Статті в журналах: "Ischimia"

1

Nagaro, Takumi, and Shigeo Kimura. "re: Reply to Ischia and Ischia." Pain 32, no. 3 (March 1988): 384. http://dx.doi.org/10.1016/0304-3959(88)90052-8.

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2

Boisset, F. "Contribución al conocimiento algológico del Litoral Levantino. I." Acta Botanica Malacitana 11 (December 1, 1986): 3–8. http://dx.doi.org/10.24310/actabotanicaabmabm.v11i.9456.

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Se señalan doce especies de algas para el litoral Levantino, con referencias sobre su hábitat y aspectos fenológicos. Destacan Antithamnion antillanos y Pseudocrouania ischiana citadas por primera vez en el litoral mediterráneo español.

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3

Davidson, Chad. "From Ischia, and: Illuminations." Hopkins Review 14, no. 1 (2021): 45–47. http://dx.doi.org/10.1353/thr.2021.0006.

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4

Szilágyi, János György. "Attikától Narcéig - via Ischia." Antik Tanulmányok 47, no. 1 (December 1, 2003): 35–61. http://dx.doi.org/10.1556/anttan.47.2003.1.2.

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Az ókorkutatás legfontosabb feladatai közé tartozik, hogy korunk aktuális problémáinak megoldásához adjon segítséget. Az egyik ezek közül az akkulturációé, vagyis annak a vizsgálata, hogyan viselkednek az egymással érintkező, különböző hagyományokra épülő kultúrák e találkozás során. Egy másik az a kérdés, mit nyújthat a kortárs művészet megértéséhez az antik művészetek hagyatékának tanulmányozása, és ennek másik oldala: miben segítheti a modern művészet jelenségeinek ismerete az antik művészetek egyes vonásainak jobb megértését. A tanulmány a Szépművészeti Múzeum egy eddig közöletlen Kr. e. 700 körül készült etruszk vázájának formáját és díszítését elemezve kísérel meg legalább részlegesen választ adni a két kérdésre, és ennek során egy Veiiben dolgozó vázafestőnek műveiből kirajzolódó portréját próbálja meg felvázolni.

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5

Hennemann, H. H., and P. Pfiester. "Kala-Azar aus Ischia." DMW - Deutsche Medizinische Wochenschrift 112, no. 40 (March 25, 2008): 1539–42. http://dx.doi.org/10.1055/s-2008-1068287.

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6

Sbrana, Alessandro, Paola Marianelli, and Giuseppe Pasquini. "Volcanology of Ischia (Italy)." Journal of Maps 14, no. 2 (August 2, 2018): 494–503. http://dx.doi.org/10.1080/17445647.2018.1498811.

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7

Lauritano, C., M. Ruocco, E. Dattolo, M. C. Buia, J. Silva, R. Santos, I. Olivé, M. M. Costa, and G. Procaccini. "Response of key stress-related genes of the seagrass <i>Posidonia oceanica</i> in the vicinity of submarine volcanic vents." Biogeosciences Discussions 12, no. 6 (March 30, 2015): 4947–71. http://dx.doi.org/10.5194/bgd-12-4947-2015.

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Abstract. Submarine volcanic vents are being used as natural laboratories to assess the effects of CO2 on marine organisms and communities, as this gas is the main component of emissions. Seagrasses should positively react to increased dissolved carbon, but in vicinity of volcanic vents there may be toxic substances, that can have indirect effects on seagrasses. Here we analysed the expression of 35 stress-related genes in the Mediterranean keystone seagrass species P. oceanica in the vicinity of submerged volcanic vents located in the Islands of Ischia and Panarea, Italy, and compared them with those from control sites away from the influence of vents. Reverse Transcription-Quantitative Polymerase Chain Reaction (RT-qPCR) was used to characterize the expression levels of genes. Fifty one per cent of genes analysed showed significant expression changes. Metal detoxification genes were mostly down-regulated in relation to controls both in Ischia and Panarea locations, indicating that P. oceanica does not increase the synthesis of heavy metal detoxification proteins in response to the environmental conditions present at the two vents. The expression levels of genes involved in free radical detoxification indicate that, in contrast with Ischia, P. oceanica at the Panarea vent face stressors that result in the production of reactive oxygen species triggering antioxidant responses. In addition, heat shock proteins were also activated at Panarea and not at Ischia. Overall, our study reveals that P. oceanica is generally under higher stress in the vicinity of the vents at Panarea than at Ischia, possibly resulting from environmental and evolutionary differences existing between the two volcanic sites. This is the first study analysing gene responses in marine plants living near natural CO2 vents and our results call for a careful consideration of factors, other than CO2 and acidification, that can cause stress to seagrasses and other organisms near volcanic vents.

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8

Pelullo, C., G. Cirillo, R. S. Iovine, I. Arienzo, M. Aulinas, L. Pappalardo, P. Petrosino, J. L. Fernandez-Turiel, and M. D’Antonio. "Geochemical and Sr–Nd isotopic features of the Zaro volcanic complex: insights on the magmatic processes triggering a small-scale prehistoric eruption at Ischia island (south Italy)." International Journal of Earth Sciences 109, no. 8 (October 1, 2020): 2829–49. http://dx.doi.org/10.1007/s00531-020-01933-6.

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Abstract The prehistoric (< 7 ka) Zaro eruption at Ischia island (Southern Italy) produced a lava complex overlaying a pyroclastic deposit. Although being of low energy, the Zaro eruption might have caused casualties among the neolithic population that inhabited that area of Ischia, and damages to their settlements. A similar eruption at Ischia with its present-day population would turn into a disaster. Therefore, understanding the magmatic processes that triggered the Zaro eruption would be important for volcanic hazard assessment and risk mitigation, so as to improve a knowledge that can be applied to other active volcanic areas worldwide. The main Zaro lava body is trachyte and hosts abundant mafic and felsic enclaves. Here all juvenile facies have been fully characterized from petrographic, geochemical and isotopic viewpoints. The whole dataset (major and trace element contents; Sr–Nd isotopic composition) leads to rule out a genetic link by fractional crystallization among the variable facies. Thus, we suggest that the Zaro mafic enclaves could represent a deep-origin mafic magma that mingled/mixed with the main trachytic one residing in the Ischia shallow magmatic system. The intrusion of such a mafic magma into a shallow reservoir filled by partly crystallized, evolved magma could have destabilized the magmatic system presumably acting as a rapid eruption trigger. The resulting processes of convection, mixing and rejuvenation have possibly played an important role in pre- and syn-eruptive phases also in several eruptions of different sizes in the Neapolitan area and elsewhere in the world.

