M. Spilde, Keely E. Miltenberger, C. Ferguson, J. Blake
One of the most remarkable features of Fort Stanton Cave is the Snowy River calcite deposit, which is likely the world’s longest speleothem (currently over 19.1 km in length). The Snowy River formation is a subaqueous coralloid pool deposit with a very low slope (<0.8 degrees over 7.5 km) that responds quickly to large surface meteoric events, filling within hours, flowing for several months, and then draining and drying over a period of several weeks. The carbonate crust has a cauliflower-like texture on the surface, and in cross section, consists of thin laminae that vary from microns to millimeters in thickness. Eight drill cores taken in 2008 indicate that the deposit thins from 83-25 mm in thickness in a northerly direction (direction of flow). Two more cores were taken in 2018 for compressional strength analysis and other tests. Muddy layers in the cores are continuous and correlate across all ten cores, enclosing a length of over a km in distance. One core was prepared as a conventional petrographic thin section; the section reveals the presence of 500 individual light and dark lamina. A dark laminae forms as a thin layer of detrital minerals settle out after initial flooding; the light layer of calcite precipitates over the top of it, continuing until the water drains out as the flood event ends. Thus, each dark and light pair forms an apparent couplet recording every flood event. The lamina couplet records a filling-draining event with 250 such events taking place over the period of deposition of 821 (+/-120) years, as determined by uranium-series dating (Land et al. 2010). This yields a calculated average of
斯坦顿堡洞穴最显著的特征之一是雪河方解石矿床，这可能是世界上最长的洞穴(目前长度超过19.1公里)。雪河地层是一个水下珊瑚池矿床，坡度非常低(<0.8度/ 7.5公里)，对大型地表大气事件反应迅速，在几小时内填满，几个月的流动，然后在几周内排水和干燥。碳酸盐地壳表面有菜花状的纹理，在横截面上，由厚度从微米到毫米不等的薄层组成。2008年采集的8个岩心显示，沉积物厚度在83 ~ 25mm之间，呈偏北方向(流向)变薄。2018年又取了两个岩心进行抗压强度分析和其他测试。岩心中的泥质层是连续的，并且在所有10个岩心中相互关联，围成一公里以上的距离。一个岩心作为常规岩石薄片制备;该部分揭示了500个单独的明暗层的存在。当一层薄薄的碎屑矿物在最初的水淹后沉淀下来时，形成了一层暗纹层;轻的方解石层沉淀在上面，一直持续到洪水事件结束时水排干。因此，每一对黑暗和光明形成了一个明显的对联，记录了每一次洪水事件。层叠对联记录了在821(+/-120)年的沉积期间发生的250次填充-排水事件，这是通过铀系列测年确定的(Land et al. 2010)。这就得到了一个计算平均值
{"title":"The Snowy River Calcite Formation Records a Complex History in Fort Stanton Cave","authors":"M. Spilde, Keely E. Miltenberger, C. Ferguson, J. Blake","doi":"10.56577/sm-2022.2869","DOIUrl":"https://doi.org/10.56577/sm-2022.2869","url":null,"abstract":"One of the most remarkable features of Fort Stanton Cave is the Snowy River calcite deposit, which is likely the world’s longest speleothem (currently over 19.1 km in length). The Snowy River formation is a subaqueous coralloid pool deposit with a very low slope (<0.8 degrees over 7.5 km) that responds quickly to large surface meteoric events, filling within hours, flowing for several months, and then draining and drying over a period of several weeks. The carbonate crust has a cauliflower-like texture on the surface, and in cross section, consists of thin laminae that vary from microns to millimeters in thickness. Eight drill cores taken in 2008 indicate that the deposit thins from 83-25 mm in thickness in a northerly direction (direction of flow). Two more cores were taken in 2018 for compressional strength analysis and other tests. Muddy layers in the cores are continuous and correlate across all ten cores, enclosing a length of over a km in distance. One core was prepared as a conventional petrographic thin section; the section reveals the presence of 500 individual light and dark lamina. A dark laminae forms as a thin layer of detrital minerals settle out after initial flooding; the light layer of calcite precipitates over the top of it, continuing until the water drains out as the flood event ends. Thus, each dark and light pair forms an apparent couplet recording every flood event. The lamina couplet records a filling-draining event with 250 such events taking place over the period of deposition of 821 (+/-120) years, as determined by uranium-series dating (Land et al. 2010). This yields a calculated average of","PeriodicalId":50244,"journal":{"name":"Journal of Cave and Karst Studies","volume":"40 1","pages":""},"PeriodicalIF":0.9,"publicationDate":"2022-04-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"82351884","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Sediment transport in ephemeral channels: Validation of physics-based model and development of data-driven model","authors":"Loc Luong, D. Cadol, S. Bilek, J. M. Mclaughlin","doi":"10.56577/sm-2022.2798","DOIUrl":"https://doi.org/10.56577/sm-2022.2798","url":null,"abstract":"","PeriodicalId":50244,"journal":{"name":"Journal of Cave and Karst Studies","volume":"31 1","pages":""},"PeriodicalIF":0.9,"publicationDate":"2022-04-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"83723968","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
