Academic literature on the topic 'Carlsbad Cave'

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Journal articles on the topic "Carlsbad Cave"

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Duncan, Tammi, Margaret Werner-Washburne, and Diana Northup. "Diversity of siderophore-producing bacterial cultures from Carlsbad Caverns National Park caves, Carlsbad, New Mexico." Journal of Cave and Karst Studies 83, no. 1 (2021): 29–43. http://dx.doi.org/10.4311/2019es0118.

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Siderophores are microbially-produced ferric iron chelators. They are essential for microbial survival, but their presence and function for cave microorganisms have not been extensively studied. Siderophores are classified based on the common functional groups (catechols, hydroxamates, carboxylates, and mixed) that coordinate to ferric (Fe3+) iron. Cave environments are nutrient-limited and previous evidence suggests siderophore usage in carbonate caves. We hypothesize that siderophores are likely used as a mechanism in caves to obtain critical ferric iron. Cave bacteria were collected from long-term parent cultures (LT PC) or short-term parent cultures (ST PC) inoculated with ferromanganese deposits (FMD) and carbonate secondary minerals from Lechuguilla and Spider caves in Carlsbad Caverns National Park, NM. LT PC were incubated for 10−11 years to identify potential chemolithoheterotrophic cultures able to survive in nutrient-limited conditions. ST PC were incubated for 1−3 days to identify a broader diversity of cave isolates. A total of 170 LT and ST cultures, 18 pure and 152 mixed, were collected and used to classify siderophore production and type and to identify siderophore producers. Siderophore production was slow to develop (>10 days) in LT cultures with a greater number of weak siderophore producers in comparison to the ST cultures that produced siderophores in <10 days, with a majority of strong siderophore producers. Overall, 64% of the total cultures were siderophore producers, with the majority producing hydroxamate siderophores. Siderophore producers were classified into Proteobacteria (Alpha-, Beta-, or Gamma-), Actinobacteria, Bacteroidetes, and Firmicutes phyla using 16S rRNA gene sequencing. Our study supports our hypothesis that cave bacteria have the capability to produce siderophores in the subsurface to obtain critical ferric iron.
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Burger, Paul A. "Cave and karst management at Carlsbad Caverns National Park." Zeitschrift für Geomorphologie, Supplementary Issues 62, no. 3 (2021): 85–124. http://dx.doi.org/10.1127/zfg_suppl/2021/0692.

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Ingraham, Neil L., Jenny B. Chapman, and John W. Hess. "Stable isotopes in cave pool systems: Carlsbad Cavern, New Mexico, U.S.A." Chemical Geology: Isotope Geoscience section 86, no. 1 (1990): 65–74. http://dx.doi.org/10.1016/0168-9622(90)90006-x.

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Read, Kaitlin, Leslie Melim, Ara Winter, and Diana Northup. "Bacterial diversity in vadose cave pools: evidence for isolated ecosystems." Journal of Cave and Karst Studies 83, no. 4 (2021): 163–88. http://dx.doi.org/10.4311/2020mb0120.

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Microbial diversity of cave pools, especially vadose pools, has received relatively little attention. To help fill this gap, this study reports on the bacterial diversity of 17 pools in three New Mexican arid land caves: Carlsbad Cavern, Lechuguilla Cave, and Hell Below Cave. These pools are spread throughout the caves and, with two exceptions, are not connected. The pools share a basic water chemistry, with fresh water of the calcium-magnesium-bicarbonate type. These 17 pools have Chao1 values between 40 and 1738; the Shannon diversity averages 4.6 ± 1.1, ranging from 2.6 to 6.4; and the Simpson averages 0.881 ± 0.099, ranging from 0.622 to 0.981. No two pools had the same communities, even at the phylum level. Nitrospirae, Alphaproteobacteria, Betaproteobacteria and Gammaproteobacteria were found >5% abundance in nine or more cave pools. Actinobacteria, Chloroflexi, Fibrobacteres, Firmicutes and Plantomycetes were at >5 % in four to six pools. Of the top ten widespread bacterial genera, Nitrospira was found in all pools, with >5 % in eleven pools. Other common genera include Polyclorovans, Propionibacterium, Polaromonas, Haliangium, Bacillus, Subgroup 6 uncultured Acidobacteria, Candidatus Omnitrophica, and uncultured Nitrosomonadaceae. Presence of several potential nitrogen cycling bacteria (e.g., Nitrospira) in the study pools suggests that nitrogen cycling may be an important bacterial role. There is some evidence of human contamination, particularly in the heavily visited Big Room, Carlsbad Cavern, but it is not the dominant control. Rather than a single stable cave pool community, adapted to the cave pool ecosystem, the data show 17 different communities, despite relatively similar conditions. The data support the hypothesis that each pool is a unique, isolated ecosystem, with differences likely caused more by the isolation of each pool than by variable chemistry. Thus, the common habit of grouping samples, while useful for some questions, may not capture the diversity present in cave ecosystems.
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Melim, Leslie A., and Michael N. Spilde. "A New Unified Model For Cave Pearls: Insights from Cave Pearls in Carlsbad Cavern, New Mexico, U.s.a." Journal of Sedimentary Research 88, no. 3 (2018): 344–64. http://dx.doi.org/10.2110/jsr.2018.21.

