bluuebunny/crossref_metadata_2025 huggingface dataset:
Accuracy of parental estimate of child's weight in a paediatric emergency department
Authors: Foster Mieke , Tagg Andrew , Klim Sharon , Kelly Anne‐Maree
Published: May 2019

Objectives

To determine the accuracy of using parental estimate of a child's weight compared to actual weight in a paediatric emergency setting.

Methods

Prospective, observational study. Age, weight and height data were collected from children aged 1 month up to 11 years with an Australian Triage score of 3 or higher. This was compared with a parent weight estimate. Analysis is descriptive.

Results

A total of 450 children were studied with a mean age of 4 years 4 months. A total of 85.3% of parents were willing to provide a weight estimate (n = 384). The mean difference between the parent estimate (where provided) and the actual weight was 0.33 kg (measured weight > estimated; 95% confidence interval [CI] −6.9 kg to +7.6 kg). There was 75% agreement within 10% of the measured weight (95% CI 71–79%) and 92% agreement within 20% of the measured weight (95% CI 89–95%). Weight was more commonly underestimated than overestimated. Children of Polynesian/Pacific ethnicity were less likely to have an accurate parental weight estimation.

Conclusions

Parent estimate is an accurate weight estimation method when parents are willing to give an estimate. There is ethnic variation in accuracy that should be taken into account when applying this method.
Development of the emerging electromagnetic methods for deep earth exploration
Authors: Di Qingyun , Xue Guoqiang , Wang Zhongxing , An Zhiguo , Fu Changmin , Wang Ruo , Lei Da , Olalekan Fayemi
Published: May 2019

Three emerging techniques for surface electromagnetic (EM) exploration with high detection accuracy and large depth of investigation, namely, WEM (wireless electromagnetic method), MTEM (multi‐channel transient electromagnetic method) and SOTEM (short‐offset grounded‐wire TEM), are introduced. In detail, we proposed a newly developed sky‐wave theory in which EM wave can propagate in full space of ionosphere‐atmosphere‐lithosphere. Correspondingly, we developed the WEM recording system to measure the sky‐wave to obtain the structures down to ∼10 km depth. We then introduced MTEM as a highly effective method for mineral exploration with target depth of 3km. Using self‐developed MTEM system, we presented the results obtained from mineral exploration study carried out in China. Lastly, we proposed the SOTEM method for a greater detection depth (1.5km) than traditional loop source TEM (500m) with a small offset and high resolution.
Water in Garnet Pyroxenite from the Sulu Orogen: Implications for Crust‐Mantle Interaction in Continental Subduction Zone
Authors: Chen Renxu , LI H.Y. , ZHENG Yongfei
Published: May 2019

Mineral water contents, together with the elements and isotopes of minerals and whole‐rock, were determined for garnet pyroxenites enclosed by ultrahigh‐pressure (UHP) metamorphic gneiss at Hujialin in the Sulu orogen. The results suggest that the garnet pyroxenites were generated in the Triassic by metasomatic reaction of the mantle wedge peridotite with hydrous felsic melts derived from partial melting of the deeply subducted continental crust. Measured water contents vary from 523 to 1213 ppm for clinopyroxene, and 55 to 1476 ppm for garnet. These mineral water contents are not only correlated with mineral major and trace element abundances but also relatively homogenous within single mineral grains. Such features preclude significant disturbance of the mineral water contents during pyroxenite exhumation from the mantle depth to the surface and thus indicate preservation of the primary water contents for the UHP metasomatites. The garnet pyroxenites are estimated to have bulk water contents of 424–660 ppm, which are higher than those for the MORB source, similar to or higher than those for the OIB sources and close to the lower limit for the arc magma source. The relationships between contents of mineral water and some elements suggest that the high water contents of garnet pyroxenites are primarily determined by the abundance of water‐rich clinopyroxene. Calculated whole‐rock H2O/Ce ratios are 63–145, higher than those for Hawaiian garnet pyroxenites and SWIR abyssal pyroxenites. These observations suggest that metasomatic pyroxene‐rich lithologies have the capacity to contribute high H2O concentrations and variable H2O/Ce ratios to the mantle. This lends support to the interpretation that the source of some intraplate basalts may be a heterogeneous mixture of peridotite and pyroxenite. On the other hand, the high water contents of garnet pyroxenites suggest that the ultramafic metasomatites are an important water reservoir in the mantle wedge.
Significance and Petrochemistry of Upper Mantle–mantle Transition Zone Metaperidotites and Oceanic Crust Metagabbros within the Kazdağı Metaophiolite: Implications for the Geological Evolution of the Izmir–Ankara–Erzincan Ocean, Northwestern Turkey
Authors: SARIFAKIOGLU Ender , SEVIN Mustafa , DILEK Yildirim , MÖLLER Andreas
Published: May 2019

The Kazdağı metaophiolite crops out in the Kazdağı (Ida) Mountains in the Biga Peninsula in northwestern Turkey. It is in stratigraphic contact with the high–grade metamorphic rocks of the Kazdağı Massif. Metaophiolitic and high–grade metamorphic rocks are tectonically overlain by low–grade metamorphic units of the Permo‐Triassic Karakaya Complex of the Sakarya Zone. Late Oligocene‐Early Miocene granites intruded these tectonic units (Okay and Satır, 2000; Duru et al. 2012).

In the Kazdağı metaophiolitic sequence, upper mantle peridotites are represented by metaharzburgite and metadunite, whereas the mantle transition zone metaperidotites are composed of metadunite, metapyroxenite and minor plagioclase‐bearing metalherzolite. The upper part of the metadunites in the mantle transition zone show intercalation with metagabbros. Gabbros of oceanic crust experienced amphibolite facies metamorphism and are transformed into amphibolite, garnet amphibolite and migmatitic gabbros. The metagabbros and amphibolites display MORB‐ and IAT‐like geochemical features.

