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Subterranean medicine: an inquiry into underground medical treatment protocols in cave rescue situations in national parks in the United States.

Caving and spelunking have become increasingly popular over the years, with hundreds of thousands of amateur spelunkers across the country visiting caves. National parks in the United States offer hundreds of caves for all levels of spelunkers and, in fact, many national parks boast caves as either their main or major attraction. In an effort to increase visitor safety and establish subterranean medical treatment protocols, we began an investigation into cave rescue, medical protocols, previously published recommendations concerning cave safety, and visitor and rescue statistics in the national parks. Our inquiry provided little guidance from either the literature or the present US National Parks database for treating underground injuries. However, 2 predominant trends did appear. First, despite the nearly 2 million visitors to the caves in the 14 parks surveyed, there were only about 200 total calls for medical care. The vast number of those calls were for minor injuries. Second, no strict evidence-based treatment protocols for underground injuries exist, probably because they are not feasible. A caving incident database for the national parks would facilitate suggestions for preventative measures for the minor injuries and would help catalog the creative solutions for the rare serious subterranean medical incident.

Emergency Treatment↗

Leptogenys khammouanensis sp. nov. (Hymenoptera: Formicidae). A possible troglobitic species of Laos, with a discussion on cave ants.

The new species Leptogenys khammouanensis sp. nov. is described from two caves of the Khammouan karst (Laos). It is characterized by a set of striking morphological characters (reduced eyes, light pigmentation, slender body and very elongated legs and antennae), which recall the troglobiomorphic traits of cave arthropods. Relations between caves and ants are discussed at this occasion, in the light of the recent biological explorations of caves in Southeast Asia. The classical view that ants are rare and unimportant in caves is challenged. Ants are actually major and regular components of guano assemblages in many caves of the region, but none of these guano species exhibit cave-related adaptation in its external morphology. Conversely, ants are very rare in low-resources habitats, where only accidental occurrence of outside species are reported in Southeast Asia. Leptogenys khammouanensis has been found only in such an oligotrophic environment, very deep in the cave and far from any guano deposits. Its presence there, together with its troglobiomorphic traits, support the idea that Leptogenys khammouanensis might be the first truly troglobitic ant.

Animals↗

Analysis of the main factors affecting the evaluation of the radon dose in workplaces: the case of tourist caves.

High concentrations of radon exist in several workplaces like tourist caves mainly because of the low ventilation rates existing at these enclosures. In this sense, in its 1990 publication, the ICRP recommended that high exposures of radon in workplaces should be considered as occupational exposure. In developed caves in which guides provide tours for the general public great care is needed for taking remedial actions concerning radon, because in some circumstances forced ventilation may alter the humidity inside the cave affecting some of the formations or paintings that attract tourists. Tourist guides can work about 1900 h per year, so the only option to protect them and other cave workers from radon exposure is to apply an appropriate system of radiation protection mainly based on limitation of exposure by restricting the amount of time spent in the cave. Because of the typical environmental conditions inside the caves, the application of these protecting actions requires to know some indoor air characteristics like particle concentration, as well as radon progeny behaviour in order to get more realistic effective dose values In this work the results of the first two set of radon measurements program carried out in 10 caves located in the region of Cantabria (Spain) are presented.

Air Pollutants, Occupational↗

Radon in the creswell crags Permian limestone caves.

An investigation of radon levels in the caves of Creswell Crags, Derbyshire, an important Site of Special Scientific Interest (SSSI) shows that the Lower Magnesian Limestone (Permian) caves have moderate to raised radon gas levels (27-7800 Bq m(-3)) which generally increase with increasing distance into the caves from the entrance regions. This feature is partly explained in terms of cave ventilation and topography. While these levels are generally below the Action Level in the workplace (400 Bq m(-3) in the UK), they are above the Action Level for domestic properties (200 Bq m(-3)). Creswell Crags has approximately 40,000 visitors per year and therefore a quantification of effective dose is important for both visitors and guides to the Robin Hood show cave. Due to short exposure times the dose received by visitors is low (0.0016 mSv/visit) and regulations concerning exposure are not contravened. Similarly, the dose received by guides is fairly low (0.4 mSv/annum) due in part to current working practice. However, the risk to researchers entering the more inaccessible areas of the cave system is higher (0.06 mSv/visit). This survey also investigated the effect of seasonal variations on recorded radon concentration. From this work summer to winter ratios of between 1.1 and 9.51 were determined for different locations within the largest cave system.

