4 research outputs found
مولود النبى (MS 60); اجازتنامه (MS 61)
No full textBirbirinden farklı 2 adet yazmanın bir araya getirilmesiyle oluşturulmuş ve ciltlenmiş bir eserdir (Yazma numaraları : MS 60, MS 61). MS 60 : Eserin ilk sayfaları eksiktir. 1a-34b: Hz. Muhammed’in doğumu, ahlakı, mucizeleri, miracı, hicreti, ve ayrıntılı olarak ölümü manzum olarak anlatılır. 35a-36a: Hatim duası; 36b-38a: Münacat duası. Mevlidin sonuna başka bir eser ciltlenmiştir (Bkz. 30/II). MS 61 : İlmiye icazetnamesidir. En sonda Ahmed Nazif Sinobi, belgenin hocası Es-seyyid el-Hâc Rif’at b. el-Hâc İbrahim el-Ankaravi’den aldığı icazet sureti olduğunu belirtir. (46a). Burada Ahmed Nazif Es-Sinobi’nin mührü de vardır. 46a’da son bulan icazetnamenin rıka yazıyla farklı bir kağıda yazılmış bir diğer kopyası da 48b-50b arasındadır. 53b-55a: Farklı bir kağıda farklı bir yazıyla muhtemelen bir mevlidden alınmış Hz. Muhammed’in hayatına ait kısa bir manzumedir
Long-term precipitation in Southwestern Europe reveals no clear trend attributable to anthropogenic forcing
Get PDF© 2020 The Author(s). Artículo firmado por 14 autores. This work was supported by the research projects CGL2017-82216-R, CGL2017-83866-C3-3-R and PCI2019-103631, financed by the Spanish Commission of Science and Technology and FEDER; CROSSDRO project financed by the AXIS (Assessment of Cross(X)—sectoral climate Impacts and pathways for Sustainable transformation), JPI-Climate cofunded call of the European Commission and INDECIS which is part of ERA4CS, an ERA-NET initiated by JPI Climate, and funded by FORMAS (SE), DLR (DE), BMWFW (AT), IFD (DK), MINECO (ES), ANR (FR) with co-funding by the European Union (Grant 690462). Dhais Peña-Angulo received a ‘Juan de la Cierva’ postdoctoral contract (FJCI2017-33652 Spanish Ministry of Economy and Competitiveness, MEC). Conor Murphy was supported by the Irish Environmental Protection Agency (Grant Nos. 2019-CCRP-MS.60). Marco Turco has received funding from the Spanish Ministry of Science, Innovation and Universities through the project PREDFIRE (RTI2018-099711-J-I00), which is cofinanced with the European Regional Development Fund (ERDF/FEDER).We present a long-term assessment of precipitation trends in Southwestern Europe (1850–2018) using data from multiple sources, including observations, gridded datasets and global climate model experiments. Contrary to previous investigations based on shorter records, we demonstrate, using new long-term, quality controlled precipitation series, the lack of statistically significant long-term decreasing trends in precipitation for the region. Rather, significant trends were mostly found for shorter periods, highlighting the prevalence of interdecadal and interannual variability at these time-scales. Global climate model outputs from three CMIP experiments are evaluated for periods concurrent with observations. Both the CMIP3 and CMIP5 ensembles show precipitation decline, with only CMIP6 showing agreement with long term trends in observations. However, for both CMIP3 and CMIP5 large interannual and internal variability among ensemble members makes it difficult to identify a trend that is statistically different from observations. Across both observations and models, our results make it difficult to associate any declining trends in precipitation in Southwestern Europe to anthropogenic forcing at this stage.Unión Europea. Horizonte 2020Ministerio de Ciencia e Innovación (MICINN)/FEDERMinisterio de Economía y Competitividad (MINECO)the AXIS (Assessment of Cross(X)—sectoral climate Impacts and pathways for Sustainable transformation)Irish Environmental Protection AgencyDepto. de Física de la Tierra y AstrofísicaFac. de Ciencias FísicasTRUEpu
Stratigraphy, magnetic susceptibility, and mineralogy of loess-paleosol sequences in southwestern Illinois and eastern Missouri
