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Journal articles on the topic 'Tremiti'

Author: Grafiati
Published: 4 June 2021
Last updated: 2 February 2022

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1

FONZI, FULVIO. "Tremiti Desalination Plant." International Journal of Solar Energy 3, no. 3 (June 1985): 153–62. http://dx.doi.org/10.1080/01425918508914391.

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2

Teofilo, Gianvito, Vincenzo Festa, Luisa Sabato, Luigi Spalluto, and Marcello Tropeano. "3D modelling of the Tremiti salt diapir in the Gargano offshore (Adriatic Sea, southern Italy): constraints in the Tremiti Structure development." Italian Journal of Geosciences 135, no. 3 (October 2016): 474–85. http://dx.doi.org/10.3301/ijg.2015.40.

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3

Miccadei, E., F. Mascioli, and T. Piacentini. "Quaternary geomorphological evolution of the Tremiti Islands (Puglia, Italy)." Quaternary International 233, no. 1 (March 2011): 3–15. http://dx.doi.org/10.1016/j.quaint.2010.04.028.

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4

Bargellini, Clara. "The Tremiti Mosaic and Eleventh-Century Floor Decoration in Eastern Italy." Dumbarton Oaks Papers 41 (1987): 29. http://dx.doi.org/10.2307/1291543.

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5

Brandone, A., P. Fumo, M. Giaccio, M. Oddone, V. Riganti, and M. Baldi. "Characterization of prehistoric pottery from the Tremiti Isles by trace elements determination." Journal of Radioanalytical and Nuclear Chemistry Articles 173, no. 1 (September 1993): 99–106. http://dx.doi.org/10.1007/bf02102702.

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6

Miccadei, Enrico, Tommaso Piacentini, and Marcello Buccolini. "Long-term geomorphological evolution in the Abruzzo area, Central Italy: twenty years of research." Geologica Carpathica 68, no. 1 (February 1, 2017): 19–28. http://dx.doi.org/10.1515/geoca-2017-0002.

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AbstractThe most recent research studies into the long-term landscape evolution of the Abruzzo area, carried out over the last twenty years at the “G. d’Annunzio” University of Chieti-Pescara, are based on an integrated approach incorporating structural geology and geomorphology and, in particular, the geomorphometry of topographic and hydrographic aspects, geological and structural-geomorphological surveys and mapping supported by morpho-stratigraphic and chronological constraints. The geomorphological analyses have allowed us to outline the main stages of geomorphological evolution and to identify the factors that have contributed to the landscape shaping of the Apennine Chain, the Adriatic Piedmont and the fluvial plains and coastal sectors, up to the Tremiti islands. In the Apennine Chain, landscape evolution — in a ridge, valley and basin system — is connected to the regional uplift, local tectonic subsidence and local base level variations, which have led to changes in the drainage systems, from exoreic to endorheic (in the intermontane basins) and then to exoreic again. In the Adriatic Piedmont, landscape shaping is connected to uplifting and eustatic sea-level fluctuations, which have induced the formation of a structure-controlled drainage system and the shaping of systems of entrenched alluvial fans and large consequent river valleys, with flights of river terraces. In the coastal Adriatic area — composed of a coastal plain-coastal slope system (northern and southern coast) and of a cliffed rocky coast (central coast, Tremiti) interrupted by river valleys — landscape shaping is the result of selective erosion due to the interaction between marine geomorphic processes and slope processes connected to Late Quaternary eustatic fluctuations.
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7

Cormaci, Mario, Giovanni Furnari, Giuseppina Alongi, Marcello Catra, and Donatella Serio. "The benthic algal flora on rocky substrata of the Tremiti Islands (Adriatic Sea)." Plant Biosystems - An International Journal Dealing with all Aspects of Plant Biology 134, no. 2 (January 2000): 133–52. http://dx.doi.org/10.1080/11263500012331358404.

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8

Andriani, G. F., N. Walsh, and R. Pagliarulo. "The influence of the geological setting on the morphogenetic evolution of the Tremiti Archipelago (Apulia, Southeastern Italy)." Natural Hazards and Earth System Sciences 5, no. 1 (January 3, 2005): 29–41. http://dx.doi.org/10.5194/nhess-5-29-2005.

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Abstract. The Tremiti Archipelago (Southern Adriatic Sea), also called Insulae Diomedae from the name of the Greek hero who first landed there, is an area of high landscape and historical value. It is severely affected by significant geomorphologic processes dominated by mass movements along the coast that constitute the most important and unpredictable natural hazard for the population and cultural heritage. Coastal erosion is favoured by the peculiar geological and structural setting, seismic activity, weathering, development of karst processes, and wave action. The present paper reports on descriptive and qualitative evaluation of the factors controlling landslides and coastline changes based on medium-term in situ observation, detailed surface surveys at selected locations since 1995, and historic and bibliographic data. The Tremiti Archipelago is part of an active seismic area characterised by a shear zone separating two segments of the Adriatic microplate that have shown different behaviour and roll back rates in the subduction underneath the Apennines since middle Pleistocene. Although coastal morphology can be basically considered to be the result of wave action, the continual action of subaerial processes contributes effectively to the mechanism of shoreline degradation. Weathering mainly affects the marly calcisiltites and calcilutites of the Cretaccio Fm. and the friable and low cemented calcarenites and biomicrites of the San Nicola Fm. The cliffs are characterised by different types of failure such as lateral spreads, secondary topples, rock falls and slides. At the Isle of San Nicola, landslides are controlled by the contrast in competence, shear strength and stiffness between the Pliocene re-crystallised dolomitic calcarenites and calcisiltites and the Miocene marly calcilutites and calcisiltites. At the Isles of San Domino and Caprara rock falls are attributed to the undercutting of waves at the base of the cliffs.
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9

Miccadei, Enrico, Paolo Orrù, Tommaso Piacentini, Francesco Mascioli, and Giuseppe Puliga. "Geomorphological map of the Tremiti Islands (Puglia, Southern Adriatic Sea, Italy), scale 1:15,000." Journal of Maps 8, no. 1 (March 2012): 74–87. http://dx.doi.org/10.1080/17445647.2012.668765.

