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Bulletin Bibliographique Spéléologique Speleological Abstracts Bulletin Bibliographique Spéléologique Speleological Abstracts 54 47e-51e année / 47th-51st year N° 54 2015-2019 Speleological Abstracts Bulletin Bibliographique Spéléologique Commission of Bibliography of the International Union of Speleology Commission de Bibliographie de l’Union Internationale de Spéléologie Swiss Speleological Society with the participation of / avec la participation de Società Speleologica British Cave Italiana Research Association Administration Commission de bibliographie de l’Union internationale de Spéléologie Patrick DERIAZ, Chemin des Invuettes 1, CH-1614 Granges E-Mail: [email protected] Ce numéro contient les analyses reçues entre 2015 et 2019. Elles sont intégrées dans la base de données disponible depuis décembre 2020 sous wikicaves.org Tirage : 20 exemplaires réservés aux centres de documentation de l’UIS ISSN : ISSN 0253-8296 Grotte de Vallorbe : siphon des blocs no 2 Liste des collaborateurs à ce numéro 54 (2015-2019) Nombre Pays Collaborateur d’analyses Période des analyses revue Divers Philipp Häuselmann 57 1995 2017 Belgique Nathalie Goffioul 152 2015 Italie Michele Sivelli 795 2012 2015 Cécile Vuilleumier Suisse Philipp Häuselmann 10 2015 2016 Suisse Ana Häuselmann 16 2015 France Christophe Bes 76 2016 Spelunca Espagne Daniela Spring 35 2013 2017 Berig Allemagne Michael Laumanns 105 2014 2019 1.1 Karstology des cavernes. L'article traite donc de sédimen- Karstologie tologie et de minéralogie: concrétion, glace, 1.11 Karst morphology and morphogenesis calcaire… (NG). Morphologie et morphogenèse 2019.0004 karstique HÄUSELMANN, Philipp (2013) : Large epi- CICCACCI, Sirio (2015) : Morfologia carsica genic caves in high-relief areas (karst morphology) in: Shroder, J., Frumkin, A. (Eds.), Treatise of Le forme del rilievo. Atlante illustrato di geo- Geomorphology, Vol. 6: Karst geomorphology morfologia : 119-161. Foto. : 207-219. (MS). Although the two conditions given in the title 2019.0001 ("large epigenic caves" and "high-relief area") already narrows down considerably the caves CWEPSS (2015) : En guise de synthèse that fall within these categories, it quickly EcoKarst, n° 100 : 30-32. Photos. becomes clear that the geomorphology of such L'article est une synthèse des différentes caves is not clear from the beginning. A closer futures missions de la cwepss et perspectives look to literature actually reveals that diverse d'actions pour la conservation et sensibilisation speleogenetic agents may influence the genesis des phénomènes karstiques. (NG). of such caves. Vertical vadose passages as well 2019.0002 as (epi)phreatic base level control are very of- ten seen in large caves in high-relief areas. The CWEPSS (2015) : Le karst : un milieu fragile key to understand the genesis of these caves is aux intérêts multiples first the notion of time (very often such caves EcoKarst, n° 100 : 5-7. Photos. are old and may even present different distinct Présentation générale du karst wallon et de ses phases of evolution) and second the evolution différents paysages: pelouses calcaires, mas- of the surface around these caves. Very often, sifs rocheux, carrières… sans oublier l'intérêt caves in mountaineous areas deliver hints to spéléologique des sites karstiques. (NG). reconstruct the (spatial and temporal) evolu- 2019.0003 tion of the surface morphology. By that, caves in mountains and in lowlands are no different, DE SWART, Herman (2015) : Over grotten en but surface information within the mountains grotvorming (4/4): het ontstaan van gesteenten is usually much more rare because of the en mineralen in grotten intensive erosional processes in such steeply Spelerpes, n° 1 : 38-43. In Dutch, photos. dipping areas. (Author, PHM). Article sur la formation des grottes, plus pré- 2019.0005 cisément la genèse des roches et des minéraux Speleological Abstracts / Bulletin Bibliographique Spéléologique N° 54 (2015-2019) 3 KNAPPE, Hartmut (2014) : Zur Entwicklung Atti del XXII congresso nazionale di speleo- der Karststrukturen im Riffkalkstein von Iberg logia. 30 maggio - 2 giugno, Pertosa-Auletta und Winterberg bei Bad Grund (Westharz). 2015, Serie II, vol. 29 (2015) : 613-618. Foto. Mitt. Verb. dt. Höhlen- u. Karstforsch., 60 (MS). (3+4) : 80-90. 2019.0010 On the development of karst structures in the western Harz/Germany. WAGNER, Thomas; FABEL, Derek; FIEBIG, 2019.0006 Markus; HÄUSELMANN, Philipp; SAHY, Diana; XU, Sheng; STÜWE, Kurt (2010) : LECOQ, Nicolas; MAGNE, Laurent; RO- Young uplift in the non-glaciated parts of the DET, Joël; CHÉDEVILLE, Stéphane (2015) Eastern Alps : Bande de Liesegang : observation et analyse Earth and Planetary Science Letters, 295 du développement de fronts de réaction-diffu- (2010) : 159-169. sion dans un milieu karstique inhomogène We report the first incision rates derived from Plaquette – programme des Journées 2015 de burial ages of cave sediments from the Mur ri- Spéléologie Scientifique, 14 et 15 novembre ver catchment at the eastern margin of the Eas- 2015. : 9, 21. tern Alps. At the transition zone between the Résumé de communication et de poster. Etude Alpine orogen