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Journal articles on the topic 'Cave'

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Author: Grafiati

Published: 4 June 2021

Last updated: 7 July 2024

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1

Jacoby, Brianne S., Eric W. Peterson, John C. Kostelnick, and Toby Dogwiler. "Approaching Cave Level Identification with GIS: A Case Study of Carter Caves." ISRN Geology 2013 (August 28, 2013): 1–7. http://dx.doi.org/10.1155/2013/160397.

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Cave passages that are found at similar elevations are grouped together and called levels. The current understanding is that passages within a level are speleogenetically linked to a common static baselevel or stratigraphic control. Cave levels have provided an interpretive framework for deciphering cave development, landscape evolution, and climatic changes. Cosmogenic dating has been successfully used to interpret levels in Mammoth Cave and the Cumberland Plateau; however, this technique is expensive and there are limited funding resources available. Geographic information systems may be used as preliminary procedures to identify cave levels and constrain the timing of level development. A GIS method is applied to the Carter Cave system in northeastern Kentucky. Cave entrance elevations along stream valleys were found by extracting elevation values from a m digital elevation model. Using a histogram generated from the frequency of cave elevations and a natural breaks classifier, four cave levels were identified in the Carter Cave system. This work improves the understanding of the Carter Cave system evolution and contributes toa methodology that can be used to ascertain an erosion history of karst systems.

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2

Gurgen, Gurcan. "Caves and cave art." New Trends and Issues Proceedings on Humanities and Social Sciences 6, no. 4 (September 24, 2019): 100–105. http://dx.doi.org/10.18844/prosoc.v6i4.4403.

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This paper aims to discuss the impact and importance of the karstic caves, which are effective on the emergence and development of cave art and the rocks that generate them. The origin of cave traces to 40 thousand years and the creation of many more works of art and the importance of the rocks to the present day is very important. In particular, carbonate rocks such as limestone and marble became important spaces and raw materials in terms of art history and development. Carbonate deposits placed in the large ocean bowls during geological periods have been elevated and altered land during orogenesis periods. The fact that the carbonate rocks are soluble due to environmental conditions has led to the formation of a large number of caves depending on the size and distribution of the masses forming them. These karstic caves, which constitute a significant part of the caves in the world, have been the habitat of old people for almost 1-1.5 million years. The caves have been very important shelters for life, which became difficult due to the cold climatic conditions during the glacial periods, which were effective during the last 2 million years (Pleistocene). Under the challenging conditions of the Paleolithic period, human societies have tried to survive on the one hand and, on the other hand, achieved their symbolic thinking skills with their developing brain capacities 100,000 years ago. In the following period, the human communities that continued to develop have left very important ruins, which dates back to 40-10 thousand years ago and are regarded as works of art. Structural features of the caves and the rocks forming them are of great importance in the emergence of these works, which are interesting in their techniques as well as their thought style. Karst caves are very suitable for processing in terms of scraping, embossing and various painting techniques depending on the mineral structure of limestone. Besides, since these caves are difficult to access and are prevented from external dangers and risks, they are of great importance for the emergence of this art and reaching to the present day. Keywords: Cave, Karstic rock, Cave art

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3

Bowery, Anne-Marie, and Scott Hunter Moore. "Neither Cave nor Cage." Inquiry: Critical Thinking Across the Disciplines 18, no. 4 (1999): 36–54. http://dx.doi.org/10.5840/inquiryctnews199918412.

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4

Schmalzgruber, Hedwig. "Cave canem." Hermes 149, no. 1 (2021): 83. http://dx.doi.org/10.25162/hermes-2021-0007.

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5

Lutz, B., and M. Weintke. "Virtual Dunhuang Art Cave: A Cave within a CAVE." Computer Graphics Forum 18, no. 3 (September 1999): 257–64. http://dx.doi.org/10.1111/1467-8659.00346.

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6

Gomell, Annika K., and Andreas Pflitsch. "Airflow dynamics in Wind Cave and Jewel Cave: How do barometric caves breathe?" International Journal of Speleology 51, no. 3 (October 2022): 163–79. http://dx.doi.org/10.5038/1827-806x.51.3.2437.