R. Mixon, J. Blake, Jeb E. Brown, S. Chavarria, C. Ferguson, D. Yager
{"title":"Source Tracking Analysis of Aluminum, Arsenic, and Lead Entering the San Juan River in the Four Corners Region, USA.","authors":"R. Mixon, J. Blake, Jeb E. Brown, S. Chavarria, C. Ferguson, D. Yager","doi":"10.56577/sm-2022.2861","DOIUrl":"https://doi.org/10.56577/sm-2022.2861","url":null,"abstract":"","PeriodicalId":50244,"journal":{"name":"Journal of Cave and Karst Studies","volume":"5 1","pages":""},"PeriodicalIF":0.9,"publicationDate":"2022-04-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"78674354","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Rachel Bosch, D. Ward, A. Bird, D. Sturmer, Rick Olson
This work presents an analysis of a debris flow deposit below Earth’s surface in the Mammoth Cave System in Kentucky, USA, and is the first study to characterize an in-cave debris flow to this level of detail. The deposit, named Mt. Ararat by cavers, has a maximum thickness of 7 m, a head-to-tail length of 75 m, and a total volume of about 3400 m3, as determined by terrestrial LiDAR and electrical resistivity surveys. The deposit is chaotic, angular, matrix-supported, and roughly inversely graded, with grain sizes, quantified through various grain-size distribution measuring techniques, ranging from clay through boulders larger than 1 m. The clasts are predominantly Mississippian Big Clifty sandstone, which is allochthonous in this part of the cave. The angularity of the blocks in the deposit indicate that they had not experienced significant erosion; and therefore, are determined to have been transported only a relatively short distance over a short time. The deposit profile is compound in appearance with two heads. We thus interpret this as a debris flow deposit resulting from two distinct flow events, and present a chronology of events leading to the present-day Mt. Ararat in Mammoth Cave. The findings of this work will inform further studies of karst-related erosional events, sediment transport, and deposition at different scales in karst aquifers, as well as the ways in which surface and subsurface processes interact to contribute to karst landscape evolution.
{"title":"A debris flow deposit in Mammoth Cave: field characterization","authors":"Rachel Bosch, D. Ward, A. Bird, D. Sturmer, Rick Olson","doi":"10.4311/2020es0108","DOIUrl":"https://doi.org/10.4311/2020es0108","url":null,"abstract":"This work presents an analysis of a debris flow deposit below Earth’s surface in the Mammoth Cave System in Kentucky, USA, and is the first study to characterize an in-cave debris flow to this level of detail. The deposit, named Mt. Ararat by cavers, has a maximum thickness of 7 m, a head-to-tail length of 75 m, and a total volume of about 3400 m3, as determined by terrestrial LiDAR and electrical resistivity surveys. The deposit is chaotic, angular, matrix-supported, and roughly inversely graded, with grain sizes, quantified through various grain-size distribution measuring techniques, ranging from clay through boulders larger than 1 m. The clasts are predominantly Mississippian Big Clifty sandstone, which is allochthonous in this part of the cave. The angularity of the blocks in the deposit indicate that they had not experienced significant erosion; and therefore, are determined to have been transported only a relatively short distance over a short time. The deposit profile is compound in appearance with two heads. We thus interpret this as a debris flow deposit resulting from two distinct flow events, and present a chronology of events leading to the present-day Mt. Ararat in Mammoth Cave. The findings of this work will inform further studies of karst-related erosional events, sediment transport, and deposition at different scales in karst aquifers, as well as the ways in which surface and subsurface processes interact to contribute to karst landscape evolution.","PeriodicalId":50244,"journal":{"name":"Journal of Cave and Karst Studies","volume":"1 1","pages":""},"PeriodicalIF":0.9,"publicationDate":"2021-12-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"90003490","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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.
