Blaualgenliteratur Aus Den Jahren 1960-1966 22() Hydrologie

Total Page:16

File Type:pdf, Size:1020Kb

Blaualgenliteratur Aus Den Jahren 1960-1966 22() Hydrologie Sonderabdruck aus SCHWEIZERISCHE ZEITSCHRIFT FDR HYDROLOGIE BIRKHAUSER VERLAG BASEL Vol. 29 1967 Fasc. 1 Blaualgenliteratur aus den Jahren 1960-1966 22() Hydrologie Blaualgenliteratur aus den Jahren 1960-1966 Am 4. Symposium der Internationalen Arbeitsgemeinschaft fiir Cyanophyten- forschung (IAC) iiber «Fragen der Cyanophyten-Systematik» in Kastanienbaum 1966 wurde wiederum beschlossen, die Blaualgenliteratur zu veroffentlichen. Da die erste Zusammenstellung der Literaturzitate aus den J ahren 1960~1963 nicht vollstandig war, wurde sie <lurch eine weitere Anzahl von Arbeiten erganzt. Somit liegen nun zwei Listen vor: Die erste enthalt die erganzten Literaturzitate aus den J ahren 1960-19631), in der zweiten sind Literaturangaben aus den Jahren 1964-1966 zu finden. Natiirlich wird wiederum ein Teil der Veroffentlichungen unberiicksichtigt bleiben. Um aber die Arbeiten <loch so liickenlos wie moglich zu erfassen, gelangten wir diesmal laut Beschluss des 4. Symposiums an eine Reihe von Spezialisten aus ver- schiedene~ Landern mit der Bitte um Mitarbeit. Die daraufhin eingegangenen Bei- trage vorl Dr. Asta ALMESTRAND (Schweden), Prof. Dr. P. BouRRELLY (Frankreich), Prof. Dr. V. J. CHAPMAN (New Zealand), Dr. S. GoLUBIC (USA), Dr. Edith KANN (Osterreich), Dr. J. KOMAREK und Blanka DESORTOVA (Tschechoslowakei), Dr. I. UM:EZAKI (Japan) uncl Dr. I. WOJCIECHOWSKI (Polen) erlaubten uns schliesslich, die nachfolgende Literatur zusammenzustellen. Wir mochten an dieser Stelle allen ge- nannten Mitarbeitern fiir ihre Bemiihungen unseren herzlichen Dank aussprechen. Die Sachgebiete der aufgefiihrten Arbeiten wurclen anhand von folgenden Stich- wortern gekennzeichnet: ]3 Biochemie p Physiologie, Varia c Cytologie, Varia PN Phys1ologie, Stickstoffbindung Cu Cytologie, Feinstruktur PT Physiologie, Toxinc K Kulturmethoden s Systcmatik M Morphologie v Varia 0 Okologie 111arianne Pavoni l) Pavoni, M., Blaualgenliteratur aus den Jahnm 1960-1963, Schweiz. Z. Hydro!. 26, 177-187 (1964). 29/1, 1967 4. Symposium iiber Cyanophytensystcmatik 227 1. Erganzungen zur Blaualgenliteratur aus den Jahren 1960-1963 AARONSON, S. and BAKER, H., Lipid and Sterol Content of Some Protozoa,]. Protozool. 8, 274-277 (1961). B (inkl. Anacystis, Cyanidium). ABELSON, P.H. and HEERING, T. C., Carbon Isotope Fractionation in Formation of Amino Acids by Photosynthetic Organisms, Proc. natn. Acad. Sci. U.S.A. 47, 623-632 (1961). P (ink!. Anacystis). AKIYAMA, M., Aerial and Terrestrial Algae in San-in Region of Honshu, Japan, Bull. Shimane Univ. (Nat. Sci.) 10, 75-89 (1961), 0. AKIYAMA, M., Ecology of Freshwater Algae in San-in Region, Japan, Mem. San-in Bunka Kenkyu 2, 77-90 (1962), 0. ALLEN, M.B., PIETTE, L. H. and MuRCHIO, J. C., Studies of Free Radical Formation in Photosynthetic Systems, Plant Physiol. 35 (suppl.), 22 (1960). Pv (inkl. Anabaena). ALLEN, M. B., PIETTE, L. H. and MuRCHIO, J. C., Studies of the Functions of Photosyn- thetic Pigments, Proc. III. int. Congress Photobiol., p. 170-171 (1961). P (inkl. Anabaena). ALMESTRAND, A., Schwierigkeiten bei der Bestimmung von Microcystisarten, Schweiz. Z. Hydro!. 23, 207-208 (1961). S. ANDERSON, G. C., Recent Changes in the Trophic Nature of Lake Washington, a Review. Aus: Algae and Metropolitan Wastes, p. 27-33 (1961). 