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Recent research on air pressure propagation through barometric caves has revealed various speleoclimatological processes, which cause a more complex relationship between surface air pressure changes and resulting pressure gradients between cave and surface air than previously assumed. So far, however, studies on barometric cave airflow have only been based on surface air pressure measurements. Thus, this study investigates and compares airflow at the openings of Wind Cave and Jewel Cave – two major barometric cave systems in South Dakota, USA – as a response to surface air pressure changes and air pressure gradients. Based on high-resolution long-term air pressure measurements from the surfaces and several locations inside the caves, as well as ultra-sonic airflow measurements at the openings, the analysis proves that for both caves, cave airflow velocity can be predicted more accurately by air pressure gradients than by previous surface air pressure changes. An inter-cave comparison also reveals substantial differences in cave airflow dynamics between Wind Cave and Jewel Cave, with the relevant period of surface air pressure variations for cave airflow velocity and the cave reaction times being significantly longer at Jewel Cave compared to Wind Cave. Therefore, the findings of this study demonstrate the effects of cave morphology on airflow and significantly contribute to a better understanding of the speleoclimatological mechanisms and dynamics of compensating airflow at the openings of barometric caves.

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7

Bahn, Paul G. "Cave art without the caves." Antiquity 69, no. 263 (June 1995): 231–37. http://dx.doi.org/10.1017/s0003598x00064632.

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It is over a decade since Palaeolithic parietal art was first spotted in Europe on exposed open-air surfaces—cave art without the caves. Now the major site in Portugal is threatened by the lake behind a river-dam under construction. Here is a report on what cave art outside the caves amounts to, and of the confrontations over the Côa site that were in the headlines early this year.

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8

Puşcaş, Cristina M., Ferenc Kristaly, Ciprian C. Stremţan, Bogdan P. Onac, and Herta S. Effenberger. "Stability of cave phosphates: Case study from Liliecilor Cave (Trascău Mountains, Romania)." Neues Jahrbuch f??r Mineralogie - Abhandlungen: Journal of Mineralogy and Geoche 191, no. 2 (February 1, 2014): 157–68. http://dx.doi.org/10.1127/0077-7757/2014/0254.

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9

Alexandrowicz, Zofia, Jan Urban, and Viacheslav Andreychouk. "Crystal Caves in the ‘Wieliczka’ Salt Mine – unique cave site." Zeitschrift für Geomorphologie, Supplementary Issues 62, no. 3 (March 12, 2021): 235–54. http://dx.doi.org/10.1127/zfg_suppl/2021/0696.

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10

Kong, Dal-Yong, Seong-Joo Lee, Chang-Pyo Jun, and Yeong-Kyoo Kim. "Mineralogy of Guano Distributed in the Limestone Cave in Korea (Gossi Cave, Baekrong Cave, and Sungryu Cave)." Journal of the Mineralogical Society of Korea 25, no. 3 (September 28, 2012): 131–41. http://dx.doi.org/10.9727/jmsk.2012.25.3.131.

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11

Kašing, Martin, and Jan Lenart. "Cave airflow mechanism of a crevice-type cave: A case study from Czechia." International Journal of Speleology 49, no. 1 (January 2020): 55–67. http://dx.doi.org/10.5038/1827-806x.49.1.2285.

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12

Osborne, R. A. L. "Cathedral Cave, Wellington Caves, New South Wales, Australia. A multiphase, non-fluvial cave." Earth Surface Processes and Landforms 32, no. 14 (2007): 2075–103. http://dx.doi.org/10.1002/esp.1507.

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13

Kumar, Akhilesh, Gokul Prasad, Siddharth Biswas, and Jayant Biswas. "The Ecotone of River Cave, a Boon for the Fisherman: a Case Study of Mandhip Khol Cave Complex of Chhattisgarh, India." AMBIENT SCIENCE 09/10, no. 03/01 & 02 (December 2022): 57–58. http://dx.doi.org/10.21276/ambi.2022.09.3.nn03.

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14

Jhawar, S., T. Nadkarni, and A. Goel. "Meckel's Cave Neurenteric Cyst. Case Report." Central European Neurosurgery 72, S 01 (August 9, 2011): 001. http://dx.doi.org/10.1055/s-0030-1269865.

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15

Jhawar, S., A. Goel, and T. Nadkarni. "Meckel's Cave Neurenteric Cyst: Case Report." Journal of Neurological Surgery Part A: Central European Neurosurgery 73, no. 06 (August 1, 2012): 413–15. http://dx.doi.org/10.1055/s-0032-1313595.

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16

Tacconi, Leonello, Tan Arulampalam, Francis Johnston, and Lindsay Symon. "Adenocarcinoma of meckel's cave: Case report." Surgical Neurology 44, no. 6 (December 1995): 553–55. http://dx.doi.org/10.1016/0090-3019(95)00224-3.

