TAK-Online
Contents and Abstracts
TAK Reviews
Tenu, A. & Davidescu, F. Environmental isotopic studies in karstic calcareous areas of Romania. pp. 9�24.
The application of the environmental isotope techniques in the study of karstic areas might offer significant contributions concerning the origin and genesis of the groundwaters, underground hydrodynamic parameters and vulnerability to pollution.
After a brief theoretical approach the results obtained by these techniques for Oradea�Felix hydrogeothermal system, Wallachian Platform, Domogled hydrostructure and South Dobrogea, are synthetically presented.
TAK Articles
Lauritzen, S.-E. & Onac, B., P. Uranium series dating of some speleothems from Romania. pp. 25�36.
In order to test the potential for Uranium-series disequilibrium dating of speleothems in Romania, nine dating analyses were performed on eight samples from various caves in Apuseni Mountains and Dobrogea. Low to moderate uranium concentrations, good chemical yields, and few samples with significant 232Th contamination, provided reliable data in most cases. The dates range between 22 kyr up to 188 kyr, which is in general accordance with speleotheme chronozones known from other areas, and with known periods of ameliorated climates during the upper Pleistocene. These preliminary dates also provide erosion rate estimates for fluvial valley incision of 0.5 to 0.6 m/kyr in the Crisul Repede basin. Attempts to date a hominid footprint from V�rtop Glacier cave, suggest so far a maximum age of about 22 kyr.
Hercman, H., Lauritzen, S.-E. & Glazek, J. Uranium-series dating of speleothems from Nied?wiedzia and Radochowska caves, Sudetes (Poland). pp. 37�48.
14 new uranium series dates were performed on speleothem samples from Nied?wiedzia (Bear Cave) and Radochowska caves in the Polish Sudetes, and are presented together with other two previous dates. All samples were low in uranium concentration, inducing relatively large errors in the dates. The oldest date from Nied?wiedzia cave (180, +21/�17 ka) provides strong evidence for the antiquity of the cave and for the fact that the cave was drained above the watertable as early as oxygen isotope stage 7. Dating of flowstone above the bone-bearing deposits in Nied?wiedzia cave has so far been unsuccessful, and the deposits still provide an interesting geochronological challenge.
Martin, P. Les travertins sont-ils les d�p�ts corr�latifs d�hydrosyst�mes karstiques ? Le cas des bassins versants proven�aux (France). pp. 49�62.
Des �tudes r�centes faites en Provence sur des �difices travertineux nous ont conduit � envisager ces constructions comme des syst�mes et � proposer l�id�e de syst�me travertineux.
Ces syst�mes travertineux re�oivent en particulier des flux modul�s par des r�seaux de drainage (r�seaux souterrains, r�seaux fluviatiles) exportateurs de mati�re et perturbent la r�alisation d�un profil longitudinal d��quilibre dynamique. En cons�quence il semble que l��volution d�un aquif�re d�un �tat non?karstifie � un �tat karstifi� puisse conduire au recoupement puis � la disparition du syst�me travertineux qui lui est associ�.
La description de ces relations entre syst�mes exportateurs d�amont et syst�mes accumulateurs d�aval nous conduit � qualifier cette association de g�osyst�me karstique. Le syst�me travertineux est r�gul� par les interactions existant entre ses sous-syst�mes (barrage�vasque; flux�bioc�nose) et par le fonctionnement et l��volution des r�seaux de drainage exportateurs de mati�re. Le g�osyst�me karstique est r�gul� � un niveau sup�rieur par le syst�me morphoclimatique, par la g�odynamique interne et par la soci�t�.
Onac, B., P., Ghergari, L. & G�l, A. Crystallographical studies on gypsum crystals in Ponoras Cave (Padurea Craiului Mountains,Romania). pp. 63�68.
About 200 gypsum crystals formed within a black clay deposit in Ponoras cave were analyzed with respect to their crystallographical features. The most developed faces are those of pinacoid and prism. Plotting the number of crystallographical forms per crystal against the frequency of combinations we found a bi-model curve characterizing two generations of gypsum crystals that have been grown in different conditions.