The Kazdağı metaophiolite is conformably overline by basal conglomerates and hemi‐pelagic carbonate rocks continuing upward into forearc‐type flysch–like detrital sedimentary rocks interspersed with mafic volcanic intervals. These cover units underwent high–grade metamorphism into gneisses, migmatites, amphibolites and marbles in a compressional regime during the Alpine orogeny. New U–Pb zircon data from the metagabbros show two crystallization peaks at ∼52 Ma and ∼73 Ma. This has implications for the age of subduction of the Izmir–Ankara–Erzincan Ocean, generally assumed to be northward under the Sakarya Zone. During the Triassic to Middle Eocene, progressive overthrusting of the Sakarya Zone via a N–S compresional regime created by the Alpine orogeny onto subduction–accretion‐ and forearc‐units resulted in high–grade metamorphic conditions in the Biga Peninsula.
Impacts and Exposed Lithospheric Mantle: A Way to Recognize large Terrestrial Impact basins?
Authors: OLDS Eric Peter
Published: May 2019

Orientale size craters are not recognized on Earth nor expected for Phanerozoic and Proterozoic eons from conventional crater size frequency distributions (Ivanov et al., 2002). Here suggested are three such Phanerozoic craters, modified by plate tectonics, and tentatively correlated with extinction and “ophiolite obduction” events. Hypothesis testing is proposed and plate tectonics implications are discussed. Such basins might manifest:

circular to elliptical rims (or rim segments), with exposed lithospheric mantle, as strain markers for plate boundary motion;

thick ejecta near rim expressed as “ophiolitic melange”;

power law decay of ejecta thickness with radial distance from rim (McGetchin et al., 1973) and/or systematic azimuthal variation of ejecta thickness for low angle impacts (Schultz, 1999);

weathering resistant shocked mantle minerals (Bohor et al., 1990) in ejecta;• global spherule layer with PGE anomalies (Alvarez et al., 1980);

rim structures consistent with cratering mechanics (Melosh, 1989; Kenkmann, 2014);

impact melt basement (Grieve et al., 1992; Pierazzo et al. 2000) recording uniform cooling age and Earth's magnetic polarity of the time. Tentatively suggested Phanerozoic impact basins:

Yucatan Basin: Greater Antilles ophiolite rim – KPg Boundary? Maastrichtian ophiolite obduction in southeast Cuba (Iturralde‐Vinent et al., 2006).

Sulu Sea Basin: Palawan, Sabah etc. ophiolite rim – Middle Miocene Disruption? MM ophiolitic mélange emplacement in Sabah (Clennell, 1991).

Loyalty Basin: New Caledonia ophiolite and d'Entrecasteaux ridge rim – EO Boundary? EO ophiolite obduction in New Caledonia (Cluzel et al., 2012).
Petrogenesis and Tectonic Significance of the Cuobuzha Peridotite, Yarlung Zangbo Suture Zone, China
Authors: FENG Guangying , YANG Jingsui , DILEK Yildirim , LIU Fei , XIONG Fahui
Published: May 2019

The Yarlung Zangbo suture zone (YZSZ) in southern Tibet includes the remnants of Neo‐Tethyan oceanic lithosphere and marks a major suture between the Indian plate to the south and the Lhasa terrane of Tibet to the north. The upper mantle section of the Cuobuzha ophiolite in the northern subbelt of the western YZSZ comprises mainly clinopyroxene (cpx)‐rich and depleted harzburgites. Spinels in the cpx‐harzburgites show lower Cr# values (12.6–15.1) than the spinels in the harzburgites (26.1–34.5), and the cpx‐harzburgites display higher heavy rare earth element concentrations than the depleted harzburgites. The harzburgites have subchondritic Os isotopic compositions (0.11624–0.11699), yielding Re‐depletion model ages (TRD) ages from 1.8 to 1.7 Ga, indicating that the Cubuzha mantle underwent at least one ancient melt extraction event ca. 1.8‐1.7Ga; whereas the cpx‐harzburgites have suprachondritic 187Os/188Os ratios (0.12831–0.13125) with higher Re concentrations (0.380–0.575 ppb), indicating subsequent addition of Re following the last partial melting event that occurred during mid‐ocean ridge melt evolution processes. Although these geochemical and isotopic signatures suggest that both peridotite types in the ophiolite represent mid‐oceanic ridge–type upper mantle units, their melt evolution trends reflect different mantle processes. The cpx‐harzburgites formed from low‐degree partial melting of a primitive mantle source, and they were subsequently modified by melt‐rock interactions in a mid‐oceanic ridge environment. The depleted harzburgites, however, were produced by remelting of the cpx‐harzburgites, which later interacted with mid‐oceanic ridge basalt– or island‐arc tholeiite–like melts, possibly in a trench–distal backarc spreading center. Our new isotopic and geochemical data from the Cuobuzha peridotites confirm that the Neo‐Tethyan upper mantle had highly heterogeneous Os isotopic compositions as a result of multiple melt production and melt extraction events during its seafloor spreading evolution.
Geochemical Characteristics of the Gabbros from the Xinlin Ophiolite in the Great Xing'an Range, NE China
Authors: GOU Jun , SUN Deyou
Published: May 2019

