Výskyt Al-Fe fosfátů ve slepencích v Kamenném Újezdu u Rokycan (Česká republika)

A new locality of zeolite mineralization has been discovered in Malý Semerink, 500 m south of the Chřibská railway station in the Rybniště municipality, the Lužické hory Mts., Czech Republic. Zeolites occur in cavities of Tertiary alkaline basalts that penetrated the quartz sandstones of the Czech Cretaceous Basin. A total of eight zeolite species were discovered here: analcime, cowlesite, erionite-Ca, chabazite-Ca, lévyne-Ca, phillipsite-K, scolecite, and thomsonite-Ca. The most notable are the colorless to white cross-intergrowths of phillipsite-K crystals up to 1 cm in size, white hemispherical cowlesite, and abundant thin tabular lévyne-Ca overgrown with fine fibrous erionite-Ca. The WDS quantitative analyses, X-ray powder patterns, and refined unit cell parameters are given for all described mineral phases.

Solanum carolinense is native to North America (USDA, NRCS, 2021).The species occurs in all states of the USA except Nevada, Montana

A very rare phosphate collinsite was found on historical samples of chamosite from the abandoned iron mine Nučice near Prague, Central Bohemia (Czech Republic) located in Ordovician sediments of the Barrandian area. Collinsite forms white to beige radial aggregates up to 15 mm in size composed by platy crystals with pearly lustre. Its chemical composition corresponds to empirical formula: (Ca1.87Sr0.12Ba0.01)Σ2.00(Mg0.57Fe0.41Al0.01)Σ0.99 (PO4)2.00·2H2O (Sr-rich zones) and (Ca1.98Sr0.01)Σ1.99(Mg0.58Fe0.40Al0.01)Σ0.99(PO4)2.00·2H2O (Sr-poor zones). Collinsite is triclinic, space group P-1, unit-cell parameters refined from X-ray powder diffraction data are a 5.734(3), b 6.779(3), c 5.441(2) Å, α 97.33(4)°, β 108.52(3)°, γ 107.25(3)° and V 185.7(1) Å3. Collinsite was found in association with siderite in fissures of chamosite iron ore.

An interesting mineral association of Cu arsenates was found at abandoned ore stope at the Geschieber vein - north at the Daniel level of the Svornost mine, the Jáchymov ore district, Krušné hory, Czech Republic. Tangdanite forms thin tabular crystals up to 3 mm in size and coatings and fine crystalline aggregates on the area up to some cm2. It has light green, bluish-green to emerald green color and perfect cleavage. It is monoclinic, space group C2/c, the unit-cell parameters refined from X-ray powder diffraction data are: a 54.335(12), b 5.579(2), c 10.459(2) Å, β 95.42(3)° and V 3156(2) Å3; its chemical analyses correspond to the empirical formula Ca1.99(Cu8.72Zn0.09Ni0.04Al0.04)Σ8.89[(AsO4)3.83 (PO4)0.14(SiO4)0.03]Σ4.00(SO4)0.41(OH)8.97·9H2O on the basis As+P+Si+V = 4 apfu. The results of Raman and infrared spectroscopy confirmed an absence of carbonate group in studied tangdanite. K-rich lavendulan was found as a relatively abundant sky blue crusts and coatings on the area up to some cm2 and hemispherical aggregates with a radial structure or rarely as a group of thin tabular crystals up to 0.2 mm in size. It is monoclinic, space group P21/n, the unit-cell parameters refined from X-ray powder diffraction data are: a 10.081(12), b 19.469(12), c 10.033(9) Å, β 90.32° and V 1969(2) Å3; its chemical analyses correspond to the empirical formula (Na0.63K0.16)Σ0.79Ca1.12(Cu4.82Al0.01)Σ4.83[(AsO4)3.86(PO4)0.07 (SO4)0.06(SiO4)0.01]Σ4.00Cl0.96·5H2O on the basis As+P+V+Si+S = 4 apfu. Olivenite occurs as olive green spherical aggregates with radial structure up to 8 mm in size and rarely as groups of acicular crystals in association with strashimirite and köttigite. It is orthorhombic, space group Pnnm, the unit-cell parameters refined from X-ray powder diffraction data are: a 8.6204(10), b 8.2332(9), c 5.9337(11) Å and V 421.13(7) Å3; its chemical analyses correspond to the empirical formula (Cu1.94Ni0.01Al0.01)Σ1.96[(AsO4)0.97(VO4)0.02(PO4)0.01]Σ1.00(OH)0.93 on the basis As+V+P = 1 apfu. Strashimirite forms there light green crystalline coatings on the area up to several cm2 and spherical aggregates with a radial structure in association with olivenite and lavendulan. Strashimirite is probably monoclinic, space group P2, the unit-cell parameters refined from X-ray powder diffraction data are: a 9.991(9), b 18.466(9), c 8.986(8) Å, β 96.5(2)° and V 1574(3) Å3; its chemical analyses correspond to the empirical formula (Cu7.83Ni0.18Ca0.09Zn0.06Co0.02Al0.02)Σ8.20 [(AsO4)3.81(PO4)0.07 (SO4)0.07(VO4)0.03(SiO4)0.02]Σ4.00 (OH)4.45·5H2O on the basis As+P+Si+V+S = 4 apfu. Chalcophyllite was found as rare emerald green thin tabular crystals up to 0.5 mm in size and crystalline aggregates. Its chemical composition is possible to express on the basis As+S+P+Si = 7 apfu by the empirical formula Cu17.83Al1.97[(AsO4)4.00(PO4)0.09]Σ4.09[(SO4)2.80(SiO4)0.11]Σ2.91 (OH)23.27·36H2O. Brochantite, devilline, köttigite, erythrite and gypsum were also found in the association with Cu arsenates. The origin of the described mineral association is connected with (sub)recent weathering of primary ore minerals (tennantite, sphalerite, nickelskutterudite) in relatively dry conditions of abandoned mine adits.

