Relevant bibliographies by topics / Guadalupien

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Academic literature on the topic 'Guadalupien'

Author: Grafiati
Published: 4 May 2024

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Journal articles on the topic "Guadalupien"

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Yulianto, Barlian. "Pegunungan Guadalupe, Cekungan Perem, Texas Barat-New Mexico." Lembaran publikasi minyak dan gas bumi 24, no. 2 (July 25, 2023): 44–50. http://dx.doi.org/10.29017/lpmgb.24.2.1399.

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Pegunungan Guadalupe yang merupakan bagian dari Cekungan Perem terletak di bagian barat Texas dan tenggara New Mexico. Cekungan ini berarah utara-selatan, berbentuk lekuk yang tidak simetri beralaskan batuandasar Prakambrium, terletak pada batas selatanlempeng Amerika Utara.Runtunan sedimen Guadalupian di daerah ini terdiri atas endapan paparan dan cekungan. Evolusi geologi runrutan sedimen Guadalupian di awali oeleh pengendapan batasan karbonat ramp barrier bank system pada Leornardian Atas. Pada Guadalupian Awal-Tengah sistem ini berkembang menjadi shelf deep rim system. Berlanjutnya progradasi dari karbonat rimmed membentuk fasies terumbu pada Guadalaupian Aias
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Nestell, Galina P., and Merlynd K. Nestell. "Late Capitanian (latest Guadalupian, Middle Permian) radiolarians from the Apache Mountains, West Texas." Micropaleontology 56, no. 1-2 (2010): 7–68. http://dx.doi.org/10.47894/mpal.56.1.02.

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A diverse radiolarian fauna is described from strata of a road cut section of the uppermost part of the Bell Canyon Formation (Capitanian, Guadalupian, Middle Permian), Apache Mountains, West Texas. Fifteen new species are described: Campanulithus insuetus, Pseudoalbaillella apachensis, Astroentactinia capitanensis, Polyedroentactinia guadalupensis, Afanasievella apachensis, Copicyntra erinacea, Paracopicyntra snyderi, Klaengspongus planus, Copiellintra orbiculata, C. fastuosa, Shangella capitanensis, Rectotormentum wardlawi, Tetratormentum ormistoni, Quadrilobata? blomei, and Nazarovispongus globosum. The diagnoses of the species Follicucullus sphaericus Takemura in Takemura et al. 1999 and the genus Raciditor Sugiyama 2000 are emended. The rank of the subspecies Raphidociclicus gemellus americanus Nazarov and Ormiston 1985a is raised to species level. The genus Nazarovispongus Kozur 1980 is considered to be a valid genus and is reinstated. Established are one new genus, Afanasievella (assigned to the family Spongentactiniidae), one new subfamily Polyedroentactiniinae (in the composition of the family Orosphaeridae), and one new family Tetratormentidae (in the composition of the order Pyramidata). The radiolarian assemblage from the described section in the Apache Mountains is at least partly coeval with the radiolarian assemblage from the Reef Trail Member of the Bell Canyon Formation in the Guadalupe Mountains, allowing a straight correlation of this age strata between the Apache and Guadalupe mountains. This correlation is supported by the conodont species that define the latest Guadalupian conodont zones and that occur together with radiolarians in both areas. The radiolarian species Albaillella yamakitai in sense of Xia et al. (2005) present in the late Guadalupian J. altudaensis conodont Zone cannot be a marker for the Guadalupian – Lopingian boundary as was proposed by Xia et al. (2005).
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Nestell, Merlynd K., and Bruce R. Wardlaw. "An apparatus reconstruction of the conodont Caenodontus serrulatus Behnken 1975." Micropaleontology 61, no. 4-5 (2015): 293–300. http://dx.doi.org/10.47894/mpal.61.4.03.

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The conodont species Caenodontus serrulatus Behnken is a rare coniform element first described in 1975 from Guadalupian strata exposed in the Guadalupe and Delaware Mountains of West Texas. Because it is rare, coniform, and occurs long after most coniform elements supposedly disappeared, it has been hauntingly mysterious. Based on new material containing a varied assemblage of coniform elements recovered from an outcrop of the Hegler Limestone (Guadalupian) in the Patterson Hills, West Texas, it is proposed that Caenodontus is comprised of a 6-7 membrate coniform apparatus and that this apparatus is very similar to the one proposed for the genus Ansella from the Ordovician.
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Matovina, Timothy. "The First Guadalupan Pastoral Manual: Luis Laso De La Vega's Huei Tlamahuiçoltica (1649)." Horizons 40, no. 2 (December 2013): 159–77. http://dx.doi.org/10.1017/hor.2013.74.

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Millions of devotees acclaim the Nahuatl-language Nican mopohua account of the apparitions of Our Lady of Guadalupe to Juan Diego as the foundational text of the Guadalupe tradition. A number of scholarly analyses have also examined the Nican mopohua as a prime source for that tradition. But no previous study has focused on a theological examination of Luis Laso de la Vega's Huei tlamahuiçoltica (1649), in which the Nican mopohua was first published. Huei tlamahuiçoltica is the premier Guadalupan pastoral manual and encompasses other important material, such as the Nican motecpana account of miracles attributed to Guadalupe's intercession, and the earliest published synopsis of Juan Diego's life posed as a model for Christian discipleship. This article explores Laso de la Vega's contributions and the ongoing significance of his treatise for the development of theological works and pastoral ministries centered on Guadalupe.
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Maldonado, Amy L., and Paula J. Noble. "Radiolarians from the upper Guadalupian (Middle Permian) Reef Trail Member of the Bell Canyon Formation, West Texas and their biostratigraphic implications." Micropaleontology 56, no. 1-2 (2010): 69–115. http://dx.doi.org/10.47894/mpal.56.1.03.