and the Pannonian basin, this du phénomène des auréoles et bandes de river passes through the Paleozoic of Graz — a Liesegang. (NG). region of karstifiable rocks called the Central 2019.0007 Styrian Karst. This river dissects the study area in a north–south direction and has left behind MASTRONUZZI, G. (a cura di); VALLET- an abundance of caves. These caves can be TA, S. (a cura di); DAMIANI, A. (a cura di); grouped into several distinct levels according FIORE, A. (a cura di); FRANCESCANGELI, to their elevation above the present fluvial base R. (a cura di); GIANDONATO, P.B. (a cura level. Age estimates of abandoned cave levels di); IURILLI, V. (a cura di); SABATO, L. (a are constrained by dating fluvial sediments cura di) (2015) : washed into caves during the waning stages of Geositi della Puglia : 394 p. Fotografie. speleogenesis with the terrestrial cosmogenic Censimento di oltre 440 emergenze geologiche nuclide method. These ages and the elevations regionali di cui una gran parte di interesse car- of the cave levels relative to the current valley so-speleologico. Scheda descrittiva, fotografie floor are used to infer a very complex history e bibliografia per ogni geosito. (MS). of 4 milWalion years of water table position, 2019.0008 influenced by the entrenchment and aggrada- tion of the Mur river. We observe rather low RODET, Joël (2015) : Du manteau d'altération rates of bedrock incision over the last 4 Ma au lapiaz : entre racine et puits (in the order of 0.1 mm/y) with an e-folding Plaquette – programme des Journées 2015 de decrease in this trend to lower rates at younger Spéléologie Scientifique, 14 et 15 novembre times. We relate this incision history to a tecto- 2015. : 1 p. nic setting where an increase of drainage area Résumé de communication. Etude sur of the Mur river due to stream piracy in Late l'aquifère suspendu dans les formations artifi- Miocene to Pliocene times is linked to surface cielles. (NG). uplift. The later decrease in valley lowering 2019.0009 rates is attributed to the rise of the base level related to aggradation of sediments within the RUGGIERI, Rosario; MESSINA PANFA- valley. Sediment transport through the valley LONE, Davide (2015) : Geositi carsici from the upstream section of the Mur river dell'area dei Monti di Capo San Vito (Sicilia limited the erosional potential of the river to a nord-occidentale) transport limited state at the later stages of the Memorie dell'Istituto italiano di speleologia. incision history. (Author, PHM). 4 Speleological Abstracts / Bulletin Bibliographique Spéléologique N° 54 (2015-2019) 2019.0011 D'ANGELI, Ilenia Maria; DE WAELE, Jo (2015) : Analisi chimico-fisiche delle acque 1.12 Hydrology campionate nei gessi di Brisighella e Rontana Hydrologie Memorie dell'Istituto italiano di speleologia, Serie II, vol. 28 [i.e. 30] (2015) : 263-273. BADINO, Giovanni (2015) : La lunga via Foto, tabelle, rilievi. dell'acqua (MS). Speleologia SSI, n. 73 (dicembre 2015) : 54- 2019.0016 59. Foto. Da un'analisi delle aste fluviali del fiume si -ap DE WAELE, Jo; D'ANGELI, Ilenia (2015) : pura che il ramo più lungo ha origini carsiche e Cinque anni di analisi chimiche delle acque proviene dal versante francese del Marguareis. nei gessi dell'Emilia-Romagna: Life+ 08nat/ (MS). it/000369 “gypsum” 2019.0012 Speleologia Emiliana, Serie V, n. 6 (2015) : 81-90. Foto, tabelle. CALANDRI, Gilberto; GOBIS, Diana (2015) Dopo i monitoraggi si rileva che le condizioni : Caratteri chimico-fisici delle sorgenti carsi- idriche ipogee sono abbastanza buone ma non che del settore di Fornovolasco (Alpi Apuane, rispetto all'uso postabile delle acque, data l'alta prov. Lucca) presenza di solfati. Alti i nitrati, dovuti alla Memorie dell'Istituto italiano di speleologia. presenza di colonie di pipistrelli. (MS). Atti del XXII congresso nazionale di speleo- 2019.0017 logia. 30 maggio - 2 giugno, Pertosa-Aulet- ta 2015, Serie II, vol. 29 (2015) : 347-352. DEWAIDE, Lorraine; ROCHEZ, Gaëtan; Grafici. HALLET, Vincent (2015) : Double pic de (MS). restitution sur le réseau de la Lesse souterraine 2019.0013 à Furfooz : des investigations de terrain au modèle réduit CERADINI, Andrea; TOSADORI, Gabriele; Plaquette – programme des Journées 2015 de VICENZI, Matteo (2015) : Indagine su alcune Spéléologie Scientifique, 14 et 15 novembre sorgenti carsiche del Monte Baldo (Prealpi 2015. : 1 p. Venete) Résumé de communication. Traçages de la Speleologia Veneta, n. 22 (2014/2015) : 107- Lesse souterraine montrant un double pic 120. Foto, diagrammi. de restitution en aval du lac à la Galerie des Monitoraggio dei parametri chimico-fisici Sources et au Trou de la Loutre. (NG). delle sorgenti: Aril, Rio dei Mulini, Fonte di 2019.0018 Preabocco. Recenti esplorazioni nella Grotta RH9 e nel Buco di Punta Ciusole. (MS). DEWAIDE, Lorraine; ROCHEZ, Gaëtan; 2019.0014 PAUWELS, Michel; HALLET, Vincent (2016) : Hydrodynamique d'un lac souterrain : CWEPSS (2015) : Les études incontour- équipement et premiers résultats (Lesse souter- nables. Les eaux souterraines karstiques : un raine) aquifère de fissures difficile à modéliser Journées 2016 de Spéléologie Scientifique. EcoKarst, n° 100 : 25-26.
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