Istvan, D., Manescu, S. & Jurca, M. Study on moonmilk from Pestera Mare, Piatra Molosnaia (Repedea, Maramures Mountains, Romania). pp. 69�74.
The moonmilk was investigated by using a complex study, including complete chemical analysis, spectral analysis, X-ray diffraction, thermal analysis and other chemical analyses.
The purpose was to analyze the water content, the way it is eliminated and to identify the factors which favor this unusual capacity to retain the water.
The analyzed moonmilk has a calcite character (about 80% is crystallized calcite) with a significant presence of aluminium silicate gel (clay gel).
The water retaining capacity is due to both the porous network of anhydrous calcite in the moonmilk, and the retaining capacity of the clay gel. The clay gel is probably an exokarstic waste product originating in the levigation of the soil that covers the limestones. The analyzed moonmilk is a recent product deposited quasi-synchronously with its sampling.
Onac, B., P., Bengeanu, M., Botez, M. & Zih, J. Preliminary report on the mineralogy of Pestera din Valea Rea. pp. 75�80.
From a mineralogical point of view, Pestera din Valea Rea presents a great interest. Gypsum is unique in what concerns its type of occurrence and abundance. Gypsum speleothems (flower, crystal, rope, snow, hair, cotton, crust and stalagmite) from Pestera din Valea Rea exhibit features never described before in a Romanian cave. The most typical speleothems are those consisting of gypsum, anhydrite and celestite, yet some may include carbonate minerals (calcite, aragonite, magnesite, hydromagnesite, dolomite, rhodochrosite, malachite) and phosphates (brushite, barrandite, bobierrite, vivianite, wavellite). Quartz, periclase, kaolinite, dickite, nacrite and illite have also been identified in various speleothems.
Silvestru, E., Tamas, T. & Fratila, G. Preliminary data on the hydrogeology of karst terrains around the springs of Somesul Cald river (Bihor-Vladeasa Montains, Romania). pp. 81�90.
Six karst drainages have been investigated in the western section of the Somesul Cald Graben. Both fluoresceine tracings and pH, temperature and conductivity measurements have been performed. The resulting data provided the grounds for delimiting of subterranean hydrographic basins and for several considerations concerning karstogenesis in the area.
Constantinescu, T. Le karst de type Movil� (Mangalia, Dobrogea de Sud, Roumanie). pp. 91�96.
L'interaction de 4 facteurs g�osyst�miques principaux (la circulation des eaux souterraines thermomin�rales, la pr�sence des calcaires lumachelliques et oolithiques sarmatiens, le climat aride et la morphologie de plateau bas situ� au voisinage de la Mer Noire), a d�termin� le d�veloppement d'un karst � part. Afin de souligner son originalit�, l'auteur consid�re que la d�nomination �karst de type Movil� est la plus opportune.
Mogosanu, D. Cretaceous paleokarst in the Moesian Platform (Romania). pp. 97�102.
The sedimentary cover of the Moesian Platform is divided into four major cycles of sedimentation, separated by three major unconformities. These unconformities correspond to emersion periods of the Moesian domain, during which the exogene factors altered the earth crust, which resulted in a topography specific to each geological period. As the Early Cretaceous deposits of the platform are mostly carbonate, the resulting topography is of karstic type. This assertion is supported by information provided by drillholes.
Martin, P. Les formes fluviatiles du massif karstique de la Sainte Baume (Bouches du Rh�ne, Var, France). pp. 103�116.
La Sainte Baume est le massif de la Basse Provence carbonat�e o� le karst est le mieux d�velopp�: 180 cavit�s dont l'aven du Petit St Cassien (�321 m et 9,3 km), le r�seau Sabre (4,3 km) et la grotte de la Castelette (grande salle de 4150 m2). En surface des r�seaux fluviatiles drainent ce massif.
Pour v�rifier si l'existence de r�seaux souterrains d�sorganise le drainage superficiel, on r�alise une analyse morphologique des bassins versants: dimension fractale des p�rim�tres, mod�lisation des talwegs principaux par une double exponentielle, �tude de la relation entre la surface du bassin versant et la longueur du talweg principal, d�termination des relations de Horton et calcul de la dimension fractale du r�seau du Caramy par diff�rentes m�thodes.