0 (inkl. Oscillatoria). AsTACHOVA, T. V., KuN, M. S. und TEPLYI D. L., Ursache der Karpfenkrankheit au/ der unteren Wolga, Dokl. Akad. Nauk SSSR 133, 1205-1208 (1960), russisch. PT (Micro- cystis, Anabaena, Aphanizomenon). BAALEN, C. van, Nutritional Characteristics of Some Marine Blue-Green Algae, Physiology 37 (suppl.), 49-50 (1962). P. BACH, M. K. and FELLIG, J., Ubiquity of Stimulation of Endogenous Respiration by Purine and Purine Analogs, Plant Physiol. 36, 85-88 (1961). P (ink!. Anacystis). BARSDATE, R. ]. and GurLLARD, R.R. L., Molybdenum Uptake of Marine Plankton Algae, Biol. Bull. 121, 373 (1961). P (inkl. Synechococcus). BASLEROVA, M. et DvoRAKOVA, ]., Algarum, Hepaticarum Muscorumque in culturis collectio, Nakl. CSAV, 56 pp. (1962). K (ink!. Cyanophyceae). BATES, J. H., Recent Aspects in the Development of a Closed Ecologic System, Aerospace Med. 32, 12-24 (1961). 0, P (inkl. Anacystis, Synechocystis). BECK, S., Licht- und elektronenmikroskopische Untersuchungen an einer sporenbildenden Cyanophyceae aus dem Formenkreis von Pleurocapsa fuliginosa Hauck, Flora 153, 194- 216 (1963). Cu. BEHRE, K., Die Algenbesiedlung einiger Hafen in Bremerhaven und ihre Beziehungen zur Verschmutzung dieser Gewasser, Veroff. Inst. Meeresforsch. Bremerhaven 8, 192-249 (1963). 0. BERNARD, F., Rapports caracteristiques entre les principaux du plancton, denombres en sept regions des mers chaudes, Compt. rend. Acad. Sci. (Paris) 251, 1585-1587 (1960). 0 (inkl. Nostoc). BERNARD, F., Density of Flagellates and Myxophyceae in the Heterotrophic Layers, Related to Environment, Bact. Proc. 38 pp. (1961). 0. BERTHOLDT, W., Fighting Blue-Green Algae, Aquar. J. 31, 17, 28, 33, 35 (1960). O,V. BEUSCHOLD, E., Biologische und chemische Beobachtungen beim Anstau der Talsperren des Bodewerlles, Wiss. Z. Univ. Leipzig, math. - nat., 10, 93-97 (1961). 0 (ink!. Cyanophy- ceae). BILLING, A., En vegetationsundersogelse a/ to baeklle ved Rorbaek So, Flora og fauna 66, 93-100 (1960). 0 (inkl. Anabaena, Aphanizomenon). BISWAS, B. B., Comparative Studies on DNA of Chlorella ellipsoidea and Anacystis nidulans, Plant Physiol. 35 (suppl.), 30 (1960). B. BISWAS, B. B. and MYERS, J., A Methyl Cytidine from the Ribonucleic Acid of Anacystis nidulans, Nature 186 (4720), 238-239 (1962). B. BISWAS, B. B. and MYERS, J., Characterization of Deoxyribonucleic Acid from Anacystis nidulans, Nature 188 (4755), 1029-1030 (1962). B. BISWAS, B. B. and SEN, S. P., The Effects of Nucleases on Photosynthetic C02-Fixation, Experientia 16, 135-136 (1960). P (inkl. Nostoc). BLACK, C. C., FEWSON, C. A. and GIBBS, M., Photochemical Reduction of Triphosphopyridine Nucleotide by Cell-Free Extracts of Blue-Green Algae, Nature 198 (4875), 88 (1963). P. 228 M. Pavoni Hydrologie R., New Locality of A phanizomenon Elenkinii Kisel, Acta Hydrobiol. 2, 63-65 (1960). 0, BOHR, R., Phytosociological Studies on the Periphyton in Lake Mamry, Stud. Soc. Sci. Torunensis 6, 1-44 (1962). 0 (inkl. Cyanophyceae). BoLYSEV, N. N., Die Rolle der Algen in der Bodenformation, Vest. Moskov. Univ., ser. Soil Biol. 6, 67-75 (1961), russisch. 0 (inkl. Anabaena, Oscillatoria, Stratonostoc). BoLYSEV, N. N. und STINA, E. A., Vegetation und Boden der Umgebung der Westseen des Wolgadeltas, Vest. Moskov. Univ., biol. - pocvoved.-geol.-geogr. 4, 63-70 (1960), rus- sisch. 