Статті в журналах: "Western imprints"

1

Chen, Yunfeng, Yu Jeffrey Gu, Ramin M. H. Dokht, and Mauricio D. Sacchi. "Crustal imprints of Precambrian orogenesis in western Laurentia." Journal of Geophysical Research: Solid Earth 120, no. 10 (October 2015): 6993–7012. http://dx.doi.org/10.1002/2014jb011353.

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2

Winterscheid, Heinrich. "Revision of a late Oligocene florule from the south-western edge of the Lower Rhine Basin (western Germany)." Acta Palaeobotanica 58, no. 1 (June 1, 2018): 49–60. http://dx.doi.org/10.2478/acpa-2018-0004.

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AbstractThe late Oligocene flora from the Nirmer Tunnel at the south-western edge of the Lower Rhine Basin was first described by Menzel (1913). A revision of Menzel’s original material indicates that most taxa are from the vegetation of riparian forests (Magnolia burseracea, Ocotea rhenana, Rhodoleia bifollicularis, Eotrigonobalanus furcinervis, Trigonobalanopsis rhamnoides, Sparganium sp. vel Typha sp.) and mesophytic forests (Carpolithes dactyliformis, Sapotacites minor). Some specimens cannot be identified, so they are named Dicotylophyllum div. spp. here. The fossil species Carpolithes dactyliformis (sandstone imprints and endocasts) belongs to Cornaceae subfamily Mastixioideae and is lectotypified here. The floral assemblage is compared with some similar floras from the Oligocene of Central Europe.

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3

Kormazina, Olga P., Dmitry A. Ruban, and Natalia N. Yashalova. "Hotel Naming in Russian Cities: An Imprint of Foreign Cultures and Languages between Europe and Asia." Societies 12, no. 2 (March 30, 2022): 58. http://dx.doi.org/10.3390/soc12020058.

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Hotel naming can contribute to cultural exchange, and big countries boasting lengthy peripheries and sharp “cores” are suitable for studying this contribution. Foreign cultural and linguistic imprints in hotel names is studied in four big cities of Russia, namely Rostov-on-Don, Nizhniy Novgorod, Krasnoyarsk, and Vladivostok. It is established that the hotels with names bearing foreign-culture elements constitute up to 20–25% of all hotels in each given city. These elements can be linked to many, chiefly West European countries. The English foreign-language elements are the most common, whereas the French and Italian elements occur in subordinate numbers. The linguistic-cultural types of the hotel names are commonly toponyms and landscape-related symbols. The imprint of foreign cultures and languages in the hotel names diminishes together with the increase in distance from the western state border.

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4

Orlova, O. A., Al V. Tevelev, D. A. Mamontov, and E. V. Anikeeva. "The Upper Carboniferous lycopsids of the locality Karantrav (Southern Urals)." Moscow University Bulletin. Series 4. Geology, no. 6 (December 28, 2016): 28–36. http://dx.doi.org/10.33623/0579-9406-2016-6-28-36.

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Numerous plant remains were first found in the Upper Carboniferous of Western slope of the Southern Urals (locality Karantrav). Plant remains are represented by cone and stem lycopsid imprints, and sporadical stem imprints of arthrophytes. A brief stratigraphic characteristic of the studied locality is given. Studied plant assemblage are represented by Lepidodendron ophiurus Brongniart, L. vaselgense Anikeeva et O. Orlova, sp. nov., Lepidodendron. sp., Lepidostrobus tevelevii O. Orlova, Mamontov et Anikeeva, sp. nov., L. ronnaensis Bek et Oplustil, Knorria sp., Calamites sp. и Mesocalamites ramifer (Stur) Hirmer. In-situ microspores of Lycospora-type were discovered in the sporangia of some strobili of genus of Lepidostrobus. Four lycopsid species (two are new) were described.

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5

Codrea, V., Ο. Barbu, and H. Bedelean. "MIDDLE MIOCENE DIATOMITE- BEARING FORMATIONS FROM WESTERN ROMANIA." Bulletin of the Geological Society of Greece 40, no. 1 (June 8, 2018): 21. http://dx.doi.org/10.12681/bgsg.16329.

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In Western Romania diatomite occurs only in the Lower Sarmatian (Middle Miocene) formations, as a consequence of intense volcanism developed in Apuseni Mountains and evolution of peculiar sedimentary basins connected to the Pannonian realm. The main basins with diatomite successions are Zar and and VadBorod. The diatomite preserves besides diatoms (centric and pennate) and other microfossils (dinoflagellates, ebriidinas, silicoflagellates, phytolites) assemblages a lot of macrofossils as plants (mainly foliar imprints), fish, reptiles and mammals. Several taxa are indicative for environment reconstruction. The Lower Sarmatian climate is estimate as wet warm temperate to subtropical. A tentative of both aquatic and land environments reconstruction is done.

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6

Abbassi, Nasrollah, and Saeed Madanipour. "Dinosaur tracks from the Jurassic Shemshak Group in the Central Alborz Mountains (Northern Iran)." Geologica Carpathica 65, no. 2 (April 1, 2014): 99–115. http://dx.doi.org/10.2478/geoca-2014-0007.

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Abstract The Shemshak Group includes alternating layers of coal-bearing shale and siliciclastic sediments in the Baladeh area in the central Alborz Mountains of northern Iran. A diverse and abundant Jurassic dinosaur footprint assemblage is now recognized in the group, which is Toarcian to Bajocian in age in the northern Baladeh. This is the first report of a diverse dinosaur ichnoassemblage from Iran that includes the footprints of sauropods. These tracks can be assigned to three groups of trackmakers: theropods, ornithopods and sauropods. Those of theropods are typically tridactyl in shape, their trackways reflecting bipedal movement. Theropod footprints are very abundant in both northern and western Baladeh. The studied theropod tracks themselves are divided into three major dimensional groups. The medium sized footprints (footprint length, 11-15 cm) are abundant and have a stride length, digit and pace angles like the coelurosaurs footprints and trackway. Theropod footprints were identified as similar to Schizograllator otariensis, Talmontopus tersi and Wildeichnus isp. Ornithopod footprints are tridactyl with rounded and thick toes and belong to bipeds. Some didactyl imprints were also observed. Skin imprints were well preserved in these footprints. The ornithopod tracks resemble Jiayinosorupus johnsoni, as well as Velociraptorichnus sichuanensis for didactyl footprints. Sauropod footprints found in the western part of Baladeh are assigned here to Eosauropus isp., which are pentadactyl pes imprints of a quadruped. The assemblage from Iran resembles similar associations from eastern Asia.

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7

Lindow, Bent E. K., and Gareth J. Dyke. "A small galliform bird from the Lower Eocene Fur Formation, north-western Denmark." Bulletin of the Geological Society of Denmark 55 (March 12, 2007): 59–63. http://dx.doi.org/10.37570/bgsd-2007-55-04.

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A pair of fossilized imprints of feet represent the first published galliform (landfowl) specimenfrom the Lower Eocene Fur Formation of northwest Denmark. The specimen is referable to Galliformes due to the presence of a distinctly asymmetric trochlea metatarsi III. The specimen appears distinct from previously described Eocene Galliformes (e.g. Gallinuloididae, Quercymegapodiidae and Paraortygidae) and may represent a new taxon of Galliformes, increasing the diversity of this group in the Lower Eocene.

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8

Lazarevic, Zorica, Ljubica Milovanovic, Jelena Milivojevic, and Ivana Vasiljevic. "Palaeoflora of Kamenica (Pranjani basin, western Serbia)." Annales g?ologiques de la Peninsule balkanique 80, no. 2 (2019): 53–63. http://dx.doi.org/10.2298/gabp1902053l.