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10

Boero, Ferdinando, Genuario Belmonte, Roberta Bracale, Simonetta Fraschetti, Stefano Piraino, and Serena Zampardi. "A salp bloom (Tunicata, Thaliacea) along the Apulian coast and in the Otranto Channel between March-May 2013." F1000Research 2 (September 10, 2013): 181. http://dx.doi.org/10.12688/f1000research.2-181.v1.

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Between March-May 2013 a massive Salpa maxima bloom was recorded by a citizen science study along the Ionian and Adriatic coast of the Salento peninsula (Italy). Citizen records were substantiated with field inspections along the coast and during an oceanographic campaign in the Otranto Channel.Salps clogged nets, impairing fishing activities along the coast. Swimmers were scared by the gelatinous appearance of the salps, and thought they were jellyfish. At the end of the bloom the dead bodies of the colonies, that were up to 6-7 m long, were accumulated along the coast and stirred by the waves, forming foams along dozens of kilometers of coast. The bloom also occurred at the Tremiti Islands, north of the Gargano Peninsula. The possible impacts of such events on the functioning of pelagic systems are discussed.
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11

Festa, Vincenzo, Gianvito Teofilo, Marcello Tropeano, Luisa Sabato, and Luigi Spalluto. "New insights on diapirism in the Adriatic Sea: the Tremiti salt structure (Apulia offshore, southeastern Italy)." Terra Nova 26, no. 3 (November 27, 2013): 169–78. http://dx.doi.org/10.1111/ter.12082.

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12

Pagliarulo, Rosa. "Relationship Between Natural Hazards and Geological Heritage: the Case of Cretaccio Island (Tremiti Archipelago, Southern Italy)." Geoheritage 7, no. 1 (March 29, 2014): 57–63. http://dx.doi.org/10.1007/s12371-014-0108-x.

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13

Di Bella, Letizia, Sara Casieri, and Maria Gabriella Carboni. "Late Quaternary paleoenvironmental reconstruction of the Tremiti structural high (Central Adriatic Sea) from benthic foraminiferal assemblages." Geobios 41, no. 6 (November 2008): 729–42. http://dx.doi.org/10.1016/j.geobios.2008.06.001.

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14

Dall'Antonia, Barbara. "Miocene ostracods from the Tremiti Islands and Hyblean Plateau: biostratigraphy and description of new and poorly known species." Geobios 36, no. 1 (January 2003): 27–53. http://dx.doi.org/10.1016/s0016-6995(02)00105-5.

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15

Elena, Fregni, Maria Grazia Faienza, Susanna De Zio Grimaldi, Paolo Tongiorgi, and Maria Balsamo. "Marine gastrotrichs from the Tremiti archipelago in the southern Adriatic Sea, with the description of two new species ofUrodasys." Italian Journal of Zoology 66, no. 2 (January 1999): 183–94. http://dx.doi.org/10.1080/11250009909356254.

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16

Egeler, Matthias. "The Plane Trees of Diomedes: Staging the Islands of the Blessed in the Adriatic Sea." Numen 62, no. 5-6 (September 7, 2015): 495–518. http://dx.doi.org/10.1163/15685276-12341389.

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Taking its starting point from the current theoretical debate about “religious aesthetics” (Religionsästhetik), this article offers a new interpretation of the landscaping of the Island of Diomedes. On the basis of a survey of the primary sources, it demonstrates that the descriptions of the Island of Diomedes have to be seen in the context of the mythological motif of the Islands of the Blessed. This in turn suggests an explanation for Theophrastus’ statement that in the Adriatic region of his day, the plane tree grew only around the shrine of Diomedes: given the typical associations of the plane tree, the planting of planes on the sanctuary island of Diomedes may have been intended to bring the appearance of the Island of Diomedes in line with contemporary stereotypes about the appearance of the Islands of the Blessed; thus, the plane trees of Diomedes constitute a historical case of direct relevance for the question of “religious aesthetics.” The article goes on to demonstrate that the plane trees of Diomedes constitute conclusive evidence against the identification of the Island of Diomedes with the island of Pelagosa (recently suggested on the basis of archaeological finds). Instead, the Island of Diomedes should be sought among the Isole Tremiti.
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17

Gallo D'Addabbo, Maria, Susanna de Zio Grimaldi, and Roberto Sandulli. "Heterotardigrada of Two Submarine Cavesin S. Domino Island (Tremiti Islands) in the Mediterranean Sea with the Description of Two New Species of Stygarctidae." Zoologischer Anzeiger - A Journal of Comparative Zoology 240, no. 3-4 (January 2001): 361–69. http://dx.doi.org/10.1078/0044-5231-00043.