No full textMagnetic susceptibility (MS) zones, controlled by silt-size magnetite concentrations, have been delineated within oxidized, C horizon Peoria and Loveland Silts along the Illinois and Mississippi Valleys. Lower Peoria and lower Loveland Silts (MS = 55-80 \times\ 10\sp{-5} SI) and Roxana Silt (MS = 60-90 \times\ 10\sp{-5}) have high MS probably reflecting greater contributions from Superior Lobe outwash. Middle Peoria and upper Loveland Silts (MS = 20-55 \times\ 10\sp{-5}) and upper Peoria Silt (MS = 40-60 \times\ 10\sp{-5}) have low MS, probably reflecting dilution by Lake Michigan Lobe outwash upon maximum advance of glaciers in Illinois. Feldspar/quartz and kaolinite/illite X-ray diffraction peak height ratios also increase in zones of high MS. Bulk and magnetic grain size distributions are generally uniform across MS zones at sections studied. Peoria Silt MS zones are particularly striking in loess proximal to the Illinois (Ancient Mississippi) Valley because of source area shifts caused by Mississippi River diversion at about 20.5 ka. MS zones are less pronounced along the Mississippi Valley south of St. Louis. Alteration of magnetite in gleyed loess can occur but is not thought to cause MS zones observed because minor increases in illite and dolomite in low MS zones are more consistent with a source area hypothesis. Jules and Gardena (interstadial) Geosol occur in upper portions of middle and lower Peoria Silt and are estimated to be 15-16 ka and 20-20.5 ka, respectively. Clay beds, deposited during peak glacial floods (16-20 ka), occur within middle Peoria Silt.Ultrafine magnetite and maghemite (0.01-0.1 m), authigenically formed, are responsible for high MS in upper solums of modern soils and paleosols, where they are preserved and can accumulate under oxidizing conditions. Highly substituted superparamagnetic and single domain magnetite probably forms extracellularly to bacteria in soils and later alters to maghemite. Soil firing can be locally important in causing high MS. Bt horizon thicknesses, clay content increases, feldspar weathering, and amounts of neoformed ferrimagnetics and mixed-layered kaolinite-expandables all indicate considerably greater time for development of the Yarmouth Geosol compared to the Sangamon Geosol. In the study area, Yarmouth Geosol is estimated to represent oxygen isotope stages 7-11 and the Sangamon Geosol stage 5 and portions of stage 4. Loveland Silt was probably deposited during stage 6 only. Crowley's Ridge Silt, into which Yarmouth Geosol formed, is estimated to have been deposited during stage 12. Bridgeton geosol (new) may represent stages 13-15 and Bonfils silt (new), stage 16.Made available in DSpace on 2011-05-07T12:02:25Z (GMT). No. of bitstreams: 2
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Cricotopus wangi Cranston & Krosch, sp. n.
No full text<i>Cricotopus wangi</i> Cranston & Krosch sp. n. <p>(Fig. 3 E, 5A,D, 9E, 12C)</p> <p>urn:lsid:zoobank.org: act:52659DBB-8F1F-471B-BF66-3047F4C10C8E</p> <p> <i>Cricotopus “wongi”</i> sp. nov. Cranston, in Cranston, 1996: 86 [Invalid; author states ‘not formal publication for nomenclatural purposes]</p> <p> <b>Type material. Holotype</b>: Le/Pe/♂, AUSTRALIA: NT, Litchfield NP, Wangi Falls, 13°10'S 130°41'E, 6.viii.1990 (<i>Cranston</i>). <b>Paratypes</b>: Le/Pe/♀, Le/Pe, 4L, as holotype; Le/Pe, Pe, NT/Qld, Border Waterhole, 18°37'S 137°59'E, 19.v.1995 (<i>Cranston</i>); WA, Hamersley Range NP, Fortescue Falls, Circular Pool, 22°28'S 118°33'E, 23–24.iv.1992 (<i>Cranston</i>).</p> <p> <b>Molecular material.</b> 2P, 2L, as holotype except 29.vii.2014 (<i>Cranston & Krosch</i>) (Mv-NT14.1.P1, P2, NT14.1.1, 1.3); L, Kakadu NP, Rockhole Ck., 13°34'S 132°15'E, 30.vii.2014 (<i>Cranston & Krosch</i>) (Mv- NT14.3.1); 2P, 3L, Kakadu NP, Gimbat, Upper S. Alligator R., 13°34'S 132°36'E, 31.vii.2014 (<i>Cranston & Krosch</i>) (Mv-NT14.6P1, P2); 3P, 2L, Kakadu NP, Gunlom, Waterfall Ck., 13°25'S 132°25'E, 1.viii.2014 (<i>Cranston & Krosch</i>) (Mv-NT14.7.P1-3).