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Moderately well-preserved radiolarians are described from two measured sections of the Reef Trail Member of the Bell Canyon Formation (Middle Permian), exposed in the Patterson Hills, Guadalupe Mountains National Park, West Texas. The Reef Trail Member is the youngest member of a series of basinal marine carbonates deposited in the Delaware basin prior to the deposition of the Castile Formation evaporites, and represents the uppermost Guadalupian (upper Capitanian). The Guadalupian-Lopingian boundary is presumed to occur at or just above the top of the Reef Trail-Castile contact because of the presence of C. postbitteri hongshuiensis ~ 2m below the top of the Reef Trail Member in sections in the Patterson Hills. A total of 30 genera containing 51 species were recovered from the Reef Trail Member, belonging to the orders Albaillellaria, Latentifistularia, Spumellaria, and Entactinaria. The following new taxa are described: Raphidociclicus scutum, Camptoalatus volaticus, Pseudoalbaillella delawarensis, Astroentactinia porosa, Stigmosphaerostylus favusa, Polyedroentactinia quadrata, Praedeflandrella firmata, P. prolata, Copicyntra spinosa, Copicyntra irregulata, and Paracopicyntra puncta, and Copicyntroides nazarovi. The following taxa are emended: Raciditor scalae (Caridroit and De Wever 1986), and Klaengspongus Sashida 2000b. Near the top of the Reef Trail Member, there are marked fluctuations in the relative abundances of albaillellarian and latentifistularian species. Fluctuations are possibly controlled by paleoenvironmental changes associated with the onset of the end-Guadalupian extinction event. Biostratigraphically, the fauna most closely correlates with the widely recognized F. bipartitus – F. charveti Zone sensu Caridroit, which we now consider to be uppermost Guadalupian, not Lopingian, and to the Guadalupian F. charveti Zone of Sun and Xia 2006 from oceanic facies in China. Both older and younger biostratigraphic markers also occur in the Reef Trail fauna, including Pseudoalbaillella longtanensis and A. yamakitai, requiring a reevaluation of the reliability of these albaillellarian taxa in biostratigraphy.
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Nestell, G. P., and M. K. Nestell. "Middle Permian (Late Guadalupian) foraminifers from Dark Canyon, Guadalupe Mountains, New Mexico." Micropaleontology 52, no. 1 (March 1, 2006): 1–50. http://dx.doi.org/10.2113/gsmicropal.52.1.1.

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Nestell, Galina P., and Merlynd K. Nestell. "Roadian (Earliest Guadalupian, Middle Permian) Radiolarians from the Guadalupe Mountains, West Texas, USA Part III: Latentifistularia." Micropaleontology 69, no. 1 (2023): 1–60. http://dx.doi.org/10.47894/mpal.69.1.01.

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Radiolarians of the order Latentifistularia are described from strata of the Roadian Stage (Guadalupian Series, middle Permian) exposed in a small roadside quarry (Quarry section) in the Guadalupe Mountains, West Texas. The families Cornellidae Kozur and Mostler and Ishigaidae Kozur and Mostler are discussed. The genus Pseudotormentus is reassigned to the family Latentifistulidae. The genus Octatormentum and species Latentifistula patagilaterala, Quinqueremis robusta, Ormistonella minima, Tetratormentum nitidus and Octatormentum cornelli are revised. The species Tormentum delicatum assigned to the genus Rectotormentum. One genus, Nabespecha, is reinstated herein. Three new genera, Murcheyella, Sashitonishella and Quadrulites, and 17 new species: Latentifistula crassa, L. macilenta, L. coniformis, Murcheyella marginata, Latentibifistula dellensis, Pseudotormentus ornatus, Cauletella caridroiti, Praedeflandrella insueta, Quinqueremis pentagonus, Q. porosus, Sashitonishella rara, Polyfistula composita, Ormistonella aetheria, O. decurvata, Tetragregnon delawarus, Tormentum lobatum, and Grandetortura sashidai are described.
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Nicklen, Brian L., Gorden L. Bell, Lance L. Lambert, and Warren D. Huff. "Tephrochronology of the Manzanita Limestone in the Middle Permian (Guadalupian) Type Area, West Texas and southeastern New Mexico, USA." Stratigraphy 12, no. 2 (2015): 123–47. http://dx.doi.org/10.29041/strat.12.2.04.

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Despite being recognized for many years, bentonites in the Guadalupian (Middle Permian Series) type area of West Texas and southeastern New Mexico have received little research attention. These important deposits offer opportunities for long distance stratigraphic correlation and high-precision radioisotopic age dating. In this study, apatite phenocryst chemistry is used to establish a tephrochronologic framework for the Manzanita Limestone Member of the Cherry Canyon Formation. Samples were collected from bentonites in one core and five field localities including Nipple Hill, which is the site of the Late Guadalupian (Capitanian Stage) GSSP and located in Guadalupe Mountains National Park. Apatite phenocrysts from these samples were analyzed for minor, trace, and rare earth element chemistry using electron microprobe techniques. Results indicate the presence of three patterns or trends of data that are repeated at multiple localities. These groups of data are interpreted to represent coeval deposits and are correlated among several localities to form a tephrochronologic framework. This framework links the strata on Nipple Hill with that of several other Guadalupian type area localities. Absolute age time control for the Guadalupian is poor, and the precise stratigraphic position of the existing radioisotopic date from Nipple Hill is uncertain. Based on a review of published reports and a new measured section of Nipple Hill presented herein, the most accurate position is in the Manzanita Member. That placement adjusts the only radioisotopic age constraint for the Capitanian GSSP lower in the Wordian Stage than previously reported. The bentonite correlations proposed herein constrain this position to the Mz-3 cycle of the Manzanita High Frequency Sequence and allow it to be traced to several outcrop localities, and across the Delaware Basin in the subsurface. Based on the correlation of a bentonite from its locus typicus near Casey’s Last Chance Well in Culberson County, Texas, the type specimen of the biostratigraphically significant ammonoid Newellites richardsoni is confirmed to have been recovered from the basal Manzanita Member (Wordian Stage), stratigraphically underlying the radioisotopic age date. The type locality of this ammonoid has been inconsistently reported in museum records and in the literature.
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Rigby, J. Keith, Gorden L. Bell, and Kirsten Thompson. "Hexactinellid and associated sponges from the upper Reef Trail Member of the Bell Canyon Formation, southern Guadalupe Mountains National Park, Texas." Journal of Paleontology 81, no. 6 (November 2007): 1241–56. http://dx.doi.org/10.1666/06-022r1.1.