To define the relative risk of malignant transformation in colorectal adenomas less than 10 mm in diameter. Prospective study. District general hospital, UK. 1228 polyps detected endoscopically in 445 patients over the 10-year period 1989-1999. Site, size, histological type and dysplastic grade of polyp. 657 of the 1228 polyps were adenomas: 281 (43%) tubular, 339 (51%) tubulovillous and 37 (6%) villous. In the 357 adenomas less than 10 mm in diameter, 11 (3%) were severely dysplastic and 2 carcinomas were detected, though neither was less than 5 mm in size. The relative risk of malignancy or severe dysplasia in adenomas of 10 mm or more compared with those of less than 10 mm was 3.8 (p < 0.0001). Although severe dysplasia and malignancy do occur in adenomas less than 10 mm in size, they are rare in lesions of less than 5 mm. We recommend routine destruction of all polyps 5 mm or more in size, though it is not essential to remove those of less than 5 mm if they are kept under surveillance.

The American College of Radiology (ACR) recommends that polyps < or =5 mm in size not be reported on computed tomography (CT) colonography studies. Patients with 1 or 2 polyps 6-9 mm in size can be offered "CTC surveillance" in 3 years in lieu of polypectomy. The aim of the study was to determine the impact of ACR recommendations on resection of high-risk adenoma findings using an endoscopic polyp/histology database. Excluding patients with inflammatory bowel disease (IBD) and polyposis, 10,034 patients underwent colonoscopy and 10,780 polyps were removed from 5,079 patients over a 5-year interval. High-risk adenoma findings were defined as an advanced adenoma (> or =1 cm in size, high-grade dysplasia (HGD), or villous elements) or 3 or more adenomas of any size, per postpolypectomy surveillance recommendations. A total of 5,079 patients (51%) had at least 1 polyp, 2,907 (29%) had at least 1 adenoma, and 1,001 (10%) had high-risk adenoma findings, of these, 293 (29%) had either 3 adenomas < or =5 mm in size (n=267) or an advanced adenoma < or =5 mm in size (or both) and no polyp of any histology > or =6 mm in size. There were 774 patients with 1 or 2 polyps 6-9 mm in size and no polyps of any histology > or =10 mm in size. Of these patients 184 (18% of the patients with high-risk adenomas) had either 3 or more adenomas < or =9 mm in size (n=149) or an advanced adenoma < or =9 mm in size (or both findings). There were 2,174 patients age > or =50 years with the primary indication of screening of whom 326 (15%) had high-risk adenoma findings. Of these, 108 (33%) had either > or =3 adenomas < or =5 mm in size or an advanced adenoma < or =5 mm in size and no polyps > or =6 mm in size. An additional 75 (23%) had no polyp > or =10 mm in size, 1 or 2 polyps 6-9 mm in size and > or =3 adenomas < or =9 mm in size or an advanced adenoma < or =9 mm in size. If computed tomographic colonography (CTC) rather than colonoscopy were used in this population, assuming 100% sensitivity of CTC for polyps > or =6 mm and ACR interpretation recommendations, then 29% of all patients and 33% of screening patients age > or =50 years with high-risk adenoma findings would be interpreted as normal, and an additional 18-23% of these groups with high-risk adenoma findings, respectively, could have polypectomy delayed at least 3 years.