Air Pollutants, Radioactive↗

An outbreak and review of cave-associated histoplasmosis capsulati.

Three male college students from Florida developed acute onsets of fever, chills, shortness of breath, and cough within one day of each other, and all were eventually hospitalized for four to 29 days. All chest x-ray films showed diffuse reticulonodularities in both lung fields. Laboratory studies confirmed the diagnosis of histoplasmosis. The three students had been 'spelunking' (cave exploring) 6 to 7 days before their onset of symptoms. One of four soil samples collected in the caves was positive for Histoplasma capsulatum by the indirect mouse inoculation procedure. Of three investigators who entered the implicated caves, two developed acute febrile illness within 15-21 days. One investigator was hospitalized for 18 days with a confirmed diagnosis of histoplasmosis. Investigation identified an additional case (the person had entered the caves 6 months before this episode), but was not reported to health authorities. Spelunkers should be aware of the potential risk of histoplasmosis and how to avoid infection. Physicians should be cognizant of cave-associated histoplasmosis, inquire about spelunking in persons who develop febrile respiratory illnesses with diffuse nodularities on chest x-ray films, and report such cases to their health department. A review of 42 reported outbreaks of cave-associated histoplasmosis and the approach to environmental control of infected caves are included.

Adult↗

Radon concentrations and exposure levels in Hungarian caves.

In addition to workers in uranium and coal mines, the staff of other underground workplaces, such as workers in caves, can be exposed to 222Rn and its progeny. In this study, radon and radon progeny concentrations were measured in four Hungarian caves. Two of them are used for speleotherapy, one is opened for tourist visits, and one is a reference cave used only for experimental purposes. Seasonal variation of radon levels, with summer maximums and winter minimums typical for cold karstic caves, were observed in all caves investigated. Non-regular diurnal variation of radon concentration was measured in the caves where indoor air was less isolated from the outdoor atmosphere. From the measured radon concentrations, cumulative WLM exposures, bronchial dose, an effective dose equivalent values were calculated for the staff, patients and visitors. The effective dose equivalent values for the cave personnel do not exceed the 20 mSv y-1 limit. The doses for visitors and patients were one or two magnitudes lower than that of the personnel.

Air Pollutants, Radioactive↗

Phlebotomine sandflies (Diptera: Psychodidae) from caves in Australia.

All three genera of phlebotomine sandflies recorded from the mainland of Australia are represented in collections from caves in Queensland. Phlebotomus (Australophlebotomus) mackerrasi Lewis and Dyce, Idiophlebotomus wellingsae (L. and D.) and Sergentomyia (Parrotomyia) trezkinni L. and D. achieve their biggest known populations in caves. Each has, however, been collected from outside environs. S. (P.) queenslandi (Hill) is most widespread and abundant across the continent and occurs less frequently in caves than in open situations where it is often associated with ground burrowing reptiles. Its occurrence in warmer caves may be linked with larger reptile predators of bats. S. (P.) curvata L. and D. is known as a single specimen from a cave. Hosts for the cave dominants are unknown but the regular concurrence with bats may be indicative. Immature stages of S. trezkinni and S. queenslandi have been recovered from isolated pellets of bat faeces and adults link reared. None of the species has been reared from mass accumulation of bat guano, and none of the species shows special adaptation for life in caves.

Animals↗

Micromorphology and site formation at Die Kelders Cave I, South Africa.