The Xinlin ophiolite in NE China is generally considered to mark the suture between the Erguna and Xing'an blocks. Compared with the Maihantewula ophiolite and Jifeng‐Gaxian ophiolite in the southern and central parts of the Xinlin–Xiguitu suture zone, the Xinlin ophiolite in the northern part of the suture has not been as thoroughly investigated. Many studies acknowledge the indicators of the Xinlin ophiolite as a suture, but detailed studies of this unit are scarce. In the present work, we provide the geochemical data to constrain the origin of the gabbros in Xinlin ophiolites. The gabbros from the Xinlin ophiolites are texturally heterogeneous, ranging from fine‐grained aplitic to coarse‐grained pegmatitic. The fine‐grained gabbros have flat to slightly enriched LREE patterns, which are geochemically comparable to transitional (T‐MORB) and enriched mid‐ocean ridge basalt (E‐MORB). The pegmatite gabbros exhibit slightly LREE‐depleted patterns, similar to typical N‐MORB that derived from a depleted mantle source. Generally, gabbros from the Xinlin ophiolites are MORB‐like, but also have some arc characteristics such as high Th and low Ta concentrations. Such features is typical in Supra‐subduction zone (SSZ) type ophiolites. Our data, combined with other regional results, suggest that the geochemical signatures of the Xinlin gabbros that vary between arc‐like and MORB‐like were possibly indicative of their derivation from a subduction‐modified depleted mantle.
Carbon and Nitrogen Isotopic, and Mineral Inclusion Studies on the Diamonds from the Pozanti‐Karsanti Chromitite, Turkey
Authors: LIAN Dongyang , YANG Jingsui , WIEDENBECK Michael , ROCHOLL Alexander , DILEK Yildirim , WU Weiwei
Published: May 2019

He Pozanti‐Karsanti ophiolite (PKO) is one of the largest oceanic remnants in the Tauride belt, Turkey. Micro‐diamonds were recovered from the podiform chromitites, and these were investigated based on morphology, color, cathodoluminescence, nitrogen content, carbon and nitrogen isotopes, internal structure and inclusions. The diamonds recovered from the PKO are mainly mixed‐habit diamonds with sectors of different brightness under the cathodoluminescence images. The total δ13C range of the PKO diamonds ranges between −18.8 ‰ and −28.4 ‰, with a principle δ13C mode at −25 ‰. Nitrogen contents of the diamonds range from 7 to 541 μg/g with a mean value of 171 μg/g, and the δ15N values range from −19.1 ‰ to 16.6 ‰, with a δ15N mode of −9 ‰. Stacking faults and partial dislocations are commonly observed in the Transmission Electron Microscopy foils whereas inclusions are rather rare. Combinations of (Ca0.81Mn0.19)SiO3, NiMnCo‐alloy and nano‐size, quenched fluid phases were observed as inclusions in the PKO diamonds, confirming a natural origin of these diamonds. We believe that the δ13C‐depleted carbon signature of the PKO diamonds is a remnant of previously subducted crustal matter. These diamonds may have crystallized in metal‐rich melts in the asthenospheric mantle at depth below 250 km which were subsequently carried rapidly upward by asthenospheric melts/fliuds. We concluded that diamond‐bearing asthenospheric melts were likely involved in the formation of the Pozanti‐Karsanti podiform chromitite.
Limited Recycling of Crustal Osmium in Forearc Mantle During Slab Dehydration
Authors: LIU Chuanzhou , XU Yang , WU Fuyuan
Published: May 2019

Elevated 187Os/188Os ratios compared to ambient oceanic mantle, i.e.,187Os/188Os>0.13, have been reported for both arc lavas and mantle wedge xenoliths, which have been ascribed to the addition of crustal Os through slab dehydration or melting. By contrast, much lower 187Os/188Os ratios of spinels from Izu‐Bonin‐Mariana boninites indicate slight or no crustal Os was transferred from the slab to the forearc mantle. Here we report Os isotopic compositions of peridotites from New Caledonia ophiolites, which represent relics of a forearc mantle. Some New Caledonia peridotites are characterized by Os concentrations of <1 ppb, yet have187Os/188Os ratios comparable to the ambient oceanic mantle (i.e., 187Os/188Os<0.13). This confirms that little crustal Os was transported to the forearc mantle via slab dehydration. Contrasting Os isotopes between forearc peridotites and mantle wedge xenoliths may reflect the changing behavior of Os in diverse agents released from the descending slab as a function of depth, which is mainly controlled by the stability of sulfides in the slabs. During dehydration at shallow depths, sulfides keep stable and thus little Os is transported to the overlying mantle. In comparison, sulfides become unstable and tend to break down at deeper depths where slab melting or supercritical fluid generation occurs, and thus Os behaves like a mobile element.
Tectonic Implications of the Carboniferous Volcanic Rocks in the Eastern Junggar — Evidence from Zircon U‐Pb Ages and Geochemistry
Authors: WANG Chong , LUO Jinglan , CHEN Chunyong , HE Xianying , MA Shangwei , XU Xuelong , DAI Jingjing , LIU Yong
Published: May 2019

Well Drilling shows that the volcanic rocks from the Carboniferous Batamayineishan Formation in the Eastern Junggar basin are mainly composed of volcaniclastic rocks (av. 52%) and volcanic lavas (32%), with a small amount of volcanic pyroclastic lavas (av. 11%). The volcanic lavas are basalt‐basaltic andesite‐andesite‐dacite assemblage. The LA‐ICP‐MS zircon U‐Pb dating of the andesite and the dacite yielded 325∼321 Ma and 310 Ma ages, respectively, which is of high agreement with the published age (300 Ma) of basalts from this Formation, it is implied that an important volcanic activity occurred in Junggar basin in the late Carboniferous. The lavas have low TiO2 and high Na2O, indicating a calc‐alkaline series. Geochemical data show that they are characterized by LREE‐enriched patterns with slightly negative Eu anomalies. The rocks have high large ion lithophile element (LILE), and low high field strength element (HFSE) concentrations, with strong negative Nb, Ta and Ti anomalies. From basic through intermediate to felsic, the depletions in Sr, Ti and P of the studied volcanic rocks increase gradually. These geochemical characteristics indicate that the volcanic rocks are magmatic evolution products attributed to partial melting of mantle‐derived spinelle lherzolite related to oceanic subduction in an island‐arc setting. In combination with the LA‐ICP‐MS zircon U‐Pb dating, it is inferred that subduction of the Junggar Ocean in eastern Junggar basin lasted to the Late Carboniferous. Consequently, the final closure of the Junggar Ocean occurred most likely after 310 Ma.
Sub‐mantle δ18O Zircons in Malani rhyolites: Clues for a Rodinia Linkage between South China and NW India
Authors: WANG Wei , CAWOOD Peter , ZHOU Meifu , PANDIT Manoj , XIA Xiaoping , ZHAO Junhong
Published: May 2019