Soil aggregates between 2 and 5mm from 35- and 45-year-old unreclaimed post-mining sites near Sokolov (Czech Republic) were divided into two groups: spherical and prismatic. X-ray tomography indicated that prismatic aggregates consisted of fragments of claystone bonded together by amorphous clay and roots while spherical aggregates consisted of a clay matrix and organic fragments of various sizes. Prismatic aggregates were presumed to be formed by plant roots and physical processes during weathering of Tertiary mudstone, while earthworms were presumed to contribute to the formation of spherical aggregates. The effects of drying and rewetting and glucose addition on microbial respiration, microbial biomass, and counts of bacteria in these aggregates were determined. Spherical aggregates contained a greater percentage of C and N and a higher C-to-N ratio than prismatic ones. The C content of the particulate organic matter was also higher in the spherical than in the prismatic aggregates. Although spherical aggregates had a higher microbial respiration and biomass, the growth of microbial biomass in spherical aggregates was negatively correlated with initial microbial biomass, indicating competition between bacteria. Specific respiration was negatively correlated with microbial biomass. Direct counts of bacteria were higher in spherical than in prismatic aggregates. Bacterial numbers were more stable in the center than in the surface layers of the aggregates. Transmission electron microscopy indicated that bacteria often occurred as individual cells in prismatic aggregates but as small clusters of cells in spherical aggregates. Ratios of colony forming units (cultivatable bacteria) to direct counts were higher in spherical than in prismatic aggregates. Spherical aggregates also contained faster growing bacteria.

Detection of colorectal polyps by multislice CT colonography with ultra-low-dose technique: comparison with high-resolution videocolonoscopy

Tvrdýite, Fe2+Fe3+2A13(PO4)4(OH)5(OH2)4·2H2O, is a new phosphate mineral from the abandoned Huber open pit, in the Krásno ore district near Horní Slavkov, western Bohemia, Czech Republic. It was found along with Al-rich beraunite, fluorapatite and pharmacosiderite in a cavity of quartz gangue. Tvrdýite forms acicular to fibrous crystals with diameters in the range 0.5–5 μm and lengths up to 300 μm, partly grouped in radiating aggregates up to 3 mm in size. It has a silvery to olive, greyish green colour with pearly lustre, greyish-white streak and is very brittle with an uneven fracture; individual fibres are somewhat flexible. Cleavage on {100} is good; the Mohs hardness is ∼3–4. The calculated density is 2.834 g cm–3. Tvrdýite is optically biaxial (–), with α = 1.650(2), β = 1.671(1) and γ = 1.677(1) (white light); 2V = 56(1)°; dispersion: r &gt; v, strong; optical orientation: Z = b, X ≈ a, Y ≈ c; pleochroism: X = greenish blue, Y = yellowish orange, Z = yellowish orange (X&gt;&gt; Y &gt; Z). Tvrdýite is monoclinic, space group C2/c, a = 20.564(4), b = 5.101(1), c = 18.883(4) Å, β = 93.68(3)° and V = 1976.7(7) Å3, Z = 4, a:b:c= 4.031:1:3.702. The strongest eight lines in the powder X-ray diffraction (XRD) pattern [d in Å (I)(hkl)] are 10.227 (100) (200), 9.400 (6) (002), 7.156 (14) (202), 5.120 (7) (400), 3.416 (11) (600), 3.278 (6) (602), 2.562 (5) (800) and 2.0511 (3) (10,0,0). Chemical analyses by electron microprobe yielded MnO 0.01, ZnO 5.08, , FeO 4.31, Fe2O3 21.16, Al2O316.71, P2O5 32.64, As2O5 2.56, F 0.53, H2O (calc.) 17.84, O = F –0.22, total 100.62 wt.%. The resulting empirical formula, calculated on the base of 27 anions, obtained from the crystal structure, is Zn0.52Fe2+0.50Fe3+2.21Al2.75(PO4)3.86(AsO4)0.19OH4.60F0.23(OH2)4·2H2O. The ideal formula, Fe2+Fe3+2Al3(PO4)4(OH)5(OH2)4-2H2O, requires FeO 8.75, Fe2O3 19.44, Al2O3 18.62, P2O5 34.56, H2O 18.64, total 100.00 wt.%. The crystal structure of tvrdýite was solved from single-crystal data (synchrotron beamline) and refined to R1 = 0.038 for 2276 reflections with I &gt; 2σ(I). Tvrdýite is isostructural with beraunite, but contains dominant Al in two of the four independent M sites, which are all occupied by Fe in beraunite.