{"title":"Bacterial diversity in vadose cave pools: evidence for isolated ecosystems","authors":"K. Read, L. Melim, Ara S. Winter, D. Northup","doi":"10.4311/2020mb0120","DOIUrl":"https://doi.org/10.4311/2020mb0120","url":null,"abstract":"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.","PeriodicalId":50244,"journal":{"name":"Journal of Cave and Karst Studies","volume":"2 1","pages":""},"PeriodicalIF":0.9,"publicationDate":"2021-12-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"90494911","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Alexandra Tsalickis, M. Waters, Joshua R. Campbell
Whereas bat guano is gaining viability in accurately reconstructing local paleoenvironmental and climatic conditions, overall reviews of methods for analyzing and collecting bat guano cores have received less attention. Guano cores have been collected from several locations (e.g., United States, Romania, Philippines, and southeast Asia), and the processing and collection methods are quite similar despite a lack of standardized techniques. Physical, chemical, and elemental analyses on guano samples have focused on the interpretation of precipitation changes over time, with additional applications from stable isotope analysis being used for other paleoenvironmental conditions. We obtained three bat guano cores from Alabama and Tennessee to evaluate the collecting and processing techniques of guano. Climatic temperature changes were not analyzed in this study. The purpose of this investigation was to summarize multiple techniques and approaches used to process and analyze bat guano cores with a focus on reconstructing paleoclimate in cave environments throughout the globe. From these three cores, we describe challenges and make recommendations for improving guano analysis.
{"title":"Methods and analysis of bat guano cores from caves for paleoecology","authors":"Alexandra Tsalickis, M. Waters, Joshua R. Campbell","doi":"10.4311/2020es0104","DOIUrl":"https://doi.org/10.4311/2020es0104","url":null,"abstract":"Whereas bat guano is gaining viability in accurately reconstructing local paleoenvironmental and climatic conditions, overall reviews of methods for analyzing and collecting bat guano cores have received less attention. Guano cores have been collected from several locations (e.g., United States, Romania, Philippines, and southeast Asia), and the processing and collection methods are quite similar despite a lack of standardized techniques. Physical, chemical, and elemental analyses on guano samples have focused on the interpretation of precipitation changes over time, with additional applications from stable isotope analysis being used for other paleoenvironmental conditions. We obtained three bat guano cores from Alabama and Tennessee to evaluate the collecting and processing techniques of guano. Climatic temperature changes were not analyzed in this study. The purpose of this investigation was to summarize multiple techniques and approaches used to process and analyze bat guano cores with a focus on reconstructing paleoclimate in cave environments throughout the globe. From these three cores, we describe challenges and make recommendations for improving guano analysis.","PeriodicalId":50244,"journal":{"name":"Journal of Cave and Karst Studies","volume":"47 1","pages":""},"PeriodicalIF":0.9,"publicationDate":"2021-12-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"79896245","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
A. Sepahvand, M. Prelovšek, A. N. Samani, R. Wasson
We conducted a one-year-long study of solute load measured three times per month in three neighboring subwatersheds (Alashtar, Khorram Abad, and Biranshahr) located in the Karkheh River basin in the Zagros region of southwestern Iran. Research was focused on the chemical composition of water (solute load), karst denudation rate, spatial and temporal variability, as well as comparison of solute load with suspended load. Results show that Ca-Mg-HCO3 is the dominant water type that reflects the lithological characteristics of the catchment areas. Lack of seasonal fluctuation of solute load and absence of dilution during high water levels but evident seasonal course of discharge defines the highest solute flux during the annual maximum of discharge in spring months. The highest solute flux is related to flood events. High annual variation of Na1 concentration compared to conservative Cl2 as well as Chloro-Alkali indexes (CAI and CAI2) suggests that Na1 adsorption and desorption during ion-exchange reactions occur in the regolith. This Na+ variability, to some extent, explains weak Ca21 and Mg21 dilution effect during high water levels. During the measurement period (2014-2015), solute flux calculated per catchment area amounted to 49-69 t km-2 a-1 (tons per km per year). The chemical composition of water and discharge shows by far the highest chemical denudation of limestones and dolomites (87−89 %), while dissolution of gypsum is of minor importance (11−13 %). As a result, the carbonate karst solutional denudation rate is between 0.010 and 0.040 mm a21 , where the higher values are more probable for longer periods due to the relatively low discharge during the spring of 2015. Comparison of dissolved and suspended loads indicates that the transport of suspended load is an order of magnitude less than transport of the dissolved load; the only exception is one flash flood event when suspended load exceeded the dissolved load. Besides a small decrease in solute flux as well as carbonate karst dissolution rates from NW to SE, no large hydrochemical differences between the three subwatersheds were detected.