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18

Pinsino, A., C. Della Torre, V. Sammarini, R. Bonaventura, E. Amato, and V. Matranga. "Sea urchin coelomocytes as a novel cellular biosensor of environmental stress: a field study in the Tremiti Island Marine Protected Area, Southern Adriatic Sea, Italy." Cell Biology and Toxicology 24, no. 6 (January 29, 2008): 541–52. http://dx.doi.org/10.1007/s10565-008-9055-0.

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19

Paglia, Giorgio, Luisa Bergamin, Marcello Buccolini, Cristiano Carabella, Francesco Cerrone, Francesco Latino Chiocci, Roberto d’Arielli, et al. "A multidisciplinary approach to the study of insular environments: the 1st Summer School on Geomorphology, Ecology, and Marine Biology in the Tremiti Islands (Southern Adriatic Sea, Puglia, Italy)." Journal of Maps 16, no. 3 (June 18, 2020): 1–9. http://dx.doi.org/10.1080/17445647.2020.1776645.

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20

Buccolini, Marcello, Cristiano Carabella, Giorgio Paglia, Alessandro Cecili, Gianluca Chiarolanza, Camilla Cioria, Camilla Conicella, et al. "Geomorphological analysis of the San Domino Island (Tremiti Islands, Southern Adriatic Sea). Results from the 2019 Geomorphological Field Camp of the MSc in Geological Science and Technology (University of Chieti-Pescara)." Journal of Maps 16, no. 3 (November 16, 2020): 10–18. http://dx.doi.org/10.1080/17445647.2020.1831979.

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21

Šilbajoris, Rimvydas, and Algimantas Bučys. "Tremtis." World Literature Today 62, no. 4 (1988): 700. http://dx.doi.org/10.2307/40144711.

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22

Apartis, E., and C. P. Jedynak. "Tremori." EMC - Neurologia 14, no. 1 (February 2014): 1–17. http://dx.doi.org/10.1016/s1634-7072(14)66663-0.

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23

Couloume, L., and P. Derkinderen. "Tremori." EMC - AKOS - Trattato di Medicina 21, no. 2 (June 2019): 1–5. http://dx.doi.org/10.1016/s1634-7358(19)42024-x.

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24

Viallet, F., L. Vercueil, D. Gayraud, B. Bonnefoi, and L. Renie. "Movimenti anomali secondari (distonie, mioclonie, tremori, discinesie)." EMC - Neurologia 12, no. 3 (August 2012): 1–15. http://dx.doi.org/10.1016/s1634-7072(12)62644-0.

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25

Okumura, Kenichi, Tetu Tezuka, Yukio Takagi, Michio Gomyoh, Isao Iida, and Eiji Yauchi. "Dumping Dredged Material with Double-Tremie." PROCEEDINGS OF CIVIL ENGINEERING IN THE OCEAN 13 (1997): 375–79. http://dx.doi.org/10.2208/prooe.13.375.

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26

Gayraud, D., B. Bonnefoi, A. Roux, and F. Viallet. "Movimenti anomali secondari (distonie, coree/ballismo, miocloni, tremori, discinesie)." EMC - Neurologia 21, no. 2 (April 2021): 1–16. http://dx.doi.org/10.1016/s1634-7072(21)44997-4.

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27

Mizuno, Naoya, Mitsuo Nagashima, Soichi Makino, and Takeji Okada. "Prevention of Blocking of Tremie for Slurry Wall Construction." Concrete Research and Technology 8, no. 1 (1997): 251–65. http://dx.doi.org/10.3151/crt1990.8.1_251.

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28

Ferrarotto, Renata, Diana Bell, M. Laura Rubin, J. Jack Lee, Jason Michael Johnson, Ryan Goepfert, Jack Phan, et al. "Checkpoint inhibitors assessment in oropharynx cancer (CIAO): Safety and interim results." Journal of Clinical Oncology 37, no. 15_suppl (May 20, 2019): 6008. http://dx.doi.org/10.1200/jco.2019.37.15_suppl.6008.

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6008 Background: Anti-PD-1/PD-L1 are active in metastatic oropharynx squamous cell carcinoma (OPC). Durvalumab (durva) and tremelimumab (tremi) target respectively PD-L1 and CTLA-4, which in combination may be synergistic. Here we report the safety and interim results of durva vs. durva+tremi prior to surgery in a window of opportunity trial in OPC. Methods: Pts were randomized 1:1 to durva 1500 mg or durva 1500 mg + tremi 75 mg IV Q4W x 2 cycles. The primary objective was to quantify pre- and post-treatment differences in CD8+ tumor infiltrating lymphocytes for the two arms. Secondary objectives included safety, toxicity, ORR by RECIST, fraction of patients undergoing surgery at 8 wks, and percentage viable tumor cells in the surgical specimen. Serial pre- and post-treatment blood and tumor specimens were collected for ongoing correlative analyses. Results: 28 pts enrolled: median age 64y, 27 (96%) male, 19 (68%) newly diagnosed, most (63%) at stage IVA (AJCC 7th Ed), 9 (32%) had locoregional recurrence, 24 (86%) p16 positive, and 22 (79%) had ≤ 10 PPY smoking history. Median follow-up was 7.6 months. The most common AEs were fatigue (36%), leukopenia/lymphopenia (25%), transaminitis (25%), and rash (21%). Grade 3 AEs occurred in 4 (14%) pts: 2 elevated lipase, 1 diarrhea, and 1 hepatitis, all were manageable. There were no grade >3 AEs. ORR was 43%: 50% had SD (including 29% tumor shrinkage in 1 pt). Treatment effect in the surgical specimen was observed in 19 (79%) of 24 evaluable pts; 2 pts had major pathologic response (≤ 10% viable tumor) at the primary site. Efficacy was equivalent in both arms. The 2 pts with PD and 1 pt with SD were switched to chemotherapy after durva +/- tremi before resection; interestingly, each achieved a pCR in the primary. Most pts (57%) didn’t receive radiotherapy after surgery. There was a statistically significant association between ORR and treatment effect (p=0.014). The median percentage of viable tumor in the primary was 37.5% in pts with PR, and 82.5% in SD (p=0.003). Conclusions: Durva +/- tremi prior to surgery was well tolerated in OPC pts. Activity is encouraging with treatment effect seen in 79% of pts. The primary endpoint and complete efficacy data will be presented. Clinical trial information: NCT03144778.
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29

