1,235 research outputs found
Large deep-seated gravitational slide off Ischia volcanic island, Eastern Tyrrhenian sea (Italy)
Ischia island develops at the edge of the shelf area and represents the sub-aerial section of a larger, E-W trending
volcanic ridge including others submerged or buried volcanic edifices. In the past decade the islandâs offshore
has been the object of extensive hydrographic and marine geophysical surveys that have shown the structural
complexity of the undersea sections and have overall shown the importance of gravity failures in islandâs evolution.
In this paper we report a previously unreported deep-seated slump structure and associated surficial mass wasting
phenomena which occur off Ischia south-western flank. Recently acquired hydrological and geophysical data lead
to identify the morphological features and the internal organization of the failed sediments which spread along
the continental slope. The extent of this deep-seated deformations and the deep structural levels involved lead to
investigate on the influence played by volcanic processes and regional tectonics on slope failure.
The Ischia southern slope was explored through a multibeam survey and a single-channel seismic survey.
Acquisition was carried out from aboard the R/V Urania at depths between 400 and 1200 m. The bathymetric data
were collected using a hull mounted Reson 8160 multibeam sonar. Resolution resulted in a 20x20 m implemented
with 50x50 gridded size provided by a previously collected data. Seismic survey consisted of 6 seismic lines run
along the slope spaced 1 km between them and 5 cross lines. The acoustic source used was a 1Kjoule high-energy
power supply system with a multi-tips (400) sparker array, fired at 2s time interval.
The collected data show that a wide submerged area of 350 km2, between 400 to 1200 m depths is undergoing
slow-moving deformation and associated secondary mass wasting phenomena. Morphological features include
trenches, counterscarps, bulging and both extensional and contractional features while internal deformations show
typical landward dipping reflectors with strong evidence of synsedimentary faulting and asymmetric anticlines.
Deformation processes operate at various scales generating folds with wavelength ranging from hundreds meters to kilometers. Extensional and rotational rupture surfaces sole out at various low-angle detachment planes located
at depths from few hundreds meters to 1 kilometer in subsurface
Large deep-seated slump structure off Ischia volcanic island, Eastern Tyrrhenian sea (Italy)
Ischia island is located over the Campania sector of Eastern
Tyrrhenian margin and represents the sub-aerial section of a
larger, E-W trending volcanic ridge including others submerged
or buried volcanic edifices. The island itself result from the
coalescence of a multitude of small to medium scale eruptions
leading to the emplacement of domes, lava flow and pyroclastic
deposits and ignimbrites (VEZZOLI et al., 1988) ranging from
alkali basalts to trachytes. The oldest basement dates back to 150
ky and crops out along the perimeter of the island especially to
the south. Latest eruption occurred in 1302 A.D. and together
with strong hydrothermal activity, ground uplift and seismic
shaking indicates the presence of a still active magmatic reservoir
at depth. Most recent (Holocene) magmatic activity with local
volcanic eruptions has clustered in the eastern islandâs sector the
while central sector is dominated by the Mt. Epomeo, consisting
of an ignimbritic tuff (Green tuff Auct.) uplifted of 600-700 m in
the past 33ka.
In the past decade the islandâs offshore has been the object of
extensive hydrographic and marine geophysical surveys that have
shown the structural complexity of the undersea sections and
have overall shown the importance of gravity failures in islandâs
evolution. In particular a 1.5-3 km3 debris avalanche due to a
subaerial and/or submarine flank collapse was emplaced along
the steep and unbuttressed islandâs flank during pre-historical or
even historical times (CHIOCCI & DE ALTERIIS, 2006; de Alteriis
et al., 2010) whereas three other similar deposits of comparable
volumes were found over the continental shelf to the west and to
the north (VIOLANTE et al, 2004; DE ALTERIIS & VIOLANTE,
2009).
