Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/92355
Title: Stalagmites from western Thailand : preliminary investigations and challenges for palaeoenvironmental research
Authors: Chawchai, Sakonvan
Liu, Guangxin
Bissen, Raphael
Jankham, Kampanart
Paisonjumlongsri, Warisa
Kanjanapayont, Pitsanupong
Chutakositkanon, Vichai
Choowong, Montri
Pailoplee, Santi
Wang, Xianfeng
Keywords: Speleothem
DRNTU::Engineering::Environmental engineering
Paleoclimate
Issue Date: 2018
Source: Chawchai, S., Liu, G., Bissen, R., Jankham, K., Paisonjumlongsri, W., Kanjanapayont, P., . . . Wang, X. (2018). Stalagmites from western Thailand : preliminary investigations and challenges for palaeoenvironmental research. Boreas, 47(1), 367-376. doi:10.1111/bor.12299
Series/Report no.: Boreas
Abstract: Locating suitable caves and stalagmites for palaeoenvironmental and palaeoclimatic studies can be challenging. Isotopic geochemical analyses, albeit commonly performed for palaeoclimatic reconstruction, are also time consuming and costly. Therefore, petrographic and non‐destructive morphological studies on speleothems are desirable to facilitate sample selection for further analysis. In this study, 20 caves were surveyed in Ban Rai district, Uthai Thani province in western Thailand. After external physical observations in the field, three stalagmite samples were collected from Tham Nam Cave to test their potential for palaeoclimatic research. Firstly, the stalagmites were scanned by X‐ray computed tomography (CT scanning) and subsequently the CT images were compared with petrographic inspections. Columnar fabrics show the highest density, whereas closed and open dendritic fabrics have medium and the lowest densities, respectively. Layers near the top and bottom of the three stalagmites were dated by U‐Th mass spectrometric techniques. All three samples were deposited between c. 87 and c. 105 ka ago; therefore, they are probably the oldest stalagmites that have been reported so far from mainland Southeast Asia. However, their physical features indicate that all the samples have suffered from postdepositional dissolution, and are unlikely to be suitable for palaeoclimatic research. The internal dissolution feature of stalagmites, however, cannot be identified by visual inspection of uncut samples. We hereby argue that CT images are useful to characterize stalagmite petrography, in particular fabric, porosity and density. Such features can be used to select the ideal plane of a stalagmite for sectioning, to maximize the chances of robust climatic reconstruction.
URI: https://hdl.handle.net/10356/92355
http://hdl.handle.net/10220/48512
ISSN: 0300-9483
DOI: http://dx.doi.org/10.1111/bor.12299
Rights: © 2017 Collegium Boreas. All rights reserved. This paper was published by John Wiley & Sons Ltd in Boreas and is made available with permission of Collegium Boreas.
Fulltext Permission: open
Fulltext Availability: With Fulltext
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