Bassett, Michael G., Leonid E. Popov, Richard J. Aldridge, Sarah E. Gabbott, and Johannes N. Theron. "Brachiopoda from the Soom Shale Lagerstätte (Upper Ordovician, South Africa)." Journal of Paleontology 83, no. 4 (July 2009): 614–23. http://dx.doi.org/10.1666/08-136.1.

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Within the Soom Shale Lagerstätte of South Africa (Upper Ordovician, Hirnantian), two brachiopod taxa preserve traces of organic tissue. In Trematis, presumed bands of periostracum are preserved on the flanks of the pedicle notch, and clay mineral casts of the pedicle are preserved in many specimens of Kosoidea. Both these genera are organophosphatic-shelled Linguliformea, together with a third genus identified as Plectoglossa. A fourth brachiopod taxon in the fauna belongs within the calcitic-shelled Rhynchonelliformea (Plectothyrella). Kosoidea cedarbergensis is a new species of discinoidean.
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30

Yauchi, Eiji, Koichi Yokobori, and Yoshiharu Matsumi. "Comparison of deposition configurations dumped by tremie pipes and barges." PROCEEDINGS OF CIVIL ENGINEERING IN THE OCEAN 13 (1997): 369–73. http://dx.doi.org/10.2208/prooe.13.369.

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31

Romano, Marco. "“Per tremoto o per sostegno manco”: The Geology of Dante Alighieri’s Inferno." Italian Journal of Geosciences 135, no. 1 (February 2016): 95–108. http://dx.doi.org/10.3301/ijg.2015.01.

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32

Das, Prabir K., Anthony L. Ricci, Huang Ni, and Paul Harrington. "Use of Soldier Pile–Tremie Concrete Slurry Walls as Permanent Tunnel Walls." Transportation Research Record: Journal of the Transportation Research Board 1541, no. 1 (January 1996): 153–62. http://dx.doi.org/10.1177/0361198196154100120.

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The analysis and design of soldier pile–tremie concrete (SPTC) slurry walls for the Massachusetts Highway Department's (MHD) Central Artery/Tunnel (CA/T) Project in downtown Boston are discussed. Unlike most slurry walls, which are used as temporary support for excavation during construction, these SPTC walls are designed also as the permanent wall system for the tunnels. The CA/T includes more than 6.1 km (20,000 ft) of slurry walls. Most of the walls are designed and are to be constructed as SPTC walls. Steel wide-flange soldier piles are installed at 1.21- to 1.83-m (4- to 6-ft) spacings in a slurry trench, and the tremie concrete is placed to form the concrete wall. The steel wide-flange piles form the primary support system for the wall. In most of the locations, the concrete is designed to act as “lagging” spanning between the structural steel members. The concrete base slab is rigidly connected to the SPTC walls, and the composite roof is pin-connected to the walls to form the tunnel. The following topics are discussed after an introduction to the project: geotechnical conditions, design concept of the SPTC slurry walls, design consideration, underpinning of the existing Central Artery, and low head-room construction.
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33

Movrin, David. "Primož Simoniti: Humanismus bei den Slovenen: Slowenische Humanisten bis zur Mitte des 16. Jahrhunderts. Priredba Marija Wakounig, prevod Jože Wakounig." Keria: Studia Latina et Graeca 11, no. 2 (December 24, 2009): 186. http://dx.doi.org/10.4312/keria.11.2.186-187.

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Simonitijeva študija Humanizem na Slovenskem, ki jo je pred tremi desetletji izdala Slovenska matica, je razmeroma meglene in nepovezane predstave o literarnem dogajanju v tem prostoru v stoletju pred začetkom reformacije nenadoma nadomestila z vse drugače natančno izrisano podobo, sestavljeno iz plastično prikazanih likov.
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34

Chiffi, Cosimo, and Davide Fiorello. "Energy intensity of maritime trades: Evidences from the EX-TREMIS database." Energy Policy 37, no. 10 (October 2009): 3752–57. http://dx.doi.org/10.1016/j.enpol.2009.07.014.

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35

Allouc, Jacques, and Jean-Georges Harmelin. "Les depots d'enduits manganoferriferes en environnement marin littoral; l'exemple de grottes sous-marines en Mediterranee nord-occidentale." Bulletin de la Société Géologique de France 172, no. 6 (November 1, 2001): 765–78. http://dx.doi.org/10.2113/172.6.765.