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17

Alexander, Jr., E., and Marsha Davis. "Hydrologic Study of Jewel Cave/Wind Cave." UW National Parks Service Research Station Annual Reports 11 (January 1, 1987): 133–40. http://dx.doi.org/10.13001/uwnpsrc.1987.2651.

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The hydrologic study at Wind and Jewel Caves has the following Objectives: 1) to evaluate the water distribution within these two park areas; 2) to determine the effects of human impact upon the natural hydrologic system; 3) to document any detrimental effects to the water quality; 4) to document any instances in which the cave environment is adversely affected by the quality or quantity of the water present; and 5) to suggest options to change present water use practices, if necessary.

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18

Tran-Streitmatter, Richard. "From Plato’s Cave to the Bat Cave." ISSUE 02 (2013): 75–79. http://dx.doi.org/10.33671/iss02tra.

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19

Shim, Joo-wan. "A Comparative Study of Korean Golgul Cave-temple and the Kizil Cave-temple Cave 38, and Cave 47." Art History Journal 56 (June 30, 2021): 119–50. http://dx.doi.org/10.24828/ahj.56.119.150.

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20

Xiong, Yong, Zhongfa Zhou, Shengjun Ding, Heng Zhang, Jing Huang, Xiaohuan Gong, and Dan Su. "Spatiotemporal Variation Characteristics and Influencing Factors of Karst Cave Microclimate Environments: A Case Study in Shuanghe Cave, Guizhou Province, China." Atmosphere 14, no. 5 (April 29, 2023): 813. http://dx.doi.org/10.3390/atmos14050813.

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To systematically analyze the spatiotemporal heterogeneity, diurnal variation characteristics, and influencing factors of karst cave microclimate environments in Mahuang Cave, a cave in the Shuanghe Cave National Geological Park in Guizhou Province, China, was investigated. Monthly monitoring of meteorological and environmental parameters, such as wind speed, air pressure, humidity, and temperature indicators inside the cave and atmospheric temperature and precipitation outside the cave, was conducted from 2019 to 2021, as well as encrypted monitoring in August and December 2019. The results showed that: (1) The meteorological parameters of Mahuang Cave exhibited seasonal characteristics and cyclical interannual variation. Cave wind speed, relative humidity, and temperature were high in summer and autumn and lowest in winter, whereas cave air pressure was high in winter and low in summer. The atmospheric temperature outside the cave was the main controlling factor. (2) On a short time scale, the dewpoint and temperature of Mahuang Cave did not change significantly, and an abrupt change phenomenon occurred mostly around noon. The warm season was more sensitive than the cold season, and the closer to the entrance of the cave, the stronger the response. (3) In terms of spatial distribution, the overall microclimate factors of Mahuang Cave became increasingly stable and entered a constant state with the increasing depth of the cave passage. The related effects of cave morphology and structure, the physical environment of the cave passage, air movement, and groundwater dynamics were important factors leading to an abrupt change phenomenon in cave microclimates. Local meteorological conditions and cave geometry controlled the temporal variability and spatial heterogeneity of the cave microclimate environment.

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21

Jurado, Valme, Yolanda del Rosal, Jose Gonzalez-Pimentel, Bernardo Hermosin, and Cesareo Saiz-Jimenez. "Biological Control of Phototrophic Biofilms in a Show Cave: The Case of Nerja Cave." Applied Sciences 10, no. 10 (May 16, 2020): 3448. http://dx.doi.org/10.3390/app10103448.

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Cyanobacteria and microalgae are usually found in speleothems, rocks and walls of show caves exposed to artificial lighting. These microorganisms develop as biofilms coating the mineral surfaces and producing aesthetic, physical and chemical deterioration. A wide number of physical, chemical and environmental-friendly methods have been used for controlling the biofilms with different results. Natural biological control has been suggested by some authors as a theoretical approach but without direct evidence or application. Here we report the finding of a natural biological control of phototrophic biofilms on the speleothems of Nerja Cave, Malaga, Spain. The formation of plaques or spots where the phototrophic microorganisms disappeared can be assumed on the basis of processes of predation of bacteria, amoebas and some other organisms on the phototrophic biofilms. This study aims at investigating the potentialities of the biological control of phototrophic biofilms in caves, but the originality of these data should be confirmed in future studies with a larger number of biofilm samples in different ecological scenarios.

