to distinguish the features of a chemical sedimentary rock that can only be attributed to biology is a challenge relevant to both geobiology and astrobiology. This study aimed to test criteria for recognizing petrographically the biogenicity of microbially influenced fabrics and fossil microbes in complex Quaternary stalactitic carbonate rocks from Caerwys, UK. We found that the presence of carbonaceous microfossils, fabrics produced by the calcification of microbial filaments, and the asymmetrical development of tufa fabrics due to the more rapid growth of microbially influenced laminations could be recognized as biogenic features.
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