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Abstract Black coating of hard substrates by Mn and Fe oxides has long been reported from shallow, dark, submarine caves. However, these littoral metallic deposits have never been studied in detail, despite expected analogies with deep-sea polymetallic crusts. Submarine caves are characterized by darkness and low rates of exchanges with the open sea. Lack of primary production and confinement of inner water bodies result in marked oligotrophy and extremely reduced biomass, i.e. conditions close to those prevailing in deep-sea habitats. Field evidences suggested that the formation of Mn-Fe coatings was closely tied to these particular environmental conditions. The goal of this study was to examine the detailed features of Mn-Fe coatings from dark caves with different local conditions, and to try to identify the processes responsible for their deposition. Study sites and methods: Three sublittoral, single-entrance, caves were sampled by scuba diving along the coasts of Provence (France, Mediterranean Sea). The first site is a large karstic cave (Tremies Cave, 16 m depth at entrance floor, 60 m long; Marseille-Cassis area) with an ascending profile which results in a buffered thermal regime and markedly oligotrophic conditions due to warm water trapping in its upper part. Wall fragments were sampled at 30 m (medium confinement: zone B) and 60 m (strong confinement: zone C) from the cave entrance. The second site is a large tubular cavity open in conglomerate formations (3PP Cave, 15 m depth at entrance floor, 120 m long; La Ciotat) with a descending profile which results in relative permanence of winter temperatures within the inner parts, complex water circulation and presumed greater input of sedimented particles than in the preceding cave. Wall samples were taken at 25 m, 70 m and 100 m from entrance. The third site is a small, horizontal, cave open in quartzite formations (Bagaud Cave, 7 m depth at entrance floor, about 10 m long; WNW of Port-Cros Island, bay of Hyeres). Sampling was performed on walls of a narrow corridor between an anterior room and a smaller inner room. A sporadic outflow of continental waters is located in the inner room. The samples were preserved in 50% ethylic alcohol or studied soon after their sampling. Before carbon coating and SEM examination, or microanalyses with SEM-associated spectrometers, they were treated in a 33% Chlorox solution and thereafter washed in demineralized water and dried. Micromorphology: At low-medium magnification (<20,000), the aspect of coatings varies between caves and, especially, between inner-cave locations. All the described structures are made up of Mn and Fe oxides. In Tremies Cave, coatings of walls from zone B are composed of irregular erected constructions (height: 10s to 100s mu m) formed by the aggregation of roughly ovoid primary concretions of about 10 mu m. The surface of those primary concretions displays numerous lacunose to reticulate films (pores, about 0.5 mu m in diameter, are often subrounded). Remnants of these films and organomorphic corpuscles occur also within the primary concretions. On younger substrates (broken wall exposed since 1970), primary concretions are poorly developed and no prominent construction is visible. In more confined conditions (zone C), the erected constructions of ancient coatings are smaller and less numerous than in zone B but are well individualized. In this zone C, besides some remnants of lacunose to reticulate films, there is an appearance of filaments and ovoid corpuscles (height/width: 10-30/5-15 mu m), which seem to be linked to filaments by a short stalk. In 3 PP Cave, at 25-70 m from entrance, wall coatings present porous heaps of primary concretions. The surface and the inside of the latter comprise remnants of lacunose to reticulate films that evoke those observed in Tremies Cave. On younger substrates (hard parts of sessile invertebrates), coatings are restricted to micrometric organomorphic corpuscles with some remnants of lacunose or fibrous films. At 100 m from the entrance, coatings are shaped by numerous erected constructions, more or less coalescing. Besides remnants of lacunose films, the primary concretions contain interlacing filaments (diameter: 0.2-0.3 mu m) forming cords or veils. In Bagaud Cave, the primary concretions are aggregated in irregular heaps. Lacunose films are particularly frequent and tend to form three-dimensional mamillated structures that were not observed in the other caves. In particular, there is an appearance of tubular structures and of numerous hemispheroidal structures (diameter: 4-5 mu m) with an upper orifice. At higher magnification (20,000), whatever the cave and inner-cave location, the aspect of oxide deposits is rather smooth or, especially, microgranular. Mineral composition: The composition of coatings is different between caves and according to their inner-cave location. In both large caves (Tremies and 3 PP), the Mn/Fe ratio increases with the distance from the cave entrance, i.e. when exchanges with the open sea diminish. This trend is particularly clear in Tremies Cave, where the confinement gradient is strongly marked.
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36

Lavié, Fernando J., and Juan L. Benedetto. "Middle Ordovician (Darriwilian) linguliform and craniiform brachiopods from the Precordillera (Cuyania Terrane) of west-central Argentina." Journal of Paleontology 90, no. 6 (October 21, 2016): 1068–80. http://dx.doi.org/10.1017/jpa.2016.111.