The Malani Igneous Suite (MIS) in NW India represents one of the largest and well‐preserved Precambrian felsic igneous provinces, with minor mafic volcanics and dykes. The SIMS (Secondary Ion Mass Spectrometric) zircon U‐Pb geochronology yielded 776.8 ± 4.5 to 758.5 ± 6.9 Ma ages for rhyolites from Jodhpur region and Sindreth Basin while dacite sample from Punagarh Basin was dated to 760.5 ± 10 Ma. Zircons from rhyolitic and dacitic lavas have oxygen isotopic compositions that can be grouped into low δ18OV‐SMOW (4.12 to ‐1.11‰) and high (δ18O = 8.23‐5.12‰) categoroes, respectively. The low δ18O zircons have highly radiogenic Hf isotopic compositions (εHf(t)= +13.0 to +3.6) suggesting high temperature bulk cannibalization of upper level juvenile crust as the essential process for magma generation. Older than 800 Ma xenocrystic zircons in dacite have high δ18O values whereas 795 Ma ones have mantle‐like Hf‐O isotopic compositions, reflecting a significant shift in tectono‐thermal regime in NW India during 800‐780 Ma. A synchronous transition in the South China Block and Madagascar suggests a spatially and temporally linked geodynamic system. Geochemical data in combination with the new isotopic results point towards an overall convergent plate margin setting undergoing localized lithospheric extension. The NW India and South China blocks together with Madagascar and the Seychelles lay either along the periphery of Rodinia or off the supercontinent with the age of convergent plate margin magmatism coinciding with breakup of the supercontinent.
Babu (SW China)‐Cao Bang (NE Vietnam) Ophiolite Complex: Implications for Tectonic Evolution between South China and the Indochina Block
Authors: XIANG Zhongjin , YAN Quanren , XIA Wenjing , XIA Lei
Published: May 2019

The convergence process between South China and the Indochina Block is still controversial. A large number of igneous rocks scattered along the current China‐Vietnam border provide a good opportunity to investigate the tectonic evolution. Babu ophiolites, cropping out in the southeastern Yunnan province (SW China), consist primarily of metaperidotite, serpentinite, pillow basalt (metabasalt), gabbro, metadiabase. Most of them are fault contacted and strongly sheared, especially between metaperidotite/serpentinite and metabasalt. U‐Pb zircon analyses yield an Early Permian formation age of ∼278 Ma. Basalts and metagabbros show light rare earth elements (LREEs)‐depleted and heavy rare earth elements (HREEs)‐flat REE patterns, and large ion lithophile elements (LILEs)‐depleted primitive‐normalized spider diagrams without Nb‐Ta anomalies, which is similar to N‐MORB. Metaperidotites have low initial 187Os/188Os (0.122‐0.126) and γOs values, and indicate that they were derived from a depleted mantle source. Relative low (87Sr/86Sr)i and high εNd(t) values of basalts and metagabbros also support their DMM origin. The petrological, geochemical and isotope characteristics suggest that Babu ophiolites were N‐MORB‐type and represent remnants of an Early Permian oceanic crust. Mafic‐ultramafic rocks exposed in Cao Bang area (NE Vietnam) have recently been considered as dismembered Paleotethyan ophiolites instead of were genetically linked to the Emeishan Large Igneous Province. U‐Pb zircon analyses suggest an Early‐Middle Permian age (274 ±18 Ma) for the formation of ultramafic rocks. Both whole rock geochemistry and Cr‐spinel mineral chemistry show MORB‐like characteristics. Field observations suggest that Babu and Cao Bang ophiolite complex structurally overlie Middle‐Triassic deposits, and form a tectonic mélange zone. It developed from the subduction of a Paleotethyan subsidiary ocean basin between the South China and Indochina blocks until their collision..
Multi‐stage Melting Processes of Ophiolitic Chromitites from Purang Peridotite, the Western Yarlung‐Zangbo Suture Zone, Tibet
Authors: XIONG Fahui , YANG Jingsui , ROBINSON Paul T , XU Xiangzhe
Published: May 2019

The Purang ophiolite, which crops out over an area of about 600 km2 in the western Yarlung‐Zangbo suture zone, consists chiefly of mantle peridotite, pyroxenite and gabbro. The mantle peridotites are mostly harzburgite and minor lherzolite that locally host small pods of dunite. Some pyroxenite and gabbro veins of variable size occur in the peridotites, and most of them strike NW. On the basis of their mineral chemistry podiform chromitites are divided into high‐alumina (Cr# = 20‐60) (Cr# = 100*Cr/(Cr+Al)) and high‐chromium (Cr# = 60‐80) varieties (Thayer, 1970). Typically, only one type occurs in a given peridotite massif, although some ophiolites contain several massifs which can have different chromitite compositions. However, the Purang massif contains both high chrome and high alumina chromitites within a single mafic‐ultramafic body. Seven small, lenticular bodies of chromitite ore have been found in the harzburgite, with ore textures ranging from massive to disseminated to sparsely disseminated; no nodular ore has been observed. Individual ore bodies are 2‐6 m long, 0.5‐2 m wide and strike NW, parallel to the main structure of the ophiolite. Ore bodies 1 and 6 consist of Al‐rich chromitite (Cr# = 52‐55), whereas orebodies 2, 3, 4 and 5 are Cr‐rich varieties (Cr # = 63 to 89). In addition to magnesiochromite, all of the orebodies contain minor olivine, amphibole and serpentine. Mineral structures show that the peridotites experienced plastic deformation and partial melting. On the basis of magnesiochromite and olivine/clinopyroxene compositions two stages of partial melting are identified in the Purang peridotites, an early low‐partial melting event (about 8%), and a later high‐partial melting event (about 40%). We interpret the Al‐rich chromitites as the products of early MORB magmas, whereas the Cr‐rich varieties are thought to have been generated by the later SSZ melts..
Zircon U‐Pb Dating and Hf Isotope of the Metavolcanics, Gabbro and Plagiogranite in the Mianxian‐Lueyang Areas of Mianlue Belt
Authors: ZHANG Chengli
Published: May 2019