A new occurrence of zeolite mineralization with phillipsite-K, phillipsite-Ca, thomsonite-Ca, natrolite and gonnardite has been discovered in an active basalt quarry in the Libá village near Cheb (Czech Republic). Phillipsites in small cavities form druses of white or colourless crystals up to 1 mm in size. Chemical analyses of phillipsite-K correspond to the empirical formula (K1.85Na1.24Ca0.83Ba0.27Sr0.01)Σ4.20(Al6.28Si10.33O32)·12H2O and phillipsite-Ca to (Ca1.84K1.33Na0.14Ba0.06)Σ3.37(Al5.97Si10.20O32)·12H2O. The unit-cell parameters were refined from the powder X-ray data for phillipsite-Ca as: a 9.924(2), b 14.309(3), c 8.7414(14) Å, β 124.92(2)° and V 1017.8(5) Å3. Thomsonite-Ca forms transparent hemispheric radial aggregates up to 1 cm in size. Its unit-cell parameters refined from the powder X-ray data are a 13.105(5), b 13.857(5), c 13.247(6) Å and V 2266.7(6) Å3 and its chemical analyses correspond to the empirical formula Ca1.79Sr0.18Na1.05(Al4.81 Si5.15)O20·6H2O. Natrolite occurs as snow white hemispheric radial clusters. Its unit-cell parameters refined from the powder X-ray data are a 18.326(7), b 18.569(7), c 6.594(3) Å and V 2243.8(9) Å3 and empirical formula is Na1.60Ca0.05(Al2.08 Si3.02)O10·2H2O. Gonnardite forms colourless or white aggregates of flat acicular crystals up to 2 mm in size. Its unit-cell parameters refined from the powder X-ray data are a 13.221(8), c 6.6233(4) Å and V 1156.9 Å3 and empirical formula is (Na3.14Ca2.21Sr0.02)Σ5.37(Al8.92Si11.41)Σ20.33O40·12H2O.

Two cases of minute carcinoid tumor of the stomach were reported and 167 cases of gastric carcinoid in Japan up to December 1984 were reviewed. In Case 1, two carcinoid tumors of the body were found as sessile polyps of 4.2 and 4.8 mm in diameter, respectively, the latter having been detected two years previously. Case 2 had 60 polypoid lesions on the body and the fundus, ranging from 1.0 to 4.5 mm in diameter. In both cases the tumor invasion was limited to the mucosa and submucosa, although many micronests were found around the polypoid lesions. Among 167 cases of gastric carcinoid in Japan, 12 were 5 mm or less in size and 12 were 6 to 10 mm in size. In the former cases, there was no metastasis while in the latter, metastasis to the lymph nodes was found in 25.0%. We propose that the minute gastric carcinoid should be defined as a tumor not exceeding 5 mm in size with the invasion limited to the mucosa or submucosa. In addition, we emphasized that radical gastrectomy should be performed even for the minute carcinoid tumor because of its multicentricity and invasiveness.

Small Nodules Detected on Chest Radiography: Does Size Predict Calcification?

