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            "title": "Eyes in the dark.. Shedding light on the antlion phylogeny and the enigmatic genus <i>Pseudimares</i> Kimmins (Neuropterida: Neuroptera: Myrmeleontidae)",
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            "abstractNote": "The systematic position of the antlion Pseudimares Kimmins has been disputed since description of the genus. Pseudimares is one of the most enigmatic and unusual members of Myrmeleontidae and probably of all Neuroptera. The taxon has been usually tied to the antlion subfamily Palparinae, although its phylogenetic affinities have never been thoroughly investigated and the monophyly of the subfamily as a whole has never been corroborated. We reconstruct for the first time the phylogenetic affinities of Pseudimares based on both morphological and molecular genetic data. The widely accepted subfamily level subdivision of antlions (Stilbopteryginae, Palparinae, Myrmeleontinae) is refuted in all our analyses, since Stilbopteryginae in the traditional sense are recovered as deeply nested within Myrmeleontidae forming a monophylum with Palparinae, while Myrmeleontinae are poorly supported by the parsimony analysis. In our morphology-based parsimony analysis, Pseudimares is the sister taxon of Stilbopteryx and Aeropteryx, which makes the traditional Palparinae paraphyletic. This result is further supported by our phylogenetic reconstruction based on molecular data, which found a clade including Pseudimares and Stilbopteryx, which is nested within the traditional Palparinae. The high genetic distances measured among the analysed taxa suggest that these groups quickly diverged in ancient times, although they remained morphologically homogeneous. In conformity with the results of the phylogenetic analyses, we propose a new classification scheme for antlions, one that merges Stilbopteryx and Aeropteryx into an expanded concept of the subfamily Palparinae.",
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            "title": "Molecular systematics of the land snail family Orculidae reveal polyphyly and deep splits within the clade Orthurethra (Gastropoda: Pulmonata)",
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            "abstractNote": "Clausiliidae (door snails) are gastropods with a very high diversity concerning shell morphology, especially of their complex closing apparatus, which provides the most important diagnostic traits for classification of taxa. Due to the high variability, a high number of taxa has been described, though their systematics and taxonomy is partially controversially discussed. Montenegrina is the second most speciose door snail genus in Europe. It is an obligate rock-dwelling land snail and has, compared to its complex systematics, a rather small distribution range in the western parts of the Balkan Peninsula. The different taxa themselves show a very narrow and patchy distribution range. As Montenegrina is comprehensively sampled over the whole distribution range, it is a perfect study system for general questions on speciation and morphological differentiation in land snails. To study the amount of gene flow between geographically close or co-occurring populations, highly polymorphic markers are needed.",
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            "title": "Anatomical and morphological variation in the eastern Alpine endemic <i>Cylindrus obtusus</i> (Draparnaud, 1805) (Gastropoda: Helicidae)",
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            "abstractNote": "<em>Cylindrus obtusus</em> is an endemic land snail of the northeastern Alps. Early studies reported geographic differences in shell size and genital anatomy. Later, molecular genetic studies revealed that the species is differentiated into genetic lineages according to geographic region, named West, Central and East clades. In microsatellite analyses, these clades proved to be different with respect to heterozygosity and Hardy–Weinberg equilibrium. In populations from the eastern part of the distributional range all loci displayed an extreme excess of homozygotes, suggesting that selfing might be the predominant reproductive mode. In the present study, we analysed a comprehensive sample with respect to shell morphology as well as anatomical and histological traits. The analysed specimens were the same as those that had been studied genetically in a previous study. We tested whether the differentiation of the geographic groups is statistically significant. A morphometric analysis of the shells verified significant differences in shell height (SH) between two geographical groups (West/Central <em>vs</em> East). Moreover, we detected concordant significant geographic differences in the size and symmetry of the mucous glands. In the eastern populations, the glands were much smaller and asymmetrical in length and much more variable. In