The deposits of Die Kelders I were previously described and studied by Tankard & Schweitzer (1974, 1976) from the standpoint of classical granulometric analysis of sand from a coastal cave in order to infer the geological history of the cave and its environs. This paper supplements these earlier works by taking a more holistic approach toward site formation processes by including investigation of the biogenic and anthropogenic influences on the cave deposits and history. The study employs the technique of soil micromorphology, which is the study of resin-impregnated, undisturbed blocks of sediment and petrographic thin sections, in which sediments from all areas of the cave were examined. The study showed that diagenesis of the deposits in the eastern areas of the excavation resulted in decalcification, which in turn brought about slumping and compaction. Equivalent stratigraphic layers exposed in the western and central areas were only mildly decalcified and consequently, these sediments contain limestone rock fall and relatively abundant marine and terrestrial mollusks, the latter not dissimilar to the Late Stone Age (LSA) midden which covers these deposits. Thus, in spite of lowered and more distant shorelines, marine resources were exploited during Middle Stone Age (MSA) times. Observations from these calcareous units also clearly demonstrates that previously recognized "occupational horizons" (e.g. Layers 6, 8 and 10) can be resolved micromorphologically into several ephemeral events, such as burning/fire, redistribution of ashes by wind and water, and non-deposition; the latter is shown by phosphatic alteration of sediments exposed on former surfaces and accumulation of guano, or the presence of millimeter-thick truncation surfaces below which aeolian dust infiltrated. Both field and microscopic observations illustrate that the deposits in caves are highly variable from wall to center, and that excavations should not be localized in just one microenvironment of the cave site.

Animals↗

Within-group human variation in the Asian Pleistocene: the three Upper Cave crania.

Numerous studies on Pleistocene samples have shown that within-group cranial variation was greater than that seen today. The three anatomically modern Upper Cave crania (UC 101, UC 102, and UC 103) from Zhoukoudian, China provide one of the best samples available for addressing the issue of the antiquity of the modern pattern of within-group cranial variability because archaeological evidence indicates that they are spatially and temporally restricted. Research on the Upper Cave fossils usually only includes UC 101 and UC 103 because of postmortem damage to UC 102's cranial vault. However, the face of UC 102 is undamaged, allowing for most facial measurements to be performed accurately. In this study we use facial dimensions to compare all three Upper Cave specimens, and we evaluate whether the variation seen among them is larger than that observed in extant populations. Using a worldwide sample of modern populations to establish a baseline, the three Upper Cave crania were compared to each other. Since there is disagreement over the sex of UC 102, this specimen is treated alternately as a female and as a male. Results show that the Upper Cave specimens exhibit significantly more variation than do individuals within more recent human populations, especially if UC 102 is considered male. Furthermore, results indicate that the fossils never fall into the same modern human group, and that each specimen is significantly atypical of its nearest modern neighbor in multivariate space. We conclude that the three Upper Cave crania do not represent a family group but are representative of the larger contemporaneous heterogeneous Asian Pleistocene population. Our results support the contention that today's within-group homogeneity is a relatively recent phenomenon, and is likely the result of a Neolithic population expansion and its many effects.

Anthropology, Physical↗

Micro-anatomical study of the carotid cave.

The surgical treatment of aneurysms located in the carotid cave is often hazardous and difficult. We studied the micro-anatomy of the carotid cave and its neighbourhood by microscopic observation and histological examination using 50 sides from 25 autopsy cases. The carotid caves were found in 34 out of the 50 sides (68%) examined and were usually located in the posteromedial aspect of the carotid dural ring. They were classified into three types according to the topographic micro-anatomy: the slit-type (17/50, 34%) which showed a small, thin recess of the dura mater with fine connective tissue loosely adhered to the carotid wall; the pocket-type (12/50, 24%) which had a definite dural pouch with the apex attached to the vessel wall; and the mesh-type (5/50, 10%) which formed a slit- or pocket-type dural cave covered with a mesh-like dural roof. The remaining 16 sides (32%) showed tight dural attachment without any caval structure around the dural ring. The posteromedial portion of the carotid dural ring had no contact with any bony structure, and this distinct anatomical feature thus appear to facilitate the formation of the carotid cave. Furthermore, the availability of this potential space and the closely situated origin of the superior hypophyseal artery as well as the haemodynamic effect of the internal carotid artery may allow the development of the carotid cave aneurysm.

Adult↗

Life on the edge: hydrogen sulfide and the fish communities of a Mexican cave and surrounding waters.