Endoscopic treatment of digestive tract diseases, such as early esophageal and gastric neoplasia, has become increasingly popular in recent years as an alternative to surgical procedures in the hope of providing an improved quality of life for these patients. However, one of the limitations of a conventional endoscopic mucosal resection, such as an aspiration mucosectomy and a strip biopsy, has been the size of the lesions to be resected. Both an aspiration mucosectomy and strip biopsy are useful variants for removing flat lesions measuring less than 20 mm in maximal diameter. To overcome such limitations, we devised a double endoscopic intraluminal operation (DEILO), which enables us to resect mucosal lesions by using 2 fine endoscopes and monopolar shears. DEILO was performed on patients with esophageal and gastric lesions measuring up to 40 mm in diameter. This novel technique is characterized by the use of 2 endoscopes (one for lifting the lesion and the other for cutting the lesions) inserted into the esophagus or stomach through an overtube. A mucosal resection is then performed by dissecting the mucosal margin with newly developed monopolar shears, thereby separating the mucosa from the submucosa. A total of 25 lesions in the esophagus (8 lesions) and stomach (17 lesions) were resected by DEILO. The sizes of the esophageal lesions ranged from 8 to 40 mm in diameter (mean, 21.1 mm) whereas gastric lesions ranged from 8 to 30 mm (mean, 13.3 mm) in diameter, and histopathologic examinations revealed the resection margin to be clear and without any tumor. No complications or instances of recurrence were observed in this series. DEILO is considered to be feasible for the mucosal resection of esophageal and gastric lesions measuring more than 10 mm in diameter without submucosal invasion, whereas conventional endoscopic mucosal resection is indicated for such lesions measuring less than 10 mm in size.

A rare uranium supergene minerals, phurcalite and uranophane-beta, were found in association with metaautunite at fissures of granitoid rocks in the active Wagner quarry in Ruprechtice near Liberec (northern Bohemia, Czech Republic). Phurcalite occurs there as bright to deep yellow coatings with an area up to 10 × 3 mm in size composed of acicular to columnar crystals up to 0.5 mm in length. It is orthorhombic, space group Pbca, the unit-cell parameters refined from X-ray powder diffraction data are: a 17.3973(18), b 16.0161(15), c 13.5693(19) Å, V 3780.9(5) Å3. Chemical analyses of phurcalite correspond to the empirical formula Ca2.20(UO2)3.06(PO4)1.96(AsO4)0.04O2.26·7H2O. Uranophane-beta forms a relatively abundant pale yellow coatings of up to 2 × 2 cm in size composed of translucent to transparent acicular crystals with a vitreous lustre and a length of up to 0.2 mm. It is monoclinic, space group P21/a, the unit-cell parameters refined from X-ray powder diffraction data are: a 13.959(2), b 15.5420(16), c 6.6227(9) Å, β 91.43(1)o and V 1436.3(2) Å3. Chemical analyses of uranophane-beta correspond to the empirical formula Ca1.09(UO2)1.99[(SiO3OH)1.68 (PO4)0.29(AsO4)0.03]Σ2.00·5H2O. Metaautunite occurs there as abundant light yellow aggregates with an area up to some cm2 in size composed of tiny (up to 0.5 mm) tabular crystals or rarely as well-developed individual tabular crystals up to several mm in size. It clearly differs from other minerals in the association by very strong yellow-green luminescence in both short- and long-wave UV radiation. It is tetragonal, space group P4/nmm, the unit-cell parameters refined from X-ray powder diffraction data are: a 7.006(2), c 16.899(4) Å and V 829.4(6) (5) Å3. Chemical analyses of metaautunite correspond to the empirical formula Ca1.03(UO2)2.09(PO4)1.96(AsO4)0.04·6H2O.

The present study focuses on Eifelian (Middle Devonian) conodont faunas, with particular emphasis on the Polygnathus pseudofoliatus Group. The material comes from the Jirsek quarry at Konprusy (Fig. (Note: In this paper we use the designation Kak Episode sensu Walliser & Bultynck 2011, which better reflects its polyphase nature). Conodonts from the Jirsek quarry were previously studied by Kalvoda & Zikmundov in Galle & Hladil (1991), Kalvoda (1992) and Kalvoda in Hladil & Kalvoda (1993a, b). The following conodonts were reported by the above mentioned authors from the 81 DOI 10.3140/bull.geosci.1774 Middle Devonian (Eifelian, australis-ensensis zones) conodonts from the Jirsek quarry near Konprusy (Barrandian area, Czech Republic) with special emphasis on the Polygnathus pseudofoliatus Group and notes on environmental changes related to the Kak Episode StaniSlava vodrkov & thomaS J. Suttner The Jirsek quarry in the Konprusy area (Barrandian area, Czech Republic) represents a unique section, where the stratigraphic equivalent of the black shales of the Kak Member (Srbsko Formation) is developed in a carbonate succession. Here we describe conodont faunas of the upper Acanthopyge Limestone (Chote Formation, australiskockelianus zones) and the Upper Dark Interval of the Acanthopyge Limestone referred to as UDI (Chote Formation, ensensis Zone) with special emphasis on the Polygnathus pseudofoliatus Group. The following taxa are discussed in