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A small faunule of silicified hexactinellid sponges and root tufts has been recovered from the upper Guadalupian Reef Trail Member of the Bell Canyon Formation, from the Patterson Hills, in the southwestern part of the Guadalupe Mountains National Park in western Texas. Some demosponges from the type section of the Reef Trail Member, near the mouth of McKittrick Canyon on the front of the Guadalupe Mountains in the park, have also been documented. Included in the faunule from the Patterson Hills localities are the new amphidiscosid hexactinellid pelicasponge Trailospongia reischi n. gen. and sp., the questionable pelicaspongiid Hexirregularia nana n. gen. and sp., and the dictyospongiid hexactinellids Microstaura doliolum Finks, 1960, and Microstaurella minima n. gen. and sp., and Microstaurella parva n. gen. and sp. They are associated with specimens of the lyssacinosid brachiosponges Toomeyospongiella gigantia Rigby and Bell, 2005, Toomeyospongia modica n. sp., and Toomeyospongia minuta n. gen. and sp., and fragments of three different types of root tufts, termed Tufts 1, 3, and 4. Two specimens of the new cylindrical demosponge Mckittrickella pratti n. gen. and sp. are associated with Tuft 2 in the collection from the type section of the Reef Trail Member, and a third specimen was collected from the member in the Patterson Hills. These sponges from Localities 1-7 are the youngest Permian sponges known from the region, and possibly from North America.
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Nestell, Galina P., and Merlynd K. Nestell. "Roadian (earliest Guadalupian, middle Permian) radiolarians from the Guadalupe Mountains, West Texas, USA Part II: Spongy radiolarians (?Entactinaria and Spumellaria)." Micropaleontology 67, no. 6 (2021): 527–55. http://dx.doi.org/10.47894/mpal.67.6.01.

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Spongy radiolarians are described from strata of the Roadian Stage (Guadalupian, middle Permian) exposed in a small quarry (Quarry section) in the Guadalupe Mountains,West Texas. These radiolarians are assigned to the orders Entactinaria (conditionally) and Spumellaria. Two new families Hegleriidae and Glomispinidae are proposed. The genus Hegleria Nazarov and Ormiston and its two species, H. mammilla (Sheng andWang) and H. mammifera Nazarov and Ormiston are discussed. Based on an analysis of the distribution and preservation of the illustrated specimens of these two species in the literature, it is proposed that the species H. mammilla should be considered as nomen dubium. The genus Uberinterna Sashida and Tonishi and one species Copicyntra simulens Nazarov and Ormiston are revised. Five new genera, Texasospongites, Allenispongus, Cutoffella, Glomispina, and Orminazarella, and ten new species Texasospongites fazleevi, Allenispongus nobilis, Cutoffella perplexa, Glomispina mirifica, Uberinterna hearstae, U. ancestralis, Provisocyntra vancouveringi, Orminazarella nuda, Paracopicyntra bella, and Copiellintra variabilis are described.
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Dissertations / Theses on the topic "Guadalupien"

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Hemmati, Soheil. "Stratigraphy and bio-event studies of the Guadalupian - Lopingian boundary in the northern margin of Sanandaj-Sirjan Zone, Central Iran and North-West of Iran." Electronic Thesis or Diss., Sorbonne université, 2024. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2024SORUS011.pdf.