The Mianlue Belt is located in the central China and regarded as a tectonic mélange belt, representative of suture zone formed in the early Mesozoic between North and South China Blocks. However, its forming age has been controversial for a long time. This study provides the reliable LA‐ICPMS U‐Pb zircon dating and in‐situ Hf isotopes from the meta‐volcanics, gabbro and plagiogranite in this belt. Of which, two meta‐andesites yielded the ages of 934 Ma and 933 Ma, two meta‐dacites give the ages of 999 Ma and 873 Ma, and another plagiogranite define an age of 923 Ma, respectively, evidently older than those previously thoughted. Their Hf isotopes are quite coincident. The andesites have the εHf(t)= ‐0.03 ∼ +11.76 with the TDMC of 1032‐1629 Ma, εHf(t) = +9.81∼ +16.06 and the TDMC = 867‐1185 Ma for dacite and εHf(t) = +8.65 ∼ +16.66 and the TDMC = 805∼1123 Ma for plagiogranite, suggesting an important crustal growth in the early Neoproterozoic. In addition, the gabbro yielded younger ages of 224‐213 Ma and variable ages from 1225 Ma to 280 Ma in some inherited zircons, consistent with early Mesozoic mafic dykes in South Qinling belt. Their TDMC range from 1.2 to 2.7 Ga, indicating early‐middle Proterozoic crustal residence involved minor Neo‐Archean crustal materials. All new results lead us to propose that most of components in the Mianlue Belt were generated in the early Neoproterozoic and related to the subduction process in the northern margin of the Yangtze block, representative of an important juvenile crust growth in South Qinling during the Neoproterozoic.
The Metamorphic Evolution and Tectonic Significance of the Eclogite in the Sumdo Complex, Tibet, China
Authors: ZHANG Cong , BADER Thomas , VAN ROERMUND Herman , YANG Jingsui
Published: May 2019

As the main tectonic component of the Himalayan–Tibetan orogen, the Lhasa terrane has received much attention as it records the entire history of the orogeny. The occurrence of high pressure eclogite in the Sumdo complex in central Lhasa terrane has a significant bearing on the understanding of the Paleo‐Tethys subduction and plate itineration processes in this area. The petrological, geochemical and geochronological data from eclogite and associated blueschist and garnet‐bearing mica schist from Sumdo, Jilang and Bailang area have been briefly review to explore the origin and metamorphic evolution of this suture. Eclogites from the Sumdo complex have experienced low temperature, high pressure to ultrahigh pressure metamorphism, revealing a fast subduction and exhumation process in a typical oceanic subduction zone. The large P‐T span between different eclogites in the literature may be affected by the big error of unappropriated using geothermobarometry and may also because of slices of subducted blocks derived from different depths juxtapose together during exhumation. By summarizing the U‐Pb, Lu‐Hf and Sm‐Nd ages of eclogites, the eclogite facies metamorphism is likely to occur in early Triassic during 245‐225 Ma, but not the previously accepted late Permian at ca. 260 Ma by the reinterpretation of the former geochronological data from literature. The opening of Paleo‐Tethys Ocean between the Lhasa terrane initiate prior to ca. 280 Ma and ultimate closure to integrate the Lhasa terrane was no earlier than 225 Ma and may triggered by the initial subduction of Bangong‐Nujiang Tethys Ocean in the north.
High Accuracy Ground Magnetic Survey was Applied in the Khammouane Potash Deposit, the Lao P.D.R: An Efficient and Fast Exploration Model of Potash Deposits in Covered Areas
Authors: CUI Minli
Published: May 2019

The period and cost of mine exploration in new strange areas are very strict and very little geological data is available. The working area is usually covered by the exuberant vegetation, so the surface observation is very difficult and the working environment is very harsh. This paper introduces the application of high‐precision ground magnetic method to the rapid, efficient and low‐cost prospecting of favourable areas for mineralization in Khammouane Potash Deposit, the Lao P.D.R.
Analyses of the Compositional Characteristics and Sources of the Organochlorine Pesticides in the Surface Sediments of Guanghai Bay, Taishan City, Guangdong Province
Authors: HE Haijun , GAN Huayang , HE Jinxian , XIA Zhen
Published: May 2019

Organochlorine pesticides (OCPs) are a class of toxic and harmful persistent organic pollutants widely found in environment. Hexachlorocyclohexane (HCHs) and DDTs are two of the most widely used OCPs (Qiu et al., 2004), so it is important to find out their compositional characteristics and sources in surface sediments. Guanghai Bay is located in the south of Guanghai Bay Industrial Park in Taishan City, Guangdong Province. It borders Huangmaohai to the east and Zhenhai Bay to the west, covering an area of about 236 square kilometers. In this study, surface sediments were collected at 16 sites in Guanghai Bay (Fig. 1). After the surface sediments were pretreated, GC‐MS was used to analyze OCPs. A total of 14 OCPs were detected and their content was shown in Table 1. The concentration of ΣOCPs ranged between 0.507∼0.860ng·g‐1, with an average of 0.680 ng•g‐1. In general, the content of ΣOCPs was the highest at No. A12 site. The concentrations of these 14 detected OCPs ordered as dieldrin > epoxy heptachlor > P, P'‐DDD > γ‐HCH >endrin >aldrin > P, P'‐DDE >mirex >hexachlorobenzene >P, P'‐DDT > α‐HCH > δ‐HCH >β‐HCH > heptachlor.
When the Flames are Licking at the Door: Standing Mechanisms for Conflict Prevention
Authors: Nathan Laurie
Published: May 2019