Cette analyse montre que les formes fluviatiles du massif de la Sainte Baume sont tr�s classiques et capables d'assurer un drainage autonome en surface. La r�alisation d'un drainage souterrain ne d�sorganise donc pas le drainage superficiel.
Nous pensons que cette situation n'est pas un �tat exceptionnel ou transitoire. Elle correspond plut�t � un �tat habituel et stable caract�ris� par une compl�mentarit� de fonctionnement.
Balogh, A. Hydrodynamical test preparation of karstic reservoirs for Chinese request. pp. 117�122.
In Hungarian petrol industrial practice several methods were developed for testing hydrodynamical properties of fluid reservoirs. In present article we briefly describe two types of testing methods, which are remarkable for karstology experts. One of them is Pulse Interference Test and the other is Cavern Volume Test, both of them developed in our company.
Pulse test is hydrodynamical examination method of fluid reservoirs surrounded by wells. With help of pulse test and analysis the existence of flow connection between test wells and the value of flow parameters can be determined. We run several pulse tests to understand karstic water supply system of H�v�z-lake in Hungary, where water production of bauxite mining may influence the rate of inflow and temperature of that thermal water. This testing method is also useful in water inrush preventing, because unknown caverns can be suspected between the wells, from the deviation of value of flow parameters.
It is very important to estimate the volume of a cavern filled up by water in underground mining area, because water inrush preventive operations can be designed on the basis of known cavern volume determined by Cavern Volume Test.
Ekmek�i, M. Effects of Quaternary tectonic activities on karstification pattern in Ceyhan-Berke dam-site, SE Turkey. pp. 123�128.
The Berke Project consists of construction of a dam and a hydropower plant on Ceyhan river running at the Eastern Mediterranean region of Turkey. There has been considerable debate on the intensity of karstification and its subsurface distribution at the damsite, a knowledge which is of great importance for grouting curtain design. Two different types of karstification were identified in the area: normal karst and thermal karst. Normal karst, progressing from the surface downward along the major faults has not been well developed. The karstification base related to normal karst is higher than the mechanical erosion base of the main river valley.
Tectonic activities that had been efective during Late Pliocene until Late Quaternary had two fold effect on the groundwater system in the region. Firstly, in some places it caused fracture eruption of basalt during Plio-Quaternary. This, consequently, had been a trigger for thermal spring occurrence. Thermal karst has therefore progressed upward from great depths, enlarging fractures to form thermal karst conduits. Secondly, the tectonic activity has continued until Late Quaternary and formerly developed karst conduits have been dissected due to dislocations. The resulted karst pattern is observed as randomly scattered, usually air or water filled cavities. This type of karst encourages construction of the dam with regard to karst problems. However, tectonic activity should be regarded as a more serious, potential risk rather than karstic leakages.
Mitrofan, H., Mafteiu, M., Povara, I. & Mitrutiu, M. Electrometric investigations on the supply channels of Hercules spring (Romania). pp. 129�136.
The thermal spring Hercules at Baile Herculane is fed by a karstic conduit, inaccessible to direct exploration. The �mise � la masse� resistivity method has been used in order to trace the path of the karstic conduit, presumably a carrier of rainfall originating, cooling water. A self potential (SP) survey has been additionally performed, in an attempt to identify hot water upflows.
Stevanovic, Z. & Dragisic, V. Some cases of accidental karst water pollution in the Serbian Carpathians. pp. 137�144.
Karst aquifers in Serbia are one of the main sources for water supply. The quality of karst water is generally very good (1st and 2nd class for drinking). A good natural predisposition for the protection of karst is the predominantly mountainous relief and uninhabited catchment areas. The results of �tracing� experiments with ground waters indicate that under convenient conditions the pollution may migrate as far as 10 km of rectilinear distance as early as 24 hours. Few cases of accidental chemical and bacteriological pollution of karstic aquifer was registred during the last 15 years: e.g. influence of copper mining activity in the zone of Bor and Majdanpek, radioactive contamination of aquifer in Golubacke Mts., and hydric epidemics happened in several small towns in Serbia ( Boljevac, Sjenica, Dimitrovgrad).
The complexity of conditions of protection in karst area (especially cavern and channel dimensions and high filtration rapidity) often requires an introduction of several zones and belts of sanitary protection.