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AbstractMiddle Ordovician lingulacean, trematid, and craniid brachiopods are described and illustrated for the first time from the uppermost part of San Juan Formation limestones of the Precordillera Basin, west-central Argentina. Sampled beds fall within theAhtiella argentinabrachiopod Zone, which, according to associated conodonts, is of early-mid Darriwilian age. The fauna consists of the linguloideansGlossella cuyanican. sp. andLingulasma? sp., the discinoideanTrematissp., the siphonotretidChilcatreta tubulatan. gen. n. sp., and a conical shell that is referred provisionally to the order Craniida. The linguliforms from the Cuyania (Precordillera) terrane, although still poorly known, display close similarities to those inhabiting low-to-intermediate latitude palaeocontinents, particularly Laurentia and Baltica, in accordance with evidence from rhynchonelliform brachiopods.
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37

Poškus, Kazys. "Lietuvos mokytojo socialinio aktyvumo raidos bruožai." Acta Paedagogica Vilnensia 1 (January 17, 2016): 12–21. http://dx.doi.org/10.15388/actpaed.0.01.9342.

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Socialinis mokytojo aktyvumas apibrėžiamas ir kaip asmeninė, ir kaip integrali visuomenės nario savybė, apimanti daugelį bruožų - idėjiškumą, pilietiškumą, humaniškumą, tautiškumą, kūrybiškumą ir t.t., ir realizuojama visuomeninėje, politinėje, kultūrinėje, profesinėje ir kitose sferose. Straipsnyje siekiama atskleisti mokytojų socialinio aktyvumo raišką įvairiomis istorinėmis aplinkybėmis. Aptariama mokytojų pasipriešinimas polonizacijai ir Rusijos caro represijoms XIX a. - XX a. pradžioje, aprašoma slaptųjų lietuviškų mokyklų mokytojų, vadinamųjų daraktorių, veikla. Vieni aktyviausių visuomenės atstovų mokytojai išliko ir nepriklausomos Lietuvos laikotarpiu (1918-1940 m). Pirmosios sovietinės okupacijos metu (1940-1941 m.) nemažai mokytojų įvardinti kaip „kenkėjiški” ir politiškai nepatikimi. Jie buvo tremiami, atleidžiami iš darbo. Represijos tęsėsi ir pokario metais. Ilgainiui daugumos mokytojų socialinis aktyvumas itin sumažėjo. Dalis mokytojų tapo įrankiu sovietinės ideologijos sklaidai.
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38

Boychuk, Irina. "History of participation of students of Bukovinian State Medical University in the “Trembita” ensemble." Current issues of social sciences and history of medicine, no. 2 (June 4, 2020): 59–69. http://dx.doi.org/10.24061/2411-6181.2.2020.180.

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39

Lagomarsino, Sergio, Andrea Penna, Alessandro Galasco, and Serena Cattari. "TREMURI program: An equivalent frame model for the nonlinear seismic analysis of masonry buildings." Engineering Structures 56 (November 2013): 1787–99. http://dx.doi.org/10.1016/j.engstruct.2013.08.002.

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40

Hasanuddin, Hasanuddin. "Jenis Jamur Kayu Makroskopis Sebagai Media Pembelajaran Biologi (Studi di TNGL Blangjerango Kabupaten Gayo Lues)." BIOTIK: Jurnal Ilmiah Biologi Teknologi dan Kependidikan 2, no. 1 (February 8, 2018): 38. http://dx.doi.org/10.22373/biotik.v2i1.234.

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Penelitian ini bertujuan mengetahui jenis-jenis jamur makroskopis yang terdapat di kawasan Taman Nasional Gunung Leuser Kecamatan Blangjerango Gayo Lues. Metode yang digunakan observasi dan jelajah yaitu melakukan pengamatan langsung ke lokasi penelitian. Luas daerah penelitian adalah 5 Ha yang dibagi menjadi 5 stasiun dan pada masing-masing stasiun dibuat 10 transek sehingga jumlah transek 50 dengan panjang 100 m, lebar kiri dan kanan 20 m. Analisis data dilakukan secara deskriptif. Hasil penelitian diperoleh 28 spesies jamur terdiri dari 18 genus yaitu Ganoderma, Grifola, Hexagonia, Hirchioporus, Pycnoporus, Tremella, Auricularia, Collybia, Coriolus, Hypholoma, Pleurotus, Phylloporus, Marasmius , Clavaria, Clitocybe, Crepidotus, Rigidoporus, Tremidis, Coriolus, Lactarius, Mycena, Clitocybe, Clitocybula, Pluteus, Pleurotus. Anggota genus yang paling banyak ditemukan adalah genus ganoderma 3 spesies. Dari hasil tersebut, disimpulkan bahwa jamur makroskopis tersebut layak digunakan sebagai media pembelajaran biologi di sekolah. Kata Kunci: Identifikasi, Jamur Makroskopis dan Media Pembelajaran biologi. This research was conducted to investigate the species of wood macroscopic fungi in National Park of Gunung Leuser, Blangjerango Gayo Lues. The methods used were direct observation and survey. The area of research was 5 Ha, divided into 5 stations with 10 transect stations for each. So, the number of transects were 50 transect stations with the length of 100 m, the width of the left and right was 20 m. The data were analyzed by descriptive analysis. The result showed that there were 28 species from 18 genera, namely Ganoderma, Grifola, Hexagonia, Hirchioporus, Pycnoporus, Tremella, Auricularia, Collybia, Coriolus, Hypholoma, Pleurotus, Phylloporus, Marasmius, Clavaria, Clitocybe, Crepidotus, Rigidoporus, Tremidis, Coriolus, Lactarius, Mycena, Clitocybe, Clitocybula, Pluteus, Pleurotus. The most common genera found in the location was 3 species from Ganoderma. It can be concluded that the wood macroscopic fungi in National Park of Gunung Leuser, Blangjerango Gayo Lues is suitable to be used for media in learning biology at school. Keywords: Macroscopic Fungi, Biology Learning and Media
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41

Serraglio, Riccardo. "Pedrinhas Paulista. Una colonia di emigranti italiani in Brasile negli anni della ricostruzione postbellica." TERRITORIO, no. 91 (June 2020): 128–37. http://dx.doi.org/10.3280/tr2019-091013.