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9

D'Auria, Luca, Flora Giudicepietro, Anna Tramelli, Patrizia Ricciolino, Domenico Lo Bascio, Massimo Orazi, Marcello Martini, Rosario Peluso, Giovanni Scarpato, and Antonietta Esposito. "The Seismicity of Ischia Island." Seismological Research Letters 89, no. 5 (July 11, 2018): 1750–60. http://dx.doi.org/10.1785/0220180084.

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10

Aiello, Gemma, and Mauro Caccavale. "From Siliciclastic to Bioclastic Deposits in the Gulf of Naples: New Highlights from Offshore Ischia and Procida–Pozzuoli Based on Sedimentological and Seismo-Stratigraphic Data." Quaternary 4, no. 4 (December 3, 2021): 44. http://dx.doi.org/10.3390/quat4040044.

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This study discusses the siliciclastic to bioclastic deposits (in particular, the rhodolith deposits) in the Gulf of Naples based on sedimentological and seismo-stratigraphic data. The selected areas are offshore Ischia Island (offshore Casamicciola, Ischia Channel), where a dense network of sea-bottom samples has been collected, coupled with Sparker Multi-tip seismic lines, and offshore Procida–Pozzuoli (Procida Channel), where sea-bottom samples are available, in addition to Sparker seismic profiles. The basic methods applied in this research include sedimentological analysis, processing sedimentological data, and assessing seismo-stratigraphic criteria and techniques. In the Gulf of Naples, and particularly offshore Ischia, bioclastic sedimentation has been controlled by seafloor topography coupled with the oceanographic setting. Wide seismo-stratigraphic units include the bioclastic deposits in their uppermost part. Offshore Procida–Pozzuoli, siliciclastic deposits appear to prevail, coupled with pyroclastic units, and no significant bioclastic or rhodolith deposits have been outlined based on sedimentological and seismo-stratigraphic data. The occurrence of mixed siliciclastic–carbonate depositional systems is highlighted in this section of the Gulf of Naples based on the obtained results, which can be compared with similar systems recognized in the central Tyrrhenian Sea (Pontine Islands).

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11

Buonocore, Berardino, Yuri Cotroneo, Vincenzo Capozzi, Giuseppe Aulicino, Giovanni Zambardino, and Giorgio Budillon. "Sea-Level Variability in the Gulf of Naples and the “Acqua Alta” Episodes in Ischia from Tide-Gauge Observations in the Period 2002–2019." Water 12, no. 9 (September 2, 2020): 2466. http://dx.doi.org/10.3390/w12092466.

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This work presents an 18-year-long (2002–2019) tide-gauge dataset collected on the Island of Ischia (Gulf of Naples, Southern Tyrrhenian Sea) that can contribute to the analysis of the basic features of sea-level variability in this region. Analysis of tidal constituents shows that the Gulf of Naples is characterized by the absence of any amphidromic system. In this area, sea-level changes due to the astronomical component of the tide are generally limited to ±20 cm with respect to the mean sea level, but the impact of this variability is enhanced by global sea-level increase and the effect of regional atmospheric perturbations that might also triple sea-level variations. The effects of these events, whose frequency has increased in recent decades, has been dramatic in coastal areas where intense social and economic activity occurs, e.g., in Ischia. On interannual time scales, the results indicate that the relative sea-level rise in Ischia has a magnitude of 3.9 mm/year. Special attention is dedicated to the “acqua alta” episodes and to their linkage with long-term sea-level trends and atmospheric forcing.

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12

BERTHELOT, JEAN-MARIE, STEPHANE VARIN, FLORENCE CAILLON, ALAIN PROST, and YVES MAUGARS. "PSEUDOMONAS AERUGINOSA OSTEOMYELITIS OF BOTH ISCHIA." Journal of Bone and Joint Surgery-American Volume 84, no. 3 (March 2002): 441–44. http://dx.doi.org/10.2106/00004623-200203000-00017.

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13

Buchner, Giorgio, Antonino Italiano, and Claudio Vita-Finzi. "Recent uplift of Ischia, southern Italy." Geological Society, London, Special Publications 110, no. 1 (1996): 249–52. http://dx.doi.org/10.1144/gsl.sp.1996.110.01.19.

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14

BERRINO, Giovanna, Peter VAJDA, Pavol ZAHOREC, Antonio G. CAMACHO, Vincenzo DE NOVELLIS, Stefano CARLINO, Juraj PAPČO, Eliana BELLUCCI SESSA, and Richard CZIKHARDT. "Interpretation of spatiotemporal gravity changes accompanying the earthquake of 21 August 2017 on Ischia (Italy)." Contributions to Geophysics and Geodesy 51, no. 4 (December 22, 2021): 345–71. http://dx.doi.org/10.31577/congeo.2021.51.4.3.

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We analyse spatiotemporal gravity changes observed on the Ischia island (Italy) accompanying the destructive earthquake of 21 August 2017. The 29 May 2016 to 22 September 2017 time-lapse gravity changes observed at 18 benchmarks of the Ischia gravimetric network are first corrected for the gravitational effect of the surface deformation using the deformation-induced topographic effect (DITE) correction. The co-seismic DITE is computed by Newtonian volumetric integration using the Toposk software, a high-resolution LiDAR DEM and the co-seismic vertical displacement field derived from Sentinel-1 InSAR data. We compare numerically the DITE field with its commonly used Bouguer approximation over the island of Ischia with the outcome that the Bouguer approximation of DITE is adequate and accurate in this case. The residual gravity changes are then computed at gravity benchmarks by correcting the observed gravity changes for the planar Bouguer effect of the elevation changes at benchmarks over the same period. The residual gravity changes are then inverted using an inversion approach based on model exploration and growing source bodies, making use of the Growth-dg inversion tool. The found inversion model, given as subsurface time-lapse density changes, is then interpreted as mainly due to a co-seismic or post-seismic disturbance of the hydrothermal system of the island. Pros and weak points of such interpretation are discussed.

