Bubble-Induced Cave Collapse

Conventional wisdom among cave divers is that submerged caves in aquifers, such as in Florida or the Yucatan, are unstable due to their ever-growing size from limestone dissolution in water. Cave divers occasionally noted partial cave collapses occurring while they were in the cave, attributing this to their unintentional (and frowned upon) physical contact with the cave walls or the aforementioned “natural” instability of the cave. Here, we suggest that these cave collapses do not necessarily result from cave instability or contacts with walls, but rather from divers bubbles rising to the ceiling and reducing the buoyancy acting on isolated ceiling rocks. Using familiar theories for the strength of flat and arched (un-cracked) beams, we first show that the flat ceiling of a submerged limestone cave can have a horizontal expanse of 63 meters. This is much broader than that of most submerged Florida caves (~ 10 m). Similarly, we show that an arched cave roof can have a still larger expanse of 240 meters, again implying that Florida caves are structurally stable. Using familiar bubble dynamics, fluid dynamics of bubble-induced flows, and accustomed diving practices, we show that a group of 1-3 divers submerged below a loosely connected ceiling rock will quickly trigger it to fall causing a “collapse”. We then present a set of qualitative laboratory experiments illustrating such a collapse in a circular laboratory cave (i.e., a cave with a circular cross section), with concave and convex ceilings. In these experiments, a metal ball represented the rock (attached to the cave ceiling with a magnet), and the bubbles were produced using a syringe located at the cave floor.     

The biogeochemical role of Actinobacteria in Altamira Cave, Spain

The walls and ceiling of Altamira Cave, northern Spain, are coated with different coloured spots (yellow, white and grey). Electron microscopy revealed that the grey spots are composed of bacteria and bioinduced CaCO(3) crystals. The morphology of the spots revealed a dense network of microorganisms organized in well-defined radial and dendritic divergent branches from the central area towards the exterior of the spot, which is coated with overlying spheroidal elements of CaCO(3) and CaCO(3) nest-like aggregates. Molecular analysis indicated that the grey spots were mainly formed by an unrecognized species of the genus Actinobacteria. CO(2) efflux measurements in rocks heavily covered by grey spots confirmed that bacteria-forming spots promoted uptake of the gas, which is abundant in the cave. The bacteria can use the captured CO(2) to dissolve the rock and subsequently generate crystals of CaCO(3) in periods of lower humidity and/or CO(2). A tentative model for the formation of these grey spots, supported by scanning electron microscopy and transmission electron microscopy data, is proposed.     

Uncovering the origin of the black stains in Lascaux Cave in France

Lascaux Cave in France was discovered in 1940. Since being opened to visitors the cave has suffered three major microbial outbreaks. The current problem is the fast dissemination of black stains which are threatening the Palaeolithic paintings. Previous data pointed to the involvement of new fungal species in the formation of black stains on the rock walls and ceiling. However, it appears that there could be other reasons for the formation of different and extensive black stains coating the surface of the clayey sediments. Our analyses reveal that black stains on clayey sediments are mainly produced by Acremonium nepalense, a manganese oxide‐depositing fungus, widely distributed in the cave. Thus, in Lascaux Cave, the black stains have a dual origin: on limestone rocks they are mainly produced by the accumulation of fungal melanins, and on clayey sediments by the biogenic deposition of black manganese oxides.     

Big family,warm home,and lots of friends: Pteronotus large colonies affect species richness and occupation inside caves

Roosts are essential for the survival of most animals. Due to homothermic requirements, mammals are particularly dependent on roost quality and availability. Bats select their roosts in a species-specific way, likely related to species´ different physiological and adaptive needs. Unlike species whose individuals roost solitarily, roost selection is critical for bats forming large colonies due to the requirements for maintaining thousands of individuals in a single shelter. This is the case of Pteronotus (Mormoopidae), whose colonies reach hundreds of thousands of bats. Using captures, bioacoustics, and automated censuses, we evaluated how cave size, ceiling characteristics, environmental stability, temperature, and humidity influence the formation of exceptionally large colonies, species richness and composition in caves in north-eastern Brazil. We expected that colonies would be positively related to cave size and stability, internal cave selection would be species-specific, but larger and more environmentally stable caves would have higher richness. Pteronotus colonies were positively related to cave size, stability, and ceiling characteristics, and their presence strongly influenced cave temperature variation. Species richness was positively correlated to a cave stability index. Species other than Pteronotus preferred different climatic and ceiling characteristics. We detected an indirect influence of the large colonies of Pteronotus on the species richness and occupation inside caves. On the other hand, such caves favor species coexistence, as they offer a range of microenvironments, reducing niche overlap in their interior. Pteronotus gymnonotus and Pteronotus personatus are both key- and umbrella-species for cave ecosystems, stressing the need for specific conservation strategies in Brazil. Abstract in Portuguese is available with online material.     

