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Speleology in Kazakhstan

Shakalov on 04 Jul, 2018
Hello everyone!   I pleased to invite you to the official site of Central Asian Karstic-Speleological commission ("Kaspeko")   There, we regularly publish reports about our expeditions, articles and reports on speleotopics, lecture course for instructors, photos etc. ...

New publications on hypogene speleogenesis

Klimchouk on 26 Mar, 2012
Dear Colleagues, This is to draw your attention to several recent publications added to KarstBase, relevant to hypogenic karst/speleogenesis: Corrosion of limestone tablets in sulfidic ground-water: measurements and speleogenetic implications Galdenzi,

The deepest terrestrial animal

Klimchouk on 23 Feb, 2012
A recent publication of Spanish researchers describes the biology of Krubera Cave, including the deepest terrestrial animal ever found: Jordana, Rafael; Baquero, Enrique; Reboleira, Sofía and Sendra, Alberto. ...

Caves - landscapes without light

akop on 05 Feb, 2012
Exhibition dedicated to caves is taking place in the Vienna Natural History Museum   The exhibition at the Natural History Museum presents the surprising variety of caves and cave formations such as stalactites and various crystals. ...

Did you know?

That solution notch is these form wherever humic soil borders on a very steep or vertical limestone surface. the rock becomes undercut by water rich in biogenic co2. in the cone karst of the humid tropics, foot caves occur which are over-sized enlargements of solution notches [3].?

Checkout all 2699 terms in the KarstBase Glossary of Karst and Cave Terms

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Browse Speleogenesis Issues:

KarstBase a bibliography database in karst and cave science.

Featured articles from Cave & Karst Science Journals
Chemistry and Karst, White, William B.
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Featured articles from other Geoscience Journals
Karst environment, Culver D.C.
Mushroom Speleothems: Stromatolites That Formed in the Absence of Phototrophs, Bontognali, Tomaso R.R.; D’Angeli Ilenia M.; Tisato, Nicola; Vasconcelos, Crisogono; Bernasconi, Stefano M.; Gonzales, Esteban R. G.; De Waele, Jo
Calculating flux to predict future cave radon concentrations, Rowberry, Matt; Marti, Xavi; Frontera, Carlos; Van De Wiel, Marco; Briestensky, Milos
Microbial mediation of complex subterranean mineral structures, Tirato, Nicola; Torriano, Stefano F.F;, Monteux, Sylvain; Sauro, Francesco; De Waele, Jo; Lavagna, Maria Luisa; D’Angeli, Ilenia Maria; Chailloux, Daniel; Renda, Michel; Eglinton, Timothy I.; Bontognali, Tomaso Renzo Rezio
Evidence of a plate-wide tectonic pressure pulse provided by extensometric monitoring in the Balkan Mountains (Bulgaria), Briestensky, Milos; Rowberry, Matt; Stemberk, Josef; Stefanov, Petar; Vozar, Jozef; Sebela, Stanka; Petro, Lubomir; Bella, Pavel; Gaal, Ludovit; Ormukov, Cholponbek;
See all featured articles from other geoscience journals

Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, Vol 237, Issue 2, p. 483-507
A 164 ka record of environmental change in the American Southwest from a Carlsbad Cavern speleothem

A horizontal core 2.8 m in length drilled from the Georgia Giant column in Carlsbad Cavern provides climate information for the last 164 ka. Forty-six alpha spectrometric U-series ages determined at intervals of ∼7.6 cm along the core indicate five periods of deposition and five hiatuses, the longest from 136 to 110 ka. Variations in growth rate (0 to 70 mm/ka), in the abundance of aragonite, chalcedony, and Fe-bearing phases, and in 13C indicate that glacial intervals of the last 164 ka, OIS 6, 4, and 2, were much wetter than today, as were the colder substages 5d and 5b of OIS 5. By contrast, during the two warmest periods of the past 164 ka, namely OIS 5e and 1, there was no deposition on either side of the speleothem, suggesting conditions as dry or drier than today. The record from Carlsbad parallels data from many other sites in the southwestern USA and northern Mexico, and data from marine sediments and ice cores, demonstrating the extent to which ice sheet fluctuations influenced conditions in southern New Mexico. Detailed correlation of δ13C values in the Georgia Giant, which range from −6.6 to +0.9‰ relative to PDB, with distant speleothem records and with data from ice cores, further documents the linkage of southwestern climate with global-scale extent of glaciation. Values of δ18O in the Georgia Giant core range from −9.7 to −4.7‰ relative to PDB and average −6.6‰. 18O-depleted carbonate in the Georgia Giant during OIS 6, at a time when the world's oceans were enriched in 18O, suggests that precipitation during cold intervals was brought largely by Pacific air masses in fall, winter and spring as a result of the southward displacement of the polar jet stream by the growth of the Laurentide Ice Sheet. Termination II, marking the end of the penultimate glaciation, is well defined in the core's δ18O data. Analytical uncertainties in the radiometric ages do not preclude a start of Termination II as late as 128 ka, as suggested by SPECMAP data. However, data from the Georgia Giant core are more compatible with an earlier start like that obtained from Devils Hole and Vostok data, raising the possibility that early warming was widespread in the U.S. southwest region by 145 ka.