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15

Conde, F., and J. Soto. "Notas corológicas del macrofitobentos de Andalucía (España)." Acta Botanica Malacitana 11 (December 1, 1986): 9–16. http://dx.doi.org/10.24310/actabotanicaabmabm.v11i.9457.

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Ampliamos el catálogo para las costas andaluzas en 32 especies, de las cuales, 7 son nuevas citas para la Península Ibérica Audouinella endozoica (Darb.) Dixon, Fosliella minutula (Fosl.) Ganesan, Lomentaria compressa (Kütz.) Kylin, Polysuphonia cladorrhiza Ardiss., P. ruchingeri C. Ag., P. stuposa Zanard. y Pseudocrouania ischiana Funk y otras 4 lo son para el Mediterráneo español: Audouinella Thuretii (Born.) Wölkerling, feldmannia simplex (Crouan frat.) Hamel, Phaeophila wittrockii (Wille) Nielsen y Ralfsia bornetti Kuckut.

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16

Murray, R. D., T. A. Cartwright, D. Y. Downham, and M. A. Murray. "Some maternal factors associated with dystocia in Belgian Blue cattle." Animal Science 69, no. 1 (August 1999): 105–13. http://dx.doi.org/10.1017/s1357729800051134.

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AbstractMeasurements of conformation and pelvic characteristics of pedigree Belgian Blue cows were compared in cattle from 11 herds. In seven herds comprising 56 cows caesarean sections were routinely used to deliver pedigree calves and in four herds comprising 52 cows they were given the opportunity to calve naturally per vaginum. Cows in the seven herds were approximately 10 months younger than those in the other herds. External pelvic measurements were linear distances between the tuber coxae, between the tuber coxarum and the tuber ischium, between the tuber ischii, the vertical distance between the underside of the tail and the tuber ischii, and heights of the tuber coxae and tuber ischii from the floor. Internal pelvic measurements were the vertical distance between the ventral body of the sacrum and the pubic symphysis and the horizontal distance between the wings of the ileum at the widest point of the pelvic inlet, both made with a Rice pelvimeter. Condition scores were assessed for all cows. There were correlations (P < 0·001) between internal pelvic height and width, external measurements, and age. For cattle that calved unassisted, pelvic height (P < 0·05) and area (P < 0·05) were significantly larger than those delivered by elective caesarean section. From internal pelvic measurements of 74 cows, those which always delivered live calves had a larger pelvic area (P < 0·01) than cows that delivered a dead foetus following any parturition.

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17

Lauritano, C., M. Ruocco, E. Dattolo, M. C. Buia, J. Silva, R. Santos, I. Olivé, M. M. Costa, and G. Procaccini. "Response of key stress-related genes of the seagrass <i>Posidonia oceanica</i> in the vicinity of submarine volcanic vents." Biogeosciences 12, no. 13 (July 15, 2015): 4185–94. http://dx.doi.org/10.5194/bg-12-4185-2015.

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Abstract. Submarine volcanic vents are being used as natural laboratories to assess the effects of increased ocean acidity and carbon dioxide (CO2) concentration on marine organisms and communities. However, in the vicinity of volcanic vents other factors in addition to CO2, which is the main gaseous component of the emissions, may directly or indirectly confound the biota responses to high CO2. Here we used for the first time the expression of antioxidant and stress-related genes of the seagrass Posidonia oceanica to assess the stress levels of the species. Our hypothesis is that unknown factors are causing metabolic stress that may confound the putative effects attributed to CO2 enrichment only. We analyzed the expression of 35 antioxidant and stress-related genes of P. oceanica in the vicinity of submerged volcanic vents located in the islands of Ischia and Panarea, Italy, and compared them with those from control sites away from the influence of vents. Reverse-transcription quantitative polymerase chain reaction (RT-qPCR) was used to characterize gene expression patterns. Fifty-one percent of genes analyzed showed significant expression changes. Metal detoxification genes were mostly down-regulated in relation to controls at both Ischia and Panarea, indicating that P. oceanica does not increase the synthesis of heavy metal detoxification proteins in response to the environmental conditions present at the two vents. The up-regulation of genes involved in the free radical detoxification response (e.g., CAPX, SODCP and GR) indicates that, in contrast with Ischia, P. oceanica at the Panarea site faces stressors that result in the production of reactive oxygen species, triggering antioxidant responses. In addition, heat shock proteins were also activated at Panarea and not at Ischia. These proteins are activated to adjust stress-accumulated misfolded proteins and prevent their aggregation as a response to some stressors, not necessarily high temperature. This is the first study analyzing the expression of target genes in marine plants living near natural CO2 vents. Our results call for contention to the general claim of seagrasses as "winners" in a high-CO2 world, based on observations near volcanic vents. Careful consideration of factors that are at play in natural vents sites other than CO2 and acidification is required. This study also constitutes a first step for using stress-related genes as indicators of environmental pressures in a changing ocean.

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18

Sandro de Vita, Mauro Antonio Di Vito, Diana Barra, Giuseppe Aiello, and Costanza Gialanella. "Disseminating the knowledge on the complex interactions between humans and volcanoes: the geological section of the Villa Arbusto archaeological museum at Lacco Ameno (Ischia, Naples - Italy)." Annals of Geophysics 64, no. 5 (December 13, 2021): VO544. http://dx.doi.org/10.4401/ag-8666.

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A room in the Archaeological Museum of Villa Arbusto (Lacco Ameno, Ischia) was set up to house rocks and fossils collected by the renowned archaeologist Giorgio Buchner during his excavation activity on the Island of Ischia. The collection is witness to a long multidisciplinary research activity that saw archaeological studies at the center of volcanological, pedological and palaeoenvironmental researches, aimed at reconstructing the archaeological contexts in the complex geological dynamics of the island. In fact, during the different phases of colonization recorded on the island, the Ischia volcanoes were very active and produced explosive and effusive eruptions, accompanied by a strong geological dynamics that included earthquakes, landslides (even gigantic ones), rapid ground uplift and strong hydrothermal activity. In the room, the samples on display “tell” the evolution of the island and its dynamics in four windows and a chest of drawers, where there is an exposition of the products of the various eruptions, from the oldest to the most recent, sedimentary rocks and the collection of macro and microfossils found in marine sediments, displaced at variable altitudes by the rapid volcano-tectonic deformations that characterize the island. A series of panels and monitors accompany the visitor along a path that, starting from the geological evolution of the island, passes through the relationship between humans and the volcano, the main volcanic phenomena and the reconstruction of an archaeological excavation of exceptional value, where it is possible to see the strong interaction between primary and secondary volcanic phenomena and a human settlement of the first Greek colony in the west: Pithecusae. The exhibition was designed with the purpose of educating the visitors and the local population about the natural history of the island and its volcanoes, and their impact on the human life through time.