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22

Jurado, Valme, Mariona Hernandez-Marine, Miguel Angel Rogerio-Candelera, Francisco Ruano, Clara Aguilar, Juan Aguilar, and Cesareo Saiz-Jimenez. "Cleaning of Phototrophic Biofilms in a Show Cave: The Case of Tesoro Cave, Spain." Applied Sciences 12, no. 15 (July 22, 2022): 7357. http://dx.doi.org/10.3390/app12157357.

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Show caves have different grades of colonization by phototrophic biofilms. They may receive a varied number of visits, from a few thousand to hundreds of thousands of visitors annually. Among them, Tesoro Cave, Rincon de la Victoria, Spain, showed severe anthropic alterations, including artificial lighting. The most noticeable effect of the lighting was the growth of a dense phototrophic community of cyanobacteria, algae and bryophytes on the speleothems, walls and ground. The biofilms were dominated by the cyanobacterium Phormidium sp., the chlorophyte Myrmecia israelensis, and the rhodophyte Cyanidium sp. In many cases, the biofilms also showed an abundance of the bryophyte Eucladium verticillatum. Other cyanobacteria observed in different biofilms along the cave were: Chroococcidiopsis sp., Synechocystis sp. and Nostoc cf. edaphicum, the green microalgae Pseudococcomyxa simplex, Chlorella sp. and the diatom Diadesmis contenta. Preliminary cleaning tests on selected areas showed the effectiveness of hydrogen peroxide and sodium hypochlorite. A physicochemical treatment involving the mechanical removal of the thickest layers of biofilms was followed by chemical treatments. In total, 94% of the surface was cleaned with hydrogen peroxide, with a subsequent treatment with sodium hypochlorite in only 1% of cases. The remaining 5% was cleaned with sodium hypochlorite in areas where the biofilms were entrapped into a calcite layer and in sandy surfaces with little physical compaction. The green biofilms from the entire cave were successfully cleaned.

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23

Gomell, Annika, Daniel Austin, Marc Ohms, and Andreas Pflitsch. "Air pressure propagation through Wind Cave and Jewel Cave: How do pressure waves travel through barometric caves?" International Journal of Speleology 50, no. 3 (September 2021): 263–73. http://dx.doi.org/10.5038/1827-806x.50.3.2393.

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In barometric caves, air pressure gradients between the outside atmosphere and the cave induce strong bidirectional compensating currents, which control almost all elements of speleoclimatology, including air temperature, humidity, and CO2 dynamics. Therefore, this study set out to investigate air pressure propagation through Wind Cave and Jewel Cave – two major barometric cave systems in the Black Hills of South Dakota, USA. Based on high-resolution air pressure data from both the surface and several measurement sites inside the caves, four systematic changes of pressure waves during their journey through the caves and their related speleoclimatological processes were identified and discussed: Compared to the outside atmosphere, the pressure signals within Wind Cave and Jewel Cave showed (1) an absolute displacement due to different altitudes of the measuring sites, (2) a delay related to the travel times of the pressure wave to the measuring sites, (3) a smoothing effect, and (4) a damping effect due to long response times of the caves to external pressure changes. The spatial distribution of the changes observed in this study shows that for Wind Cave, the cave opening and the narrow entrance area represent the main obstacle for pressure propagation, while for Jewel Cave, the deep areas have the greatest influence on the development of air pressure gradients. Our analyses provide completely new insights into the processes and mechanisms inside barometric caves, which will significantly contribute to the understanding of pressure-related airflow dynamics and all related elements of speleoclimatology.

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24

Sinaga, Firman, Angelia Hendri, and Gusti Ayu Praminatih. "Strategi Pemasaran Cafe Monkey Cave Espresso Pada Era New Normal." Jurnal Ilmiah Pariwisata dan Bisnis 2, no. 7 (July 30, 2023): 1471–87. http://dx.doi.org/10.22334/paris.v2i7.466.