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Palaeofloras of the Paleogene in Serbia are relatively rare, especially in comparison with floras from Neogene sediments. Most Paleogene phytoassociations from the territory of Serbia existed in a dry and warm climate. The youngest Paleogene phytoassociation originates from the Pranjani Basin (Western Serbia), locality Kamenica. The age of this palaeoflora is determined as Late Oligocene. This fossil plant assemblage is different from other Paleogene phytoassociations. The palaeoflora from Kamenica is characterized with leaf imprints larger than in other Paleogene fossil floras. Furthermore, it differs in taxonomical composition. The prevailing forms are conifers and representatives of broad-leaved evergreen forests. In other Paleogene phytoassociations, elements of broad-leaved evergreen forests are extremely rare. The dominating elements in the palaeoflora of Kamenica are the conifers, especially Glyptostrobus, Pinus, Sequoia and Tetraclinis. The representatives of the broad-leaved evergreen forests are Laurus, Magnolia, ?Quercus?, etc.

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9

Gera, Parshotam K., Andrew P. Barker, Ian Gollow, Jillian Orford, Sue Wicks, and Liz Whan. "Bicycle handlebar injuries in Western Australia: from imprints to abdominal wall hernias." Medical Journal of Australia 189, no. 5 (September 2008): 295. http://dx.doi.org/10.5694/j.1326-5377.2008.tb02037.x.

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10

Schenker, F. L., M. G. Fellin, and J. P. Burg. "Polyphase evolution of Pelagonia (northern Greece) revealed by geological and fission-track data." Solid Earth Discussions 6, no. 2 (November 10, 2014): 3075–109. http://dx.doi.org/10.5194/sed-6-3075-2014.

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Abstract. The Pelagonian zone, between the External Hellenides/Cyclades to the west and the Axios/Vardar/Almopia zone (AVAZ) and Rhodope to the east, was involved in late Early Cretaceous and in Late Cretaceous-Eocene orogenic events whose duration are still controversial. This work constrains their late thermal imprints. New and previously published zircon (ZFT) and apatite (AFT) fission-track ages show cooling below 240°C of the metamorphic western AVAZ imbricates between 102 and 93–90 Ma, of northern Pelagonia between 86 and 68 Ma, of the eastern AVAZ at 80 Ma and of western Rhodope at 72 Ma. At the regional scale, this heterogeneous cooling is coeval with subsidence of Late Cretaceous marine basin(s) that unconformably covered since 100 Ma the Early Cretaceous (130–110 Ma) thrust system. Thrusting restarted at 70 Ma in the AVAZ and migrated across Pelagonia to reach the External Hellenides at 40–38 Ma. Renewed thrusting in Pelagonia is attested at 68 Ma by abrupt and rapid cooling below 240°C and erosion of the basement rocks. ZFT and AFT in western and eastern Pelagonia, respectively, set at 40 Ma the latest thermal imprint related to thrusting. Central-eastern Pelagonia cooled rapidly and uniformly from 240 to 80°C between 24 and 16 Ma in the footwall of a major extensional fault. Extension started even earlier, at 33 Ma in the western AVAZ. Post-7 Ma rapid cooling is inferred from inverse modeling of AFT lengths. It occurred while E–W normal faults were cutting Pliocene-to-recent sediment.

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11

Schenker, F. L., M. G. Fellin, and J. P. Burg. "Polyphase evolution of Pelagonia (northern Greece) revealed by geological and fission-track data." Solid Earth 6, no. 1 (February 25, 2015): 285–302. http://dx.doi.org/10.5194/se-6-285-2015.

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Abstract. The Pelagonian zone, situated between the External Hellenides/Cyclades to the west and the Axios/Vardar/Almopias zone (AVAZ) and the Rhodope to the east, was involved in late Early Cretaceous and in Late Cretaceous–Eocene orogenic events whose duration and extent are still controversial. This paper constrains their late thermal imprints. New and previously published zircon (ZFT) and apatite (AFT) fission-track ages show cooling below 240 °C of the metamorphic western AVAZ imbricates between 102 and 93–90 Ma, of northern Pelagonia between 86 and 68 Ma, of the eastern AVAZ at 80 Ma and of the western Rhodope at 72 Ma. At the regional scale, this heterogeneous cooling is coeval with subsidence of Late Cretaceous marine basin(s) that unconformably covered the Early Cretaceous (130–110 Ma) thrust system from 100 Ma. Thrusting resumed at 70 Ma in the AVAZ and migrated across Pelagonia to reach the External Hellenides at 40–38 Ma. Renewed thrusting in Pelagonia is attested at 68 Ma by abrupt and rapid cooling below 240 °C and erosion of the gneissic rocks. ZFT and AFT in western and eastern Pelagonia, respectively, testify at ~40 Ma to the latest thermal imprint related to thrusting. Central-eastern Pelagonia cooled rapidly and uniformly from 240 to 80 °C between 24 and 16 Ma in the footwall of a major extensional fault. Extension started even earlier, at ~33 Ma in the western AVAZ. Post-7 Ma rapid cooling is inferred from inverse modeling of AFT lengths. It occurred while E–W normal faults were cutting Pliocene-to-recent sediment.

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12

Yadav, R. R. "Tree ring imprints of long-term changes in climate in western Himalaya, India." Journal of Biosciences 34, no. 5 (November 2009): 699–707. http://dx.doi.org/10.1007/s12038-009-0058-7.

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13

Bradic-Milinovic, Katarina, Dragana Djuric, Nevenka Djeric, Ivana Petrovic, Nemanja Krstekanic, and Uros Stojadinovic. "First record of fossil fish (Enchodontoidei, Actinopterygii) in the Struganik quarry in Western Serbia." Annales g?ologiques de la Peninsule balkanique, no. 00 (2022): 8. http://dx.doi.org/10.2298/gabp221021008b.

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This paper presents the first Upper Cretaceous remains of fish in Serbia, discovered near the village of Struganik. This is also the first described find of Mesozoic fish in Serbia. A stone slab with visible contours of an almost complete fish, with a total body length of about 20 cm, was excavated from the Struganik quarry. Most bones are preserved as imprints. The number of vertebrae, the shape and position of the cranial bones, the type of teeth, and the position of the first dorsal fin all indicate that the studied specimen belongs to the genus Enchodus known from several Upper Cretaceous localities in the Tethys domain.

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14

K., KIRYUSHIN, and KIRYUSHIN Yu. "CERAMICS OF THE PESTRYAKOVO LAKE SETTLEMENT (SOUTH OF WESTERN SIBERIA)." Preservation and study of the cultural heritage of the Altai Territory 27 (2021): 205–12. http://dx.doi.org/10.14258/2411-1503.2021.27.32.

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The article is devoted to the publication of finds of fragments of ceramic dishes discovered at the settlement of Pestryakovo Lake (Zavyalovsky district of Altai Territory). A group of ceramics which belongs to the early Iron Age and the Middle Ages, is pointed out. Single fragments find analogies in the materials of the sites of the Early and Late Bronze Age. The ceramic collection of the Pestryakovo Lake settlement includes groups of ceramics that belong to the Neolithic or Eneolithic. These are fragments of vessels ornamented with prints of a “string”, pricks, imprints of a short comb stamp, a dingle-dingle stamping. Linear-pricked and receding-pricked ceramics are quite informative. On the outer and inner surfaces, as well as in the fractures, traces of burnt-out organic matter (animal hair) are recorded. Such ceramics are widely represented in the south of Western Siberia and are associated with various settlement and burial complexes from the Ob to the Irtysh and various cultural formations of the Neolithic and Eneolithic. Keywords: settlement, ceramics, ornamentation technique, comparative typological analysis, neolithic, eneolithic

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15

Solek, Vivian Lea. "Karen Nipps. Lydia Bailey: A Checklist of Her Imprints. University Park, Pa.: The Pennsylvania State University for the Bibliographical Society of America in association with the Houghton Library, Harvard University, and the Library Company of Philadelphia, 2013. xiii + 310 p. $79.95 (ISBN: 978-0-271-05571-8)." RBM: A Journal of Rare Books, Manuscripts, and Cultural Heritage 15, no. 1 (March 1, 2014): 77–78. http://dx.doi.org/10.5860/rbm.15.1.418.