0 (inkl. Cyanophyceae). BosE, B. B., An Experimental Study of the Optimum Salinity for the Growth of the Benthic Blue-Green Alga Oscillatoria splendida Greville of Brackishwater Ponds, Proc. nat. Inst. Sci. India, biol. Sci., 26, 19-21 (1960). 0, K. BouRRELLY, P., Un nouveau genre africain d'endocyanose: Glaucocystopsis africana, nov. gen. et nov. sp., Compt. rend. Seances Acad. Sci. 251, 416-418 (1960). S. BouRRELLY, P., Les grands problemes ecologiques en algologie d'eau douce. Aus: Ecology of Freshwater Algae, Recent Adv. Bot., p. 198-201, (1961). 0 (inkl. Cyanophyceae). BowEN, C. C., and PANKRATZ, H. S., Formation of Photosynthetic Lamellae in the Blue- Green Algae, Cell. Biol. [A] 19, 8 (1963). Cu. BRUNNER, G., Die Blaualgensymbiose des W asserfarns Azolla, Mikrokosmos 49, 360-363 (1960). 0 (inkl. Anabaena). BURKHOLDER, P. R., Some Nutritional Relationships Among Microbes of Sea Sediments, Bact. Proc., 36 (1961). 0, P (inkl. Cyanophyceae). CALVIN, M., Some Photochemical and Photophysical Reactions of Chlorophyll and its Relatives. Aus: ELROY et GLASS edit., A Symposium on Light and Life, p. 317-355, (1961). P (inkl. Nostoc). CASTENHOLZ, R. W., Seasonal Changes in the Attached Algae of Freshwater and Saline Lakes in the Lower Grand Coulee, Washington, Limnol. Oceanogr. 5, 1-28 (1960). 0 (inkl. Cyano- phyceae). V., Marine Phytoplankton in New Zealand Waters, Bot. Mar., Vol. 2, suppl. (1961). 0, CERNJAVSKAJA, M. A., Ad morphologiam Lyngbyae aestuarii (Mert.) Liebm. Not. syst. Sect. cryptog. Inst. bot. V. L. Komarovii Acad. Sci. UH.SS 15, 15-19 (1962), russisch. S,M. CHAP:.vIAN, V. J., A Contribution to the Ecology of the Kermadec Islands, Pac. Sci. 15, No. 3, 347 (1961). 0. CHAPMAN, J. A. and SALTON, U.R.Y.,A Study of Several Blue-GreenAlgae in the Electron Microscope, Arkiv Mikrobiol. 44, 311-321 (1962). Cu. CLAUS, G., Comparative Studies of the Algae of Danube River near Vienna, Year Book Amer. philos. Soc. 2753, 277-282 (1961). 0 (inkl. Cyanophyceae). G., Observations on Cyanotheca longipes Pascher, Ost. bot. Z. 108, 286-299 (1961). S, CLAUS, G., Comments on the Species of the Genits Tetrapedia Reinsch (Chroococcaceae, Cyanophyta), Hydrobiologia 21, 266-274 (1963). S. CLAUS, G., Wolskyella, a New Genus of Blue-Green Algae and its Phylogenetic Significance, Nova Hedwigia 6, 29-38 (1963). S. COBB, H. D. and MYERS, J., Interrelationships Between Nitrogen Fixation and Photo- synthesis in a Blue-Green Alga, Plant Physiol. 36 (suppl.), 25 (1961), PN (inkl. Anabaena). CONTI, S. F., Fine Structure of Blue-Green Algae, Bact. Proc. [G] 87 (1963). Cu. CORRELL, D. L., A Study of the Ribonucleic-Acid-Polyphosphate Complexes Isolated from Anabaena variabilis and Synchronized Chlorella pyrenoidosa, Diss. Abstr. Michigan State Univ. 22, 1811-1812 (1961). B. CORRELL, D. L., ToLBERT, N. E. and BALL, R. C., RNA-Polyphosphate Complexes from Anabaena variabilis, Plant Physiol. 35 (suppl.), 30 (1960). B. CRESPI, H. I., MANDEVILLE, S. E., and KATZ,
Recommended publications
  • THE PROBLEM of LAMPENFLORA in SHOW CAVES – Arrigo A