Exceptional record of submarine cave communities from the Pleistocene of Sicily (Italy)

An Early Pleistocene benthic community, discovered inside the Rumena Cave in NW Sicily, Italy, was studied. Analysis of the community led to the recognition of several encrusting species – notably scleractinians, bryozoans, serpuloideans, cirripeds, foraminifera and brachiopods – and borings mostly referable to the ichnogenus Gastrochaenolites. All fossils detected are typical of the present‐day hard‐surface submarine cave biota, at both high taxonomic rank and species level. The biogenic crust, restricted to a few sectors of the cave but locally up to few centimetres thick, largely consist of scleractinians, mainly represented by dendrophylliids. Bryozoans and serpuloideans are also present with Hippaliosina depressa and Spiraserpula massiliensis, locally forming multi‐layered sheets and dense specimen aggregates, respectively. Basing mostly on the composition of the encrusting community and on morphological/morphometric features of some species, it has been hypothesized that at least part of the cave was blind when the crust formed, possibly at relatively shallow depth in a sheltered setting or, more probably, at higher depths, below the fair weather swell zone. Encrustations and borings on the rocky cave ceiling and on occasional speleothems broken surfaces document subsequent phases of cave submersion/colonization separated by emersion/erosion phases. The importance of the Early Pleistocene fossils of the Rumena Cave for the knowledge of submarine cave communities through time and for the understanding of sea‐level variations and the uplift of the area has been remarked.     

Geomicrobiological Study of the Grotta dei Cervi,Porto Badisco,Italy

Speleothems (active stalactites, wall concretions), rock walls, ceiling, and soils from the galleries of Grotta dei Cervi, Porto Badisco, Italy, were sampled to investigate the culturable heterotrophic microbial communities present in this cave. Sampling was carried out in a transect of about 230 m from the entrance to the central gallery where numerous Gram-positive bacteria were isolated from all studied sites. Members of the genera Agromyces, Arthrobacter, Rhodococcus , and particularly Streptomyces , of the order Actinomycetales, are spread throughout the whole cave. The ability of actinomycetes, and particularly of Nocardiopsis , to colonize salt-stressed environments is favored by the presence of ectoine, a compatible solute for osmotic adaptation. Selected actinomycete isolates were tested for the formation of crystals. Strains from all tested genera, except isolates of Gordonia and Nocardia , produced vaterite and/or calcite. Production of Mgcalcite was restricted to strains of Brachybacterium, Rhodococcus , and Streptomyces , whereas struvite was only precipitated by an unidentified isolate. These findings indicate that actinomycetes may play a role in the formation of mineral deposits in caves.     

Micromammals (rodents and insectivores) from the early Late Pleistocene cave site of Bois Roche (Charente, France): Systematics and paleoclimatology

We present the study of rodents and insectivores from the 1995 season of excavation at the early Late Pleistocene site of Bois Roche (Charente, France). The site is a small cave with a low ceiling, used as a den by hyenas. It contains a large herbivore assemblage (mainly bovids and equids) with a smaller representation of medium-size taxa (cervids), many microvertebrates, abundant coprolites and deciduous hyena teeth, and a few lithic artifacts (Middle Paleolithic) introduced into the cave by gravity and slope wash. The rodent fauna consists of Eliomys quercinus cf. quercinus, Apodemus sp., Microtus gregalis, Microtus oeconomus, Arvicola terrestris and Dicrostonyx torquatus. Insectivores are represented by Neomys cf. fodiens. The most common species is M. gregalis which forms 93.7% of the total MNI. The micromammal fauna suggests an open landscape, with some vegetation mainly of the steppe or tundra type, with areas of water and more wet vegetation and some areas with trees. The micromammal association of Bois Roche is characteristic of a cold or very cold dry climate.     