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From a review of the earlier published scholarship in the field of printing history, an inquiring reader would surmise that women were not a significant part of commercial letterpress printing during the handpress period. Scholarship in the last 20 years, however, has revealed that this is not the case. In fact, many recent studies document women’s high degree of involvement from the earliest days of printing in the Western world.Lydia Bailey: A Checklist of Her Imprints is an important addition to the study of the history of the book and of women’s roles in letterpress printing. It is a . . .

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16

Jacobs, Joachim, and Alexander Golynsky. "Grenville-Age Versus Pan-African Magnetic Anomaly Imprints in Western Dronning Maud Land, East Antarctica." Gondwana Research 4, no. 4 (October 2001): 638–39. http://dx.doi.org/10.1016/s1342-937x(05)70441-x.

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17

Golynsky, A., and J. Jacobs. "Grenville‐Age versus Pan‐African Magnetic Anomaly Imprints in Western Dronning Maud Land, East Antarctica." Journal of Geology 109, no. 1 (January 2001): 136–42. http://dx.doi.org/10.1086/317964.

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18

Gutschick, Raymond C., and Joaquin Rodriguez. "By-the-wind-sailors from a Late Devonian foreshore environment in western Montana." Journal of Paleontology 64, no. 1 (January 1990): 31–39. http://dx.doi.org/10.1017/s0022336000042219.

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Three remarkable fossil medusoid hydrozoans (Plectodiscus latinautilus n. sp.) with disc, topsail, and pendant tentacular appendages were recovered from the latest Late Devonian beds of the Sappington Member of the Three Forks Formation in the Gallatin Range, southwest Montana. This is the first velellid reported from a Paleozoic beach paleoenvironment. Top and underside patterns of these chondrophorine velellids display well-preserved casts and mold imprints in fine siltstone. Outlines of the circular disc and the profile of the wide sail and tentacular structures embedded in soft tissue can be recognized.These floating colonial animals were moved along the southeast shores of the Sappington Basin during a time of eustatic sea level lowering and regression in a tropical setting. Colonies were washed up on the upper beach where they were stranded in the bubbling swash left behind by the surf. The foreshore was constructed of tabular, planar cross-bedded, seaward-dipping, foreset accretionary beds which contain parallel laminations and lime-coated grains. Bedding is inclined 17° to 24° seaward.

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19

Peterson, James W. "The Czech Republic in the World: Conflicting Loyalties, Organizational Memberships, and Changed National Images." Carl Beck Papers in Russian and East European Studies, no. 1907 (January 1, 2008): 39. http://dx.doi.org/10.5195/cbp.2008.144.

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Czech foreign policy in the post-Cold War period bears three significant imprints. First, a country that had been torn by conflicting loyalties solved that dilemma by firmly positioning itself in the orbit of the West. Second, NATO and the EU became the organizational anchors of that western orbit. Third, fresh images of the possibility of choice and control over history replaced past national images of submission to dependence and fate. Thus, new loyalties, organizations, and images interacted to create a different foreign policy chemistry. That chemistry could enable the Czech Republic to move from its protected Central European base to a purposeful international role in a proactive way.

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20

Sri Lakshmi, S., and R. K. Tiwari. "Wavelet analysis of the singular spectral reconstructed time series to study the imprints of Solar–ENSO–Geomagnetic activity on Indian climate." Nonlinear Processes in Geophysics Discussions 2, no. 5 (September 28, 2015): 1447–79. http://dx.doi.org/10.5194/npgd-2-1447-2015.

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Abstract. In order to study the imprints of solar–ENSO–geomagnetic activity on the Indian Subcontinent, we have applied the Singular Spectral Analysis (SSA) and wavelet analysis to the tree ring temperature variability record from the western Himalayas. The data used in the present study are the Solar Sunspot Number (SSN), Geomagnetic Indices (aa Index), Southern Oscillation Index (SOI) and tree ring temperature record from western Himalayas (WH), for the period of 1876–2000. The SSA and wavelet spectra reveal the presence of 5 years short term ENSO variations to 11 year solar cycle indicating the influence of both the solar–geomagnetic and ENSO imprints in the tree ring data. The presence of 33-year cycle periodicity suggests the Sun-temperature variability probably involving the induced changes in the basic state of the atmosphere. Our wavelet analysis for the SSA reconstructed time series agrees with our previous results and also enhance the amplitude of the signals by removing the noise and showing a strong influence of solar–geomagnetic and ENSO patterns throughout the record. The solar flares are considered to be responsible for cause in the circulation patterns in the atmosphere. The net effect of solar–geomagnetic processes on temperature record thus appears to be the result of counteracting influences on shorter (about 5–6 years) and longer (about 11–12 years) time scales. The present analysis thus suggests that the influence of solar processes on Indian temperature variability operates in part indirectly through ENSO, but on more than one time scale. The analyses hence provides credible evidence for teleconnections of tropical pacific climatic variability with Indian climate ranging from interannual-decadal time scales and also demonstrate the possible role of exogenic triggering in reorganizing the global earth–ocean–atmospheric systems.

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Pham, Manh Duc. "Dong Son Imprints in the South of Vietnam (research summary)." Science and Technology Development Journal 17, no. 4 (December 31, 2014): 13–35. http://dx.doi.org/10.32508/stdj.v17i4.1562.

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In the paper, the author reviews the most recent important archaeological discoveries with Dong Son bronze drums (Heger I) found from Highlands (Kontum, Gia Lai, DakLak, Lam Dong provinces), Southern Part of Central Vietnam (Quang Nam, Quang Ngai, Binh Dinh, Phu Yen, Khanh Hoa provinces) and Southern Vietnam (Binh Dương, Binh Phuoc, Ba Ria-Vung Tau, Ben Tre, Kien Giang provinces). The author points out “key sites” in the South Vietnam – the typical sites and artifacts most lively showing “the convergance of Indigenous - Exogenous culture” in ancient villages, workshops for metallurgy, cemeteries, treasures, etc., which are related to the Dong Son and other inhabitants of the protohistorical epoch in Vietnam and Southeast Asia and beyond. There are Cemeteries or Tresors which contained Bronze Dong Son drums (Heger I type), bronze halberds (Ko), Western Han mirrors, Indian Nephrite or Glass and Golden Ornaments – artifacts not only representing the multi-linear relationship of the owners of Southern Vietnam with other Asian centres, but also were considered to be the symbol of power, authority, potential of military and polical function, social ranks and they reflected the unpeaceful situation of the contemporary society. The author emphasizes the very appearance of these Dongson drums as shown with 2 subtypes of Bronze Drum Collections: Original Dong Son (Heger I) Bronze Drum Collection and Imitative Bronze Drum Collection which was created according to "Dongsonian Style" thousands of years ago. The author emphasizes the very early appearance of the “exogenous” elements of culture-technique-art-religion in Southern Vietnam, which were adapted or completely modified to match the knowledge and psychology, aesthetic needs, and “Indigenous” beliefs – especially clear in traditional funeral concept thousands of years ago, as shown with distinction in “chiefdom cemetery”. Finallly, the author generalized data related to Bronze metallurgy at the Southern Vietnam area and came to some following remarks: 1/ Nam Bo - Vietnam was the early centre of Bronze Metallurgy at the Mainland Asia in the Proto-history, with the technology of casting in sandstone moulds. 2/ This Bronze casting industry together with its copper and alloy materials probably came from “Native land of Dong Son culture” – the “Bronze Triangle” or “Bronze Quadrilateral”: Dong Son – Yunnan – Guangxi – Guangdong – Khorat. Through various ways: directly via the East Sea to the South of Vietnam or indirectly through roads – via Sa Huynh cultural area and Tay Nguyen (Highlands) along the Mekong River to the South of Vietnam in the end. 3/ However, the southern metallurgy had their “own features” that were considered “non-Dong Son” by the author. The big and sophisticated bronze products such as Dong Son drums (Heger I type) or Chinese halberd (Ko or halberd), Art figurines such as statues of a pangolin (Manis javanica) or Amulets, statues depicting a dog chasing another animal, etc. only appeared in the Early Iron Age. Apart from some exotic intact goods such as Dong Son drums from Son Tinh, Daglao, Ben Tre, Bu Dang etc. and Western Han mirrors from Binh Yen, Go Dua, Phu Chanh, Kem Nac, most of the bronze products in the Early Iron Age in the South of Vietnam were cast on site, with their own characteristics that were “non-Dong Son” and “non-Chinese”. 4/ According to the author, the large bronze object like Dong Son – styled drums or “Ko” appeared a lot here to the regalia expressing power of the Bigmen (the leaders) in the early historical period in the South of Vietnam and they were just replaced in the early Christian Era under the influence of Indian civilization – process by which French scholars call “Hinduism” and “Buddhism”.