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La position de la limite Guadalupien - Lopingien (GLB) a longtemps été un sujet de controverse Parmi les nombreuses coupes étudiées, trois régions spécifiques : Julfa (coupe d'Ali-Bashi), Tabas (coupe de Bagh-e-Vang) et Abadeh (coupe de Baghuk) ont été choisies pour une étude ciblée. La coupe d'Ali-Bashi a fait l'objet d'un échantillonnage et d'une vaste collecte de plus de 240 échantillons de roche sur une épaisseur mesurée de 189 mètres et dans la coupe de Bagh-e-Vang, plus de 160 échantillons sur 200 mètres d'épaisseur dans la Formation de Jamal. L'échantillonnage de la section Baghouk a rencontré des obstacles spécifiques qui ont entravé notre progression, notamment : les conditions climatiques, la crise économique en Iran et la pandémie de covid-19. Une étude lithostratigraphique très détaillée de la Formation de Khachik sur la coupe d'Ali-Bashi a permis d'identifier 14 unités rocheuses distinctes au sein des trois membres principaux. Ceci permet un nouvel inventaire lithostratigraphique de ces séquences, qui peut être compré avec les recherches existantes sur la Formation de Khachik. De plus, dans la section Bagh-e-Vang, 10 unités de la Formation de Jamal appartenant aux trois membres ont également été identifiées. De plus, des méthodes d'extraction, au CH₂O₂, au CH₃COOH, l'acétolyse à chaud et les protocoles à l'HF, ont été testées pour l'extraction des microfossiles. Après d'importants efforts de préparation et un protocole soigneusement élaboré destiné à l'obtention de conodontes, l'application des techniques CH₂O₂ et CH₃COOH, les coupes d'Ali-Bashi et Bagh-e-Vang, n'ont pas livré de conodontes. Trois autres méthodes ont été testées pour l'extraction d'ostracodes sur des échantillons de la coupe d'Ali-Bashi. Les échantillons ont été préparés avec de l'acide formique à 10 % (CH₂O₂) et de l'acide acétique à 15 % (CH₃COOH). Le protocole CH₂O₂ a été productif avec des ostracodes bien conservés, avec dix taxons dans des calcaires dolomitisés durs, tandis que les autres processus (CH₃COOH à froid) n'ont rien donné. L'application du protocole d'acétolyse à chaud s'est avérée efficace pour extraire une quantité importante de carapaces d'ostracodes bien conservées, conduisant à l'identification d'un total de 56 espèces. La technique à l'HF dans le traitement de 12 échantillons de cherts des coupes d'Ali-Bashi et Bagh-e-Vang n'a pas permis d'isoler de radiolaires. L'analyse des microfaciès dans la coupe d'Ali-Bashi a permis d'identifier 15 microfaciès distincts subdivisés en 28 sous-microfaciès. L'assemblage de groupes de microfaciès sont de MKL1 à MKL2 (milieu lagunaire), de MKR2 à MKR3 (restreint) présente des caractéristiques d'un cadre restreint de rampe intérieure, MKO1 à MKO4 (marine ouvert) en zone de rampe interne. Les microfaciès MKM1 à MKM3 se sont déposés dans un environnement marin ouvert, dans les zones de la rampe médiane, tandis que MKT1 à MKT3 ont été identifiés dans les parties inférieures de la rampe extérieure, correspondant à la position du pied de pente de la plate-forme carbonatée. De plus, en se rapportant aux microfaciès standards défnis par Flugel (2010), l'étude propose 10 microfaciès de type RMF, ainsi que leurs 4 SMF correspondants. De plus, sur la base des zones de faciès standard (ZF) introduites par Wilson (1975), trois ZF présentant une tendance ascendante peu profonde, à savoir FZ8, FZ7 et FZ3, ont été délimitées avec succès
The position of the Guadalupian-Lopingian Boundary (GLB) has long been a subject of contention among researchers. Among the numerous sections investigated, three specific regions Julfa (Ali-Bashi section), Tabas (Bagh-e-Vang section), and Abadeh (Baghuk section) have been chosen for focused study in this project. The Ali-Bashi section where sampling and an extensive collection of over 240 rock samples from a measured thickness of 189 meters and in the Bagh-e-Vang section a meticulous effort resulted in the collection of more than 160 rock samples from an outcrop measuring 200 meters in thickness in the Jamal Formation. Sampling the Baghuk section, encountered specific obstacles that impeded our progress including: climatic conditions, economic crisis in Iran and covid-19 pandemic. High-detailed lithostratigraphical investigation of the Khachik Formation in the Ali-Bashi section, led to identified 14 distinct rock units within the three main members. This discovery has the potential to stimulate the creation of a new lithostratigraphic inventory for these sequences, which can be aligned with the existing background research on the Khachik Formation in this particular section. Furthermore, in the Bagh-e-Vang section, 10 rock units from Jamal Formation strata's belonging to the three members have also been identified. Moreover, Various extraction methods, including CH₂O₂, CH₃COOH, hot acetolysis, and HF protocols, were evaluated for the isolation of microfossils. After extensive preparation efforts and carefully crafted protocol intended for conodont element identification, applying both the CH₂O₂ and CH₃COOH techniques, in the Ali-Bashi and the Bagh-e-Vang sections were not achieved any conodonts. Three other methods were tested for ostracod extraction from Ali-Bashi section samples. The samples were prepared with cold 10% formic acid (CH₂O₂) and 15% acetic acid (CH₃COOH). The CH₂O₂ protocol was productive with well-preserved ostracods, allowed us to determine ten taxa were obtained exclusively through the diluted CH₂O₂ protocol from the hard dolomitized limestones, while the other cold CH₃COOH procedures were unsuccessful. The application of the hot acetolysis protocol proved successful in extracting a significant quantity of excellently preserved ostracods, leading to the identification of a total of 56 species. Despite our unwavering commitment to the recommended protocol applied the HF technique in the processing of 12 cherty samples obtained from the Ali-Bashi and Bagh-e-Vang sections yielded a disheartening outcome for the radiolarian microfossils. Microfacies analysis in the Ali-Bashi section led to identified 28 sub-microfacies which, derived with 15 distinct microfacies. The assemblage of microfacies groups are, ranging from MKL1 to MKL2 (lagoonal environment), MKR2 to MKR3 (restricted), MKO1 to MKO4 (open-marine) of the inner ramp zone. The MKO1 to MKO4, suggests a confined setting, occurring in the final part of the inner ramp under an open marine environment. Microfacies groups MKM1 to MKM3 are inferred to have been deposited in open marine environment, within the mid-ramp zones, whereas MKT1 to MKT3 were identified in the basal parts of the outer ramp, corresponding to the lower part of the slope within the carbonate shelf setting. Additionally, adhering to the standard microfacies designated by Flugel (2010), the study proposes 10 microfacies of the RMF type, along with their corresponding 4 SMFs for the studied strata. Besides, based on the standard facies zones (FZ) introduced by Wilson (1975), three FZs exhibiting a shallowing-upward trend, namely FZ8, FZ7, and FZ3, have been successfully delineated
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Maldonado, Amy L. "Taxonomy and biostratigraphy of upper Guadalupian radiolaria from the reef trail member of the Bell Canyon formation, Guadalupe Mountains National Park, West Texas, USA /." abstract and full text PDF (UNR users only), 2008. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:1459467.

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Thesis (M.S.)--University of Nevada, Reno, 2008.
"August, 2008." Includes bibliographical references (leaves 142-149). Library also has microfilm. Ann Arbor, Mich. : ProQuest Information and Learning Company, [2008]. 1 microfilm reel ; 35 mm. Online version available on the World Wide Web.
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Verna, V. "GUADALUPIAN BRACHIOPODS FROM TUNISIA AND TURKEY: SYSTEMATICS AND PALAEOBIOGEOGRAPHIC IMPLICATIONS." Doctoral thesis, Università degli Studi di Milano, 2011. http://hdl.handle.net/2434/152907.