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Tujuan dari dilakukannya penelitian ini adalah untuk menganalisis faktor IFAS dan EFAS dengan menggunakan analisis SWOT di Monkey Cave Espresso Ubud. Jenis data yang digunakan yaitu data kuatitaif dan kualitatif. Yang merupakan data kualitatif dari penelitian ini adalah strategi pemasaran dan sejarah Monkey Cave Espresso dan yang merupakan data kuantitatif adalah kuisioner IFAS dan EFAS serta harga produk di Monkey Cave Espresso Ubud. Data sekunder diperoleh dari internet, media sosial dan kerabat sedangkan data primer diperoleh dari hasil obeservasi, kuisioner dan wawancara mengenai indikator-indikator yang dirumuskan dalam penelitian ini serta hasil dari pemberian bobot dan rating IFAS dan EFAS. Teknik analisis data yang digunakan adalah metode deskriptif kualitatif, analisis SWOT, IFAS, EFAS, kuadran dan matriks SWOT. Berdasarkan hasil dari analisis SWOT, Hasil dari analisis IFAS dan EFAS di Monkey Cave Espresso Ubud yaitu berada pada koordinat X=0,6 dan koordinat Y= 0,17 atau berada kuadran 2 (diversifikasi) yang artinya Monkey Cave Espresso Ubud menghadapi beberapa ancaman perusahaan, maupun strategi pemasaran namun Monkey Cave Espresso masih memiliki kekuatan dari segi internal. Jadi, fokus dari Monkey Cave Espresso adalah dengan memaksimalkan kekuatan yang dimiliki untuk memanfaatkan peluang. Monkey Cave Ubud disarankan untuk merubah strateginya untuk lebih memaksimalkan strategi pemasaran melalui Digital Marketing, Endorsement dan WOM (Word Of Mouth) yang berbasis MLM (Multi Level Marketing) hal ini dapat disimpulkan karena dilihat dari target pasar yang dimiliki sebagian besar adalah para generasi Z yang sangat aktif di media sosial atau dunia maya. The result of this research is to analyze the IFAS and EFAS factors by using SWOT analysis at Monkey Cave Espresso Ubud. The types of data used are quantitative and qualitative data. The qualitative data from this research is the marketing strategy and history of Monkey Cave Espresso and quantitative data is the IFAS and EFAS questionnaires and product prices at Monkey Cave Espresso Ubud. Secondary data was obtained from the internet, social media and relatives while primary data was obtained from the results of observations, questionnaires and interviews regarding the indicators formulated in this study as well as the results of weighting and rating of IFAS and EFAS. The data analysis technique used is descriptive qualitative method, SWOT analysis, IFAS, EFAS, quadrant and SWOT matrix. Based on the results of the SWOT analysis, the results of the IFAS and EFAS analysis at Monkey Cave Espresso Ubud are located at coordinates X = 0.6 and coordinates Y = 0.17 or are in quadrant 2 (diversification) which means Monkey Cave Espresso Ubud faces several corporate threats. , as well as marketing strategies, but Monkey Cave Espresso still has internal strength. So, the focus of Monkey Cave Espresso is to maximize its strengths to take advantage of opportunities. Monkey Cave Ubud is advised to change its strategy to further maximize its marketing strategy through Digital Marketing, Endorsement and WOM (Word Of Mouth) based on MLM (Multi Level Marketing). very active on social media or cyberspace.

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25

Frieda Wiley, special to C&EN. "Etosha Cave." C&EN Global Enterprise 99, no. 6 (February 22, 2021): 68–69. http://dx.doi.org/10.1021/cen-09906-feature20.

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26

Isaakyan, Irina L. "Cyclops Cave." Symbolic Interaction 32, no. 3 (August 2009): 207–35. http://dx.doi.org/10.1525/si.2009.32.3.207.

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27

Privett, Katharine. "Outlaws' Cave." College English 48, no. 5 (September 1986): 459. http://dx.doi.org/10.2307/377089.

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28

Cazabon, Lynn. "Plato’s Cave." Afterimage 33, no. 2 (September 2005): 45–46. http://dx.doi.org/10.1525/aft.2005.33.2.45.

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29

Ernst, Edzard. "Cave kava?" Focus on Alternative and Complementary Therapies 7, no. 4 (December 2002): 323–24. http://dx.doi.org/10.1211/fact.2002.00431.

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30

Fava, Giovanni Andrea. "CAVE CANEM." Ärztliche Psychotherapie 16, no. 4 (November 2021): 273–74. http://dx.doi.org/10.21706/aep-16-4-273.

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31

Sellars, Shaun. "The cave." British Dental Journal 231, no. 2 (July 2021): 75. http://dx.doi.org/10.1038/s41415-021-3277-4.

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32

Postel-Vinay, Olivier. "Cave hominem." Books N° 49, no. 12 (December 1, 2013): 5. http://dx.doi.org/10.3917/books.049.0005.