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Kim, Sung Won, Deung-Lyong Cho, Seung-Bae Lee, Sanghoon Kwon, Seung-Ik Park, M. Santosh, and Weon-Seo Kee. "Mesoproterozoic magmatic suites from the central-western Korean Peninsula: Imprints of Columbia disruption in East Asia." Precambrian Research 306 (March 2018): 155–73. http://dx.doi.org/10.1016/j.precamres.2017.12.038.

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23

Zinke, J., M. Pfeiffer, O. Timm, W. –C Dullo, and G. R. Davies. "Atmosphere–ocean dynamics in the Western Indian Ocean recorded in corals." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 363, no. 1826 (January 15, 2005): 121–42. http://dx.doi.org/10.1098/rsta.2004.1482.

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We present a set of Porites coral oxygen isotope records from the tropical and subtropical Western Indian Ocean covering the past 120–336 years. All records were thoroughly validated for proxy response to regional climate factors and their relation to large–scale climate modes. The records show markedly different imprints of regional climate factors. At the same time, all coral records show clear teleconnections between the Western Indian Ocean and the El Niño–Southern Oscillation (ENSO). The multi–proxy site analysis enables the detection of the covariance structure between individual records and climate modes such as ENSO. This method unravels shifts in ENSO teleconnectivity of the Western and Central Indian Ocean on multi–decadal time–scales (after 1976). The Seychelles record shows a stationary correlation with ENSO, Chagos corals show evidence for non–stationary d 18 O/ENSO relationships and the Southwestern Indian Ocean corals show a strong relationship with ENSO when the forcing is strong (1880–1920, 1970 to present). Our results indicate that the coral δ 18 O, in combination with other proxies, can be used to monitor temporal and spatial variations in the sea–surface temperature and the fresh water balance within the Indian Ocean on interannual to interdecadal time–scales.

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Beuthe, Tatjana. "New Insights into the Step Pyramid Complex: Klasens’ Unpublished Seal Impression Drawings." Journal of Egyptian Archaeology 105, no. 1 (June 2019): 135–41. http://dx.doi.org/10.1177/0307513319889333.

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The Egypt Exploration Society archive contains unpublished pencil drawings by A. Klasens of seal impressions found in the Step Pyramid complex of Saqqara. Digitally inked versions of these drawings are published here for the first time. The seal impressions can be sourced to the Northern Galleries of the complex. The impressions were sealed on clay formerly plastered on a wall, and also bore the imprints of the end(s) of cylinder seals. To explain the presence of seal impressions of Khasekhemwy among the sealings drawn by Klasens, an attempt is made to trace the construction and use history of the Northern Galleries and the contemporary Western Galleries. Possible parallels between some of the Step Pyramid sealings and Beit Khallaf sealings are also discussed.

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Goutiers, Vladimir, and Christopher Carcaillet. "Geochemistry and Sedimentology of a Minerotrophic Peat in a Western Mediterranean Mountain Wilderness Area." Quaternary 5, no. 4 (November 21, 2022): 48. http://dx.doi.org/10.3390/quat5040048.

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Sedimentological and biogeochemical measurements were conducted on minerotrophic peat in a wilderness area on a granitic plateau to reconstruct the local ecosystem’s history and clarify the peat’s response to local and global changes. The peat is less than 1900 years old. Its clay and iron (Fe) concentration profiles revealed an increasing atmospheric influx over time, whereas the levels of its nutrients (P, K, Ca, Mg) have increased since the 19th century. Additionally, changes in the relative abundance of amorphous aluminium indicated a gradual decrease in soil weathering. The dominant metallic trace elements were cadmium during the Roman epoch and early Middle Ages, then lead and mercury during the modern and the industrial eras. Unexpectedly, the peat proved to be sub-modern and lacks wildfire proxies, probably indicating an absence of nearby woodlands over the last 1900 years. Its concentrations of Ca and Mg indicate that airborne transport of particles released by soil erosion in lowland agricultural plains has strongly affected the peat’s composition since the 18th–19th century. The site has also been heavily influenced by metallic contamination due to regional metallurgy and agriculture, producing a peat that has been modified by social imprints over several centuries.

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Sharma, Vijay, and Aditya Kumar Verma. "Lithological variations and drainage evolution in a marginal region: A case study from Chandrapur block of the Pranhita-Godavari Basin, Central India." Journal of The Indian Association of Sedimentologists 37, no. 2 (December 31, 2020): 103–14. http://dx.doi.org/10.51710/jias.v37i2.102.

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Field mapping and interpretation of sedimentary structures in Gojoli region of Chandrapur block along the eastern margin of the Pranhita-Godavari valley suggests westward flowing channels during the Neoproterozoic. Present channels in this part of Chandrapur block are south/ southeast flowing and possess clear imprints of the basin-margin faults and lineaments. Drainage parameters in its Neoproterozoic stratigraphic sequence suggest impervious substrates probably due to high degree of consolidation and filling of rock-fractures by hydrothermal solution activities. However, the same for the Gondwana’s friable sandstone (towards western region) and Archaean gneisses (in the eastern part) has been observed consistent probably due to its porous nature and development of thick weathering profile. The affiliation of drainage with tectonism is therefore, from Neoproterozoic to Cenozoic era within contrasting lithology, was out of synchronization intermittently.

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27

Grisha, E. A. "Book monument imprint: Identifying via foreign information resources." Scientific and Technical Libraries, no. 10 (November 12, 2021): 131–48. http://dx.doi.org/10.33186/1027-3689-2021-10-131-148.

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The author reviews foreign science publication, websites, digital databases, catalogs and methods to be used to specify imprints of book monuments and their history as exemplified by 16-th century collection of Russian Academy of Arts Library. The collection comprises over 60 books published in Western Europe; with the special attention to the collection in architecture, in particular books published by Sebastiano Serlio (1475 – c. 1554). To attribute the publications, the catalogs of foreign museums and libraries, bibliographic, fulltext, factographic and objectographic databases in the art market, e. g. ArtPrice, MutualArt, Invaluable, were used to reveal various guides in 16-th century architecture, catalogs of private collections, and auction sale catalogs. The author discusses the methods to use the identified sources to attribute book monuments, as exemplified by Sebastiano Serlio’s books in architecture, and to investigate into this area further.

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Majumdar, Satabdwa, Ritesh Patel, Vaibhav Pant, Dipankar Banerjee, Aarushi Rawat, Abhas Pradhan, and Paritosh Singh. "A Coronal Mass Ejection Source Region Catalog and Their Associated Properties." Astrophysical Journal Supplement Series 268, no. 1 (September 1, 2023): 38. http://dx.doi.org/10.3847/1538-4365/aceb62.