Most eucaryotic organisms classified as living in an extreme habitat are invertebrates. Here we report of a fish living in a Mexican cave (Cueva del Azufre) that is rich in highly toxic H(2)S. We compared the water chemistry and fish communities of the cave and several nearby surface streams. Our study revealed high concentrations of H(2)S in the cave and its outflow (El Azufre). The concentrations of H(2)S reach more than 300 muM inside the cave, which are acutely toxic for most fishes. In both sulfidic habitats, the diversity of fishes was heavily reduced, and Poecilia mexicana was the dominant species indicating that the presence of H(2)S has an all-or-none effect, permitting only few species to survive in sulfidic habitats. Compared to habitats without H(2)S, P. mexicana from the cave and the outflow have a significantly lower body condition. Although there are microhabitats with varying concentrations of H(2)S within the cave, we could not find a higher fish density in areas with lower concentrations of H(2)S. We discuss that P. mexicana is one of the few extremophile vertebrates. Our study supports the idea that extreme habitats lead to an impoverished species diversity.

Adaptation, Physiological↗

Geostatistical spatiotemporal analysis of air temperature as an aid to delineating thermal stability zones in a potential show cave: implications for environmental management.

Air temperature in several galleries of the Covadura System (Sorbas Gypsum Karst, Almería) was measured at monthly intervals over a period of 1 year. The spatial temperature distribution for each month was modeled in a geostatistical framework. The mean trend of the air temperature and the difference between each experimental temperature measurement and this trend were calculated over space and time. Both the trend and residual component were characterized using a geostatistical space-time model. A large spatial trend of the air temperature was found due to the orientation of galleries within the cave system and as a function of the distance from the main cave entrance. Kriging was used for the spatial estimation of the time covariance of the residuals. This enabled the delimitation of the cave into three zones of varying environmental risk in the event of being opened to visits by the public, according to the degree of stability of air temperature over space and time. The influence of human presence on the spatial temperature distribution was assessed using data collected during a year (2000/2001) in pilot galleries opened to the public. An average visit corresponding to August was selected comprising 16 people over a period of 53 min. This average visit influenced the spatial temperature pattern at distances of more than 90 m from the cave entrance, according to the geostatistical model adopted. Within this zone the mean thermal increment generated by human presence was estimated to be 0.26 degrees C. The spatiotemporal mathematical model of the cave air temperature has been revealed as a useful tool for the environmental management of show caves.

Conservation of Natural Resources↗

Molecular phylogeny of the extinct cave lion Panthera leo spelaea.

To reconstruct the phylogenetic position of the extinct cave lion (Panthera leo spelaea), we sequenced 1 kb of the mitochondrial cytochrome b gene from two Pleistocene cave lion DNA samples (47 and 32 ky B.P.). Phylogenetic analysis shows that the ancient sequences form a clade that is most closely related to the extant lions from Africa and Asia; at the same time, cave lions appear to be highly distinct from their living relatives. Our data show that these cave lion sequences represent lineages that were isolated from lions in Africa and Asia since their dispersal over Europe about 600 ky B.P., as they are not found among our sample of extant populations. The cave lion lineages presented here went extinct without mitochondrial descendants on other continents. The high sequence divergence in the cytochrome b gene between cave and modern lions is notable.

Animals↗

Phylogeography of surface and cave Astyanax (Teleostei) from Central and North America based on cytochrome b sequence data.

Astyanax fasciatus has become a model organism for the study of regressive and adaptive evolution in cave animals. To fully understand these processes, it is important to have background information on the systematics and phylogeography of surface and cave populations of this species. Here we investigate the phylogeography of A. fasciatus in North and Central America and also the historical biogeography of this region. Phylogenetic analysis of part of the mtDNA cytochrome b gene from 26 surface and nine cave A. fasciatus populations revealed seven major clades, which, in principle, represent geographical patterns of distribution. However, the four strongly eye and pigment reduced cave populations, Piedras, Sabinos, Tinaja, and Curva, form a separate cluster, which is not sister group to the surface populations from the same locality. Similarly the Belizean populations do not cluster with their geographic neighbors from the Yucatan. The analyses indicate that there have been recurrent invasions of surface Astyanax from the south, that were most likely influenced by major climate changes during the Pleistocene. During this period, ancestors of the strongly eye and pigment reduced cave populations were able to survive underground as thermophilic relics when the surface populations became extinct. The high level of genetic divergence among the different clades shows that differing haplotype lineages must have reinvaded the surface waters from the south and/or back-colonized them from residual habitats and also penetrated into the caves. Nested clade analyses show that recurrent gene flow as well as historic processes like past fragmentation and range expansion have influenced current populations of A. fasciatus in Central and North America. Different haplotype clades of the phylogeny are not compatible with the present taxonomy of Astyanax and, therefore, we propose the application of a single systematic unit, called A. fasciatus.