Here we report a previously unrecognized deep-seated slump
structure and associated surficial mass wasting phenomena which
occur off Ischia south-western flank. Recently acquired
hydrological and geophysical data lead to identify the
morphological features and the internal organization of the failed
sediments which spread along the continental slope. The extent
of this deep-seated deformations and the deep structural levels
involved lead to investigate on the influence played by volcanic
processes on slope failure.
DATA AND METHODS
Our dataset was acquired during the geophysical cruise
PECOS 2010 carried out on R/V Urania (Consiglio Nazionale
delle Ricerche, CNR, Italy) between December 22th 2010 and
January 2nd 2011 in the frame of a project leaded by Istituto per
lâAmbiente Marino Costiero, (IAMC-CNR), Naples-Italy with
the collaboration of Dipartimento di Scienze della Terra e del
Mare (Palermo University), Palermo-Italy regarding coastal and
offshore slope instability in the Bay of Napoli.
The Ischia southern slope was explored through a multibeam
survey and a single-channel seismic survey. Acquisition was
carried out between 400 and 1200 m. The bathymetric data were
collected using a hull mounted Reson 8160 multibeam sonar.
Resolution resulted in a 20x20 m implemented with 50x50
gridded size provided by a previously collected data. The seismic
survey consisted of 6 dip-lines NNE-SSW run along the slope
and 5 cross lines parallel to the slope totalling 170 km. Average
spacing between diplines was slightly less than 1 km while
spacing between crosslines was variable from 1.2 to 2.5 km.
NNE-SSW and WNW-ESE directions. The acoustic source used
was a 1Kjoule high-energy power supply system with a multitips
(400) sparker array, fired at 2s time interval.
RESULTS
The collected data show that a wide submerged area of 350
km2, between 400 to 1200 m depths is undergoing slow-moving
deformation and associated secondary mass wasting phenomena.
Morphological features include trenches, counterscarps, bulging
and both extensional and contractional features while internal
deformations show typical landward dipping reflectors with
strong evidence of synsedimentary faulting and asymmetric
anticlines.
Deformation processes operate at various scales generating
folds with wavelength ranging from hundreds meters to
kilometers. Extensional and rotational rupture surfaces sole out at
various low-angle detachment planes located at depths from few
hundred meters to 1 kilometer in subsurface.
The internal organization of the failing mass shows different
pattern of deformation that allows the identification of three main units: 1) a basal unit consisting of a very broad, asymmetric
slump fold with a wavelength of about 5 km and amplitude of
some 100 m. The fold axis is not vertical and the three
dimensional interpretation indicates that the structure is not
cylindrical. The fold strictly correlates with a morphological
bulge seen on bathymetry at about 20 km south of Ischia Island.
2) A wedge shaped intermediate unit characterized by
discontinuous and folded reflectors, locally showing basal
detachment planes and compressional features. 3) A surficial
slump unit affecting the upper and middle slope characterized by
a basal decollément surface and normal growth faults that sole
out at depths ranging from 70 to 40 m in subsurface. It is still
unclear whether the landslide process can be favored by the
volcano-tectonic evolution and rapid vertical accretion of Ischia
volcano or is solely due to possibly volcanic spreading of the
Ischia Island.
REFERENCES
CHIOCCI, F. L. & DE ALTERIIS, G. (2006) - The Ischia debris
avalanche. First, clear submarine evidence in the
Mediterranean of a volcanic island pre-historic collapse.
Terra Nova, 18, 202â209.
DE ALTERIIS, G., INSINGA D. ET AL. (2010) - Age of submarine
debris avalanches and tephrostratigraphy offshore Ischia
Island, Tyrrhenian Sea, Italy. Marine Geology 278 (2010) 1â
18.
DE ALTERIIS, G. & VIOLANTE, C. (2009) - Catastrophic
landslides off Ischia volcanic island (Italy) during prehistory.
In: C. Violante, (ed.) Geohazard in Rocky Coastal Areas.