    ANDYSEZ 56 LAMPENFLORA YET AGAIN! Thus Lampenflora Part 4 – Andy Spate The very distinguished and knowledgeable results for lampenflora growth control were very Professor Arrigo Cigna has contributed a great promising. This procedure is especially useful deal to our understanding of cave environments when applied to actively growing lampenflora. particularly in relation to radon, carbon dioxide, Once lampenflora is covered with flowstone, the cave environmental monitoring – and to the oxidizing effect of H2O2 is drastically reduced lampenflora problem. Below you will find a recent [as with hypochlorite]. presentation from Arrigo given at the ISCA Congress in Slovakia in October 2010 (Cigna in So what is meant by buffering and why and how press, 2010). do we do it? Many of us have tried to re-invent the wheel Faimon’s et al (2003) details extensive and in- playing about with concentrations of sodium depth research on the use of hydrogen peroxide hypochlorite and calcium hypochlorite in spite of for lampenflora control. Unlike hypochlorite, the admonishments of Tom Aley, for example, peroxide can erode calcite – not much, but some. who has very fixed views on 5.25% hypochlorite (Aley and Aley 1992). Adding some of your local limestone or calcite to the peroxide solution for a few hours or overnight We have discussed other chemicals including reduces or halts this issue. It just adds to the potent biocides, altering light frequencies and the more complex approach of using peroxide rather use of ultraviolet light in earlier ANDYSEZs than hypochlorite. (Numbers 48, 49 & 50 – look on your ACKMA CD ROM). All of these have drawbacks and some – The disadvantages include: such as the use of hypochlorite – may have very considerable impacts on cave environments – • The need to buffer the peroxide solution; especially their biota.
    [Show full text]
  • Caves of Aggtelek Karst and Slovak Karst Hungary & Slovakia
    CAVES OF AGGTELEK KARST AND SLOVAK KARST HUNGARY & SLOVAKIA The variety and concentration of their formations make these cave systems of 712 caves excellent representatives of a temperate-zone karstic network. They also display an extremely rare combination of tropical and glacial climatic effects, making it possible to study geological history over tens of millions of years. COUNTRY Hungary and Slovakia NAME Caves of Aggtelek Karst and Slovak Karst NATURAL WORLD HERITAGE TRANSBOUNDARY SERIAL SITE 1995: The cave systems of the two protected areas jointly inscribed on the World Heritage List under Natural Criterion viii. 2000: Extended to include Dobšinská cave in Slovakia (660 ha). 2008: Extended by 87.8 ha. STATEMENT OF OUTSTANDING UNIVERSAL VALUE [pending] INTERNATIONAL DESIGNATIONS 1977: Slovensky Kras Protected Landscape Area designated a Biosphere Reserve under the UNESCO Man & Biosphere Programme (36,166 ha). 1979: Aggtelek National Park designated a Biosphere Reserve under the UNESCO Man & Biosphere Programme (19,247 ha); 2001: Baradla Cave System & Related Wetlands, Hungary (2,075 ha) and Domica Wetland in the Slovensky Kras, Slovak Republic (627 ha) both in Aggtelek National Park, designated a transboundary Wetland of International Importance under the Ramsar Convention. IUCN MANAGEMENT CATEGORY II National Parks BIOGEOGRAPHICAL PROVINCE Middle European Forest (2.11.5) GEOGRAPHICAL LOCATION Straddles the Slovensky Kras foothills of the Carpathian mountains on the border of southern Slovakia and northern Hungary 152 km northeast
    [Show full text]
  • Downloaded 10/01/21 04:52 AM UTC IAGA-REPORT 2007–2010 159