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Nel 1952 la Compagnia Brasiliana di Colonizzazione e Immigrazione Italiana istituì la colonia agricola di Pedrinhas Paulista, riservata a lavoratori provenienti dall'Italia. L'architetto Rosario Megna curò la pianificazione urbana e territoriale del nuovo insediamento attenendosi ai principi della razionalità e dell'economia. Nel mezzo del latifondo organizzò un villaggio all'interno del quale erano distinti settori per gli edifici comunitari, per i quartieri residenziali e per gli impianti di trasformazione dei prodotti agricoli. Le case per i lavoratori, sia quelle disposte nell'area urbanizzata sia quelle nelle aree agricole, furono dotate di accessori adeguati alle condizioni locali. Le soluzioni urbanistiche e architettoniche elaborate da Megna hanno posto le basi per il successo della colonia di Pedrinhas, che al giorno d'oggi è una città di circa tremila abitanti sostenuta da una fiorente economia agricola.
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42

Mabija, Siviwe. "3D HYDRODYNAMIC MODELING TO CHARACTERISE THE BEHAVIOUR OF THE DISPOSAL OF DREDGED MATERIAL USING A VERTICAL TREMIE PIPE." Coastal Engineering Proceedings, no. 36 (December 30, 2018): 26. http://dx.doi.org/10.9753/icce.v36.sediment.26.

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Dredge plume modelling forms an integral part of the supporting studies for EIA applications for both capital and maintenance dredging projects. The behaviour of dredge plumes is function of many variables, many of which are unknown at the time of undertaking the studies. As such engineering judgment, previous project experience (including engaging dredging contractors) and available literature form part of the tools used to characterize the behaviour of dredge plumes. This paper summarises two case studies where underwater disposal (using a vertical tremie pipe) of dredge material from a cutter section (CSD) was simulated in order to meet the regulatory standard at the edge of mixing zone.
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43

Lee, Jung Ah, Jong Wook Kim, and Wan Soo Kim. "Effect of tremata closures on the oxygen consumption rhythm of ezo abalone Haliotis discus hannai." Aquaculture 270, no. 1-4 (September 2007): 312–20. http://dx.doi.org/10.1016/j.aquaculture.2007.04.007.

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44

Mansfield, Phyllis Kernoff, Molly Carey, Amy Anderson, Susannah Heyer Barsom, and Patricia Bartholow Koch. "Staging the menopausal transition: Data from the TREMIN Research Program on Women’s Health." Women's Health Issues 14, no. 6 (November 2004): 220–26. http://dx.doi.org/10.1016/j.whi.2004.08.002.

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45

Frýda, Jiří, Robert B. Blodgett, Alfred C. Lenz, and Štěpán Manda. "New porcellioidean gastropods from early Devonian of Royal Creek area, Yukon Territory, Canada, with notes on their early phylogeny." Journal of Paleontology 82, no. 3 (May 2008): 595–603. http://dx.doi.org/10.1666/07-024.1.

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This paper presents a description of new gastropods belonging to the superfamily Porcellioidea (Vetigastropoda) from the richly diverse Lower Devonian gastropod fauna of the Road River Formation in the Royal Creek area, Yukon Territory. This fauna belongs to Western Canada Province of the Old World Realm. The Pragian speciesPorcellia(Porcellia)yukonensisn. sp. andPorcellia(Paraporcellia) sp. represent the oldest presently known members of subgeneraPorcellia(Porcellia) andPorcellia(Paraporcellia). Their simple shell ornamentation fits well with an earlier described evolutionary trend in shell morphology of the Porcellinae. Late Pragian to early EmsianPerryconcha pulchran. gen. and n. sp. is the first member of the Porcellioidea bearing a row of tremata on adult teleoconch whorls. The occurrence of this shell feature in the Porcellioidea is additional evidence that the evolution of the apertural slit was much more complicated than has been proposed in classical models of Paleozoic gastropod evolution.
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46

Lihtenvalner, Katja. "»Pred tremi desetletji je bila evropa drugačna« - Srečanje z Lauretto Macauley." Andragoška spoznanja 21, no. 3 (October 28, 2015): 93–95. http://dx.doi.org/10.4312/as.21.3.93-95.

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47

Laufer, Y., L. Gattenio, E. Parnas, D. Sinai, Y. Sorek, and R. Dickstein. "Time-Related Changes in Motor Performance of the Upper Extremity Ipsilateral to the Side of the Lesion in Stroke Survivors." Neurorehabilitation and Neural Repair 15, no. 3 (September 2001): 167–72. http://dx.doi.org/10.1177/154596830101500303.