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In the present PhD Thesis two Guadalupian brachiopod faunas are described respectively from succession cropping out at Djebel Tebaga de Medenine, S Tunisia, and from the Guadalupian lower-middle part of the Pamuçak Formation at Çürük Dağ, Antalya (Turkey). The study is based on collection already available in Dipartimento di Scienze della Terra “A. Desio”, Milano and on material newly collected by the writer. The taxonomic study and description of the brachiopod collections, based on the observations of the macro- and micro- external and internal morphological features, with critical comparison with the available literature, has allowed the determinations of 1260 specimens at generic and specific level into 68 species (including the undetermined ones) and 42 genera; they belong to orders Productida, Orthotetida, Orthida, Rhynchonellida, Athyridida, Spiriferida and Terebratulida for the Tunisian fauna; to the orders Productida, Orthotetida, Orthida, Rhynchonellida, Athyridida, Spiriferida, Spiriferinida and Terebratulida for the Turkish fauna. Five new species and two new genera are identified and established and are in press in two publications (Verna et al. in press a, b). Several brachiopod taxa are revised and their diagnostic characters better identified in order to make their determination, up to now problematic, easier (i.e. Squamularia Gemmellaro, 1899 and Permophricodothyris Pavlova). In the course of this research, the Gemmellaro collection of brachiopods from Sosio, Sicily has been also revised in part. The stratigraphic range of the Tunisian brachiopods is consistent with the Wordian- early Capitanian age suggested by the associated fusulinids and conodonts which are the tools on which the Permian Time Scale is based, allowing the correlation of the International (Global) with the Tethyan regional scale, particularly for the Guadalupian part. The age of the Turkish brachiopods coming from the lower middle part of the Pamuçak Formation is mid-Roadian to Capitanian, based on conodonts, fusulinids and already published data (Angiolini et al. 2007). The brachiopod record at Çürük Dağ section (Turkey) has implications to understand the pattern of the end-Guadalupian biotic crisis which is here represented by highly diversified pre-crisis assemblages terminating rather abruptly and being followed by Lopingian brachiopod taxa which show a significantly lower biodiversity. The last part of this study consists of a palaeobiogeographic analysis based on the comparison of the brachiopod faunas from Tunisia and Turkey originally collected and studied by the writer, with coeval ones described in several publications in the recent and distant past coming from the successions of Sosio (Sicily), Oman, N Iran, Central Afghanistan, Karakorum, Salt Range, SE Thailand. This palaeobiogeographic analysis aims to test the palaeogeographic reconstructions, independently derived from palaeomagnetic data and to derive the possible dispersal pattern of the brachiopod genera during the Guadalupian. The methods used for this analysis are cluster analysis and principal coordinate analysis (PCO), based on the similarity indices of Jaccard and Simpson applied to a presence/absence data matrix (taxa per geographic areas) of the brachiopod genera coming from Tunisia, Turkey and the other faunal stations quoted above, using the software PAST (Hammer et al. 2001). The palaeobiogegraphic affinities of the analyzed faunal stations are in agreement with the Guadalupian palaeogeographic reconstruction based on palaeomagnetic data of Muttoni et al. (2009) and indicates a consistent degree of isolation of Tunisia and Sosio from the other regions and strong faunal links between Turkey and the Gondwanan margins, represented by Oman, Salt Range and S Thailand.
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Gibson, Christopher. "Guadalupan novena in the context of Advent." Theological Research Exchange Network (TREN), 1996. http://www.tren.com.

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Miranda, Bruno Soares. "Peregrinações portuguesas a Nuestra Señora de Guadalupe." Universidade de São Paulo, 2011. http://www.teses.usp.br/teses/disponiveis/8/8138/tde-14052011-100321/.

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Durante a Idade Média, o homem português expressava sua fé de algumas formas. A peregrinação se constituía em uma dessas formas. Neste sentido, observamos um Mosteiro na região da Estremadura Castelhana, onde frades da Ordem de São Jerônimo guardavam uma imagem de Nossa Senhora de Guadalupe. Este Mosteiro foi alvo de peregrinação de simples portugueses, passando por membros de vários estratos sociais e até de um monarca, D. Afonso V. Para analisarmos esta peregrinação no século XV, utilizamos como fonte o Livro de Milagres do Mosteiro, onde os Jerónimos recolhiam os motivos da peregrinação e, assim, possuindo instrumentos para a divulgação do culto à virgem de Guadalupe. A análise da documentação leva-nos a descobrir aspectos da espiritualidade do português medieval, assim como também a observarmos que não somente de fé vivia a rota para o Mosteiro, visto que um jogo político igualmente fazia sua peregrinação.
During the Middle Age, portuguese man used to express their faith in many ways. Peregrination was one of theses ways. In this sense, we observed a Monastery located in the region of the Castilian Extremadura, in which friars of the Order of Saint Jerome kept an image of Saint Mary of Guadalupe. This Monastery was the target of peregrination of mere Portuguese man, members of different social classes and even a monarch, D. Afonso V. The analysis of XV century peregrination was based on the Book of Miracles of the Monastery, where hieronymites collected the reasons of the peregrination and, thus, had instruments to spread the cult to the virgin of Guadalupe. The analysis of the documentations reveals aspects of Portuguese man spirituality. We also observe that the route for the Monastery was not motivated only by faith, considering that the peregrination also constituted a political game.
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Heeren, Larissa Requa. "Recommendations for Economic Development in Guadalupe, CA." DigitalCommons@CalPoly, 2011. https://digitalcommons.calpoly.edu/theses/571.