Geological Society, London, Special Publications, 322, 73â
104.
VEZZOLI, L. (1988) Island of Ischia. Quaderni de âLa Ricerca
Scientificaâ Progetto finalizzato âGeodinamicaâ, CNR
Monografie finali, 10.
VIOLANTE, C., BUDILLON, F., ET AL. (2004) - Submerged
hummocky topographies and relations with landslides on the
northwestern flank of Ischia island, southern Italy. In:
âOccurrence and mechanisms of flow-like landslides in
natural slopes and earthfillsâ, Sorrento, 14â16 May 2003.
AGI, 2, 309â315
Flood Historical Data for Flood Risk Estimation in Coastal Areas, Eastern Tyrrhenian Sea, Italy
A reconstruction of historical floods occurred along the Amalfi coast, during the last five
7 centuries is presented. The analysis of historical sources allowed to achieve a chronological
8 reconstruction of more than 100 floods, four of which classified as catastrophic events. In this
9 task, the level of information was decisive to carry out spaceâtime identification, estimate the
10 affected area and define the type of damage to the structures, and the environment (e.g. mud
11 flow, debris flow, rock falls, shoreline progradation, fan deltas), which may be relevant for the
12 recognition of similar events within the geologic record. The magnitude of the events was
13 finally estimated, taking into account the size of the areas affected by flooding as well as the
14 type of effects induced on the urban and physical environment and the recurrence intervals
Efficacy and toxicity of bevacizumab in recurrent ovarian disease: an update meta-analysis on phase III trials
Background: To analyze the efficacy and toxicity of bevacizumab on survival outcomes in recurrent ovarian cancer.
Results: Bevacizumab was associated with significant improvement of PFS and OS compared with standard treatment with HRs of 0.53 (95% CI 0.44 - 0.63; p < 0.00001) and 0.87 (95% CI, 0.77 to 0.99; p = 0.03), respectively.
Bevacizumab increased the incidence of G3/G4 hypertension (RR 19.01, 95% CI 7.77 - 46.55; p < 0.00001), proteinuria (RR 17.31, 95% CI 5.42 - 55.25; p < 0.00001), arterial thromboembolic events (ATE) (RR 4.99, 95% CI 1.29 - 19.27; p = 0.02) and bleeding (RR 3.14, 95% CI 1.35 - 7.32; p = 0.008).
Materials and Methods: Three randomized phase III trials representing 1502 patients were identified.
Pooled hazard ratio (HR), odd ratio (OR), risk ratio (RR) with 95% confidence interval (CI) were calculated using fixed or random effects model.
Conclusions: Adding bevacizumab to standard chemotherapy improved ORR, PFS and OS, and it had a higher, but manageable, incidence of toxicities graded 3 to 4
The geological record of storm events over the last 1000 years in the Salerno Bay (Southern Tyrrhenian Sea): new proxy evidences
International audienceThe shallow marine Late Holocene wedge of the northern Salerno Bay shelf (Southern Tyrrhenian Sea) discloses the presence of four decimetric shelf-tapering sand beds. Their internal features, depicted by cores analysis and their stratigraphic position, revealed by VHR seismic investigations, inferred sandy layers as being the result of flash deposition, storm controlled, thus episodic. Stratigraphic correlations among cores lead to constrain sandy layers deposition to storm events falling in the 11th, 16th, 19th and 20th centuries. A certain attribution of the most recent event bed to the major cloudburst that hit the Salerno region in 1954A.D. and resulted in a disastrous flood of the Bonea stream, was formerly achieved. A tentative link with two sea-storms that occurred in the 1544A.D. and in the 1879A.D. and well documented by historical sources is here proposed to explain the deposition of the two previous event beds. The deposition of these sandy layers must be related to major storm events, since their preservation in the stratigraphic record is not common. Lithostratigraphic and textural differences between flood and sea-storm emplacement emerge from the study of sandy layers in cores and point to a prevalence of sea-storm deposits in the middle shelf compared to flood deposits. Seismic stratigraphic evidence lead us to suppose that the style of episodic flash deposition has been running on for the last 2-3kyr and is probably linked to a climatic trend of the region