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Polyak, Victor J. "Alunite, Natroalunite and Hydrated Halloysite in Carlsbad Cavern and Lechuguilla Cave, New Mexico." Clays and Clay Minerals 44, no. 6 (1996): 843–50. http://dx.doi.org/10.1346/ccmn.1996.0440616.

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Cunningham, K. I., D. E. Northup, R. M. Pollastro, W. G. Wright, and E. J. LaRock. "Bacteria, fungi and biokarst in Lechuguilla Cave, Carlsbad Caverns National Park, New Mexico." Environmental Geology 25, no. 1 (1995): 2–8. http://dx.doi.org/10.1007/bf01061824.

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8

Calaforra, Jose-Maria, and Waele Jo De. "New peculiar cave ceiling forms from Carlsbad Caverns (New Mexico, USA): The zenithal ceiling tube-holes." Geomorphology 134, no. 1-2 (2011): 43–48. https://doi.org/10.5281/zenodo.13438801.

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(Uploaded by Plazi for the Bat Literature Project) During a trip to the Hall of the White Giant, Carlsbad Caverns (NM, USA) cigar-shaped vertically upward developing holes were observed on the ceiling at different heights of the passages. They have a circular crosssection with diameters of 1 to some centimetres and taper out towards their upper end. Their walls are smooth and their bottom edges are sharp, while their length can reach several decimetres. Sometimes gypsum can be found inside. They often occur randomly distributed in groups and their development is not necessarily controlled by fractures or other bedrock structures.
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Calaforra, Jose-Maria, and Waele Jo De. "New peculiar cave ceiling forms from Carlsbad Caverns (New Mexico, USA): The zenithal ceiling tube-holes." Geomorphology 134, no. 1-2 (2011): 43–48. https://doi.org/10.5281/zenodo.13438801.

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(Uploaded by Plazi for the Bat Literature Project) During a trip to the Hall of the White Giant, Carlsbad Caverns (NM, USA) cigar-shaped vertically upward developing holes were observed on the ceiling at different heights of the passages. They have a circular crosssection with diameters of 1 to some centimetres and taper out towards their upper end. Their walls are smooth and their bottom edges are sharp, while their length can reach several decimetres. Sometimes gypsum can be found inside. They often occur randomly distributed in groups and their development is not necessarily controlled by fractures or other bedrock structures.
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10

Calaforra, Jose-Maria, and Waele Jo De. "New peculiar cave ceiling forms from Carlsbad Caverns (New Mexico, USA): The zenithal ceiling tube-holes." Geomorphology 134, no. 1-2 (2011): 43–48. https://doi.org/10.5281/zenodo.13438801.

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Abstract:
(Uploaded by Plazi for the Bat Literature Project) During a trip to the Hall of the White Giant, Carlsbad Caverns (NM, USA) cigar-shaped vertically upward developing holes were observed on the ceiling at different heights of the passages. They have a circular crosssection with diameters of 1 to some centimetres and taper out towards their upper end. Their walls are smooth and their bottom edges are sharp, while their length can reach several decimetres. Sometimes gypsum can be found inside. They often occur randomly distributed in groups and their development is not necessarily controlled by fractures or other bedrock structures.
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Books on the topic "Carlsbad Cave"

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United States. National Park Service, ed. Carlsbad Caverns National Park, New Mexico. National Park Service, U.S. Dept. of the Interior, 2009.

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2

United States. Congress. House. Committee on Natural Resources. Subcommittee on National Parks, Forests, and Public Lands. Protection of Lechuguilla Cave: Hearing before the Subcommittee on National Parks, Forests, and Public Lands of the Committee on Natural Resources, House of Representatives, One Hundred Third Congress, first session, on H.R. 698, to protect Lechuguilla Cave and other resources and values in and adjacent to Carlsbad Caverns National Park, hearing held in Washington, DC, March 2, 1993. U.S. G.P.O., 1993.

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3

Hill, Carol A. Geology of Carlsbad Cavern and other caves in the Guadalupe Mountains, New Mexico and Texas. New Mexico Bureau of Mines & Mineral Resources, 1987.

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Jenkins, Scott A. Hydrodynamic modeling of dispersion and dilution of concentrated seawater produced by the ocean desalination project at the Encina Power Plant, Carlsbad, CA, Part II: Saline anomalies due to theoretical extreme case hydraulic scenarios. Poseidon Resources, 2005.

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Running Scared A Mystery In Carlsbad Caverns National Park. National Geographic Society, 2008.

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Book chapters on the topic "Carlsbad Cave"

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Hose*, Louise D., Harvey R. DuChene*, Daniel Jones, et al. "Hypogenic karst of the Great Basin." In Field Excursions from the 2021 GSA Section Meetings. Geological Society of America, 2021. http://dx.doi.org/10.1130/2020.0061(05).