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Abstract The primary objective of this study is to connect coronal mass ejections (CMEs) to their source regions, primarily to create a CME source region catalog, and secondarily to probe the influence that the source regions have on the different statistical properties of CMEs. We create a source region catalog for 3327 CMEs from 1998 to 2017, thus capturing the different phases of cycles 23 and 24. The identified source regions are segregated into three classes—active regions, prominence eruptions, and active prominences—while the CMEs are segregated into slow and fast groups, based on their average projected speeds. We find the contributions of these three source region types to the occurrences of slow and fast CMEs to be different in the above period. A study of the distribution of the average speeds reveals different power laws for CMEs originating from different sources, and the power laws are different during the different phases of cycles 23 and 24. A study of the statistical latitudinal deflections shows equatorward deflections, while the magnitudes of the deflections again bear imprints of the source regions. An east–west asymmetry is also noted, particularly in the rising phase of cycle 23, with the presence of active longitudes for the CMEs, with a preference toward the western part of the Sun. Our results show that different aspects of CME kinematics bear strong imprints of the source regions they originate from, thus indicating the existence of different ejection and/or propagation mechanisms of these CMEs.

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Mavroulis, Spyridon, Marilia Gogou, and Efthymios Lekkas. "Earthquake-Induced Tsunamis in Western Greece (Ionian Sea and Western and Southern Peloponnese): Use of Tsunami Quantities, Impact and ITIS-2012 Intensities for Highlighting Susceptible Areas." Geosciences 13, no. 2 (January 25, 2023): 28. http://dx.doi.org/10.3390/geosciences13020028.

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Taking into account recent studies on the tsunamigenic potential of strike-slip faults, it is concluded that there is a need to reassess their near-source tsunami hazard and risk. One of the areas which needs reassessment is Western Greece, especially the Ionian Islands and the western coastal Peloponnese, where major seismogenic strike-slip structures occur. In this context, an extensive review of the available literature is conducted, including not only earthquake and tsunami catalogues but also tsunamis’ imprints on the stratigraphic record. It is concluded that the Ionian Islands and the western Peloponnese have a rich history of tsunamis since 6000 BC, revealing that they are subjected to high tsunami hazard. In addition to the teletsunami effects of distant earthquakes, there are also local tsunamis with smaller physical quantities and slighter coastal impact that are attributed mainly to local offshore faults and earthquake-triggered landslides. The fact that no destructive local tsunamis have been detected so far does not exclude the possibility of future triggering. In order to identify areas susceptible to future tsunami impact, we extract tsunami quantities and coastal impact data from available sources and we apply the Integrated Tsunami Intensity Scale 2012 (ITIS-2012) for all the events with available and adequate information. The highly susceptible areas comprise straits, funnel-shaped bays and extensive coastal areas exposed to major strike-slip seismogenic sources in the Ionian Sea and the western Hellenic Trench. Based on the aforementioned information, the inclusion of the Ionian Sea in the tsunamigenic zones of Greece is strongly recommended.

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Sara Amber and Dr Shahid Rasool. "WESTERN POETIC INFLUENCES ON MAJEED AMJAD'S POETRY." Tasdiqتصدیق۔ 4, no. 2 (January 10, 2023): 245–65. http://dx.doi.org/10.56276/tasdiq.v4i2.129.

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Majeed Amjad is a great poet of the 20th century who primarily loved his fellow humans, and who expressed this love through his account of deep affection for nature. His poetic grandeur has long been denied, and his artistic status has not been acknowledged the way he deserved it, yet he continued working his own way. Despite facing serious financial hardships, he utilized his artistic abilities aptly and stamped an unerasable shadow of his artistic self on Urdu Literature that will remain with it till the point time this literature will exist. Majeed Amjad, who had been ignored through the efforts of belittling, receives strong impressions of what is all around him and also he gets influenced by the poets and literary artists of the West. As a result of it, he produced such works of art that were apparently seen as derived from the western art canon. Despite western influence, his work stands alone as of independent stature without any blame for plagiarism or even for flat production of copying foreign content. The present work will investigate the western influence and its imprints upon the poetry of Majeed Amjad, and we will try to understand those nooks and corners of his poetry which are not much known to a systematic critical investigation to date. This research, hence, will open up new pathways for fresh researchers who would invest their critical insight into Amjad’s such poetic interpretations that have remained under surface. Through the present research, we will try to introduce a renewed Majeed Amjad who, despite having been influenced by the western artistic tradition, remained successful in establishing his own independent artistic identity. In our present investigative attempt, we will also explore his artistic independence by looking at whether he succeeded not in establishing his own voice even after absorbing western influence. This research will primarily engage such questions for the consequent debate in the analytical chapters. Hence, after critically looking at western poetic influence on Amjad’s work, this research will introduce the reader to a new Majeed Amjad who had a unique identifying accent that had been unknown till now.

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Tartarotti, Paola, Silvana Martin, Andrea Festa, and Gianni Balestro. "Metasediments Covering Ophiolites in the HP Internal Belt of the Western Alps: Review of Tectono-Stratigraphic Successions and Constraints for the Alpine Evolution." Minerals 11, no. 4 (April 14, 2021): 411. http://dx.doi.org/10.3390/min11040411.

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Ophiolites of the Alpine belt derive from the closure of the Mesozoic Tethys Ocean that was interposed between the palaeo-Europe and palaeo-Adria continental plates. The Alpine orogeny has intensely reworked the oceanic rocks into metaophiolites with various metamorphic imprints. In the Western Alps, metaophiolites and continental-derived units are distributed within two paired bands: An inner band where Alpine subduction-related high-pressure (HP) metamorphism is preserved, and an outer band where blueschist to greenschist facies recrystallisation due to the decompression path prevails. The metaophiolites of the inner band are hugely important not just because they provide records of the prograde tectonic and metamorphic evolution of the Western Alps, but also because they retain the signature of the intra-oceanic tectono-sedimentary evolution. Lithostratigraphic and petrographic criteria applied to metasediments associated with HP metaophiolites reveal the occurrence of distinct tectono-stratigraphic successions including quartzites with marbles, chaotic rock units, and layered calc schists. These successions, although sliced, deformed, and superposed in complex ways during the orogenic stage, preserve remnants of their primary depositional setting constraining the pre-orogenic evolution of the Jurassic Tethys Ocean.

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WEN, W., S. X. HU, Q. Y. ZHANG, M. J. BENTON, J. KRIWET, Z. Q. CHEN, C. Y. ZHOU, T. XIE, and J. Y. HUANG. "A new species of Platysiagum from the Luoping Biota (Anisian, Middle Triassic, Yunnan, South China) reveals the relationship between Platysiagidae and Neopterygii." Geological Magazine 156, no. 4 (February 12, 2018): 669–82. http://dx.doi.org/10.1017/s0016756818000079.

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AbstractFour complete platysiagid fish specimens are described from the Luoping Biota, Anisian (Middle Triassic), Yunnan Province, southwest China. They are small fishes with bones and scales covered with ganoine. All characters observed, such as nasals meeting in the midline, a keystone-like dermosphenotic, absence of post-rostral bone, two infraorbitals between dermosphenotic and jugal, large antorbital, and two postcleithra, suggest that the new materials belong to a single, new Platysiagum species, P. sinensis sp. nov. Three genera are ascribed to Platysiagidae: Platysiagum, Helmolepis and Caelatichthys. However, most specimens of the first two genera are imprints or fragmentary. The new, well-preserved specimens from the Luoping Biota provide more detailed anatomical information than before, and thus help amend the concept of the Platysiagidae. The Family Platysiagidae was previously classed in the Perleidiformes. Phylogenetic analysis indicates that the Platysiagidae is a member of basal Neopterygii, and its origin seems to predate that of Perleidiformes. Moreover, platysiagid fishes are known from the Middle Triassic of the western Tethys region. The newly found specimens of platysiagids from Luoping provide additional evidence that both eastern and western sides of the Tethys Ocean were biogeographically more connected than previously thought.