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It is recommended that the City of Guadalupe prepare and implement a small-scale business expansion and retention program using existing service providers in the area. This type of program model seems to hold the most potential for Guadalupe. A mixed-methods approach including in-depth cases studies of existing economic development programs and an analysis of opportunities and constraints in Guadalupe informs a set recommendations for future economic development in the City. Data was collected in three phases: short interviews with a variety of economic development program staff, short interviews with Guadalupe business owners and City officials and in-depth interviews with staff from five selected case-study programs.
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Ortiz-Ramirez, Eduardo A. "The Virgin of Guadalupe and Mexican nationalism : expressions of criollo patriotism in colonial images of the Virgin of Guadalupe /." abstract and full text PDF (UNR users only), 2008. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:1455656.

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Thesis (M.A.)--University of Nevada, Reno, 2008.
"May, 2008." Includes bibliographical references (leaves 120-126). Library also has microfilm. Ann Arbor, Mich. : ProQuest Information and Learning Company, [2009]. 1 microfilm reel ; 35 mm. Online version available on the World Wide Web.
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Hebbard, Matthew S. "The virgin of Guadalupe and Mexican religious belief." Theological Research Exchange Network (TREN) Access this title online, 2003. http://www.tren.com.

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Crémoux, Françoise. "Pèlerinages et miracles à Guadalupe au XVIe siècle /." Madrid : [Paris] : Casa de Velázquez ; [diff. Association française des presses universitaires], 2001. http://catalogue.bnf.fr/ark:/12148/cb400406139.

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Hood, Robert L. (Robert Leroy). "Discursive Horizons of Human Identity and Wilderness in Postmodern Environmental Ethics: A Case Study of the Guadalupe Mountains of Texas." Thesis, University of North Texas, 1993. https://digital.library.unt.edu/ark:/67531/metadc500395/.

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Using a genealogy of the narratives of the Guadalupes, I explore three moral identities. The Mescalero Apache exist as caretakers of sacred space. Spanish and Anglo settlers exist as conquerors of a hostile land. The park service exists as captives, imprisoned in the belief that economic justifications can protect the intrinsic value of wilderness. The narrative shift from oral to abstract text-based culture entails a shift from intrinsic to instrumental valuation. I conclude that interpretation of narratives, such as those of the Guadalupes, is not by itself a sufficient condition for change. Interpretation is, however, a necessary condition for expanding the cultural conversation beyond merely instrumental justifications to include caring for wilderness's intrinsic values.
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Books on the topic "Guadalupien"

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R, Wardlaw Bruce, Grant Richard E. 1927-1994, and Rohr David Malcolm 1947-, eds. The Guadalupian symposium. Washington, D.C: Smithsonian Institution Press, 2000.

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Jenzen, Doug. Guadalupe. Charleston, South Carolina: Arcadia Publishing, 2014.

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Rigby, J. Keith. Sponges from the Reef Trail Member of the Upper Guadalupian (Permian) Bell Canyon formation, Guadalupe Mountains National Park, Texas. Lawrence, Kan: Allen Press, 2006.

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David, Cáceres González, ed. Guadalupe topo. Barcelona: Blume, 2010.

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Fernández, José Antonio Santos. Guadalupe Zurita. Saltillo, Coahuila, Mexico]: Icocult, Instituto Coahuilense de Cultura, 2009.

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Chinchilla, Perla. Guadalupe Victoria. Col. Juárez [Mexico City]: Comisión Nacional para las Celebraciones del 175 Aniversario de la Independencia Nacional y 75 Aniversario de la Revolución Mexicana, 1985.

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Fernández, José Antonio Santos. Guadalupe Zurita. Saltillo, Coahuila, Mexico]: Icocult, Instituto Coahuilense de Cultura, 2009.

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1786-1843, Victoria Guadalupe, and Salas Rodríguez Gonzalo, eds. Guadalupe Victoria. [Mexico City, Mexico]: Senado de la República, 1987.

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Léa, Fluck, ed. Guadalupe Ruiz. Bogotá: La Silueta Ediciones, 2008.

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González, José Luis González. Guadalupe Victoria. Durango, DGo., México: UJED Editorial, 2006.

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Book chapters on the topic "Guadalupien"

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Thorsen, Jakob Egeris, and R. Andrew Chesnut. "Virgin of Guadalupe." In Encyclopedia of Latin American Religions, 1–3. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-08956-0_239-1.

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Thorsen, Jakob Egeris, and R. Andrew Chesnut. "Virgin of Guadalupe." In Encyclopedia of Latin American Religions, 1616–18. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-27078-4_239.

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Vázquez, Margarita Vega. "Zúñiga Lira, Guadalupe." In The Palgrave Biographical Encyclopedia of Psychology in Latin America, 1–3. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-38726-6_77-1.

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Vázquez, Margarita Vega. "Zúñiga Lira, Guadalupe." In The Palgrave Biographical Encyclopedia of Psychology in Latin America, 1379–81. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-030-56781-1_77.

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Torres, Theresa L. "Las Guadalupan as Speak." In The Paradox of Latina Religious Leadership in the Catholic Church, 71–92. New York: Palgrave Macmillan US, 2013. http://dx.doi.org/10.1057/9781137370327_4.

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Leeming, David A. "Our Lady of Guadalupe." In Encyclopedia of Psychology and Religion, 1680–81. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-24348-7_9095.

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Leeming, David A. "Our Lady of Guadalupe." In Encyclopedia of Psychology and Religion, 1271. Boston, MA: Springer US, 2014. http://dx.doi.org/10.1007/978-1-4614-6086-2_9095.

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Caycho-Rodríguez, Tomás. "Oblitas-Guadalupe, Luis Armando." In The Palgrave Biographical Encyclopedia of Psychology in Latin America, 1–2. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-38726-6_437-1.