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19

Cusano, Paola, Simona Petrosino, Enza De Lauro, Salvatore De Martino, and Mariarosaria Falanga. "Characterization of the seismic dynamical state through joint analysis of earthquakes and seismic noise: the example of Ischia Volcanic Island (Italy)." Advances in Geosciences 52 (April 9, 2020): 19–28. http://dx.doi.org/10.5194/adgeo-52-19-2020.

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Abstract. This work is devoted to the study of both earthquakes and background seismic noise at Ischia Island (Italy) recorded pre and post the Md 4.0 earthquake occurred on 21 August 2017 (18:57 UTC). We compare and characterize noise and earthquakes in terms of Independent Component Analysis, energy and polarization properties. The earthquakes' waveforms and the background noise are decomposed into a few independent components with two main common signals peaked around 1–2 and 3–4 Hz, respectively. A slight increase of the energy of the background seismic noise is observed comparing samples recorded in 2016 and 2017, whereas no variations are detected in 2017 pre and post the main earthquake. The polarization analysis, performed in the frequency bands individuated by Independent Component Analysis and applied to the background seismic noise, indicates a shallow propagation and the azimuthal pattern is mainly controlled by the local structural features. These results suggest that noise and earthquakes are ascribable to a common phenomenon of fluid-solid interaction in the hydrothermal system of Ischia Island.

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20

Galvani, Alessandro, Giuseppe Pezzo, Vincenzo Sepe, and Guido Ventura. "Shrinking of Ischia Island (Italy) from Long-Term Geodetic Data: Implications for the Deflation Mechanisms of Resurgent Calderas and Their Relationships with Seismicity." Remote Sensing 13, no. 22 (November 18, 2021): 4648. http://dx.doi.org/10.3390/rs13224648.

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The identification of the mechanisms responsible for the deformation of calderas is of primary importance for our understanding of the dynamics of magmatic systems and the evaluation of volcanic hazards. We analyze twenty years (1997–2018) of geodetic measurements on Ischia Island (Italy), which include the Mt. Epomeo resurgent block, and is affected by hydrothermal manifestations and shallow seismicity. The data from the GPS Network and the leveling route show a constant subsidence with values up to −15 ± 2.0 mm/yr and a centripetal displacement rate with the largest deformations on the southern flank of Mt. Epomeo. The joint inversion of GPS and levelling data is consistent with a 4 km deep source deflating by degassing and magma cooling below the southern flank of Mt. Epomeo. The depth of the source is supported by independent geophysical data. The Ischia deformation field is not related to the instability of the resurgent block or extensive gravity or tectonic processes. The seismicity reflects the dynamics of the shallow hydrothermal system being neither temporally nor spatially related to the deflation.

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21

Carlino, Stefano. "Review article: Brief history of volcanic risk in the Neapolitan area (Campania, southern Italy): a critical review." Natural Hazards and Earth System Sciences 21, no. 10 (October 15, 2021): 3097–112. http://dx.doi.org/10.5194/nhess-21-3097-2021.

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Abstract. The presence of three active volcanoes (Vesuvius, Campi Flegrei and Ischia island) along the coast of Naples did not contain the huge expansion of the urbanized zones around them. In contrast, since the Greco-Roman era, volcanoes have featured among the favourite sites for people colonizing the Campania region. The stable settlements around Vesuvius, Campi Flegrei caldera and Ischia were progressively enlarged, attaining a maximum growth rate between 1950 and 1980. Between 1982 and 1984, Neapolitans faced the last and most dramatic volcanic crises, which occurred at Campi Flegrei (Pozzuoli) without an eruption. Since that time, volcanologists have focused their attention on the problem of risks associated with eruptions in the Neapolitan area, but a systematic strategy to reduce the very high volcanic risk of this zone is still lacking. A brief history of volcanic risk in the Neapolitan district is narrated here in an effort to provide new food for thought for the scientific community that works for the mitigation of volcanic risk in this area.

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22

De Martino, Prospero, Mario Dolce, Giuseppe Brandi, Giovanni Scarpato, and Umberto Tammaro. "The Ground Deformation History of the Neapolitan Volcanic Area (Campi Flegrei Caldera, Somma–Vesuvius Volcano, and Ischia Island) from 20 Years of Continuous GPS Observations (2000–2019)." Remote Sensing 13, no. 14 (July 11, 2021): 2725. http://dx.doi.org/10.3390/rs13142725.

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The Neapolitan volcanic area includes three active and high-risk volcanoes: Campi Flegrei caldera, Somma–Vesuvius, and Ischia island. The Campi Flegrei volcanic area is a typical example of a resurgent caldera, characterized by intense uplift periods followed by subsidence phases (bradyseism). After about 21 years of subsidence following the 1982–1984 unrest, a new inflation period started in 2005 and, with increasing rates over time, is ongoing. The overall uplift from 2005 to December 2019 is about 65 cm. This paper provides the history of the recent Campi Flegrei caldera unrest and an overview of the ground deformation patterns of the Somma–Vesuvius and Ischia volcanoes from continuous GPS observations. In the 2000–2019 time span, the GPS time series allowed the continuous and accurate tracking of ground and seafloor deformation of the whole volcanic area. With the aim of improving the research on volcano dynamics and hazard assessment, the full dataset of the GPS time series from the Neapolitan volcanic area from January 2000 to December 2019 is presented and made available to the scientific community.

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23

West, M. L. "Grated Cheese Fit for Heroes." Journal of Hellenic Studies 118 (November 1998): 190–91. http://dx.doi.org/10.2307/632242.