{"title":"Solute transport and solutional denu-dation rate of carbonate karst in the semi-arid Zagros region (southwes-tern Iran)","authors":"A. Sepahvand, M. Prelovšek, A. N. Samani, R. Wasson","doi":"10.4311/2020es0102","DOIUrl":"https://doi.org/10.4311/2020es0102","url":null,"abstract":"We conducted a one-year-long study of solute load measured three times per month in three neighboring subwatersheds (Alashtar, Khorram Abad, and Biranshahr) located in the Karkheh River basin in the Zagros region of southwestern Iran. Research was focused on the chemical composition of water (solute load), karst denudation rate, spatial and temporal variability, as well as comparison of solute load with suspended load. Results show that Ca-Mg-HCO3 is the dominant water type that reflects the lithological characteristics of the catchment areas. Lack of seasonal fluctuation of solute load and absence of dilution during high water levels but evident seasonal course of discharge defines the highest solute flux during the annual maximum of discharge in spring months. The highest solute flux is related to flood events. High annual variation of Na1 concentration compared to conservative Cl2 as well as Chloro-Alkali indexes (CAI and CAI2) suggests that Na1 adsorption and desorption during ion-exchange reactions occur in the regolith. This Na+ variability, to some extent, explains weak Ca21 and Mg21 dilution effect during high water levels. During the measurement period (2014-2015), solute flux calculated per catchment area amounted to 49-69 t km-2 a-1 (tons per km per year). The chemical composition of water and discharge shows by far the highest chemical denudation of limestones and dolomites (87−89 %), while dissolution of gypsum is of minor importance (11−13 %). As a result, the carbonate karst solutional denudation rate is between 0.010 and 0.040 mm a21 , where the higher values are more probable for longer periods due to the relatively low discharge during the spring of 2015. Comparison of dissolved and suspended loads indicates that the transport of suspended load is an order of magnitude less than transport of the dissolved load; the only exception is one flash flood event when suspended load exceeded the dissolved load. Besides a small decrease in solute flux as well as carbonate karst dissolution rates from NW to SE, no large hydrochemical differences between the three subwatersheds were detected.","PeriodicalId":50244,"journal":{"name":"Journal of Cave and Karst Studies","volume":"26 1","pages":""},"PeriodicalIF":0.9,"publicationDate":"2021-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"73893607","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Rhythmic Karst Springs (RKSs) are rare geologic features that rhythmically outflow water. A mechanical model for the rhythmic flow with rhythmic spill-over configuration was constructed in this work. The evolution of the RKS was revealed by using geological process analysis. The analytical model can directly explain the existence of RKSs in soluble rock regions and their formation mechanism in nature. Visual observations and flow measurements were performed using a laboratory physical model of RKS. The physical model components included a soluble rock simulation area, karst pipes, cave-reservoir, karst depression terrain, water tank, rhythmic spring, and the outflow measurement system. Groups of tests were carried out to recreate the process of RKS functioning and to confirm the rhythmic cycle duration and the threshold of replenishment intensity. This research helped to interpret the behavior of rhythmic springs using the recharge and evacuation of the subsurface cave-reservoir by means of fluid mechanics and groundwater hydraulics theories.