addition, the stylophore was significantly shorter. There was no correlation between these characters and shell size. Furthermore, love-darts were more frequently present in eastern populations. A comparative histological analysis revealed no significant differences in the cell structure of the mucous glands between the two geographic groups. Moreover, the presence of darts in the eastern populations does not indicate any dysfunction of these structures. Gland size, however, might influence the amount of secretion. Altogether, the results show consistent geographic differences in shell morphology and genital anatomy. The results corroborate the assumption of an altered mode of reproduction (predominantly via selfing) in eastern populations.",
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            "title": "Polloneite, a new complex Pb(-Ag)-As-Sb sulfosalt from the Pollone mine, Apuan Alps, Tuscany, Italy",
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                    "creatorType": "author",
                    "firstName": "Dan",
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                    "firstName": "Frank N.",
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            "abstractNote": "Polloneite, ideally AgPb46As26Sb23S120, is a new N = 4 member of the sartorite homologous series. It occurs in a matrix of baryte from the Pizzone level of the Pollone baryte-pyrite-(Pb-Zn-Ag) deposit at Valdicastello Carducci, near Pietrasanta, in the Apuan Alps, Tuscany, Italy, as anhedral grains up to 0.5 mm across. The mineral is opaque, greyish black with a metallic lustre. In reflected light polloneite is white, bireflectance is moderate. Internal reflections are absent. Under crossed polars, anisotropism is moderate with rotation tints in brown-violet and deep grey. The reflectance data (%, air) are: 30.2, 42.4 at 470 nm, 28.8, 41.0 at 546 nm, 27.9, 39.8 at 589 nm and 26.0, 37.4 at 650 nm. Mohs hardness is 3–3½, microhardness VHN50 exhibits a mean value of 200 kg mm-2. The average results of 15 electronmicroprobe analyses of three grains are Ag 0.71(5), Pb 52.05(21), As 10.61(22), Sb 15.40(12), S 21.16(8), total 99.92(15) wt.%, corresponding to Ag1.20Pb45.76As25.79Sb23.04S120.21 (on the basis of Me + S = 216 apfu). The simplified formula AgPb46As26Sb23S120 is in accordance with the results of a crystal structure determination. The calculated density is 5.77 g cm–3. Polloneite is monoclinic, space group P21, a = 8.413(2), b = 25.901(5), c = 23.818(5) Å, β = 90.01(3)°, V = 5189.8(18)Å3, Z = 1. The strongest eight lines in the calculated powder-diffraction pattern [d in Å(I)hkl] are 3.795(100)(026), 3.414(60)(233), 3.238(69)(080), 3.020(97)(253), 2.922(82)(066), 2.738(73)(236), 2.375(79)(290) and 2.103(64)(400). Polloneite is a new N = 4 member of the sartorite homologous series with substantial Sb and small, but important, Ag content. It is a three-fold superstructure with a tripled unit-cell parameter, 7.9 Å, of sartorite homologues. In the As-Sb rich slabs, several types of crankshaft chains and isolated (As,Sb)–S polyhedra occur. A sequence of three different, tightly bonded double-layer fragments (broad ribbons) contains two asymmetric fragments with long crankshaft chains whereas the third fragment type, with Ag, contains small mirror-symmetrical metalloid groups and no crankshaft chains. This configuration can potentially cause order-disorder phenomena in the structure. The threefold superstructure and the mixed As-Sb character distinguish polloneite from veenite and from dufrénoysite, respectively.",
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            "title": "New <i>M</i><sup>1+</sup>, <i>M</i><sup>3+</sup>-arsenates - the framework-structures of Ag<i>M</i><sup>3+</sup>(HAsO<sub>4</sub>)<sub>2</sub> (<i>M</i><sup>3+</sup> = Al, Ga) and <i>M</i><sup>1+</sup>GaAs<sub>2</sub>O<sub>7</sub> (<i>M</i><sup>1+</sup> = Na, Ag)",
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            "pages": "785-790",
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            "journalAbbreviation": "Acta Cryst E",
            "DOI": "10.1107/S2056989017005631",
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            "title": "First high-pressure synthesis of rossmanitic tourmaline and evidence for the incorporation of Li at the X site",
            "creators": [
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                    "creatorType": "author",
                    "firstName": "Martin",
                    "lastName": "Kutzschbach"
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                {
                    "creatorType": "author",
                    "firstName": "Bernd",
                    "lastName": "Wunder"
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                {
                    "creatorType": "author",
                    "firstName": "Marija",