    Acta Geod. Geoph. Hung., Vol. 46(2), pp. 158–214 (2011) DOI: 10.1556/AGeod.46.2011.2.4 HUNGARIAN NATIONAL REPORT ON IAGA 2007–2010 LSzarkaand GSatori´ Geodetic and Geophysical Research Institute of the Hungarian Academy of Sciences, POB 5, H-9401 Sopron, Hungary, e-mail: [email protected] This report is a collection of institutional and individual reports, edited by the Hungarian national delegates (L Szarka: 2007–2010 and G S´atori: 2010). In the reference lists the readers find papers published mainly between 2007 and 2010 in various geophysical journals (including journals edited in Hungary as Acta Geodaetica et Geophysica Hungarica, Geophysical Transactions, Magyar Geofizika, F¨oldtani K¨ozl¨ony,etc.). The major IAGA-related conferences in Hungary between 2007–2010 were as follows: the IAGA XI. Scientific Assembly (Sopron, 2009) as the most remarkable event of geo-science in Hungary, in that year; the VERSIM Workshop (Tihany, 2008), as an other international meeting; Ionosphere and Magnetosphere Seminars (Budapest, 2008; Baja, 2010); Inversion Workshop (Miskolc, 2008); annual meetings of the Association of Hungarian Geophysicists; annual meetings of Young Geologists and Geophysicists. The structure of this report follows more or less the structure of Hungarian activities in frames of IAGA. The numbering of sections (I–V) indicates the number of IAGA divisions, but the individual sections does not follow exactly the structure of IAGA working groups. Instead, each of the sections is divided into several subsections, corresponding to the related Hungarian results. Several scientific results are described in Section V, under the observatory de- scriptions, where activities of two Hungarian geo-electromagnetic observatories: Nagycenk and Tihany are summarized.
    [Show full text]
  • Water Regime: Physical Features of the Site
    Ramsar Site: 1092 – Baradla Cave System Ramsar Information Sheet May 2014 Additional information Water Regime: 1. Ground waters 1.1. Karstic water As the the Domica-Baradla Cave System is in a karstic region, the major part of the groundwater is stored in the tectonic fissures, fractures and dissolutional cavities of the karstified Triassic limestones and dolomites. The recharge derives from the rainfall infiltrating through the surface, and from meteoric waters flowing into the karst system through sinkholes. 1.2. Confined groundwater In the Domica-Baradla Cave System area confined groundwater occurs only south from Aggtelek, in the 50-100 m thick Pannonian clayey-sandy-pebbly sediments. This sequence is considered more or less impervious because of its clay content, therefore only 5% of the rainfall can infiltrate. A part of the infiltrating water feeds the karst beneath, another part flows laterally towards the springs on the south. Some local springs discharge on the surface of the clayey pebble horizons. 1.3. Unconfined groundwater Unconfined groundwater occurs only in the valleys of major streams, and in the fluvial pebbly sediments of basins. 2. Springs Springs can be best characterised by discharge, which is determined by the geological-morphological build-up of the catchment area, and basically by climatic conditions (rainfall, evaporation, melting). Depending on these conditions, the discharge of a spring may vary between a few l/min and a few thousand l/min. In this area the Jósva spring has the biggest discharge with a minimum of 3900 l/min and a maximum of 450.000 l/min (and 1.200.000 l/min in 1959).