Enhancing the effectiveness of conflict prevention is a major preoccupation of the international community. This article focuses on operational prevention of conflict, which entails diplomatic efforts to avert imminent violence in crisis situations. The conventional understanding is that these efforts are short‐term and sporadic. In contrast, this article identifies and analyzes a type of operational prevention that has been institutionalized in order to engage in continuous preventive action in a particular conflict. I define ‘institutionalized operational prevention’ as a standing mechanism that aims to prevent a conflict from becoming violent and prevent low‐level violence from escalating into large‐scale violence. The article discusses a number of such mechanisms that have been successful in this regard, and offers an explanation for their success. Policymakers should consider establishing standing prevention mechanisms in other situations that have a persistent risk of large‐scale violence. Where structural reforms are required to reduce this risk but are politically unfeasible, the standing mechanisms may be the only viable means of avoiding violence.
Effects of roads on small mammal diversity and abundance in the northern Serengeti, Tanzania
Authors: Sangiwa Michael W. , Magige Flora J.
Published: May 2019

The high biodiversity of small mammal species in the Serengeti ecosystem provides this ecosystem with important conservation value. However, whether the extensive development of roads has negative impacts on the small mammal population has not been tested. Small mammal population diversity and abundance were examined in this study using live trapping at sites close to (experimental) and away (control) from the main gravel road during the short rainy seasons in November and December 2011 and 2012. A total of 138 individuals from three orders representing six families and fourteen species were collected over 4,860 trap nights. There were no significant differences in the species richness, diversity or abundance of small mammals between the control and experimental sites (p > 0.05), suggesting that the current gravel road does not have a significant impact on the small mammal population. These findings were ascribed to the availability of favourable habitats at both distances as a result of little road usage due to poor conditions. Should the road be improved, the control of anthropogenic activities in the area should be given high priority. Continuous monitoring of the small mammal populations in the area is recommended.
The outcomes of pregnancies with reduced fetal movements: A retrospective cohort study
Authors: Bhatia Meena , Mitsi Vaia , Court Lisa , Thampi Premila , El‐Nasharty Mohamed , Hesham Saeed , Randall Wendy , Davies Rachel , Impey Lawrence
Published: May 2019

Introduction

The objective of this study was to examine the outcomes and interventions in pregnant women presenting with a perception of reduced fetal movements (RFM), and to determine if repeated episodes of RFM increase the risk of adverse outcomes.

Material and methods

This was a retrospective cohort study conducted in six NHS hospitals within the Thames Valley network region, UK and one neighboring hospital, an area with approximately 31 000 births annually. All women with a primary presentation of perceived RFM after 24 completed weeks of gestation during the month of October 2016 were included in the study.

Prospective records in all units were examined and individual case‐notes were reviewed. Pregnancy and neonatal outcomes and their relation with recurrent presentations with RFM were examined using relative risks with 95% CI. The main outcome measures are described. Neonatal outcomes measured were perinatal mortality, neonatal unit admission, abnormal cardiotocography at presentation, a composite severe morbidity outcome of Apgar <7 at 5 minutes or arterial pH <7.0 or encephalopathy, and birthweight. Pregnancy outcomes measured were induction of labor, cesarean section, admission and ultrasound usage rates.

Results

In all, 591 women presented with RFM during the month; using annual hospital birth figures, the incidence of RFM was estimated at 22.6% (range 14.9%‐32.5%). More than 1 presentation of RFM occurred in 273 (46.2%). All 3 deaths (0.5%) were at the first presentation. More than 1 presentation was associated with higher induction rates (56.0% vs 31.9%), but no increase in any adverse outcomes including small‐for‐gestational‐age.

Conclusions

Reduced fetal movements, and recurrent episodes, are common, and lead to considerable resource usage and obstetric intervention. We found no evidence to suggest that recurrent episodes increase pregnancy risk.
Review article: emerging role of the gut microbiome in the progression of nonalcoholic fatty liver disease and potential therapeutic implications
Authors: Jayakumar Saumya , Loomba Rohit
Published: May 2019

Background

Nonalcoholic fatty liver disease (NAFLD) is a prevalent disorder associated with obesity and diabetes. Few treatment options are effective for patients with NAFLD, but connections between the gut microbiome and NAFLD and NAFLD‐associated conditions suggest that modulation of the gut microbiota could be a novel therapeutic option.

Aim

To examine the effect of the gut microbiota on pathophysiologic causes of NAFLD and assess the potential of microbiota‐targeting therapies for NAFLD.

Methods

A PubMed search of the literature was performed; relevant articles were included.

Results

The composition of bacteria in the gastrointestinal tract can enhance fat deposition, modulate energy metabolism and alter inflammatory processes. Emerging evidence suggests a role for the gut microbiome in obesity and metabolic syndrome. NAFLD is often considered the hepatic manifestation of metabolic syndrome, and there has been tremendous progress in understanding the association of gut microbiome composition with NAFLD disease severity. We discuss the role of the gut microbiome in NAFLD pathophysiology and whether the microbiome composition can differentiate the two categories of NAFLD: nonalcoholic fatty liver (NAFL, the non‐progressive form) vs nonalcoholic steatohepatitis (NASH, the progressive form). The association between gut microbiome and fibrosis progression in NAFLD is also discussed. Finally, we review whether modulation of the gut microbiome plays a role in improving treatment outcomes for patients with NAFLD.