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Objective: The objective of the present study was to examine time-related changes in motor performance of daily tasks of the upper extremity ipsilateral to the side of le sion in poststroke hemiparetic patients Methods: Nine patients after an acute uni lateral cerebrovascular accident and 10 age-matched healthy controls were studied. Functional motor abilities of the upper extremity ipsilateral to side of lesion were ex amined over a 4-month time course, using validated measurement tools (Jebsen test of hand function, nine-hole peg test, and three functional activities of daily living). Results: The results indicated a significant impairment in the motor function of the hand ipsilateral to the side of brain lesion in comparison with the matched extremity in control subjects. They also pointed to time-related improvement in performance speed, implying that the deterioration in the functional performance of the upper ex tremity on the uninvolved body side of poststroke hemiparetic patients is not static and may improve with time. The findings further suggested that the left hand of pa tients with an intact right cerebral hemisphere improves more than does the right hand of their peers whose left cerebral hemisphere is intact. Conclusions: Due to the small sample size and methodologic considerations, further and more extensive work is re quired to determine difference in improvement in motor abilities of the ipsilateral left versus the ipsilateral right upper extremities in stroke survivors. Key Words: Stroke—Hand—Recovery.
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48

Wachtel, Nathan. "Francisco Maldonado de Silva." Annales. Histoire, Sciences Sociales 54, no. 4 (August 1999): 895–914. http://dx.doi.org/10.3406/ahess.1999.279787.

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Francisco Maldonado de Silva est l'un des plus fameux martyrs de l'histoire des judaïsants du Nouveau Monde. La vocation de martyr est certes rare : parmi les centaines de marranes condamnés au bûcher par l'Inquisition, bien peu finalement (une demi-douzaine environ sur le continent américain) consentirent à être brûlés vivants, c'est-à-dire à mourir en proclamant leur fidélité à la loi de Moïse. La mort de Francisco Maldonado de Silva lors de l'autodafé de 1639, à Lima, eut une immense répercussion dans les milieux juifs de l'Ancien Monde : son martyre, ainsi que ceux de Isaac de Castro Tartas (transféré du Brésil) lors de l'autodafé de Lisbonne en 1646, et de Tomas Tremino de Sobremonte lors de l'autodafé de Mexico en 1649, sont presque aussitôt glorifiés par Menasseh ben Israël dans son célèbre ouvrage, Espérance d'Israël, publié en 1652 à Amsterdam. Celuici inscrit ces événements tragiques parmi les épreuves contemporaines du peuple juif, et les interprète comme autant de signes annonçant l'approche des temps messianiques.
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49

Bacchielli, Lidiano. "Un Santuario di Frontiera, fra Polis E Chora." Libyan Studies 25 (January 1994): 45–59. http://dx.doi.org/10.1017/s0263718900006233.

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Nella campagna di scavi condotta a Cirene tra l'ottobre del 1910 ed il maggio del 1911 la Missione Archeologica Americana diretta da Richard Norton portava alia luce circa tremila statuine fittili, intere o quasi, ed una quantità innumerevole di testine ed altri frammenti.L'occasione per la scoperta era stata del tutto fortuita. Agli inizi di novembre del 1910 un arabo si era presentato al campo portando un cesto con 765 statuette di terracotta, che erano state scavate nel suo giardino posto alle pendici dell'Acropoli, nella parte nord-occidentale, al livello della Terrazza del Santuario di Apollo (la Myrtousa).Molte conversazioni e molti caffè consentirono al Norton l'inizio dello scavo, in una striscia piana posta a valle di un gradino roccioso. Nel sito non si rinvennero resti di edifici, ma diverse nicchie rettangolari scavate in alcuni speroni di roccia. Immediatamente davanti a queste vennero trovate le statuette di terracotta: esse formavano uno strato dello spessore di una novantina di centimetri.
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Baškienė, Audronė. "Šiaulių apskrities Povilo Višinskio viešosios bibliotekos darbuotojų egodokumentai: atsiminimai iš tremties, dienoraščiai." Bibliotheca Lituana 4 (November 4, 2018): 233–46. http://dx.doi.org/10.15388/biblita.2017.12138.

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[straipsnis ir santrauka lietuvių kalba; santrauka anglų kalba] Straipsnyje nagrinėjami bibliotekos rankraščių fonde saugomi darbuotojų, gimusių tremtyje ar išgyvenusių tremtį, atsiminimai bei dienoraščiai. Bibliotekininkė Nijolia Kasparavičienė buvusių politinių kalinių ir tremtinių, dirbančių bibliotekoje, atsiminimus sudėjo į kraštotyros darbą „Ilgi tremties metai“ (1991). Užrašyti dešimties darbuotojų atsiminimai, kurie papildyti nuotraukomis ir dokumentais. 1991 m. ir 1992 m. tremtiniai organizavo ekspedicijas į Kazachstaną ir Sibirą. Taip atsirado du dienoraščiai „Antroji ekspedicija į Karlagą“ (1991 rugpjūčio 9–19 d.) ir „Po Sibiro platybes“ (1992 rugpjūčio 4–22 d.). Įspūdžius dienoraščio forma užrašė bibliotekininkė, tremtinių dukra Nijolia Kasparavičienė. Pagrindinė mintis atsiminimuose – asmeninis likimas siejamas su Lietuvos likimu. Dienoraščiuose fiksuojamos aplankytos vietos, minimi sutikti žmonės, perteikiamas jų požiūris į praeitį, nuomonė apie nepriklausomos Lietuvos ateitį. Dienoraščių autorė nesinaudojo jokia literatūra, istorine medžiaga. Tai padieniui užfiksuoti faktai ir asmeniniai išgyvenimai.
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