Involvement of Microorganisms in the Formation of Carbonate Speleothems in the Cervo Cave (L'Aquila-Italy)

Much is known about the bacterial precipitation of carbonate rocks, but comparatively little is known about the involvement of microbes in the formation of secondary mineral structures in caves. We hypothesized that bacteria isolated from calcareous stalactites, which are able to mediate CaCO₃ precipitation in vitro, play a role in the formation of carbonate speleothems. We collected numerous cultivable calcifying bacteria from calcareous speleothems from Cervo cave, implying that their presence was not occasional. The relative abundance of calcifying bacteria among total cultivable microflora was found to be related to the calcifying activity in the stalactites. We also determined the δ ¹³C and δ ¹⁸ O values of the Cervo cave speleothems from which bacteria were isolated and of the carbonates obtained in vitro to determine whether bacteria were indeed involved in the formation of secondary mineral structures. We identified three groups of biological carbonates produced in vitro at 11°C on the basis of their carbon isotopic composition: carbonates with δ ¹³C values (a) slightly more positive, (b) more negative, and (c) much more negative than those of the stalactite carbonates. The carbonates belonging to the first group, characterized by the most similar δ ¹³C values to stalactites, were produced by the most abundant strains. Most of calcifying isolates belonged to the genus Kocuria. Scanning electron microscopy showed that dominant morphologies of the bioliths were sherulithic with fibrous radiated interiors. We suggest a mechanism of carbonate crystal formation by bacteria.     

织金洞钟乳石沉积物表面可培养细菌多样性和网络分析

【背景】洞穴环境中蕴含丰富而独特的细菌资源,对洞穴环境中细菌的分离培养有助于了解洞穴细菌多样性及细菌资源的挖掘和利用。【目的】利用不同培养基分离细菌,探究钟乳石表面可培养细菌的多样性及其种间互作关系。【方法】通过11种培养基对织金洞内钟乳石沉积物表面的细菌进行分离纯化,并利用16S rRNA基因序列分析初步确定分离菌株的分类地位。在R软件下,通过Bipartite包分析可培养细菌属间的相互作用。【结果】从钟乳石沉积物表面共分离出206株细菌,它们隶属于4门25属45种,香农(Shannon)指数为4.78,辛普森(Simpson)指数为0.95。变形菌门(Proteobacteria)和芽孢杆菌属(Bacillus)分别为样品中可培养细菌的优势门(47.09%)和优势属(29.61%)。无机寡营养培养基有助于洞穴钟乳石沉积物细菌的分离。属水平-采样点网络分析表明,可培养细菌分布具有非随机、显著的嵌套性。芽孢杆菌属(Bacillus)、德沃斯氏菌属(Devosia)、产碱杆菌属(Alcaligenes)、节杆菌属(Arthrobacter)和短杆菌属(Brevibacterium)在细菌群落中存在较多的有效合作值(Effective Partners)和亲密度(Closeness),被其他细菌所依赖程度(Species Strength)较高,是该群落中的重要组成类群。【结论】织金洞内钟乳石沉积物表面存在丰富的细菌资源,分析细菌类群在群落中的作用应结合细菌相对丰度和网络分析。     

An Artiodactyl Tracksite at Musandam Peninsula,Sultanate of Oman

Here we report an artiodactyl trackway from Musandam Peninsula, Sultanate of Oman. Epireliefs of the tracks are preserved in poorly consolidated aeolian deposits now making up the ceiling of a coastal cave. As an interesting morphological feature, the trackway documents the trackmaker negotiating a slippery dune slope at an angle.     

Detection of bacterial cytotoxic activities from water-damaged ceiling tile material following incubation on blood agar

Samples of ceiling tiles with high levels of bacteria exhibited cytotoxic activities on a HEP-2 tissue culture assay. Ceiling tiles containing low levels of bacterial colonization did not show cytotoxic activities on the HEP-2 tissue culture assay. Using a spread plate procedure on blood agar plates, the levels of bacteria colonizing portions of cellulosic indoor ceiling tiles were easily identified. Levels of bacteria measured by this simple procedure may be a good indicator of microbial colonization of indoor building materials especially in the case of water damage. We suggest that bacterial levels above 150 CFU g⁻¹ of ceiling tile material indicate colonization has occurred. Received 24 December 1998/ Accepted in revised form 26 March 1999     

Refuge from predation, the benefit of living in an extreme acidic environment?

Organisms living in extreme habitats require costly adaptations to cope with these conditions. Among the suggested potential benefits that trade off these costs is refuge from predation. To study these interactions in extreme environments, samples were taken in the cave Cueva de Villa Luz, Tabasco, Mexico, where more than 32 subterranean springs, some H(2)S rich, rise from the floor. Hydrogen sulfide gas plus oxygen is absorbed by freshwater, and oxidation forms concentrated sulfuric acid. Snottites, whitish hollow mucous tubes, hang from the ceiling of the cave. Fluid drops from these snottites were recorded as having pH values of 0-3. We report the discovery of a new species of nematode that thrives in the highly acidic environment of the snottite. Micro CT scan of snottites reveals a complex interaction between the acidic snottite, nematodes, and abundant nematode-eating mites. The nematode adaptation to low pH probably protects them against mite predation, for which nematodes are most likely the most important source of carbon in this sulfur-driven ecosystem.     