Quality of life, firm productivity, and the value of amenities across Canadian cities
We estimate qualityâofâlife and productivity differences across Canada's metropolitan areas in a hedonic generalâequilibrium framework. These are based on the estimated willingnessâtoâpay of heterogeneous households and firms to locate in various cities, which differ in their wage levels, housing costs, and land values. Using 2006 Canadian Census data, our metropolitan qualityâofâlife estimates are somewhat consistent with popular rankings, yet find Canadians care more about climate and culture. Quality of life is highest in Victoria for anglophones, Montreal for francophones, and Vancouver for allophones, and lowest in more remote cities. Toronto is Canada's most productive city; Vancouver is the overall most valuable city. QualitĂ© de vie, productivitĂ© des entreprises, et la valeur des avantages dans les diverses villes canadiennes . On Ă©value les diffĂ©rences entre la qualitĂ© de vie et la productivitĂ© des entreprises entre les zones mĂ©tropolitaines au Canada Ă l'aide d'un cadre d'analyse d'Ă©quilibre gĂ©nĂ©ral hĂ©donique. Ces mĂ©triques sont basĂ©es sur l'estimation de la volontĂ© de payer de mĂ©nages et d'entreprises hĂ©tĂ©rogĂšnes pour se localiser dans diverses villes, qui diffĂšrent tant pour ce qui est des niveaux de salaires, des coĂ»ts de l'habitation, et des prix des terrains. A l'aide des donnĂ©es du recensement canadien de 2006, on construit des Ă©valuations de la qualitĂ© de vie des diverses zones mĂ©tropolitaines qui s'arriment convenablement aux ordonnancements en vogue, mais on dĂ©couvre que les Canadiens portent une attention particuliĂšre au climat et Ă la culture. La qualitĂ© de vie est la plus Ă©levĂ©e Ă Victoria pour les anglophones, Ă Montreal pour les francophones, et Ă Vancouver pour les allophones, et la plus faible pour les villes Ă©loignĂ©es des grands centres. Toronto est la ville la plus productive; Vancouver est gĂ©nĂ©ralement la plus apprĂ©ciĂ©e.Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/98300/1/caje12017.pd
Inhaled CO2 Concentration While Wearing Face Masks: A Pilot Study Using Capnography
Background: Face masks are recommended based on the assumption that they protect against SARS-CoV-2 transmission, however studies on their potential side effects are still lacking. We aimed to evaluate the inhaled air carbon dioxide (CO2) concentration, when wearing masks. Methods: We measured end-tidal CO2 using professional side-stream capnography, with water-removing tubing, (1) without masks, (2) wearing a surgical mask, and (3) wearing a FFP2 respirator (for 5 minutes each while seated after 10 minutes of rest), in 146 healthy volunteers aged 10 to 90 years, from the general population of Ferrara, Italy. The inhaled air CO2 concentration was computed as: ([mask volume Ă end-tidal CO2] + [tidal volume â mask volume] Ă ambient air CO2)/tidal volume. Results: With surgical masks, the mean CO2 concentration was 7091 ± 2491 ppm in children, 4835 ± 869 in adults, and 4379 ± 978 in the elderly. With FFP2 respirators, this concentration was 13 665 ± 3655 in children, 8502 ± 1859 in adults, and 9027 ± 1882 in the elderly. The proportion showing a CO2 concentration higher than the 5000 ppm (8-hour average) acceptable threshold for workers was 41.1% with surgical masks, and 99.3% with FFP2 respirators. Adjusting for age, gender, BMI, and smoking, the inhaled air CO2 concentration significantly increased with increasing respiratory rate (mean 10 837 ±3712 ppm among participants â©Ÿ18 breaths/minute, with FFP2 respirators), and among the minors. Conclusion: If these results are confirmed, the current guidelines on mask-wearing should be reevaluated
Sarcoidosis in a dental surgeon: a case report