Rotaru, A., Bulgar, A. & Povara, I. L��tude hydrodynamique du syst�me karstique de Motru Sec�Baia de Arama (Roumanie). pp. 145�156.
Le syst�me karstique de la zone de Motru Sec�Baia de Arama est un syst�me complexe, avec une alimentation � la fois diffuse par pr�cipitation et organis�e par les pertes situ�es dans le lit de la rivi�re de Motru Sec. La d�charge du syst�me se produit par la ligne de sources de la zone de Baia de Arama. Les tra�ages ont prouv� la continuit� des d�p�ts calcaires de l 'Autochtone Danubien de m�me que du syst�me karstique au dessous de la Nappe G�tique.
L'�tude du syst�me karstique a �t� r�alis�e par la m�thodologie de l 'analyse syst�mique mise au point et d�velopp�e dans le cadre du Laboratoire Souterrain de Moulis (France).
Les r�sultats obtenus en utilisant cette m�thode sur les hydrogrammes de sources apportent des renseignements sur la complexit� du syst�me. Cette complexit� se traduit par un "effet m�moire" important et une faible corr�lation avec les pr�cipitations. Cependant, l 'analyse a r�v�l� l�importance de la contribution des pertes de Motru Sec dans l 'alimentation du syst�me karstique.
Stiuca, E. & Ilinca, H. Pleistocene mammals (Rodentia) from Movile Cave (Romania). pp. 157�162.
The excavations undertaken in the Movile Cave (Mangalia, Southern Dobrogea) yielded a vertebrate fauna containing several species of rodents characteristic of a dry open environment (Sicista subtilis, Lagurus lagurus thracicus, Eolagurus luteus axshaenicus) in association with species indicative of grassland with shrubs (Apodemus sylvaticus, Microtus cf. epiroticus). A marshy facies was also present as shown by fish and amphibian remains. The vertebrate species recognised so far are small enough to have fallen prey to predatory birds. The occurrence of fossil remains in the sediments accumulated in the Main Gallery is a strong evidence that the cave, isolated at present, was in communication with the outside environment during certain time intervals. Judging from the evolutionary stage of the rodent species present, the faunal assemblage can be correlated with a late phase of the last glacial cycle (W�rmian/Vistulian) which should be situated within the isotopic stage 2 of deep sea cores (24 to 12 kyr BP).
Radulescu, C. & Samson, P., M. On some Middle and Late Pleistocene rare small mammal elements from the karst deposits of central Dobrogea (Romania). pp. 163�174.
Fossiliferous karst deposits located in the Jurassic limestones of Central Dobrogea yielded micromammalian assemblages belonging to the Middle and Late Pleistocene. Pleistocene climatic fluctuations registered for this area influenced the peculiar aspects of the fauna containing various amounts of elements with eastern European and central Asiatic affinities. Some rare species such as Visternomys cortezi (beginning of the Middle Pleistocene, �Cromerian complex�), Alactagulus cf. acontion, Ellobius cf. talpinus (penultimate glacial cycle, Rissian/Saalian) and Scirtopoda telum (end of the last glacial cycle, W�rmian/Vistulian) are presented and discussed. In addition, other elements showing Aegean and Anatolian relationships are also commented (Allactaga orghidani, Rattus casimcensis, Microtus guentheri group characteristic of the Gura Dobrogei�2 phase, late Cromerian or post-Cromerian in age). Three new taxa are described: Alticola (s.1.) remaxi n. sp. from the Gura Dobrogei�5 rock-shelter (uncertain phase within the first half of the Middle Pleistocene), Ellobius calabaei n. sp. from Pestera Liliecilor (Bats Cave) at Gura Dobrogei (Gura Dobrogei�2 phase) and Microtus guentheri vistierensis n. ssp. from the upper layers of the Gura Dobrogei�4 rock-shelter (penultimate glacial cycle).
Short Notes
Lascu, C. Split stalactites. pp. 175�178.
Paunescu, A.-C. Pr�cisions sur les Arvicola terrestris (Linn�us) (Rodentia, Mammalia) du dernier cycle glaciaire de Roumanie. pp. 179�182