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The scene inIliad11 where Nestor's slave Hekamede prepares a restorative κυκεών for his guests in his great cup, which only he can lift when it is full, has often been cited in connection with the skyphos from Ischia, dated toc.735–720 BC, with its verse inscription that alludes to Nestor's εὔποτον ποτήριον. Now that scholarly opinion is increasingly swinging towards a seventh-century dating for theIliad, it seems more prudent than ever to see the Ischia inscription as a reflex not of ourIliadbut of a similar Nestorian drinking episode in earlier epic tradition. His cup, as described, has features of a Bronze Age vessel; and the motif of the mighty goblet is paralleled in the Ugaritic Baal epic, current not later than the fourteenth century.Here I want to consider another element in the scene, namely the grated cheese which Hekamede adds to her posset. I hope to show, by a combination of metrics and archaeology, that this too, even though it cannot be traced back to the Bronze Age, belongs to a traditional account that is many generations older than ourIliad.

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24

Perrotta, Silverio, Bruno Nobili, Marcella Ferraro, Carmela Migliaccio, Adriana Borriello, Valeria Cucciolla, Vincenzo Martinelli, et al. "Von Hippel-Lindau–dependent polycythemia is endemic on the island of Ischia: identification of a novel cluster." Blood 107, no. 2 (January 15, 2006): 514–19. http://dx.doi.org/10.1182/blood-2005-06-2422.

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Abstract Chuvash polycythemia (MIM 263400) is an autosomal recessive disorder characterized by a high hemoglobin level, relatively high serum erythropoietin, and early death. It results from a Von Hippel-Lindau (VHL) gene mutation (C598T) that causes increased HIF-1α activity and erythrocyte production in the face of normoxia. This polycythemia is endemic in Chuvashia, whereas its worldwide frequency is very low. We investigated the incidence of the Chuvash-type VHL mutation in Campania (South Italy) and identified 14 affected subjects (5 families). Twelve live on the island of Ischia (Bay of Naples). From analysis of the mutated allele, we found that the disease was more frequent on Ischia (0.070) than in Chuvashia (0.057). The haplotype of all patients matched that identified in the Chuvash cluster, thereby supporting the single-founder hypothesis. We also found that nonaffected heterozygotes had increased HIF-1α activity, which might confer a biochemical advantage for mutation maintenance. In conclusion, we have identified the first large cluster of Chuvash erythrocytosis outside Chuvashia, which suggests that this familial polycythemia might be endemic in other regions of the world.

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25

Pugliese, Mariagabriella, Maria Quarto, Filomena Loffredo, Agostino Mazzella, and Vincenzo Roca. "Indoor Radon Concentrations in Dwellings of Ischia Island." Journal of Environmental Protection 04, no. 08 (2013): 37–39. http://dx.doi.org/10.4236/jep.2013.48a2005.

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26

Pecoraino, G., L. Brusca, W. D'Alessandro, S. Giammanco, S. Inguaggiato, and M. Longo. "Total CO2 output from Ischia Island volcano (Italy)." GEOCHEMICAL JOURNAL 39, no. 5 (2005): 451–58. http://dx.doi.org/10.2343/geochemj.39.451.

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27

Ricciardi, M., R. Nazzaro, G. Caputo, A. De Natale, and G. Vallariello. "La flora dell'isola di Ischia (Golfo di Napoli)." Webbia 59, no. 1 (January 2004): 1–113. http://dx.doi.org/10.1080/00837792.2004.10670763.

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28

KOMAI, TOMOYUKI, and TIN-YAM CHAN. "A new genus and two new species of alvinocaridid shrimps (Crustacea: Decapoda: Caridea) from a hydrothermal vent field off northeastern Taiwan." Zootaxa 2372, no. 1 (February 26, 2010): 15–32. http://dx.doi.org/10.11646/zootaxa.2372.1.3.

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Two new species of alvinocaridid shrimps are described from a hydrothermal vent field off northeastern Taiwan at depths of 252–300 m. Alvinocaris chelys n. sp. is morphologically very similar to A. williamsi Shank & Martin, 2003 from the Mid-Atlantic Ridge, and A. alexander Ahyong, 2009 from the southern Kermadec Ridge. These three species can be differentiated by the shape of the postrostral ridge, telson, the second segment of the antennular peduncle and the armature of the meri and ischia of the third pereopod. The second new species, although rather similar to Alvinocaris niwa Webber, 2004 from the Kermadec-Arc, is assigned to a new genus Alvinocaridinides gen. nov., which appears to be intermediate between Shinkaicaris Komai & Segonzac, 2005 and other derived genera including Opaepele Williams & Dobbs, 1995, Chorocaris Martin & Hessler, 1990 and Rimicaris Williams & Rona, 1986. Alvinocaridinides formosa n. sp. differs from Alvinocaris niwa by completely lacking any armature on the ischia of the third to fifth pereopods and by bearing two movable spines at the posterolateral angle of the uropodal exopod. These records constitute the first discovery of the family Alvinocarididae in Taiwanese waters and represent the shallowest occurrence for alvinocaridid shrimps.

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Schweickard, Wolfgang. "Ven. schena / schina." Zeitschrift für romanische Philologie 135, no. 4 (November 12, 2019): 1074–79. http://dx.doi.org/10.1515/zrp-2019-0061.

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Abstract The term schena / schina ‘measure of length in use in the field of cloth trade’ mainly appears in Venetian sources. The meaning derives from the special terminology of cloth manufacturing, where schena / schina refer to the centre of the surface of the cloth and to its central vertical fold. So far the etymology has not yet been explicitly and convincingly explained. In consideration of the material history of cloth production, the respective terminology, the equivalents in other languages and the forms of the word (schena, schina, schiena, ischiena), however, there is no doubt that the Venetian group has the same origin as It. schiena ‘back’.

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30

Guidetti, Paolo, Carlo Nike Bianchi, Gabriele La Mesa, Milena Modena, Carla Morri, Giampietro Sara, and Marino Vacchi. "Abundance and size structure of Thalassoma pavo (Pisces: Labridae) in the western Mediterranean Sea: variability at different spatial scales." Journal of the Marine Biological Association of the United Kingdom 82, no. 3 (June 2002): 495–500. http://dx.doi.org/10.1017/s0025315402005775.