中华菊头蝠的栖息生态特征及种群保护

中华菊头蝠(Rhinolophus sinicus)主要分布于我国境内,属于典型的洞栖食虫性蝙蝠,具有重要的研究意义与保护价值。近年,在湘西州境内的16个溶洞中对其栖息生态特征进行了观察,共记录到其个体12942只次,数据分析结果显示：该蝠是该区域溶洞中的居留型优势蝠种,具有集群冬眠的习性。每年的9月中下旬开始逐步聚群冬眠,翌年的3月底开始苏醒,其夏季的繁育场所非常隐蔽,通常位于人无法进入的洞段或人迹罕至的洞穴。总体上,其栖点主要集中于距洞口150—200 m(91.60%)的洞段,离地高度6—10 m(91.75%),多以“双足悬挂”的栖姿将身体悬空倒挂于洞道的顶壁。其体温与栖点温度之间不存在显著性差异(P>0.05),但具有明显的线性正相关关系(R~2=0.8886)。其栖点安全性春夏季高,秋冬季中等偏低。中华菊头蝠作为该区域洞栖性蝙蝠的优势种,在维持洞穴生态系统的稳定中发挥着至关重要的作用,加强对洞穴生态系统中蝙蝠伞护性的研究有助于洞穴生态保护教育及对蝙蝠种群的保护实践。     

Quartz et quartzite dans le site de Payre (MIS 7 et 5, Ardèche,France) : données techno-économiques sur la gestion de roches locales au Paléolithique moyen

The results of studies applied to pieces made of quatrz and quartzite at the site of Payre (isotopic stages 7 and 5) testify to the peculiar handling of these stones which were collected in the neighbourhood of the site and are little abundant in the assemblages found. The two rocks were worked outside the cave, according to techniques similar to those applied in the case of silex. These observations concern all the levels of the sequence. The techno-economic study of the artefacts indicates a handling of these materials that exceeds the strict frame of the site, such as rocks being often considered as a makeshift complement and little used in the sites of the Rhone middle valley.     

Multivariate Analysis of Copepod Assemblages in Epikarstic Waters of Some Slovenian Caves

A series of sampling sites in 6 caves was established in order to assess the importance of the epikarst as a habitat of high diversity of meiofauna. Special attention was given to the stygobiotic species of copepods (Crustacea), which was the most abundant group of animals in water percolating from the epikarst. In total, 37 species of Copepoda were identified from nearly 4000 individuals. To understand epikarst as a habitat, 14 structural and physico-chemical factors were analysed and compared for two types of habitats, i.e., trickles and pools filled with percolation water. Results of canonical correspondence analysis indicated that the significant factors influencing faunal composition in trickles were the thickness of the cave ceiling and the concentrations of sodium, nitrate, and potassium ions, while in pools correlations between individual species and pH, temperature, volume, conductivity and thickness of the cave ceiling were statistically significant. Aquatic copepod assemblages in epikarst encompass species of different taxonomic affinities, living in severe environmental conditions. The pattern of the system reflects both high taxonomic diversity and environmental severity.     

The Occurrence of Fungi in the Recently Discovered Jarkowicka Cave in the Karkonosze Mts. (Poland)

Our study is one of the very few cases of speleomycological research in recently discovered caves. The aim of this research was to assess the population size of fungal colonies and their species composition in the Jarkowicka cave, discovered in 2012. The air samples were taken from one location outside the cave and from two locations inside of it. Mycological evaluation of the rocks inside the cave was performed usingswab sampling procedure. In the Jarkowicka cave we found 22 species of fungi, including 13 isolated from air at the entrance and from the walls, and 8 species from air inside the cave. Cladosporium spp. were the fungi most frequently isolated from internal atmosphere of the Jarkowicka cave, and from the external air. On the other hand, the fungi most frequently isolated from the rocks were Mucor spp. We found several species not yet described as cave inhabitants: Hypocrea pachybasioides, Cladosporium uredinicola, and Embellisia abundans. Our study may provide a basis for comparison to other similar studies conducted in frequently visited caves by tourists.     