</p> <p> <b>Description.</b> MALE (n=1, immature pharate). 3.0 mm.</p> <p>Head. Ant 505 µm; Fl 1–12, 300 µm, Fl 13, 225 µm; A.R. 0.75. Palp 308–324 µm. Clyp sparsely setose, 9.</p> <p>Thorax. Brown. Laps 2–3; Ac 20, Dc 20 biserial. Pa and Scts not visible.</p> <p>Wing, legs and abdomen not measurable.</p> <p>Hypopygium (Fig. 3 E). Gcx 175, iv with medio-posteriorly rounded lobe; Gst 85 µm, about 1/2 (0.48) gcx; crista dorsalis not developed.</p> <p>FEMALE (n = 1, pharate). 3.2 mm.</p> <p>Head. Ant 245 µm. Fr 2, Po 2, Clyp 17; Palp 350 µm.</p> <p>Thorax. Laps 2, Ac 9, Dc 20–21, Pa 2–4, Scts 6–8.</p> <p>Wing, legs and abdomen not measurable.</p> <p>Genitalia. Spermathae comprising ovoid capsules with tapering "neck" and gently curved ducts (as in Fig. 4 B).</p> <p>PUPA (n=6). 2.7–3.2 mm, pale to mid-brown.</p> <p>Cephalothorax. Moderately rugose dorsally. Th 100–138 µm, width 37–50 µm; hyaline, elongate ovoid, without apical scales or spines (Fig 7 B). Fs 120–138, long, semi-taeniate, on frons (Fig. 5 A).</p> <p>Abdomen (Fig. 9 E). PSB on I, II and III. Hook row broad, about 2/3 of segment (0.65–0.72). No spinules or spines on TI or anterior to hook row on TII; anterolateral patches of very weak spinules on VII, VIII and IX. Paraterga bare. Ls 3 VIII 20 –25 µm, <1/15 segment width (0.06) (Fig. 5 D).</p> <p>Ms 60–80 µm, anteriormost displaced medially from margin 44–70 µm, <1/25 length of abdomen (0.04).</p> <p>4TH INSTAR LARVA (Fig. 12C). 3.7–4.1 mm. H.l. 350 µm, dark-brown; mandibles, mentum, occipital margin black; thorax yellow-green, abdomen blue-pigmented; procercus hyaline; procercal anal setae and posterior parapod claws black.</p> <p>Head. Ant 52–55 µm; 1, 30–32 µm; 2–5, 21–22 µm; A.R. 1.36–1.41; blade 25–27 µm extending beyond apical segment.</p> <p>Md 107–120 µm, outer margin strongly crenulate, inner smooth, completely dark brown (a little paler basally); seta subdentalis a spine.</p> <p>Mentum 80–85 µm, dark brown; 6–7 pairs laterals, first well developed, second slightly reduced, outermost mentum may be worn or appressed with 7th lateral indistinct.</p> <p>Abdomen. l4 seta not plumose. Pc very short, with brown pigment patches, 12–14 µm, A.s. 250–280 µm.</p> <p> <b>Etymology.</b> The epithet <i>wangi</i> derives from the name of the waterfall in Litchfield National Park, Northern Territory where the first specimens were collected (although in manuscript spelled as ‘wongi’). The name is a noun in apposition.</p> <p> <b>Remarks.</b> The combination of long frontal setae located on the frons, short L setae on VIII, hyaline nonspinose thoracic horn and short anal macrosetae with displaced basal setae allow easy recognition of the pupa of <i>C. wangi</i>. Larvae are characterised by the fully dark head capsule, including all-dark mandible. The mandible has strong crenulations on the outer margin and smooth mola, with a simple lance-shaped seta subdentalis. The antenna is uniquely short, maximally 55 µm long.</p> <p> <i>Cricotopus wangi</i> <b>sp. n.</b> appears to be restricted to northern Australia where the immature stages live on hygropetric surfaces of waterfalls, with few exceptions in riffles in permanent creeks.</p>Published as part of <i>Drayson, Nick, Cranston, Peter S. & Krosch, Matt N., 2015, Taxonomic review of the chironomid genus Cricotopus v. d. Wulp (Diptera: Chironomidae) from Australia: keys to males, females, pupae and larvae, description of ten new species and comments on Paratrichocladius Santos Abreu, pp. 1-40 in Zootaxa 3919 (1)</i> on pages 21-22, DOI: 10.11646/zootaxa.3919.1.1, <a href="http://zenodo.org/record/287861">http://zenodo.org/record/287861</a>