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The present study was carried out during the summer of 1997 in three locations of the western Italian coast (La Spezia, Ligurian Sea; Ischia, central Tyrrhenian Sea; Ustica, southern Tyrrhenian Sea) to investigate variability in abundance and size structure of the labrid fish Thalassoma pavo along a latitudinal gradient and over different spatial scales. Fish abundance and size were estimated by visual census in shallow rocky reefs. Significant differences were detected in average abundances of T. pavo (with and without the contribution of juveniles) among locations (separated by a distance of hundreds of kilometres from each other) and over the smallest scale examined (i.e. among sites located tens of metres from each other). However, most variability was explained considering the largest spatial scale associated with the latitudinal gradient. Average abundances generally decreased from the southern Tyrrhenian to the Ligurian Sea. In terms of frequency, juveniles (<5 cm total length (TL)) increased from north to south, while the largest fish (16–20 cm) displayed an opposite trend. The intermediate size-classes (6–10 and 11–15 cm) did not show any distinct patterns. In terms of abundance, small T. pavo (0–5 cm) showed significantly higher densities at Ustica, followed by Ischia and La Spezia. Fish 6–10 and 11–15 cm long were significantly less abundant at La Spezia than at Ischia and Ustica, while those between 16 and 20 cm TL did not differ numerically among the three locations. The results of the present study provide suggestive evidence that factors acting on a geographical scale are likely to influence distribution patterns of the thermophilic fish T. pavo, although significant effects have been also observed at the smallest spatial scale examined. Climatic conditions (e.g. water temperature along the latitudinal gradient) and substrate features (e.g. macroalgal cover, physical complexity, slope) are thus likely to affect average abundances and size structures of T. pavo populations along the western Italian coast.

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Hahn, S., R. Rodolfo-Metalpa, E. Griesshaber, W. W. Schmahl, D. Buhl, J. M. Hall-Spencer, C. Baggini, K. T. Fehr, and A. Immenhauser. "Marine bivalve geochemistry and shell ultrastructure from modern low pH environments." Biogeosciences Discussions 8, no. 5 (October 24, 2011): 10351–88. http://dx.doi.org/10.5194/bgd-8-10351-2011.

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Abstract. Bivalve shells can provide excellent archives of past environmental change but have not been used to interpret ocean acidification events. We investigated carbon, oxygen and trace element records from different shell layers in the mussels Mytilus galloprovincialis (from the Mediterranean) and M. edulis (from the Wadden Sea) combined with detailed investigations of the shell ultrastructure. Mussels from the harbour of Ischia (Mediterranean, Italy) were transplanted and grown in water with mean pHT 7.3 and mean pHT 8.1 near CO2 vents on the east coast of the island of Ischia. The shells of transplanted mussels were compared with M. edulis collected at pH ~8.2 from Sylt (German Wadden Sea). Most prominently, the shells recorded the shock of transplantation, both in their shell ultrastructure, textural and geochemical record. Shell calcite, precipitated subsequently under acidified seawater responded to the pH gradient by an in part disturbed ultrastructure. Geochemical data from all test sites show a strong metabolic effect that exceeds the influence of the low-pH environment. These field experiments showed that care is needed when interpreting potential ocean acidification signals because various parameters affect shell chemistry and ultrastructure. Besides metabolic processes, seawater pH, factors such as salinity, water temperature, food availability and population density all affect the biogenic carbonate shell archive.

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32

D'Antonio, Massimo, Ilenia Arienzo, Richard J. Brown, Paola Petrosino, Carlo Pelullo, and Biagio Giaccio. "Petrography and Mineral Chemistry of Monte Epomeo Green Tuff, Ischia Island, South Italy: Constraints for Identification of the Y-7 Tephrostratigraphic Marker in Distal Sequences of the Central Mediterranean." Minerals 11, no. 9 (August 31, 2021): 955. http://dx.doi.org/10.3390/min11090955.

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The 56 ka Monte Epomeo Green Tuff (MEGT) resulted from the largest volume explosive eruption from Ischia island (south Italy). Its tephra is one of the main stratigraphic markers of the central Mediterranean area. Despite its importance, a detailed characterisation of the petrography and mineral chemistry of MEGT is lacking. To fill this gap, we present detailed petrographic description and electron microprobe mineral chemistry data on samples collected on-land from the MEGT. Juvenile clasts include pumice, scoria, and obsidian fragments with porphyritic/glomeroporphyritic, vitrophyric, and fragmental textures. The porphyritic index is 13–40 vol.%, and phenocryst phases include alkali-feldspar, plagioclase, clinopyroxene, ferrian phlogopite, and titano-magnetite, in order of decreasing abundance; accessory phases include sphene, hydroxy-fluor-apatite, and rare edenite. Plagioclase varies from predominant andesine to subordinate oligoclase, whereas alkali-feldspar is more variable from sanidine to anorthoclase; quasi-pure sanidine commonly occurs as either rim or recrystallisation overgrowth of large phenocrysts due to hydrothermal alteration. Secondary minerals include veins and patches of carbonate minerals, Fe-Mn oxyhydroxides, clay minerals, and zeolites. Clinopyroxene is ferroan diopside (En45–29Fs7–27) and never reaches Na-rich compositions. This feature allows the discrimination of MEGT from aegirine-bearing, distal tephra layers erroneously attributed to MEGT, with implications for the areal distribution of Ischia explosive deposits.

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33

de Alteriis, G., and C. Violante. "Catastrophic landslides off Ischia volcanic island (Italy) during prehistory." Geological Society, London, Special Publications 322, no. 1 (2009): 73–104. http://dx.doi.org/10.1144/sp322.3.

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34

Alberico, Ines, and Paola Petrosino. "Territorial evolution and volcanic hazard, Ischia Island (Southern Italy)." Journal of Maps 10, no. 2 (March 7, 2014): 238–48. http://dx.doi.org/10.1080/17445647.2014.893846.

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35

Carlino, Stefano, Nicola Alessandro Pino, Anna Tramelli, Vincenzo De Novellis, and Vincenzo Convertito. "A common source for the destructive earthquakes in the volcanic island of Ischia (Southern Italy): insights from historical and recent seismicity." Natural Hazards 108, no. 1 (March 15, 2021): 177–201. http://dx.doi.org/10.1007/s11069-021-04675-z.