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Yunus, Ali P., Takashi Oguchi, and Yuichi S. Hayakawa. "Remote identification of fluvial knickzones and their imprints on landscape morphology in the passive margins of Western Arabia." Journal of Arid Environments 130 (July 2016): 14–29. http://dx.doi.org/10.1016/j.jaridenv.2016.02.016.

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34

Biswas, Mery, Adrija Raha, Soumyajit Mukherjee, and Vinit Shailesh Kotak. "Geomorphic Imprints of Active Tectonics of the Bikaner-Nagaur Petroliferous Rift Basin and its Surroundings (Western Rajasthan, India)." Journal of the Geological Society of India 100, no. 3 (March 1, 2024): 377–90. http://dx.doi.org/10.17491/jgsi/2024/173844.

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Abstract Geology of sedimentary rift-basins require strong geomorphic input for a proper interpretation of active tectonics. Rift-related sedimentation took place in western Rajasthan of the Indian shield, which includes the Bikaner-Nagaur basin (BNB) and a few other adjacent basins. The sedimentation history of the BNB includes Proterozoic, Cambrian, Permo-Carboniferous and from Paleocene to the Recent. This study analyses river profiles with the best-fit curve (R2) model for the BNB and the surrounding regions. The research shows that the watershed 3 within the study area is most active tectonically, through which multiple faults and lineaments pass. Hypsometric Curves (HCs) of watersheds 1, 2 and 3 indicate that these watersheds are tectonically active. This inference is based on the concave profiles of HCs at the head, and convex profiles of HCs at the body and toe sections. Clustering of sixty segments (S) of the considered rivers based on linear-scale morphometric parameters, e.g., sinuosity index (SI), stream length gradient index (SL) and concavity (θ) enabled segment-wise comparison of river profiles with similar values. These segments were compared pair-wise, and Euclidean-based dissimilarity (dR) values were calculated between each such pair. The findings too imply that tectonic activeness exists in parts of watersheds 1, 2 and 3. The channel flow lines are controlled by faults/lineaments as per the micro-scale examination of the drainage network and faults/ lineaments analysis. Under structural control, nine major geomorphic units emerged with distinct erosional surfaces, denudational hillocks, dissected hills and inselbergs. Detailed geomorphic map with micro-scale studies revealed a slope retreat process that resulted in landforms viz., pediment, pediment slope and active flood plains.

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Omar, Abdalla A., Fadhil A. Lawa, and S. H. Sulaiman. "Tectonostratigraphic and structural imprints from balanced sections across the north-western Zagros fold-thrust belt, Kurdistan region, NE Iraq." Arabian Journal of Geosciences 8, no. 10 (January 30, 2015): 8107–29. http://dx.doi.org/10.1007/s12517-014-1682-6.

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36

Emenike, P. C., C. C. Nnaji, I. T. Tenebe, and J. C. Agunwamba. "Hydrogeochemical imprints and spatio-temporal health risk assessment of lead in drinking water sources of Abeokuta, south-western Nigeria." International Journal of Environmental Science and Technology 17, no. 1 (August 16, 2019): 343–60. http://dx.doi.org/10.1007/s13762-019-02506-0.

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37

Staneva, Krasimira. "PALEONTOLOGICAL HERITAGE RESOURCES FOR TOURISM IN BULGARIA." Knowledge International Journal 28, no. 7 (December 10, 2018): 2475–78. http://dx.doi.org/10.35120/kij28072475k.

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A specific approach is needed based on a comprehensive study of both tourist resources and habitats / natural findings of fossils for develop a successful tourist product targeting customers who have interests in paleontology. The aim of the study is to evaluate the possibilities of modeling paleontological destinations in the country using leaf imprints and fossils. Fossils have their unique origins. They are formed at a certain point in geological development and in a specific geographic location. In this respect, by their genesis and common character, they are non-renewable resources of high scientific, educational, commercial and amateur value, which can be considered as a tourist resource. Two different paleontological outcrops have been studied: the Lovech Urgonian Group in Northern Bulgaria and the Smolyan Palaeogene Basin in the Western Rhodopes. Destination Lovech Urgonian Group: sampling rocks with finds of Orbitolina, Foraminifera, Algae, coral, Gastropoda, Bivalvia associated with coral reefs in the sedimentary rocks of the Lovech Urgonian Group are situated in the region of Veliko Tarnovo and Lovech. They are connected to a Urgonian paleo Sea, whose age is Low Cretaceous.Destination Smolyan Paleogene basin: different leaf imprints are found in the sedimentary rocks, representatives of the families Platanacea, Fagacaea, Lauraceae, Pinaceae, Podocarpaceae and others with different ecological characteristics. The paleo-floristic diversity shows a dynamic climatic situation through the Paleogene period in this region. The tourists accessibility to the natural revelations of paleo-reefs in North Bulgaria and of the palaeoflora outcrops in the Smolyan region is assessed. An assessment of the tourist infrastructure, the existence of geological landscapes, panoramic views and paleontological museum expositions has been made. The specialized paleontological museums in the country are limited in number. And the offering of paleontological tourist destinations is the opportunity for tourists with interests in the natural history and the live evolution to find a suitable form for satisfying their special interests.

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Staneva, Krasimira. "PALEONTOLOGICAL HERITAGE RESOURCES FOR TOURISM IN BULGARIA." Knowledge International Journal 28, no. 7 (December 10, 2018): 2475–78. http://dx.doi.org/10.35120/kij29082475k.

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Анотація:

A specific approach is needed based on a comprehensive study of both tourist resources and habitats / natural findings of fossils for develop a successful tourist product targeting customers who have interests in paleontology. The aim of the study is to evaluate the possibilities of modeling paleontological destinations in the country using leaf imprints and fossils. Fossils have their unique origins. They are formed at a certain point in geological development and in a specific geographic location. In this respect, by their genesis and common character, they are non-renewable resources of high scientific, educational, commercial and amateur value, which can be considered as a tourist resource. Two different paleontological outcrops have been studied: the Lovech Urgonian Group in Northern Bulgaria and the Smolyan Palaeogene Basin in the Western Rhodopes. Destination Lovech Urgonian Group: sampling rocks with finds of Orbitolina, Foraminifera, Algae, coral, Gastropoda, Bivalvia associated with coral reefs in the sedimentary rocks of the Lovech Urgonian Group are situated in the region of Veliko Tarnovo and Lovech. They are connected to a Urgonian paleo Sea, whose age is Low Cretaceous.Destination Smolyan Paleogene basin: different leaf imprints are found in the sedimentary rocks, representatives of the families Platanacea, Fagacaea, Lauraceae, Pinaceae, Podocarpaceae and others with different ecological characteristics. The paleo-floristic diversity shows a dynamic climatic situation through the Paleogene period in this region. The tourists accessibility to the natural revelations of paleo-reefs in North Bulgaria and of the palaeoflora outcrops in the Smolyan region is assessed. An assessment of the tourist infrastructure, the existence of geological landscapes, panoramic views and paleontological museum expositions has been made. The specialized paleontological museums in the country are limited in number. And the offering of paleontological tourist destinations is the opportunity for tourists with interests in the natural history and the live evolution to find a suitable form for satisfying their special interests.

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Sadikov, A. V. "Like in a Drop of Water: colloquial Cuban Spanish in just one Joke." Cuadernos Iberoamericanos 11, no. 1 (April 24, 2023): 113–31. http://dx.doi.org/10.46272/2409-3416-2023-11-1-113-131.