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ABSTRACT Discoveries in the 1980s greatly expanded speleologists’ understanding of the role that hypogenic groundwater flow can play in developing caves at depth. Ascending groundwater charged with carbon dioxide and, especially, hydrogen sulfide can readily dissolve carbonate bedrock just below and above the water table. Sulfuric acid speleogenesis, in which anoxic, rising, sulfidic groundwater mixes with oxygenated cave atmosphere to form aggressive sulfuric acid (H2SO4) formed spectacular caves in Carlsbad Caverns National Park, USA. Cueva de Villa Luz in Mexico provides an aggressively active example of sulfuric acid speleogenesis processes, and the Frasassi Caves in Italy preserve the results of sulfuric acid speleogenesis in its upper levels while sulfidic groundwater currently enlarges cave passages in the lower levels. Many caves in east-central Nevada and western Utah (USA) are products of hypogenic speleogenesis and formed before the current topography fully developed. Wet climate during the late Neogene and Pleistocene brought extensive meteoric infiltration into the caves, and calcite speleothems (e.g., stalactites, stalagmites, shields) coat the walls and floors of the caves, concealing evidence of the earlier hypogenic stage. However, by studying the speleogenetic features in well-established sulfuric acid speleogenesis caves, evidence of hypogenic, probably sulfidic, speleogenesis in many Great Basin caves can be teased out. Compelling evidence of hypogenic speleogenesis in these caves include folia, mammillaries, bubble trails, cupolas, and metatyuyamunite. Sulfuric acid speleogenesis signs include hollow coralloid stalagmites, trays, gypsum crust, pseudoscallops, rills, and acid pool notches. Lehman Caves in Great Basin National Park is particularly informative because a low-permeability capstone protected about half of the cave from significant meteoric infiltration, preserving early speleogenetic features.
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Conference papers on the topic "Carlsbad Cave"

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Ulbrich, Joseph, Daniel S. Jones, and Thomas L. Kieft. "Spelunking into the Virosphere: Characterizing Viral Communties from Carlsbad Caverns National Park." In 2022 New Mexico Geological Society Annual Spring Meeting & Ft. Stanton Cave Conference. New Mexico Geological Society, 2022. http://dx.doi.org/10.56577/sm-2022.2832.

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Perrone-Vogt, Morgan, and Katherine Giles. "Got moonmilk? The characterization of moonmilk in Spider Cave, Carlsbad Caverns National Park, New Mexico." In 57th Annual Fall Field Conference. New Mexico Geological Society, 2006. http://dx.doi.org/10.56577/ffc-57.175.

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Polyak, Victor J., W. C. McIntosh, Paula P. Provencio, and Necip Guven. "Alunite and natroalunite tell a story-the age and origin of Carlsbad Cavern, Lechuguilla Cave, and other sulfuric-acid type caves of the Guadalupe Mountains." In 57th Annual Fall Field Conference. New Mexico Geological Society, 2006. http://dx.doi.org/10.56577/ffc-57.203.

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Hill, Carol A. "Mineralogy of Carlsbad Cavern and other caves in the Guadalupe Mountains, New Mexico." In 9th Annual New Mexico Mineral Symposium. New Mexico Bureau of Geology and Mineral Resources, 1988. http://dx.doi.org/10.58799/nmms-1988.96.

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Land, Lewis. "Second-day road log: From Washington Ranch to Rattlesnake Spring and Black River, Carlsbad Spring and Carlsbad Flume, and Gypsum Caves of the Seven Rivers Hills." In 73rd Annual Fall Field Conference. New Mexico Geological Society, 2023. http://dx.doi.org/10.56577/ffc-73.41.

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Reports on the topic "Carlsbad Cave"

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Olstad, Tyra, Erik Meyer, Erik Meyer, and Tyra Olstad. Carlsbad Caverns National Park: Acoustic monitoring report, 2019. National Park Service, 2024. http://dx.doi.org/10.36967/2305265.

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This study arose from Carlsbad Cavern National Park?s (CAVE) Technical Assistance Request (TAR; #9250), which identified the need for a baseline acoustic inventory to help understand the park?s existing wilderness character and evaluate potential acoustic impacts from military and civilian overflights. From late October to mid-December 2019, the Natural Sounds and Night Skies Division (NSNSD) gathered acoustic data at one site in CAVE to provide park managers with baseline information about the acoustic environment, including existing ambient sound levels and time-above noise level metrics in the park?s wilderness area. Overall, existing median ambient sound levels (LA50) at CAVE were remarkably quiet at 21.0 dB during the day and 20.1 dB at night. In the lower frequency range (20 ? 1,250 Hz), the sound level of 35 dB (LAeq, 1s), indicative of quiet environments was exceeded only 3.18% of the day and 0.81% of the night. All other key sound levels (i.e., 45 dB and above) were exceeded less than 0.25% of the time. Due to an error with the acoustic recording device, metrics requiring off-site listening could not be determined. As a supplement, a geospatial sound model is used to predict existing and natural ambient sound levels of 32.3 (dBA) and 29.8 (dBA), respectively, with localized impacts from anthropogenic noise.
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