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AbstractThe island of Ischia, located in the Gulf of Naples, represents an unusual case of resurgent caldera where small-to-moderate magnitude volcano-tectonic earthquakes generate large damage and catastrophic effects, as in the case of 4 March 1881 (Imax-VIII-IXMCS) and 28 July 1883 (Imax X-XI MCS) historical earthquakes, and of the recent 21 August 2017 MW = 3.9, event. All these earthquakes struck the northern area of the island. With about 65,000 inhabitants, Ischia is a popular touristic destination for thermals baths, hosting more than 3,000,000 visitors per year, thus representing a high seismic risk area. Assessing its seismic potential appears a fundamental goal and, to this end, the estimate of the magnitude of significant historical events and the characterization of their source are crucial. We report here a reassessment of historical data of damage of 1881 and 1883 earthquakes to evaluate the main source parameters of these events (obtained with the BOXER and EXISM software) and quantitatively compare, for the first time, the results with the source characteristics, obtained from instrumental data, of the recent 2017 earthquake. The results allowed us to assess the location, as well as the possible dimension and the related maximum magnitude, of the seismogenic structure responsible for such damaging earthquakes. Our results also provide an additional framework to define the mechanisms leading to earthquakes associated with the dynamics of calderas.

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36

Cusano, P., S. Petrosino, E. De Lauro, and M. Falanga. "The whisper of the hydrothermal seismic noise at Ischia Island." Journal of Volcanology and Geothermal Research 389 (January 2020): 106693. http://dx.doi.org/10.1016/j.jvolgeores.2019.106693.

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37

Pace, Daniela S., Angelo Miragliuolo, Monica Mariani, Carlotta Vivaldi, and Barbara Mussi. "Sociality of sperm whale off Ischia Island (Tyrrhenian Sea, Italy)." Aquatic Conservation: Marine and Freshwater Ecosystems 24, S1 (June 20, 2014): 71–82. http://dx.doi.org/10.1002/aqc.2459.

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38

Di Napoli, Rossella, Cinzia Federico, Alessandro Aiuppa, Massimo D’Antonio, and Mariano Valenza. "Quantitative models of hydrothermal fluid–mineral reaction: The Ischia case." Geochimica et Cosmochimica Acta 105 (March 2013): 108–29. http://dx.doi.org/10.1016/j.gca.2012.11.039.

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39

Buffetaut, Eric, Valérie Martin, Nares Sattayarak, and Varavudh Suteethorn. "The oldest known dinosaur from southeast Asia: a prosauropod from the Nam Phong Formation (late Triassic) of northeastern Thailand." Geological Magazine 132, no. 6 (November 1995): 739–42. http://dx.doi.org/10.1017/s0016756800018951.

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AbstractThe distal part of the fused ischia of a prosauropod from the Nam Phong Formation (late Triassic) of Phetchabun Province, in northeastern Thailand, is described. Comparisons with various prosauropods, as well as with an early sauropod, show that the Thai specimen is especially robust. However, the available material is too incomplete to warrant a precise identification. It is the first vertebrate fossil found in the Nam Phong Formation, the oldest known dinosaur from southeast Asia, and the first prosauropod to be reported from that region.

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40

La Verde, Giuseppe, Adelaide Raulo, Vittoria D’Avino, Vincenzo Roca, Riccardo de Asmundis, and Mariagabriella Pugliese. "Green Tuff: Gamma Index in a Typical Building Material of Ciglio Area (Ischia Island)." Solid State Phenomena 319 (June 14, 2021): 24–29. http://dx.doi.org/10.4028/www.scientific.net/ssp.319.24.

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Radiological characterization of tuff of Ciglio area in Ischia Island was performed to assess the potential radiological hazard associated with its use. For this purpose, high resolution gamma-ray spectroscopy was used. In five green tuff samples was measured the activity concentration of natural gamma-ray emitting radionuclides 226Ra, 232Th and 40K so, the mean gamma index was calculated. The mean value of the gamma index resulted lower than the reference level and it meets the dose criterion for the safety use of green tuff as building material.

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41

Piscopo, Vincenzo, Fulvio Formica, Luigi Lana, Francesca Lotti, Luigi Pianese, and Marco Trifuoggi. "Relationship Between Aquifer Pumping Response and Quality of Water Extracted from Wells in an Active Hydrothermal System: The Case of the Island of Ischia (Southern Italy)." Water 12, no. 9 (September 15, 2020): 2576. http://dx.doi.org/10.3390/w12092576.

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The thermal waters of the Island of Ischia, an active volcano located in Southern Italy, are widely used for supplying numerous spas. Groundwater withdrawals occur mainly through wells in the coastal strip. This study explores the impact of withdrawals on the quality of the waters used in thermal facilities, which is required to be constant in terms of composition and temperature by law. For this purpose, specific investigations were conducted including 155 pumping tests, 124 water temperature measurements during pumping tests, 31 temperature and electrical conductivity logs and periodic chemical analysis of the waters of 21 selected wells. By comparing the response to pumping of the aquifer and the quality of the water extracted from the wells, it turned out that the quality of groundwater supplying spas depends not only on natural phenomena (meteoric recharge, seawater intrusion, and rising of deep hydrothermal fluids) but also relies on the island sector where groundwater is pumped and on the pumping method. The distance of the wells from the coast, the type of aquifer formation intersected by the wells, and the field of groundwater temperature of the hydrothermal system strongly affect the aquifer pumping response, determining the quality of water extracted from wells and its variation over time. In Ischia, techniques and regimes of groundwater withdrawals should adapt to the local aquifer pumping response, more than in another hydrogeological context. The concomitant analysis of drawdown, water temperature, and salinity during pumping turned out to be a valuable tool to define the sustainable yield of the single well.

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42

Becker, Johannes, M. Winkler, C. von Rüden, E. Bliven, P. Augat, and H. Resch. "Comparison of two reinforcement rings for primary total hip arthroplasty addressing displaced acetabular fractures: a biomechanical analysis." Archives of Orthopaedic and Trauma Surgery 140, no. 12 (April 8, 2020): 1947–54. http://dx.doi.org/10.1007/s00402-020-03433-3.