{"title":"Physical and analytical modeling of rhythmic karst springs","authors":"Xianxuan Xiao, Qiang Zhang","doi":"10.4311/2020es0119","DOIUrl":"https://doi.org/10.4311/2020es0119","url":null,"abstract":"Rhythmic Karst Springs (RKSs) are rare geologic features that rhythmically outflow water. A mechanical model for the rhythmic flow with rhythmic spill-over configuration was constructed in this work. The evolution of the RKS was revealed by using geological process analysis. The analytical model can directly explain the existence of RKSs in soluble rock regions and their formation mechanism in nature. Visual observations and flow measurements were performed using a laboratory physical model of RKS. The physical model components included a soluble rock simulation area, karst pipes, cave-reservoir, karst depression terrain, water tank, rhythmic spring, and the outflow measurement system. Groups of tests were carried out to recreate the process of RKS functioning and to confirm the rhythmic cycle duration and the threshold of replenishment intensity. This research helped to interpret the behavior of rhythmic springs using the recharge and evacuation of the subsurface cave-reservoir by means of fluid mechanics and groundwater hydraulics theories.","PeriodicalId":50244,"journal":{"name":"Journal of Cave and Karst Studies","volume":"34 1","pages":""},"PeriodicalIF":0.9,"publicationDate":"2021-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"88980281","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
C. Campos, José Luis Punzo-Díaz, Verónica Delgado, A. Goguitchaichvili, J. Morales
Cueva de la Huachizca is located in the humid forests of the Municipio of Santa Clara del Cobre, Michoacán. During the Postclassic period (1300−1520 ad), Santa Clara del Cobre was a part of the Tarascan Señorio. Ethnographic accounts describe the use of Cueva de la Huachizca as a place of refuge during the Cristero Rebellion (1921−1926). Recent investigations suggest a long history of use including graffiti and inscriptions from the 1800s–1900s and a rock art panel. The panel consists of pecked petroglyphs depicting a man facing an eagle, above a spiral motif. Stylistic analysis of the panel suggests that the rock art was created during pre-Hispanic times, likely by the Postclassic Tarascans. As observed in several regions of Mesoamerica, for the Tarascans, caves were also liminal spaces and had an important role in Postclassic Tarascan cosmology. A ceramic resinera, a pine resin pot, an eagle’s feather, and charcoal were also recovered. The resinera age was estimated by researchers at Archaeomagnetic Services, Geophysics Institute at the National Autonomous University of México-Campus Morelia, Michoacán to between 1921 and 1980. Ethnographic and ethnohistoric accounts describe caves as houses of fertility and rain deities, an idea that while slightly transformed, has survived over 500 years of colonization, and remains in the communities’ social memories. These findings demonstrate the cave’s significance among the descendent communities and Cueva de la Huachizca as an important sacred site.
Cueva de la Huachizca位于Santa Clara del Cobre市的潮湿森林中，Michoacán。在后古典时期(公元1300 - 1520年)，圣克拉拉是塔拉斯坎Señorio的一部分。民族志记述了Cristero叛乱(1921 - 1926)期间，Cueva de la Huachizca作为避难所的使用。最近的调查表明，它的使用历史很长，包括19世纪至20世纪的涂鸦和铭文，以及岩石艺术面板。该面板由一幅雕刻的岩画组成，描绘了一个男人面对一只鹰，上面是一个螺旋图案。对面板的风格分析表明，这些岩石艺术创作于前西班牙时代，很可能是由后古典时期的塔拉斯坎人创作的。正如在中美洲的几个地区所观察到的那样，对于塔拉斯坎人来说，洞穴也是阈值空间，在后古典塔拉斯坎人的宇宙观中起着重要作用。此外，还发现了一个陶瓷树脂罐、一个松脂罐、一根鹰羽和木炭。这些树脂的年龄是由莫雷利亚国立自治大学地球物理研究所考古磁学服务处的研究人员估计的，在1921年到1980年之间，Michoacán。民族志和民族史学将洞穴描述为生育和雨神的住所，这一想法虽然略有改变，但在500多年的殖民统治中幸存下来，并保留在社区的社会记忆中。这些发现证明了该洞穴对后代社区的重要性，以及夸瓦奇斯卡作为一个重要的圣地。
{"title":"An interpretation of Cueva de la Huachizca, Santa Clara del Cobre, Michoacan, Mexico","authors":"C. Campos, José Luis Punzo-Díaz, Verónica Delgado, A. Goguitchaichvili, J. Morales","doi":"10.4311/20182ss0134","DOIUrl":"https://doi.org/10.4311/20182ss0134","url":null,"abstract":"Cueva de la Huachizca is located in the humid forests of the Municipio of Santa Clara del Cobre, Michoacán. During the Postclassic period (1300−1520 ad), Santa Clara del Cobre was a part of the Tarascan Señorio. Ethnographic accounts describe the use of Cueva de la Huachizca as a place of refuge during the Cristero Rebellion (1921−1926). Recent investigations suggest a long history of use including graffiti and inscriptions from the 1800s–1900s and a rock art panel. The panel consists of pecked petroglyphs depicting a man facing an eagle, above a spiral motif. Stylistic analysis of the panel suggests that the rock art was created during pre-Hispanic times, likely by the Postclassic Tarascans. As observed in several regions of Mesoamerica, for the Tarascans, caves were also liminal spaces and had an important role in Postclassic Tarascan cosmology. A ceramic resinera, a pine resin pot, an eagle’s feather, and charcoal were also recovered. The resinera age was estimated by researchers at Archaeomagnetic Services, Geophysics