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Cuban Spanish, its colloquial variety included, is quite a peculiar, perhaps a unique phenomenon. Fruit of the unique history of the Cuban ethnic community, the Cuban colloquial speech has become an amalgam of imprints of many languages, as well as of a host of ethnic and religious traditions. Here, as nowhere else in the Western Hemisphere, with the exception, perhaps, of Brazil, the African heritage stayed very much alive and came afloat first in the language of the Afro-Cuban community as a whole, and then in Cuban Spanish as such. And yet other sources of colloquial Cuban should also be mentioned: first, the colloquial speech of native Spaniards, which were plenty on the Island before the Revolution of 1959 and contributed a lot to the patterns of word-formation in Cuban; and, finally, two more elements: the Portuguese one and the Gipsy one, as units thereof have found a prominent place among the most commonly used Cuban colloquialisms.

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40

Riaz, Sana, Marina khan, and Saddam Ul Islam. "Analyzing the social and ideological effects of 9/11: A Meta-critical analysis of The Blind Man's garden and Kite Runner." Global Language Review VII, no. III (September 30, 2022): 19–26. http://dx.doi.org/10.31703/glr.2022(vii-iii).03.

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This study explains the social, economic, geographical and political imprints of an imposed war as a result of an unfortunate incident known to the world as 9/11.The study specifically unveils the traumatic effects of the identity that the West has related to symbolising Muslims and Islam. The purpose of the study is to bring under discussion the opinionated and judgmental approach of Western nations/media towards Islam and Muslims. The study purposes to frame a scheme against violence non-violently by highlighting the sense of hatred that has developed as a result of misapprehension between Islam and other nationalities. The basic purpose of the study is to clarify the image of Islam to the world that the ugliness of 9/11 has affected not only the West, as they picture it, rather Muslims specifically and other religions, The Sikhs for instance, have also faced the adverse circumstances because of an imposed 9/11 war.

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Chen, Shuangling, Mark L. Wells, Rui Xin Huang, Huijie Xue, Jingyuan Xi, and Fei Chai. "Episodic subduction patches in the western North Pacific identified from BGC-Argo float data." Biogeosciences 18, no. 19 (October 13, 2021): 5539–54. http://dx.doi.org/10.5194/bg-18-5539-2021.

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Abstract. Subduction associated with mesoscale eddies is an important but difficult-to-observe process that can efficiently export carbon and oxygen to the mesopelagic zone (100–1000 dbar). Using a novel BGC-Argo dataset covering the western North Pacific (20–50∘ N, 120–180∘ E), we identified imprints of episodic subduction using anomalies in dissolved oxygen and spicity, a water mass marker. These subduction patches were present in 4.0 % (288) of the total profiles (7120) between 2008 and 2019, situated mainly in the Kuroshio Extension region between March and August (70.6 %). Roughly 31 % and 42 % of the subduction patches were identified below the annual permanent pycnocline depth (300 m vs. 450 m) in the subpolar and subtropical regions, respectively. Around half (52 %) of these episodic events injected oxygen-enriched waters below the maximum annual permanent thermocline depth (450 dbar), with >20 % occurring deeper than 600 dbar. Subduction patches were detected during winter and spring when mixed layers are deep. The oxygen inventory within these subductions is estimated to be on the order of 64 to 152 g O2/m2. These mesoscale events would markedly increase oxygen ventilation as well as carbon removal in the region, both processes helping to support the nutritional and metabolic demands of mesopelagic organisms. Climate-driven patterns of increasing eddy kinetic energies in this region imply that the magnitude of these processes will grow in the future, meaning that these unexpectedly effective small-scale subduction processes need to be better constrained in global climate and biogeochemical models.

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42

Andreassen, K., C. M. Ødegaard, and B. Rafaelsen. "Imprints of former ice streams, imaged and interpreted using industry three-dimensional seismic data from the south-western Barents Sea." Geological Society, London, Special Publications 277, no. 1 (2007): 151–69. http://dx.doi.org/10.1144/gsl.sp.2007.277.01.09.

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43

Nilsson, Gunnar, Min Wang, Johan Wejde, Andris Kreicbergs, and Olle Larsson. "Detection of EWS/FLI-1 by Immunostaining. An Adjunctive Tool in Diagnosis of Ewing's Sarcoma and Primitive Neuroectodermal Tumour on Cytological Samples and Paraffin-Embedded Archival Material." Sarcoma 3, no. 1 (1999): 25–32. http://dx.doi.org/10.1080/13577149977839.

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Purpose.Recently we showed that the 68-kDa fusion protein derived from theEWS/FLI1hybrid gene can be specifically detected by Western blotting using a polyclonal antibody to the C-terminal of FLI1 on biopsy material from Ewing's sarcoma. The aim of this study was to investigate whether this antibody also could be used for immunocytochemistry and immunohistochemistry in diagnosis of Ewing's sarcoma.Methods.Immunostaining on paraffin-embedded archival material, fine-needle aspirates and tumour touch imprints from Ewing's sarcomas and primitive neuroectodermal tumours (PNET) for detection of the fusion protein was performed. Most cases were also analysed by Western blotting.Tumours of differential diagnostic importance were also included.Results. Eighty per cent (12/15 cases) of the Ewing tumours exhibited a positive immunoreactivity for the FLI1 antibody. The signal was mainly localised in the nuclei of the tumour cells, which seems reasonable sinceEWS/FLI1is a transcription factor. The signal was found to be specific since it did not appear when the blocking peptide was added to the antibody solution.Moreover, two other types of small-round cell tumours (i.e. neuroblastoma and alveolar rhabdomyosarcoma) were negative as well as most normal tissues.Discussion.Immunostaining of histological and cytological specimens with the FLI1 antibody can be of diagnostic relevance in Ewing tumours carrying t(11;22).The absence of immunoreactivity in non-Ewing cells is most likely due to a low expression of the wild-type FLI1 protein.

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Petti, Fabio Massimo, Heinz Furrer, Enrico Collo, Edoardo Martinetto, Massimo Bernardi, Massimo Delfino, Marco Romano, and Michele Piazza. "Archosauriform footprints in the Lower Triassic of Western Alps and their role in understanding the effects of the Permian-Triassic hyperthermal." PeerJ 8 (December 18, 2020): e10522. http://dx.doi.org/10.7717/peerj.10522.

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The most accepted killing model for the Permian-Triassic mass extinction (PTME) postulates that massive volcanic eruption (i.e., the Siberian Traps Large Igneous Province) led to geologically rapid global warming, acid rain and ocean anoxia. On land, habitable zones were drastically reduced, due to the combined effects of heating, drought and acid rains. This hyperthermal had severe effects also on the paleobiogeography of several groups of organisms. Among those, the tetrapods, whose geographical distribution across the end-Permian mass extinction (EPME) was the subject of controversy in a number of recent papers. We here describe and interpret a new Early Triassic (?Olenekian) archosauriform track assemblage from the Gardetta Plateau (Briançonnais, Western Alps, Italy) which, at the Permian-Triassic boundary, was placed at about 11° North. The tracks, both arranged in trackways and documented by single, well-preserved imprints, are assigned to Isochirotherium gardettensis ichnosp. nov., and are here interpreted as produced by a non-archosaurian archosauriform (erytrosuchid?) trackmaker. This new discovery provides further evidence for the presence of archosauriformes at low latitudes during the Early Triassic epoch, supporting a model in which the PTME did not completely vacate low-latitude lands from tetrapods that therefore would have been able to cope with the extreme hot temperatures of Pangaea mainland.

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Duggal, Ekta, and Harsh V. Verma. "Cool perspectives, Indian cool and branding." South Asian Journal of Business Studies 8, no. 2 (June 3, 2019): 130–45. http://dx.doi.org/10.1108/sajbs-07-2018-0083.