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Abstract Introduction Aim of this study was to biomechanically compare two different acetabular cup fixation constructs in terms of fracture fixation for displaced acetabular fractures involving the anterior column with hemitransverse fracture under partial and full weight-bearing conditions. Methods Two different reinforcement rings designed as cages for primary THA were biomechanically tested in terms of managing a complex acetabular fracture. Single-leg stance cyclic loading was performed to assess fracture gap movement and fragment rotation. Twelve hemi pelvis Sawbones were divided into two groups: primary THA with acetabulum roof reinforcement plate (ARRP) (n = 6) and primary THA with Burch–Schneider reinforcement cage (BSRC) (n = 6). Results During loading under partial weight-bearing (250 N) fracture gap movement tended to be larger in the BSRC group as compared to the ARRP group. Under full weight-bearing conditions, the ARRP showed 60% significantly less motion (p = 0.035) of the os ilium to os ischii gap compared to BSRC. Fracture gap movements between the os ilium and spina iliaca fragments were significantly reduced by 76% (p = 0.048) for ARRP in contrast to BSRC. The ARRP group also demonstrated significantly less movement in the fracture gaps os ischii to quadrilateral plate (62% reduction, p = 0.009) and quadrilateral plate to spina iliaca (87% reduction, p < 0.001). Significantly less rotational movement of the quadrilateral plate to the os ilium was exhibited by the ARRP group (p = 0.015). Conclusions The presented acetabulum roof-reinforcement plate (ARRP) provides stable conditions at the acetabular component with adequate stabilization of a displaced acetabular fracture.

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43

Selnekovič, Dávid, Katarína Goffová, Ján Šoltýs, Eva Kováčová, and Ján Kodada. "Mordellistena platypoda, a new species of tumbling flower beetle from the island of Ischia in Italy (Coleoptera, Mordellidae)." ZooKeys 1148 (February 14, 2023): 41–63. http://dx.doi.org/10.3897/zookeys.1148.86845.

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Mordellistena A. Costa, 1854, the most species-rich genus of tumbling flower beetles comprises more than 800 species worldwide and more than 150 reported from Europe. Here, a new species Mordellistena (s. str.) platypoda is described from the island of Ischia in Italy. The species hypothesis is based primarily on morphological characters which are visualised using scanning electron microscopy images, high-resolution photographs, and drawings. The species hypothesis is supported by analysis of a 658 bp fragment of cytochrome c oxidase subunit I (COI). Divergences in the COI gene are evaluated using maximum likelihood and Bayesian inference analyses. The species delimitation is assessed using Assemble Species by Automatic Partitioning (ASAP) and Poisson Tree Processes (PTP) methods. Genetic distances are visualised using multidimensional scaling. Mordellistena platypoda Selnekovič, Goffová & Kodada, sp. nov. is recovered as a well-separated species by both molecular and morphological analyses. Our results show that M. platypoda Selnekovič, Goffová & Kodada, sp. nov. is most closely related to M. tarsata Mulsant, 1856, although the two species differ significantly in vestiture colouration, presence of lateral ctenidia on the third metatarsomere, and presence of sexual dimorphism on the protibia. The results indicate that such morphological differences, which were traditionally used to distinguish between species groups, may in fact be present between closely related species. Interestingly, examination of the numerous museum material did not reveal additional specimens of the new species, and therefore M. platypoda Selnekovič, Goffová & Kodada, sp. nov. is currently known only from the Italian island of Ischia.

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44

Daniele, Linda, Daniele Tardani, Diego Schmidlin, Ignacio Quiroga, Claudia Cannatelli, and Renato Somma. "Seawater intrusion and hydrogeochemical processes in the Ischia Island groundwater system." Journal of Geochemical Exploration 234 (March 2022): 106935. http://dx.doi.org/10.1016/j.gexplo.2021.106935.

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45

NAGAI, Itaru, Junji KYOUGOKU, Akira MIYAKAWA, Makoto NOGUTI, Ryoji TSUTSUMIDA, Hiroyoshi HIRATSUKA, Tetsuyo ODAJIMA, Gen-iku KOHAMA, and Etsuhide YAMAMOTO. "A case of eosinophilic granuloma in the jaw, ischia and lung." Japanese Journal of Oral & Maxillofacial Surgery 36, no. 4 (1990): 1096–103. http://dx.doi.org/10.5794/jjoms.36.1096.

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46

Inguaggiato, S., G. Pecoraino, and F. D'Amore. "Chemical and isotopical characterisation of fluid manifestations of Ischia Island (Italy)." Journal of Volcanology and Geothermal Research 99, no. 1-4 (June 2000): 151–78. http://dx.doi.org/10.1016/s0377-0273(00)00158-x.

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47

Chiodini, Giovanni, Rosario Avino, Tatjana Brombach, Stefano Caliro, Carlo Cardellini, Sandro De Vita, Francesco Frondini, Domenico Granirei, Enrica Marotta, and Guido Ventura. "Fumarolic and diffuse soil degassing west of Mount Epomeo, Ischia, Italy." Journal of Volcanology and Geothermal Research 133, no. 1-4 (May 2004): 291–309. http://dx.doi.org/10.1016/s0377-0273(03)00403-7.

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48

Tibaldi, Alessandro, and Luigina Vezzoli. "Late Quaternary monoclinal folding induced by caldera resurgence at Ischia, Italy." Geological Society, London, Special Publications 169, no. 1 (1999): 103–13. http://dx.doi.org/10.1144/gsl.sp.2000.169.01.08.

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49

Miliaresis, George Ch, Guido Ventura, and Giuseppe Vilardo. "Terrain modelling of the complex volcanic terrain of Ischia Island, Italy." Canadian Journal of Remote Sensing 35, no. 4 (January 2009): 385–98. http://dx.doi.org/10.5589/m09-027.

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50

Carlino, S., E. Cubellis, G. Luongo, and F. Obrizzo. "On the mechanics of caldera resurgence of Ischia Island (southern Italy)." Geological Society, London, Special Publications 269, no. 1 (2006): 181–93. http://dx.doi.org/10.1144/gsl.sp.2006.269.01.12.

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