    [Show full text]
  • Characterizing the Eemian-Weichselian Transition in Northwestern Europe with Three Multiproxy Speleothem Archives from the Belgi
    Quaternary Science Reviews 208 (2019) 21e37 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Characterizing the Eemian-Weichselian transition in northwestern Europe with three multiproxy speleothem archives from the Belgian Han-sur-Lesse and Remouchamps cave systems * Stef Vansteenberge a, , Sophie Verheyden a, Dominique Genty b, Dominique Blamart b, Steven Goderis a, Stijn J.M. Van Malderen c, Frank Vanhaecke c, Florent Hodel d, David Gillikin e, Camille Ek f, Yves Quinif g, Hai Cheng h, i, R. Lawrence Edwards i, Philippe Claeys a a Analytical, Environmental and Geochemistry, Vrije Universiteit Brussel, Pleinlaan 2, 1050, Brussels, Belgium b Labaratoire des Sciences du Climat et de l’Environnement, 91400, Gif-sur-Yvette, France c Atomic and Mass Spectrometry Group, Department of Analytical Chemistry, Universiteit Gent, Krijgslaan 281 S12, 9000, Gent, Belgium d Geosciences Environnement Toulouse, OMP, Univ. Toulouse III Paul Sabatier, CNRS, IRD, 31400, Toulouse, France e Department of Geology, Union College, Schenectady, NY, 12308, USA f UniversitedeLiege, 4000, Liege, Belgium g Centre d’etudes et de Recherches Appliquees au Karst (CERAK), Faculte Polytechnique de Mons, 7000, Mons, Belgium h Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an, China i Department of Earth Sciences, University of Minnesota, Minneapolis, USA article info abstract Article history: Interglacial to glacial transitions represent the most drastic turnovers in the Quaternary climate system. Received 15 March 2018 Yet, millennial-scaled climate variability and stochastic internal variability that result in (inter)glacial Received in revised form transitions remain poorly understood. Here, three speleothems from two different cave systems in 12 January 2019 Belgium are investigated to characterize the Eemian to early Weichselian transition.
    [Show full text]
  • Exposure of Workers to Radon Progeny in the Baradla Cave at Aggtelek
    exposure of workers to radon progeny in the baradla cave at aggtelek Z. Dezso Dep. of Environmental Physics, Debrecen University H-4001 Debrecen, POBox 51, Hungary The number of those countries where radiation protection considers not only radiation workers but all employees in general is growing. An Euro conform regulation assumes that at least worker's exposure to radon be assessed and limited to a certain value. This is based on ICRP 65 recommendations [1] in most countries. In the new Hungarian radiation protection regulation [2], in accordance with EU legislation, rules have been adopted also for the protection of workers from radon exposure at work. The limit of exposure for non-radiation workers is expressed in action level and is set to 1000 Bq/m3 yearly mean radon concentration and is in effect from 1st January 2003. In case of 2000 hours/year working time, this corresponds to 3-12 mSv effective dose, depending on the local circumstances. Among others, show caves are explicitly mentioned in the new directive where the exposure of personnel must be monitored because of the likely high radon levels. This is probably because of the extensive radon related research work done in caves in the past 20 years in Hungary [3]. These studies revealed that the mean radon level in Hungarian caves is around 2 kBq/m3. Furthermore, it turned out that the well known show caves of Budapest all have yearly mean radon level much higher than the current action level. Some 10 years ago, radon research in these caves included also the assessment of radiation dose of tour guides and speleotherapy personnel [4].
    [Show full text]
  • Microscopic Fungi on Cadavers and Skeletons from Cave and Mine Environments
    CZECH MYCOLOGY 70(2): 101–121, AUGUST 19, 2018 (ONLINE VERSION, ISSN 1805-1421) Microscopic fungi on cadavers and skeletons from cave and mine environments 1 2 1,2 1,2 ALENA NOVÁKOVÁ *, ALENA KUBÁTOVÁ ,FRANTIŠEK SKLENÁŘ ,VÍT HUBKA 1 Laboratory of Fungal Genetics and Metabolism, Institute of Microbiology of the CAS, v.v.i., Vídeňská 1083, CZ-142 20 Praha 4, Czech Republic 2 Department of Botany, Faculty of Science, Charles University, Benátská 2, CZ-128 01 Praha 2, Czech Republic *corresponding author: [email protected] Nováková A., Kubátová A., Sklenář F., Hubka V. (2018): Microscopic fungi on ca- davers and skeletons from cave and mine environments. – Czech Mycol. 70(2): 101–121. During long-term studies of microscopic fungi in 80 European caves and mine environments many cadavers and skeletons of animals inhabiting these environments and various animal visitors were found, some of them with visible microfungal growth. Direct isolation, the dilution plate method and various types of isolation media were used. The resulting spectrum of isolated fungi is presented and compared with records about their previous isolation. Compared to former studies focused mainly on bat mycobiota, this paper contributes to a wider knowledge of fungal assemblages colonising various animal bodies in underground environments. The most interesting findings include ascocarps of Acaulium caviariforme found abundant on mam- mals cadavers, while Botryosporium longibrachiatum isolated from frogs, Chaetocladium jonesiae from bats and Penicillium vulpinum from spiders represent the first records of these species from cadavers or skeletons. Key words: European caves, abandoned mines, dead bodies, bones, mammals, frogs, spiders, isopods, micromycetes.