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Purpose Cool has been studied mostly in consumer samples drawn from Western countries. This study was inspired by paucity of literature on “cool” in an Indian context. There is certainty that “cool” adds value and bestows desirability but there is uncertainty about what “cool” means. Since “cool” is a cultural phenomenon, the purpose of this paper is to explore its meaning in the Indian context. Design/methodology/approach The data were obtained on an open-ended questionnaire followed by depth probes on a sample of young consumers. The obtained scripts were coded and classified into semantic categories based on the grounded theory. Findings The study found that cool is indicated by seven facets, including being oneself, living life to the fullest, sense of humor and socially networked, and calm disposition. Unlike Western notions, in India, cool is not being deviant and hedonistic. The cultural and religious imprints are palpable in what is construed as cool in India. Research limitations/implications Transplanting the Western notions of cool for brand building is likely to be a risky proposition. It may not resonate with the inner cords of the Indian youth. The implication of this study is that it reveals possible ways in which cool can be incorporated in brand identity. Practical implications Cool is valued because it bestows distinction in subtle ways. Brands can gain traction among consumers by incorporating cool symbolism in their identity. Originality/value This study expands the understanding of cool in the context of an emerging market. This is one of the first studies to have probed the concept of “cool” in India.

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Ivashkiv, Halyna. "Construction earthenware in Western Ukraine: continuity of ethnographical tradition (based on the examples of bricks)." JOURNAL OF ETHNOLOGY AND CULTUROLOGY 33 (August 2023): 38–43. http://dx.doi.org/10.52603/rec.2023.33.04.

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The article highlights the specificity of the brick as one of major types of construction material in the ХІV–ХХ c. in Western Ukraine. On the territory of the region, namely in Lviv, the brick has been used in construction since the second half of the ХІV c. when city walls and three main cathedrals were built (in particular, we mean the Roman-Catholic, the Armenian and St. George’s Cathedrals). Among the rare findings, there is a brick with a scratched motif of a Greek-type cross that was excavated by archaeologists in the center of Lviv. In the XVI–XVIII c., constructors used a widespread type of brick called “paltsivka”, the name of which originates from the method of its production, i. e., on one of the wider sides of the brick craftsmen made “gutters” with their fingers (Lviv, Zhovkva). This type of bricks was used in building fortifications, monasteries and castles. There are rare samples of bricks with imprints of a child’s or an adult’s foot or a dog’s paw (Lviv, Kopychyntsi). Bricks of the 19th century, which were produced industrially, contained embossed and engraved Cyrillic or Latin initials, sometimes surnames of enterprise owners, the year and place of production. Bricks from Ivan Levynskyi’s factory were used to build Lviv Opera and Ballet Theater, the railway station and later other buildings in the city, namely in the district of Kastelivka. At that time, brickworks functioned in Boikivshchyna, Pokuttia, Western Podillia and Volyn. Using the example of items from museums and private collections, as well as the author’s own expedition notes, the article has traced the evolution of brick shapes and the inscriptions on them.

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Ferraccioli, F., P. C. Jones, M. L. Curtis, and P. T. Leat. "Subglacial imprints of early Gondwana break-up as identified from high resolution aerogeophysical data over western Dronning Maud Land, East Antarctica." Terra Nova 17, no. 6 (December 2005): 573–79. http://dx.doi.org/10.1111/j.1365-3121.2005.00651.x.

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OKAY, ARAL I., İZVER TANSEL, and OKAN TÜYSÜZ. "Obduction, subduction and collision as reflected in the Upper Cretaceous–Lower Eocene sedimentary record of western Turkey." Geological Magazine 138, no. 2 (March 2001): 117–42. http://dx.doi.org/10.1017/s0016756801005088.

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Late Cretaceous–Early Eocene Tethyan evolution of western Turkey is characterized by ophiolite obduction, high-pressure/low-temperature metamorphism, subduction, arc magmatism and continent–continent collision. The imprints of these events in the Upper Cretaceous–Lower Eocene sedimentary record of western Anatolia are studied in thirty-eight well-described stratigraphic sections. During the Late Cretaceous period, western Turkey consisted of two continents, the Pontides in the north and the Anatolide-Taurides in the south. These continental masses were separated by the İzmir-Ankara Neo-Tethyan ocean. During the convergence the Pontides formed the upper plate, the Anatolide-Taurides the lower plate. The arc magmatism in the Pontides along the Black Sea coast is biostratigraphically tightly constrained in time between the late Turonian and latest Campanian. Ophiolite obduction over the passive margin of the Anatolide-Tauride Block started in the Santonian soon after the inception of subduction in the Turonian. As a result, large areas of the Anatolide-Tauride Block subsided and became a region of pelagic carbonate sedimentation during the Campanian. The leading margin of the Anatolide-Tauride Block was buried deeply and was deformed and metamorphosed to blueschist facies during Campanian times. The Campanian arc volcanic rocks in the Pontides are conformably overlain by shaley limestone of Maastrichtian–Palaeocene age. However, Maastrichtian sedimentary sequences north of the Tethyan suture are of fore-arc type suggesting that although arc magmatism ceased by the end of the Campanian age, continent–continent collision was delayed until Palaeocene time, when there was a change from marine to continental sedimentation in the fore-arc basins. The interval between the end of the arc magmatism and continent–continent collision may have been related to a northward jump of the subduction zone at the end of Campanian time, or to continued obduction during the Maastrichtian.

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Wu, Yihao, Yikai Qiu, and Hong Wang. "Urban cartography and spatial politics: Ethnic tensions, westernization, and decolonization in Hangzhou’s transformation within the global south." Journal of Geography and Cartography 6, no. 2 (October 19, 2023): 2853. http://dx.doi.org/10.24294/jgc.v6i2.2853.

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Urban morphologies in the global south are shaped by a complex interplay of historical imprints, from colonial legacies and ethnic tensions to waves of modernization and decolonization efforts. This study delves into the urban morphology of Hangzhou during the late 19th and early 20th centuries, unraveling its transformative patterns steered by a convergence of spatial politics, economic forces, and cultural dynamics. Drawing upon a unique blend of historical map restoration techniques, we unearth pivotal morphological nuances that bridge Hangzhou’s transition from its pre-modern fabric to its modern-day urban layout. We uncover key shifts such as the movement from intricate street layouts to systematic grids, the strategic integration of public spaces like West Lakeside Park, and the city’s evolving urban epicenter mirroring its broader socio-political and economic narratives. These insights not only spotlight Hangzhou’s distinct urban journey in the context of ethnic conflicts, Western influences, and decolonization drives but also underscore the value of context-sensitive urban morphological research in the global south. Our findings emphasize the criticality of synergizing varied methodologies and theoretical perspectives to deepen our comprehension of urban transitions and to sculpt place identities and invigorate public imagination in global urban planning.

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Lamanilao, Randy P., and Francis Mervin L. Agdana. "Acculturation of American English as Philippine English: An affective critique." International Journal of Multidisciplinary Research and Growth Evaluation 5, no. 1 (2024): 453–58. http://dx.doi.org/10.54660/.ijmrge.2024.5.1.453-458.

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This paper posits that Philippine English is a Filipino nativized variant of General American English, a unique linguistic outcome shaped by the historical imprints of Western Colonialism under Spain and the United States. Employing a Qualitative Research design, specifically a reader-response critique, the study delves into the acculturated lexicon processing of Philippine English. The findings indicate that English has evolved into the functional native tongue of Filipinos, serving diverse functions across linguistic and cultural groups. Filipinos demonstrate a tendency to overgeneralize word meanings and utilize derivational suffixes creatively. Notably, the preservation and widespread use of archaic or obsolete words persist in contemporary discourse. The Filipino English lexicon showcases analogical constructions, clippings, and coined words, contributing to the evolution of language. Spanish loanwords further enrich this linguistic tapestry. The study concludes that Philippine English is indeed a Filipino nativized variant of General American English. Recommendations include the creation of a monograph detailing English words and their functions in the Philippine context. Additionally, educators are urged to disseminate research insights within educational institutions or to higher authorities, fostering a deeper understanding of Philippine English and informing potential language education enhancements.

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