Conclusions

Multiple pathophysiologic pathways connect the gut microbiome with the pathophysiology of NAFLD. Therefore, therapeutics that effectively target the gut microbiome may be beneficial for the treatment of patients with NAFLD.
Debate: Different strokes for different folks
Authors: Zucker Kenneth J.
Published: May 2019

A gender social transition in prepubertal children is a form of psychosocial treatment that aims to reduce gender dysphoria, but with the likely consequence of subsequent (lifelong) biomedical treatments as well (gender‐affirming hormonal treatment and surgery). Gender social transition of prepubertal children will increase dramatically the rate of gender dysphoria persistence when compared to follow‐up studies of children with gender dysphoria who did not receive this type of psychosocial intervention and, oddly enough, might be characterized as iatrogenic. Parents who bring their children for clinical care hold different philosophical views on what is the best way to help reduce the gender dysphoria, which require both respect and understanding.
Hsa_circ_0005519 increases IL‐13/IL‐6 by regulating hsa‐let‐7a‐5p in CD4+ T cells to affect asthma
Authors: Huang Zhenli , Cao Yong , Zhou Min , Qi Xuefei , Fu Bohua , Mou Yong , Wu Guorao , Xie Jungang , Zhao Jianping , Xiong Weining
Published: May 2019

Background

Circular RNAs (circRNAs) are a class of non‐coding RNAs that could serve as novel biomarkers for the diagnosis and treatment of diseases. We hypothesized that circRNAs of CD4+ T cells are involved in asthma.

Objective

In this study, we investigated the circRNA expression profile and the possible mechanism by which hsa_circ_0005519 participates in asthma.

Methods

The expression profiles of circRNAs in CD4+ T cells were revealed by circRNA microarray. Hsa_circ_0005519 expression in CD4+ T cells was confirmed in asthmatic patients (n = 65) and healthy subjects (n = 30). Hsa‐let‐7a‐5p, the target of hsa_circ_0005519, was predicted by online algorithms and verified by a dual‐luciferase reporter assay. Correlation assays between the expression of hsa_circ_0005519 and hsa‐let‐7a‐5p, the mRNA levels of interleukin (IL)‐13 and IL‐6 in CD4+ T cells, and the clinical characteristics of asthmatic patients were performed. The role of hsa_circ_0005519 in proinflammatory cytokine expression was investigated in CD4+ T cells from asthmatic patients in vitro. Hsa_circ_0005519 expression in PBMCs was determined in another cohort including 30 asthmatic patients and 24 controls. Correlation assays of hsa_circ_0005519 expressions between CD4+ T cells and PBMCs were performed.

Results

Hsa_circ_0005519 was up‐regulated and negatively correlated with hsa‐let‐7a‐5p expression in CD4+ T cells of asthmatic patients. Both the fraction of exhaled nitric oxide (FeNO) and the peripheral blood eosinophil ratio were positively correlated with hsa_circ_0005519 expression in CD4+ T cells. These outcomes were also different in asthmatic patients with low vs high hsa_circ_0005519 levels. Hsa_circ_0005519 expressions between CD4+ T cells and PBMCs were concordant in asthmatic patients. Mechanistically, hsa_circ_0005519 might bind to hsa‐let‐7a‐5p and relieve suppression for IL‐13/IL‐6 in CD4+ T cells.

Conclusions and clinical relevance

Our data suggest that hsa_circ_0005519 may induce IL‐13 and IL‐6 expression by regulating hsa‐let‐7a‐5p in CD4+ T cells to affect asthma. And hsa_circ_0005519 may be a potential biomarker of asthma.
Primary cutaneous acral CD8+ T‐cell lymphoma of the ear: A case report
Authors: Ormerod Emma , Murigu Timothy , Pawade Joya , Beasley Matthew , Dunnill Giles
Published: May 2019

Primary cutaneous acral CD8+ T‐cell lymphoma (TCL) is a rare, distinct type of cutaneous TCL. Despite its worrisome histological appearance it has a benign clinical course. It is therefore important to recognize this as a distinct entity from other more aggressive CD8+ lymphomas, for which the management is very different.
Perianal and perineal keratoacanthoma: Two cases demonstrating histologic similarity to subungual keratoacanthoma
Authors: Paulson Nathan , Gibson Joanna , Glusac Earl
Published: May 2019

Perianal keratoacanthomas are rare, with 10 cases reported to date. Perineal keratoacanthoma has not previously been described. In this report, we describe two cases of keratoacanthoma, one perianal and one perineal. Both lesions show prominent dyskeratotic keratinocytes, with striking and curious histologic resemblance to subungual keratoacanthoma.
Joint roles of parenting and nutritional status for child development: Evidence from rural Cambodia
Authors: Berkes Jan , Raikes Abbie , Bouguen Adrien , Filmer Deon
Published: May 2019

Substantial work has demonstrated that early nutrition and home environments, including the degree to which children receive cognitive stimulation and emotional support from parents, play a profound role in influencing early childhood development. Yet, less work has documented the joint influences of parenting and nutritional status on child development among children in the preschool years living in low‐income countries. Using panel data from 2016 to 2017 on the parenting, nutritional status, and early developmental outcomes (executive function, language, early numeracy, and socioemotional problems) of 6,508 Cambodian children ages 3–5 years, our findings demonstrate that inequities in early development associated with family wealth are evident at age 3 and increase among children ages 4 and 5 years. Using hierarchical regression analysis, a significant share of these inequalities is explained by differences in parenting and early nutritional status, measured by stunting. Better‐educated parents engage in more stimulating and supportive parenting practices. However, the positive association between parenting and language and early numeracy outcomes is 35–54% stronger for non‐stunted children, and parental activities explain only about 8–14% of the cognitive gap between the lowest and highest wealth quintiles. The results highlight the need for additional research outlining interactions between environmental factors that link family wealth and child development.
Interpreting the Reformation in Africa: Transformative hermeneutics of Manas Bethulezi in light of 500 years of the Reformation
Authors: Mtata Kenneth
Published: May 2019