    [Show full text]
  • A Global Resource to Document Oxygen and Carbon Isotope Records from Speleothems.', Earth System Science Data., 10 (3)
    Durham Research Online Deposited in DRO: 18 September 2018 Version of attached le: Published Version Peer-review status of attached le: Peer-reviewed Citation for published item: Atsawawaranunt, Kamolphat and Comas-Bru, Laia and Mozhdehi, Sahar Amirnezhad and Deininger, Michael and Harrison, Sandy P. and Baker, Andy and Boyd, Meighan and Kaushal, Nikita and Ahmad, Syed Masood and Brahim, Yassine Ait and Arienzo, Monica and Bajo, Petra and Braun, Kerstin and Burstyn, Yuval and Chawchai, Sakonvan and Duan, Wuhui and Hatvani, Istv¡an G¡abor and Hu, Jun and Kern, Zolt¡anand Labuhn, Inga and Lachniet, Matthew and Lechleitner, Franziska A. and Lorrey, Andrew and P¡erez-Mej¡as, Carlos and Pickering, Robyn and Scroxton, Nick and Members, SISAL Working Group (2018) 'The SISAL database : a global resource to document oxygen and carbon isotope records from speleothems.', Earth system science data., 10 (3). pp. 1687-1713. Further information on publisher's website: https://doi.org/10.5194/essd-2018-17 Publisher's copyright statement: c Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders.
    [Show full text]
  • Medical/Wellness Tourism Development in the World Heritage Caves of the Aggtelek and Slovak Karst (SKHU/1601/1.1/035) Press Rele
    Medical/Wellness Tourism Development in the World Heritage Caves of the Aggtelek And Slovak Karst (SKHU/1601/1.1/035) Press Release The cross-border project of the Aggtelek National Park Directorate and its partner, the State Nature Conservancy of Slovak Republic was awarded a non-refundable grant of € 1,616,098 from the Interreg V-A Slovakia - Hungary Cooperation Programme. The project was implemented between November 2017 and July 2021. The 30+ km long Baradla-Domica cave system - split between Hungary (22 km) and Slovakia (approx. 8 km) - is the most significant representative of the underground world added to the list of World Heritage Sites as the caves of the Aggtelek karst and the Slovak karst. The aim of the project was to study the therapeutic effects of climate therapy in the Baradla-Domica cave system, to provide objective survey results, to renew the certification of Béke [Peace] Cave in Jósvafő and to develop adequate visitor infrastructure needed for the corresponding services. The connection between the cave climate and the improvement of the health of patients suffering from respiratory illnesses was first examined in the 19th and 20th centuries. Today, this connection is undoubtedly proven and cave therapy, as a part of medical tourism, has now a growing potential in tourism and preservation of health. Cave climate has certain constant features including the relatively constant temperature (annual temperature changes do not exceed 1°C), the purity of cave air (caves are free of dust, pollen and germs - at least the parts completely separated from the surface); the CO2-content and the relative humidity values exceed those measured at the surface.