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Leeming, David A. "Our Lady of Guadalupe." In Encyclopedia of Psychology and Religion, 1–2. Berlin, Heidelberg: Springer Berlin Heidelberg, 2016. http://dx.doi.org/10.1007/978-3-642-27771-9_9095-2.

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Caycho-Rodríguez, Tomás. "Oblitas-Guadalupe, Luis Armando." In The Palgrave Biographical Encyclopedia of Psychology in Latin America, 896–97. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-030-56781-1_437.

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Conference papers on the topic "Guadalupien"

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Sonnenfeld, Mark D. "Anatomy of offlap: Upper San Andres Formation (Permian, Guadalupian), Last Chance Canyon, Guadalupe Mountains, New Mexico." In 44th Annual Fall Field Conference. New Mexico Geological Society, 1993. http://dx.doi.org/10.56577/ffc-44.195.

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Ferris, Malcolm A., Charles Kerans, and Jr Sharp. "Outcrop permeabilities within four facies of a single depositional parasequence, upper San Andres Formation (Permian, Guadalupian/Leonardian), Lawyer Canyon, Guadalupe Mountains, Otero County, New Mexico." In 44th Annual Fall Field Conference. New Mexico Geological Society, 1993. http://dx.doi.org/10.56577/ffc-44.205.

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Lucas, Spencer G. "The Guadalupian series and the Permian timescale." In 73rd Annual Fall Field Conference. New Mexico Geological Society, 2023. http://dx.doi.org/10.56577/ffc-73.82.

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Land, Lewis. "Pre-conference field trip one: Guadalupe Peak Trail, Guadalupe Mountains National Park." In 73rd Annual Fall Field Conference. New Mexico Geological Society, 2023. http://dx.doi.org/10.56577/ffc-73.2.

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Lara Peña, R. Aaron, and Pilar Navas-Parejo. "PALEOBIOGEOGRAPHIC IMPLICATIONS OF GUADALUPIAN FAUNAS FROM NORTHWESTERN SONORA." In Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-313902.

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Wheeler, Dale. "Aragonite pseudomorphs of Guadalupe County, New Mexico." In 21st Annual New Mexico Mineral Symposium. Socorro, NM: New Mexico Bureau of Geology and Mineral Resources, 2000. http://dx.doi.org/10.58799/nmms-2000.237.

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Smith, Benjamin Paul, and Charles Kerans. "GUADALUPIAN/LOPINGIAN CHEMOSTRATIGRAPHY OF THE DELAWARE BASIN: UNRAVELLING REGIONAL VERSUS GLOBAL FACTORS." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-305568.

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Genrich, J. F., and J. Mark Stevenson. "GPS‐positioned gravity survey of Guadalupe Island, Mexico." In SEG Technical Program Expanded Abstracts 1992. Society of Exploration Geophysicists, 1992. http://dx.doi.org/10.1190/1.1822159.

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Isozaki, Yukio, and Thomas Sevais. "THE HIRNANTIAN (LATE ORDOVICIAN) AND END-GUADALUPIAN (MIDDLE PERMIAN) MASS EXTINCTION EVENTS COMPARED." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-307891.

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Spilde, Michael N., Diana E. Northrup, and Penelope J. Boston. "Ferromanganese deposits in the caves of the Guadalupe Mountains." In 57th Annual Fall Field Conference. New Mexico Geological Society, 2006. http://dx.doi.org/10.56577/ffc-57.161.

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Reports on the topic "Guadalupien"

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Fuller, Billy D. Upper Guadalupe River Flood Control Weir, San Jose, California. Fort Belvoir, VA: Defense Technical Information Center, November 2003. http://dx.doi.org/10.21236/ada419476.

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Muldavin, Esteban, Yvonne Chauvin, Teri Neville, Hannah Varani, Jacqueline Smith, Paul Neville, and Tani Hubbard. A vegetation classi?cation and map: Guadalupe Mountains National Park. National Park Service, 2024. http://dx.doi.org/10.36967/2302855.