A cursory look at the various histories of religious renewal shows three interrelated aspects; there is an experience of injustice that is followed by the religious movement's new revitalization through the special encounter or reference to divine communication, and then an effort to reorganize the socio‐economic and political structures of society in light of the newly discovered religious vitality. This article observes in the phenomenology of religious renewal that cultural renewal and cultural distinctiveness tend to accompany religious renewal.
Big Data and diabetes: the applications of Big Data for diabetes care now and in the future
Authors: Rumbold J. M. M. , O'Kane M. , Philip N. , Pierscionek B. K.
Published: May 2019

We review current applications of Big Data in diabetes care and consider the future potential by carrying out a scoping study of the academic literature on Big Data and diabetes care. Healthcare data are being produced at ever‐increasing rates, and this information has the potential to transform the provision of diabetes care. Big Data is beginning to have an impact on diabetes care through data research. The use of Big Data for routine clinical care is still a future application. Vast amounts of healthcare data are already being produced, and the key is harnessing these to produce actionable insights. Considerable development work is required to achieve these goals.
Diabetic foot ulcer incidence and survival with improved diabetic foot services: an 18‐year study
Authors: Paisey R. B. , Abbott A. , Paisey C. F. , Walker D.
Published: May 2019

Aims

To ascertain the effects of improvements in diabetic foot services over 18 years on incidence of diabetic foot ulceration. We also compared survival time from first ulcer development with presence of neuropathy, peripheral vascular disease, age and healing.

Methods

Persons with new ulceration and those at high risk of ulcer development were referred to community podiatry from 1998. Their details were recorded, with verbal consent, on a central database. The effects of neuropathy, peripheral vascular disease, healing and age on survival were analysed by Cox proportional hazards ratios.

Results

The incidence of first ulcer presentation decreased from 11.1 to 6.1 per 1000 persons between 2003 to 2017 (P <0.0001). Recurrent ulceration incidence remained stable. Prevalence of chronic and new foot ulceration combined increased from 20.7 to 33.1 per 1000 persons (P <0.0001). Ten‐year survival was 85% for persons presenting with first ulcer and aged < 65 years, 50% for those aged 65–74 years and 25% for those aged 75–81 years (P < 0.0001). In those with peripheral vascular disease 5‐year survival was 35% (P <0.001).

Conclusions

Integrated care for the diabetic foot in one National Health Service (NHS) health service area over 18 years was associated with a reduction in first presentations of diabetic foot ulceration, but failed to reduce recurrent ulceration. Cumulative prevalence of all ulcers continues to increase. Monitoring ulceration incidence can inform audit and planning of diabetic foot care services. Survival is better than reported previously in persons < 65 years and in the absence of peripheral vascular disease.
Left atrial compliance index predicts exercise capacity in patients with heart failure and preserved ejection fraction irrespective of right ventricular dysfunction
Authors: Bytyci Ibadete , Bajraktari Gani , Fabiani Iacopo , Lindqvist Per , Poniku Afrim , Pugliese Nicola Riccardo , Dini Frank L. , Henein Michael Y.
Published: May 2019

Background and Aim

Predictors of exercise capacity in heart failure (HF) with preserved ejection fraction (HFpEF) remain of difficult determination. The aim of this study was to identify predictors of exercise capacity in a group of patients with HFpEF and right ventricle (RV) dysfunction

Methods

In 143 consecutive patients with HFpEF (age 62 ± 9 years, LV EF ≥45) and 41 controls, a complete echocardiographic study was performed. In addition to conventional measurements, LA compliance was calculated using the formula: [LAV max − LAV min/LAV min × 100]. Exercise capacity was assessed using the six‐minute walking test (6‐MWT). Tricuspid annular plane systolic excursion (TAPSE) < 1.7 cm was utilized to categorize patients with RV dysfunction (n = 40) from those with maintained RV function (n = 103).

Results

Patients with RV dysfunction were older (P = 0.002), had higher NYHA class (P = 0.001), higher LV mass index (P = 0.01), reduced septal and lateral MAPSE (all P < 0.001), enlarged LA (P = 0.001) impaired LA compliance index (P < 0.001) and exhibited a more compromised 6‐MWT (P = 0.001). LA compliance index correlated more closely with 6‐MWT (r = 0.51, P < 0.001) compared with the other LA indices (AP diameter, transverse diameter and volume indexed; r = −0.30, r = −0.35 and r = −0.38, respectively). In multivariate analysis, LA compliance index <60% was 88% sensitive and 61% specific (AUC 0.80, CI = 0.67–0.92 P = 0.001) in predicting exercise capacity.

Conclusion

An impairment in LA compliance was profound in patients with HFpEF and RV dysfunction and seems to be most powerful independent predictor of limited exercise capacity.
STRUCTURAL ESTIMATION OF LABOR ADJUSTMENT COSTS WITH TEMPORALLY DISAGGREGATED DATA
Authors: Yaman Firat
Published: May 2019

I estimate a dynamic optimization model of labor adjustment of establishments based on data that permit: specifying any desired adjustment frequency; estimating the model based on net and on gross employment flows; and allowing for simultaneous hirings and separations. The unit of observation is an establishment. Results for adjustment costs depend crucially on the model specification. Only a monthly adjustment model yields cost parameters in a reasonable range, while estimates from quarterly and annual adjustment models imply negative or excessive adjustment costs. Estimating the model on net employment changes implies hiring and separation costs of four annual median salaries, while the model on gross changes implies costs on the order of 1.7 annual median salaries. (JEL C25, D22, J23)