                    "lastName": "Krstulovic"
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                {
                    "creatorType": "author",
                    "firstName": "Andreas",
                    "lastName": "Ertl"
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                    "creatorType": "author",
                    "firstName": "Robert",
                    "lastName": "Trumbull"
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                    "creatorType": "author",
                    "firstName": "Alexander",
                    "lastName": "Rocholl"
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                    "firstName": "Gerald",
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            "abstractNote": "Lithium is an important component of some tourmalines, especially in chemically evolved granites and pegmatites. All attempts at synthesizing Li-rich tourmaline have so far been unsuccessful. Here we describe the first synthesis of rossmanitic tourmaline at 4 GPa and 700 °C in the system Li2O–Al2O3–SiO2–B2O3–H2O (LASBH) from seed-free solid starting materials consisting of a homogenous mixture of Li2O, γ-Al2O3, quartz and H3BO3. The solid run products after 12-day run duration comprise rossmanitic tourmaline (68 wt%), dumortierite (28 wt%) and traces of spodumene (3 wt%) and coesite (1 wt%). Tourmaline forms idiomorphic, large prismatic crystals (30 × 100 μm), which are inclusion free and chemically unzoned. The refined cell dimensions of the tourmaline are: a = 15.7396(9) Å, c = 7.0575(5) Å, V = 1514.1(2) Å3. Conventionally, the Li+ ion is assumed to exclusively occupy the octahedral Y site in the tourmaline structure to a maximum of 2 Li per formula unit (pfu). However, the chemical composition of our synthetic tourmaline determined by electron microprobe and secondary ion mass spectroscopy results in the formula: X(☐0.67(11)Li0.33(11))Y(Al2.53(10)Li0.47(10))Z(Al6)T(Si5.42(15)B0.58(15))O18B(BO3)3V+W[(OH)2.40(3)O1.60(3)], wherein a significant amount of Li occupies the X site for charge balance requirements. Reliable assignment of the OH-stretching vibrations in a polarized single-crystal Raman spectrum such as a single-crystal XRD structure refinement, confirms the incorporation of Li at the X site [0.24(9) and 0.15(5) XLi pfu, respectively]. The SREF data show that the Li–O1 distances are shortened significantly in order to compensate for the smaller ionic radius of Li+ compared to Na+, K+ or Ca2+ at the X site, i.e., Li is closer to the Si6O18 ring and to a sevenfold coordination with oxygen.",
            "publicationTitle": "Physics and Chemistry of Minerals",
            "publisher": "",
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            "volume": "44",
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            "pages": "353-363",
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            "DOI": "10.1007/s00269-016-0863-0",
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                    "tag": "Li isotope fractionation",
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            "title": "Crystal structures and photoluminescence properties of two novel sorosilicates with an unprecedented ratio of di- and trisilicate groups: Ba<sub>2</sub>Ho<sub>10</sub>(Si<sub>2</sub>O<sub>7</sub>)<sub>3</sub>(Si<sub>3</sub>O<sub>10</sub>)<sub>2</sub> and isotypic Ba<sub>2</sub>Er<sub>10</sub>(Si<sub>2</sub>O<sub>7</sub>)<sub>3</sub>(Si<sub>3</sub>O<sub>10</sub>)<sub>2</sub>",
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            "abstractNote": "Ba2Ho10(Si2O7)3(Si3O10)2 and isotypic Ba2Er10(Si2O7)3(Si3O10)2 represent a new mixed-framework structure type with an unprecedented ratio of di- and trisilicate groups among silicates. The atomic arrangement features asymmetric zigzag chains of edge-sharing Ln3+O6 (Ln = Ho, Er) octahedra corner-linked by isolated Si2O7 and horseshoe-shaped Si3O10 groups in the ratio of 3:2. Single-crystal X-ray diffraction investigations yielded the triclinic space group P-1 (no. 2), with a = 5.5494(11)/5.5360(11) Å, b = 6.8795(14)/6.6870(13) Å, c = 23.703(5)/23.691(5) Å, α = 83.60(3)/83.64(3)°, β = 88.80(3)/88.77(3)°, γ = 73.43(3)/73.38(3)°,V = 861.9(3)/835.2(3) Å3, R(F) = 0.0289/0.0559, respectively. The laser-induced photoluminescence emission of trivalent holmium und erbium in both framework silicates was studied using a dispersive single-stage spectrometer and compared to the emission spectra of other framework Ba-Er and Ba-Ho silicates. The 4S3/2→4I15/2 transition of Er in Ba2Er10(Si2O7)3(Si3O10)2 causes a photoluminescence emission in the visible green spectral range whereas its Ho representative with the 5F3→5I7 transition in the red spectral region.",
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                    "tag": "Flux synthesis"
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                    "tag": "Lanthanides"