Prokaryotic and Eukaryotic Airborne Microorganisms as Tracers of Microclimatic Changes in the Underground (Postojna Cave, Slovenia)

Bioaerosols in cave air can serve as natural tracers and, together with physical parameters, give a detailed view of conditions in the cave atmosphere and responses to climatic changes. Airborne microbes in the Postojna Cave system indicated very dynamic atmospheric conditions, especially in the transitory seasonal periods between winter and summer. Physical parameters of cave atmosphere explained the highest variance in structure of microbial community in the winter and in the summer. The airborne microbial community is composed of different microbial groups with generally low abundances. At sites with elevated organic input, occasional high concentrations of bacteria and fungi can be expected of up to 1,000?colony-forming units/m(3) per individual group. The most abundant group of airborne amoebozoans were the mycetozoans. Along with movements of air masses, airborne algae also travel deep underground. In a cave passage with elevated radon concentration (up to 60?kBq/m(3)) airborne biota were less abundant; however, the concentration of DNA in the air was comparable to that in other parts of the cave. Due to seasonal natural air inflow, high concentrations of biological and inanimate particles are introduced underground. Sedimentation of airborne allochthonous material might represent an important and continuous source of organic material for cave fauna.     

A Study on actinobacterial diversity of Hampoeil cave and screening of their biological activities

Caves are oligotrophic, dark and less-explored environments and are considered as sources of promising microbial strains in biotechnology. Hampoeil Cave is located in massive dolomite with thin bedded limestone in northwestern of Iran. In an isolation and screening program, various samples from soil, water, floor, wall and ceiling of Hampoeil cave and its invertebrates were collected. Four various treatments and 10 different isolation media were used for the isolation of the actinobacteria. Screening of the isolates for antimicrobial activity against 10 bacteria and fungi, 5 hydrolytic enzymes production and resistance to 5 heavy metals have been performed. Among 33 various samples, 76 actinobacteria from various genera, including Streptomyces, Micromonospora, Micrococcus, Kocuria and Corynebacterium were isolated. Eighty percent of the strains had one of the studied hydrolytic enzyme activity. At least one type of antimicrobial activity was seen in 25.3% of the isolates. Resistance to one metal or more was seen in 26.32% of the isolates. The ratio of rare-actinobacteria in the oligotrophic samples to enriched samples is 20% more than Streptomyces. Percentage of strains with the highest activity in esterase, amylase, DNase, protease or lipase activity that were isolated from organic-rich environmental samples were 100, 100, 100, 82 and 82%, respectively. Also, 26.32% of the actinobacterial isolates resisted to heavy metals. It was concluded that Hampoeil cave is a good source in finding cave-living actinobacteria potent in producing hydrolytic enzymes and bioremediation.     

Cultivable microscopic fungi from an underground chemosynthesis-based ecosystem: a preliminary study

Movile Cave, a unique groundwater ecosystem in southern Romania, was discovered in 1986. This chemoautotrophic cave contains an abundant and diverse fauna with terrestrial and aquatic invertebrate communities, including 33 endemic species. Since its discovery, studies have focused mainly on cave chemoautotrophic bacteria, while the microfungal community has been largely neglected. In this study, we determined the microfungal species living on various substrates in Movile Cave and compared this spectrum with the mycobiota detected outside the cave (outside air-borne and soil-borne microfungi). To investigate all of the niches, we collected samples for two consecutive years from the dry part of the cave (cave air and sediment, corroded limestone walls, isopod feces, and isopod and spider cadavers) and from the post-siphon part of the cave, i.e., Airbell II (sediment and floating microbial mat). A total of 123 microfungal species were identified from among several hundred isolates. Of these, 96 species were only detected in the cave environment and not outside of the cave, while 90 species were from the dry part of the cave and 28 were from Airbell II. The most diverse genera were Penicillium (at least 18 species) and Aspergillus (14 species), followed by Cladosporium (9 species). Surprisingly, high CFU counts of air-borne microfungi were found inside the cave; they were even higher than outside the cave during the first year of investigation.     

洞穴微生物组:已知与未知

洞穴是由于岩石受到溶蚀或火山岩浆冷却形成的地下空间和通道。洞穴遍布世界各地,蕴藏着大量的微生物资源。洞穴内黑暗潮湿,温度相对稳定,营养比较贫瘠,是一种极端的生态系统,存在着高度特异性的洞穴微生物。对洞穴微生物组的研究,有助于认知洞穴微生物群体结构、组成及其地理学分布,加深对洞穴生态系统的理解,并为保护和开发洞穴资源提供指导。本文主要介绍了洞穴微生物组的研究方法,总结分析了洞穴微生物的研究进展,并着重阐述了含特殊化合物成分的洞穴中化能自养的特色微生物组。