<p>Abstract</p> <p>Introduction</p> <p>Although the causes of sarcoidosis are still unknown, past and current studies have provided evidence that this disease may be associated with occupational exposure to specific environmental agents. We describe a case of sarcoidosis in a dental surgeon with long exposure to inorganic dusts. To the best of our knowledge, this is the first report of this kind in the literature.</p> <p>Case presentation</p> <p>At the beginning of 2000, a 52-year-old Caucasian man, who worked as a dental surgeon, presented with shortness of breath during exercise, cough and retrosternal pain. After diagnosis of sarcoidosis, a scanning electronic microscopy with X-ray microanalysis of biopsy specimens was used in order to determine whether the disease could be traced to an occupational environmental agent. Results showed the presence of inorganic dust particles within sarcoidotic granulomas, and demonstrated that the material detected was identical to that found in a powder used by our patient for several years.</p> <p>Conclusions</p> <p>Although these results cannot be considered as definitive proof, they do however provide strong evidence that this disease may be associated with material used by dental surgeons.</p
Flood Risk Estimation through Document Sources Analysis: the Case of the Amalfi Rocky Coast
In the last century the Amalfi Coast was affected by numerous severe floods in
conjunction with exceptional rainfall that caused major damage in terms of lost lives
and economic cost. Historical documentary sources are an important source of information
for reconstructing exceptional flood events occurring prior to the instrumental
era. Historical analysis also provides an opportunity to extend the time scale window
for flood risk studies. To study historical floods we collected all the available information
concerning the period between the 16th and the 20th centuries by analysing
both published and unpublished sources. The great variety of historical sources made
it necessary to formulate an ad hoc scientific procedure that takes into account not
only the completeness and reliability of documents related to the period, but also
the intrinsic quality of the material. Experience in historical data collection shows
that not all documentary sources can provide useful information for flood characterization,
but it is necessary to have a selective criteria in order to obtain the best
information rather than the best dataset quality.
Analysis of the data in question allowed us to achieve a chronological reconstruction
of more than 100 floods. In this task, the level of information was decisive to carry
out spaceâtime identification, estimate the affected area and define type of damage
to public and private structures, and the geological effects induced
Role of Nanoclays in Carbon stabilization in Andisols and Cambisols
Greenhouse gas (GHG) emissions and their consequent effect on global warming are an issue of global environmental concern. Increased carbon (C) stabilization and sequestration in soil organic matter (SOM) is one of the ways to mitigate these emissions. Here we evaluated the role of nanoclays isolated from soil on C stabilization in both a C rich Andisols and C depleted Cambisols. Nanoclays were analyzed for size and morphology by transmission electron microscopy, for elemental composition and molecular composition using pyrolysis-GC/MS. Moreover, nanoclays were treated with H2O2 to isolate stable SOM associated with them. Our result showed better nanoclay extraction efficiency and higher nanoclay yield for Cambisol compared to Andisols, probably related to their low organic matter content. Nanoclay fractions from both soils were different in size, morphology, surface reactivity and SOM content. Nanoclays in Andisols sequester around 5-times more C than Cambisols, and stabilized 6 to 8-times more C than Cambisols nanoclay after SOM chemical oxidation. Isoelectric points and surface charge of nanoclays extracted from the two soils was very different. However, the chemical reactivity of the nanoclay SOM was similar, illustrating their importance for C sequestration. Generally, the precise C stabilization mechanisms of both soils may be different, with nanoscale aggregation being more important in Andisols. We can conclude that independent of the soil type and mineralogy the nanoclay fraction may play an important role in C sequestration and stabilization in soil-plant systems
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