Animals↗

Using CAVE technology for functional genomics studies.

We have established the first Java 3D-enabled CAVE (CAVE automated virtual environment). The Java application programming interface allows the complete separation of the program development from the program execution, opening new application domains for the CAVE technology. Programs can be developed on any Java-enabled computer platform, including Windows, Macintosh, and Linux workstations, and executed in the CAVE without modification. The introduction of Java, one of the major programming environments for bioinformatics, into the CAVE environment allows the rapid development applications for genome research, especially for the analysis of the spatial and temporal data that are being produced by functional genomics experiments. The CAVE technology will play a major role in the modeling of biological systems that is necessary to understand how these systems are organized and how they function.

Automation↗

Ancient DNA and the population genetics of cave bears (Ursus spelaeus) through space and time.

The cave bear spread from Western Europe to the Near East during the Riss glaciation (250 KYA) before becoming extinct approximately 12 KYA. During that period, the climatic conditions were highly dynamic, oscillating between glacial and temperate episodes. Such events have constrained the geographic repartition of species, the movements of populations and shaped their genetic diversity. We retrieved and analyzed ancient DNA from 21 samples from five European caves ranging from 40 to 130 KYA. Combined with available data, our data set accounts for a total of 41 sequences of cave bear, coming from 18 European caves. We distinguish four haplogroups at the level of the mitochondrial DNA control region. The large population size of cave bear could account for the maintenance of such polymorphism. Extensive gene flow seems to have connected European populations because two haplogroups cover wide geographic areas. Furthermore, the extensive sampling of the deposits of the Scladina cave located in Belgium allowed us to correlate changes in climatic conditions with the intrapopulational genetic diversity over 90 KY.

Amino Acid Sequence↗

Radon and thoron in cave dwellings (Yan'an, China).

222Rn and 220Rn concentrations were measured in cave dwellings and brick houses in the region of Yan'an (China) during summer 1997. The underground dwellings are built into Quaternary loess, and all investigated houses are founded on it. The median values of indoor 222Rn and 220Rn concentrations are 42 (n = 18) and 77 Bq m(-3) (n = 15) for brick houses and 92 (n = 23) and 215 (n = 17) Bq m(-3) for cave dwellings. To classify the dwellings in respect to their "cave-character," the fraction of walls having a direct contact to the loses is calculated for each dwelling. While the 222Rn concentrations are increasing with higher fractions, the 220Rn concentrations are not correlated with this fraction. On the other hand, due to the short half-life of 220Rn the distance from the measuring point to the walls is negatively correlated with the 220Rn concentration, while there is no correlation with the 222Rn concentration. Therefore, concentric isolines of 220Rn concentrations showing a strong gradient were detected in cave dwellings. An influence of the ventilation rate is distinct for 222Rn but weak for 220Rn. The effective dose rates for 222Rn and 220Rn and their progenies are calculated for brick houses (2.7 mSv y(-1)), cave dwellings (7.1 mSv y(-1)), and for traditional cave dwellings with a bed foundation built with loess (16.7 mSv y(-1)). These calculations are based on summer measurements only. It is expected that the true effective dose rates will be significantly higher.

China↗

Central role for the lens in cave fish eye degeneration.

Astyanax mexicanus is a teleost with eyed surface-dwelling and eyeless cave-dwelling forms. Eye formation is initiated in cave fish embryos, but the eye subsequently arrests and degenerates. The surface fish lens stimulates growth and development after transplantation into the cave fish optic cup, restoring optic tissues lost during cave fish evolution. Conversely, eye growth and development are retarded following transplantation of a surface fish lens into a cave fish optic cup or lens extirpation. These results show that evolutionary changes in an inductive signal from the lens are involved in cave fish eye degeneration.

Animals↗