    [Show full text]
  • Journal of Cave and Karst Studies
    September 2017 Volume 79, Number 2 JOURNAL OF ISSN 1090-6924 A Publication of the National CAVE AND KARST Speleological Society STUDIES DEDICATED TO THE ADVANCEMENT OF SCIENCE, EDUCATION, EXPLORATION, AND CONSERVATION Published By The National Speleological Society http://caves.org/pub/journal Office 6001 Pulaski Pike NW Huntsville, AL 35810 USA Editorial EDITORIAL: CHANGES TO THE JOURNAL OF CAVE AND KARST STUDIES Scott A. Engel Production Editor In 2011, the Journal of Cave and Karst Studies began transitioning to an electronic distribution process. While not all readership agreed with this change, it was done, in part, to address budgetary limitations within the National Speleologi- cal Society. But more importantly, it was done to conform with to similar changes being done by peer publications and across the publication industry. As predicted, in the six years since we made this transition, the movement away from print distribution and toward electronic only distribution has continued to expand and evolve across the scientific com- munity and the globe. In that respect, our experiment has been a success, and it is increasingly apparent that a return to full print distribution is unlikely and unnecessary. With that in mind, this issue represents the next evolution of the Journal as we continue to modernize our production process. As you look through this issue, you will find that we have made two major changes to improve the Journal. A brief description of the changes and the reasons behind them are presented below. Publication Schedule By transitioning to a predominantly electronic distribution, we have been able to control and reduce costs incurred by the National Speleological Society to produce and distribute individual issues of the Journal.
    [Show full text]
  • Development, Management and Economy of Show Caves
    In!. J. SpeleoI.. 29 B (1/4) 2000: I - 27 DEVELOPMENT, MANAGEMENT AND ECONOMY OF SHOW CAVES Arrigo A. CIGNA International Show Caves Association Scientific Advisor to the President Ezio BURRI Dept. of Environmental Sciences University of L'Aquila ABSTRACT The problems concerning the development of show caves are here considered by taking into account different aspects of the problem. A procedure to carry out an Environmental Impact Assessment (EIA) has been established in the last decade and it is now currently applied. Such an assessment starts with a pre-opera- tional phase to obtain sufficient information on the undisturbed status of a cave to be devel- oped into a show cave. Successively a programme for its development is established with the scope to optimise the intervention on the cave at the condition that its basic environmental parameters are not irre- versibly modified. The last phase of the assessment is focussed to assure a feedback through a monitoring network in order to detect any unforeseen difference or anomaly between the pro- ject and the effective situation achieved after the cave development. Some data on some of the most important show caves in the world are reported and a tenta- tive evaluation of the economy in connection with the show caves business is eventually made. Introduction Nearly twenty years ago, two great experts of cave management, Russell and Jeanne Gurnee (1981), wrote: "The successful development and operation of a tourist cave depends on a combination of factors, including 1) Scientific investigation 2) Art 3) Technology 4) Management Scientific study is recommended at the beginning of the first phase in order to deter- mine what hydrologic and geologic factors may have an influence on the develop- 2 Arrigo A.
    [Show full text]
  • Complete Issue
    J. Mulec and G. Kosi – Lampenflora algae and methods of growth control. Journal of Cave and Karst Studies, v. 71, no. 2, p. 109–115. LAMPENFLORA ALGAE AND METHODS OF GROWTH CONTROL JANEZ MULEC1 AND GORAZD KOSI2 Abstract: Karst caves are unique natural features and habitats where specialized organisms live. Some caves are also important as cultural heritage sites. In recent decades, many caves have experienced intensified tourist visits. To attract visitors, artificial illumination was installed that changed conditions in the caves. As a result, communities of organisms called lampenflora develop in close and remote proximity to lights. These phototrophic organisms are inappropriate from an aesthetic point of view and cause the degradation of colonized substrata, which is a particular problem in caves with prehistoric art. Key factors that allow lampenflora to grow are light and moisture. Illuminated spots in caves can be quickly colonized by algae, some of which have broad tolerances for different substrata. Several phototrophs can survive in caves even at photon flux densities lower than the photosynthetic compensation point. In this paper, the pros and cons of physical, chemical, and biological methods to control phototrophic growth are reviewed and discussed. Experiences in show caves can be helpfulin controlling undesirable algal growth in other environments. INTRODUCTION show no oscillations in light intensity. Dobat (1972) named spots with growing lampenflora ecosystems in formation. Caves have a special place in human history. Early in One of the characteristics of the natural cave environ- prehistory, humans discovered that caves can provide ment is low nutrient input (Simon et al., 2007) that is suitable temporary or permanent shelters.
    [Show full text]