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            "title": "Écrinsite, AgTl<sub>3</sub>Pb<sub>4</sub>As<sub>11</sub>Sb<sub>9</sub>S<sub>36</sub>, a new thallium-rich homeotype of baumhauerite from the Jas Roux sulphosalt deposit, Parc national des Écrins, Hautes-Alpes, France",
            "creators": [
                {
                    "creatorType": "author",
                    "firstName": "Dan",
                    "lastName": "Topa"
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                {
                    "creatorType": "author",
                    "firstName": "Uwe",
                    "lastName": "Kolitsch"
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                {
                    "creatorType": "author",
                    "firstName": "Emil",
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                    "creatorType": "author",
                    "firstName": "Chris",
                    "lastName": "Stanley"
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            ],
            "abstractNote": "Écrinsite, ideally AgTl3 Pb4 As11 Sb9 S36, is a new thallium sulphosalt species found in the Jas Roux As–Sb–Pb–Tl–Hg–Ag deposit, Parc national des Écrins, Département des Hautes-Alpes,\nFrance. Associated minerals in four different samples are jasrouxite, stibnite, smithite, guettardite, chabournéite, pierrotite and As-bearing zinkenite. Écrinsite is opaque with metallic lustre. It is brittle without any discernible cleavage and with conchoidal fracture. In\nreflected light écrinsite is white, pleochroism is not discernible. Internal reflections are absent. In crossed polarisers, anisotropism is distinct, with rotation tints in shades of grey. The reflectance data (%, air) are: 37.3, 38.6 at 470 nm, 35.2, 36.7 at 546 nm, 34.0, 35.5 at 589\nnm and 32.0, 33.3 at 650 nm. Mohs hardness is 3–3½, microhardness VHN25 is in the range 175–201, with a mean value of 189 kg mm-2. Average results of 20 electron-microprobe analyses for the structurally investigated grain are (in wt%): Ag 2.03(10),\nCu 0.02(1), Tl 14.57(20), Pb 16.23(32), Sb 23.97(25), As 17.87(17), S 25.20(15), total 99.88 (15), corresponding to Ag0.87 Cu0.02 Tl3.28 Pb3.61 Sb9.06 As10.98 S36.19 (on the basis of 28 Me + 36S = 64 apfu).\nThe simplified formula, AgTl3 Pb4 Sb9 As11 S36, is in accordance with the results of the crystal-structure analysis and may be derived from the ideal baumhauerite formula, Pb12 As16 S36, by substitution\nof Sb for As and [(Tl, Ag)+ + (As, Sb)3+]↔2Pb2+. The density, 4.96 g cm-3, was calculated using the ideal formula. Écrinsite has a triclinic cell, space group P 1, with a = 8.080(2), b = 8.533(2), c = 22.613(4)\nÅ, α = 90.23(3)°, β = 97.17 (3)°, γ = 90.83(3)°, V = 1546.7(6)Å3, and Z = 1. The strongest five lines in the (calculated) powder-diffraction pattern are [d in A(I)(h k l)]: 4.14 (68)(1 0 5), 3.72(92)(1 0\n5), 3.56(100)(1 0 6)3.53(80)(1 2 2) and 3.48(72)(1 2 2). Écrinsite is a new member of the sartorite homologous series with N\n1,2 = 3, 4, i. e., N = 3.5. Four other members share the same N value as écrinsite: baumhauerite, argentobaumhauerite,\nboscardinite and bernarlottiite. By comparison to the closely related boscardinite (ideally Tl2 Pb8 Sb14 As4 S36), écrinsite is characterised by both an excess of As over Sb and a distinctly higher substitution of [(Tl, Ag)+\n+ (As, Sb)3+]↔ 2Pb2+ . Baumhauerite and bernarlottiite are basically unsubstituted members, whereas argentobaumhauerite has a Ag substitution, without Tl.",
            "publicationTitle": "European Journal of Mineralogy",
            "publisher": "",
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            "date": "2017-10-10",
            "volume": "29",
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            "pages": "689-700",
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            "DOI": "10.1127/ejm/2017/0029-2639",
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            "url": "https://www.schweizerbart.de/papers/ejm/detail/29/88097/Ecrinsite_AgTl3Pb4As11Sb9S36_a_new_thallium_rich_h?af=crossref",
            "accessDate": "2022-04-28T15:46:07Z",
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            "extra": "Publisher: Schweizerbart'sche Verlagsbuchhandlung",
            "tags": [
                {
                    "tag": "CRYSTAL STRUCTURE"
                },
                {
                    "tag": "FRANCE"
                },
                {
                    "tag": "JAS ROUX DEPOSIT"
                },
                {
                    "tag": "NATIONAL DES ÉCRINS"
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                {
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            "shortTitle": "The influence of the habitat on morphological species delimita6on characters",
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