Institute at the National Autonomous University of México-Campus Morelia, Michoacán to between 1921 and 1980. Ethnographic and ethnohistoric accounts describe caves as houses of fertility and rain deities, an idea that while slightly transformed, has survived over 500 years of colonization, and remains in the communities’ social memories. These findings demonstrate the cave’s significance among the descendent communities and Cueva de la Huachizca as an important sacred site.","PeriodicalId":50244,"journal":{"name":"Journal of Cave and Karst Studies","volume":"77 4 1","pages":""},"PeriodicalIF":0.9,"publicationDate":"2021-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"89237362","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Li Xinru, Z. Min, Mi Yidong, Haiyan Chen, Su Hailei, Wei Yuan, F. Guo, Wang Fanfan
Little is known about the difference between bacterial and fungal genetic and functional diversity in karst regions of south China. In this study, the genetic and functional diversity of bacteria and fungi in nine types of soil microenvironments in the karst region in Maolan National Nature Reserve in Guizhou were investigated by PCR-DGGE (Denaturing Gradient Gel Electrophoresis) and BIOLOG EcoPlates. Maolan National Nature Reserve is a UNESCO Biosphere Reserve and plays an important role in protecting the karst forest ecosystem and rare and endangered wild animals and plants in central Asia. The results showed that the diversity of both bacteria and fungi was high and the main factors influencing the diversity of bacteria and fungi were different. The bacterial community structure from different microhabitats under the same vegetation type had higher similarity than similar microhabitats in different vegetation types, which could indicate that the bacterial community structure was mainly controlled by vegetation. For fungi, similar microhabitat species under different vegetation types had higher similarities than different microhabitats species under the same vegetation type, which could indicate that the fungal community structure is mainly controlled by microhabitats. In addition, the metabolic patterns of similar microhabitats in different vegetation were different, while the metabolic patterns of different microhabitats in the same vegetation were not obviously different. In conclusion, the effect of vegetation types on soil microbial functional diversity was greater than that of microhabitats, and this difference was reflected by the different degrees of influence on soil microbial genetic diversity and community structure.
{"title":"Genetic and functional diversity of soil bacteria and fungi from different microhabitats in a karst region in Southern China","authors":"Li Xinru, Z. Min, Mi Yidong, Haiyan Chen, Su Hailei, Wei Yuan, F. Guo, Wang Fanfan","doi":"10.4311/2020mb0106","DOIUrl":"https://doi.org/10.4311/2020mb0106","url":null,"abstract":"Little is known about the difference between bacterial and fungal genetic and functional diversity in karst regions of south China. In this study, the genetic and functional diversity of bacteria and fungi in nine types of soil microenvironments in the karst region in Maolan National Nature Reserve in Guizhou were investigated by PCR-DGGE (Denaturing Gradient Gel Electrophoresis) and BIOLOG EcoPlates. Maolan National Nature Reserve is a UNESCO Biosphere Reserve and plays an important role in protecting the karst forest ecosystem and rare and endangered wild animals and plants in central Asia. The results showed that the diversity of both bacteria and fungi was high and the main factors influencing the diversity of bacteria and fungi were different. The bacterial community structure from different microhabitats under the same vegetation type had higher similarity than similar microhabitats in different vegetation types, which could indicate that the bacterial community structure was mainly controlled by vegetation. For fungi, similar microhabitat species under different vegetation types had higher similarities than different microhabitats species under the same vegetation type, which could indicate that the fungal community structure is mainly controlled by microhabitats. In addition, the metabolic patterns of similar microhabitats in different vegetation were different, while the metabolic patterns of different microhabitats in the same vegetation were not obviously different. In conclusion, the effect of vegetation types on soil microbial functional diversity was greater than that of microhabitats, and this difference was reflected by the different degrees of influence on soil microbial genetic diversity and community structure.","PeriodicalId":50244,"journal":{"name":"Journal of Cave and Karst Studies","volume":"111 1","pages":""},"PeriodicalIF":0.9,"publicationDate":"2021-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"77245788","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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