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A vegetation classi?cation and map for Guadalupe Mountains National Park (NP) is presented as part of the National Park Service Inventory & Monitoring - Vegetation Inventory Program to classify, describe, and map vegetation communities in more than 280 national park units across the United States. Guadalupe Mountains NP lies in far west Texas and contains the highest point in the state, Guadalupe Peak (8,751 ft; 2,667 m). The mountain escarpments descend some 5,000 ft (1,500 m) to the desert basins below forming a complex geologic landscape that supports vegetation communities ranging from montane coniferous forests down to desert grasslands and scrub. Following the US National Vegetation Classi?cation (USNVC) standard, we identi?ed 129 plant associations hierarchically tiered under 29 groups and 17 macrogroups, making it one of the most ecologically diverse National Park Service units in the southwestern United States. An aspect that adds to this diversity is that the park supports communities that extend southward from the Rocky Mountains (?ve macrogroups) and Great Plains (one macrogroup) and northward from the Chihuahuan Desert (two macrogroups) and Sierra Madre Orientale of Mexico (three macrogroups). The remaining six macrogroups are found in the Great Basin (one macrogroup), and throughout the southwestern United States (remaining ?ve macrogroups). Embedded in this matrix are gypsum dunelands and riparian zones and wetlands that add further complexity. We describe in detail this vegetation classi?cation, which is based on 540 vegetation plots collected between 2006 and 2010. Full descriptions and diagnostic keys to the plant associations along with an overall plant species list are provided as appendices. Based on the vegetation classi?cation and associated plot data, the vegetation map was developed using a combined strategy of automated digital object-oriented image classi?cation and direct-analog image interpretation of four-band National Agricultural Imagery Program (NAIP) aerial photography from 2004 and 2008 and Landsat Thematic Mapper satellite imagery. The map is designed to facilitate ecologically-based natural resource management at a 1:24,000 scale with 0.5-ha minimum map unit size. The map legend is hierarchically structured: the upper Level 1 consists of 16 map units corresponding in most cases to the USNVC group level, and an additional map unit describing built-up land and agriculture; Level 2 is composed of 48 nested map units re?ecting various combinations of plant associations. A ?eld-based accuracy assessment using 341 vegetation plots revealed a Level 1 overall accuracy of 79% with 90% CI of 74?84% and 68% with 90% CI of 59?76% at Level 2. An annotated legend with summary descriptions of the units, distribution maps, aerial photo examples of map unit polygons, and representative photos are provided in Appendix D. Large wall-size poster maps at 1:35,000 scale were also produced following NPS cartographic standards. The report, plot data, and spatial layers are available at National Park Service Vegetation Mapping Program https://www.nps.gov/im/vegetation-inventory.htm). Outcomes from this project provide the most detailed vegetation classi?cation and highest resolution mapping for Guadalupe Mountains NP to date to support many uses including ?re, recreation, vegetation, and wildlife management, among others. The upper Level 1 map is particularly suited to landscape-scale, park-wide planning and linkages to its sister park, Carlsbad Caverns NP. The Level 2 mapping provides added detail for use at a more localized project scale. The overall accuracy of the maps was good, but because Guadalupe Mountains NP is primarily wilderness park, there were logistical challenges to map development and testing in remote areas that should be considered in planning management actions. In this context, some map units would bene?t from further development and accuracy assessment. In particular, a higher resolution mapping of McKittrick Creek riparian habitat at 1:6,000 scale or ?ner is recommended for this important habitat in the park. In addition, developing a structural canopy height model from LiDAR imagery would be useful to more accurately quantify woody canopy density and height to support ?re management and other habitat management issues. With respect to understanding vegetation dynamics in this time of rapid environmental change, the 540 vegetation plots themselves are su?ciently georeferenced and have the data resolution to be useful in detecting change at the decadal scales across much of the park. To this end, an additional recommendation would be to install more plots to ?ll the gaps among the main vegetation units of the park, both spatially and thematically. Overall, the Vegetation and Classi?cation Map for Guadalupe Mountains NP will support the park?s management e?orts and enhance regional understanding of vegetation and ecology of ecosystems of the southwestern United States.
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Hite, John E., and Jr. Guadalupe River and Bypass Culvert, San Jose, California. Hydraulic Model Investigation. Fort Belvoir, VA: Defense Technical Information Center, February 1998. http://dx.doi.org/10.21236/ada339432.

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Kelson, Keith I., Paul W. Bauer, and Ren Thompson. Geologic map of the Guadalupe Mountain quadrangle, Taos County, New Mexico. New Mexico Bureau of Geology and Mineral Resources, 2008. http://dx.doi.org/10.58799/of-gm-168.

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Lucas, Spencer G., G. L. Weadock, K. K. Kietzke, and A. P. Hunt. Geologic map of the Ima NW quadrangle, Guadalupe and Quay Counties, New Mexico. New Mexico Bureau of Geology and Mineral Resources, 1994. http://dx.doi.org/10.58799/ofr-399.

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Amarante, Jose F. Alberto. Characterization of basement rocks in the Mescalero 1 Well, Guadalupe County, New Mexico. New Mexico Bureau of Geology and Mineral Resources, 2002. http://dx.doi.org/10.58799/ofr-468.

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Skotnicki, Steven J., and Ann D. Knight. OFR-610: Geologic Map of the Guadalupe Mountains National Park, Culberson and Hudspeth Counties, Texas. New Mexico Bureau of Geology and Mineral Resources, 2021. http://dx.doi.org/10.58799/ofr-610.

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Carriazo Osorio, Fernando. La economía de los lugares emblemáticos: una valoración económica de una conexión entre Monserrate y Guadalupe. Universidad del Rosario, October 2023. http://dx.doi.org/10.12804/issne.2745-2085_10336.41147_feipu.

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La contribución de los lugares emblemáticos al bienestar individual y colectivo no siempre es tenida en cuenta cuando se evalúan elecciones sociales con respecto a la provisión pública, privada o mixta de estos sitios. En esta aplicación estimamos la disponibilidad a pagar (DAP) por un proyecto que conecta los cerros emblemáticos de Monserrate y Guadalupe en Bogotá (Colombia), bajo diferentes escenarios hipotéticos que describen un paisaje urbano-rural, utilizando la metodología de valoración contingente (VC). Exploramos el efecto que tienen visualizaciones dinámicas y estáticas usadas en la descripción de escenarios sobre la DAP promedio. Se encuentra que, en promedio, los encuestados están dispuestos a pagar 36 113 pesos como usuarios del proyecto de conectividad. La DAP promedio para las estimaciones con escenarios de visualización dinámica ($35 080) fue estadísticamente menor que la dap promedio para estimaciones con escenarios de visualización estática ($37 176). A partir de las estimaciones de VC se estiman los beneficios sociales generados por el proyecto de conectividad suponiendo diferentes tamaños de flujo anual de visitantes. Estos varían entre $81 885 181 134, para un escenario de bajo flujo, y $409 425 905 670, para un escenario de alto flujo. Los resultados del modelo de vc aplicado sugieren que una política pública dirigida a preservar o mejorar los lugares emblemáticos de patrimonio natural puede traer beneficios significativos que garanticen su provisión.
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Broadhead, Ronald F., and Glen E. Jones. Petroleum Potential of the Sin Nombre area, De Baca, Roosevelt, Curry , Lincoln, Guadalupe, and Chaves Counties, New Mexico. New Mexico Bureau of Geology and Mineral Resources, 2002. http://dx.doi.org/10.58799/ofr-467.

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Bayliss, G. S. Hydrocarbon source rock evaluation, A. G. Hill No. 1 Federal A well, sec. 27 T9N R19E, Guadalupe County, New Mexico. New Mexico Bureau of Geology and Mineral Resources, 2000. http://dx.doi.org/10.58799/ofr-446.

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