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33

Morris, T. F. "Plato's Cave." Southwest Philosophy Review 23, no. 2 (2007): 85–110. http://dx.doi.org/10.5840/swphilreview200723241.

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34

Morris, T. F. "Plato’s Cave." South African Journal of Philosophy 28, no. 4 (January 2009): 415–32. http://dx.doi.org/10.4314/sajpem.v28i4.52982.

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35

Taleb-Khyar, Mohamed B. "Syto Cave." Callaloo 15, no. 2 (1992): 538. http://dx.doi.org/10.2307/2931275.

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36

Maren, Mesha. "Organ Cave." Ecotone 14, no. 2 (2019): 118–33. http://dx.doi.org/10.1353/ect.2019.0045.

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37

MERIKANGAS, JAMES R. "The Cave." American Journal of Psychiatry 161, no. 12 (December 2004): 2335–36. http://dx.doi.org/10.1176/appi.ajp.161.12.2335.

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38

Huebner, J., and C. R. Arciola. "Cave Enterococcum!" International Journal of Artificial Organs 30, no. 9 (September 2007): 852–53. http://dx.doi.org/10.1177/039139880703000915.

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39

Ezzell, Carol. "Cave Creatures." Science News 141, no. 6 (February 8, 1992): 88. http://dx.doi.org/10.2307/3976505.

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40

Gabel-Hartman, Laura. "Man Cave." Red Cedar Review 45, no. 1 (2010): 77–88. http://dx.doi.org/10.1353/rcr.0.0082.

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41

O'Mahony, C. "The cave." Sexually Transmitted Infections 78, no. 1 (February 1, 2002): 70. http://dx.doi.org/10.1136/sti.78.1.70.

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42

M.K. "Cave Paintings." Americas 42, no. 2 (October 1985): 248. http://dx.doi.org/10.1017/s0003161500051683.

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43

PRAG, JONATHAN R. W. "CAVE NAVEM." Classical Quarterly 56, no. 2 (December 2006): 538–47. http://dx.doi.org/10.1017/s0009838806000528.

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44

McGrath, Sean E. "Cave hominem." Mnemosyne 73, no. 1 (January 20, 2020): 87–111. http://dx.doi.org/10.1163/1568525x-12342553.

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Abstract This article explores two episodes from Pseudo-Oppian’s Cynegetica which both feature domestic animals: the horse in 1.239-270 and the dog in 4.354-376. Both of these episodes are highly intertextual, alluding to, respectively, Sophocles’ Oedipus Tyrannus and the abduction narratives from Moschus’ Europa and the Homeric Hymn to Demeter. I argue that the poet of the Cynegetica invites his readers to reflect on the potentially problematic nature of the power dynamic for these animals through sophisticated allusions to the poetic tradition, through which the relationship between man and animal is compared to that between the gods and humans.

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45

Graffin, B., C. Landais, J. M. Cournac, A. S. Lecot, C. Treglia, J. F. Paris, P. Carli, and O. Lambotte. "Cave judokanem." La Revue de Médecine Interne 30, no. 1 (January 2009): 91–95. http://dx.doi.org/10.1016/j.revmed.2008.09.002.

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46

Burki, Talha. "The Cave." Lancet Respiratory Medicine 7, no. 12 (December 2019): 1013. http://dx.doi.org/10.1016/s2213-2600(19)30412-6.

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47

Sabancı, Pulat Akın, Funda Batay, Erdinç Civelek, Ossama Al Mefty, Muhammad Husain, Saleem I. Abdulrauf, and Aykut Karasu. "Meckel's Cave." World Neurosurgery 76, no. 3-4 (September 2011): 335–41. http://dx.doi.org/10.1016/j.wneu.2011.03.037.

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48

Luce, Cynthia Newby. "Cave writing." New Scientist 205, no. 2752 (March 2010): 25. http://dx.doi.org/10.1016/s0262-4079(10)60656-2.

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49

Bischoff, Angelika. "Cave: Kardionotfall!" MMW - Fortschritte der Medizin 158, S3 (November 2016): 12–16. http://dx.doi.org/10.1007/s15006-016-8929-y.

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Cuchet, M., A. L. Lepage, M. Auzou, C. Picard, and L. Verneuil. "Cave canum !" Annales de Dermatologie et de Vénéréologie 144, no. 12 (December 2017): S283. http://dx.doi.org/10.1016/j.annder.2017.09.467.

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