188 research outputs found
Skilled and Unskilled Wage Dynamics in Italy in the â90s: Changes in the individual characteristics, institutions, trade and technology.
In this paper we use individual micro data on workers combined with industry and regional data to study the wage dynamics of skilled and unskilled workers in Italy in the period 1991-1998. Being different to previous empirical studies, our data allow us to explore in a unique framework the role of many of the factors indicated in the literature as possible causes of the widening of the wage gap between skilled and unskilled workers: changes in the individual characteristics of workers, changes in the institutions of the labour market, increasing international integration and skill-biased technological progress. Our results show that international integration, both in terms of trade in goods and in terms of international labour mobility, plays a role in determining the wage dynamics of skilled (white collar) and of unskilled (blue collar) workers. In addition, in line with the research in labour economics, our findings show that the individual characteristics of workers, and the institutional variables matter more in explaining skilled and unskilled wage dynamics than differential wage one.Skilled and unskilled wages, individual characteristics, labour market institutions, international trade.
Foreign Direct Investment, Wage Inequality, and Skilled Labor Demand in EU Accession Countries
During the 1990s Poland, Hungary and the Czech Republic have experienced rapid increases in wage inequality between skilled and unskilled workers and received the largest FDI inflow in Central and Eastern Europe. This paper analyzes whether FDI has contributed to the raise in earning inequality via a change in the skill composition of labor demand in the three countries. While we find that in Hungary and the Czech Republic FDI exerts a positive direct impact on the skill-premium, in none of the countries considered FDI has worsened wage inequality by favoring labor demand shifts.Foreign direct investment; Labor demand; Wage inequality
IMPORTING JOBS AND EXPORTING FIRMS? ON THE WAGE AND EMPLOYMENT IMPLICATIONS OF ITALYâS TRADE AND FOREIGN DIRECT INVESTMENT FLOWS
International economic integration is often blamed for the deteriorating fortunes of unskilled workers in industrial countries. We look at the labor market impact of trade and foreign direct investment in the case of Italy. Our empirical framework allows for trade, technology and factor supply effects. We find that international trade did not contribute to Italyâs labor market problems. Indeed, given that Italy holds quite a distinct pattern of trade specialization, compared to other industrialized countries, international integration as reflected in falling import prices may have boosted the demand for labor there. We also argue that the inability of the Mezzogiornoâs economy to adjust to the changing international environment is one of the main stumbling blocks in Italyâs economy. Finally, we find that greater firmâs mobility may have weakened the power of trade unions and contributed to wage moderation.international trade, foreign direct investment,wages, employment
Shell size measurements of the planktonic foraminiferal species Rotalipora cushmani and Whiteinella brittonensis across the Oceanic Anoxic Event 2 (middle Cretaceous)
A morphometric methodology to assess planktonic foraminiferal response to environmental perturbations: the case study of Oceanic Anoxic Event 2, Late Cretaceous
Dwarfism of planktonic foraminiferal specimens is recognised across several intervals subject to globally extended environmental disturbances such as the Cretaceous/Palaeogene boundary and the latest Cenomanian-earliest Turonian Oceanic Anoxic Event 2 (OAE 2) in the Late Cretaceous. However, the occurrence of dwarfed specimens is generally based on the observation of a decrease in the size of specimens at the stereomicroscope without acquiring morphometric data. This approach prevents from assessing the inter-sample morphometric variation of species, reconstructing species-specific trends, and comparing data from different localities to extrapolate global from local signals.
We present herein a first step toward the development of a morphometry-based methodology to assess planktonic foraminiferal response to past environmental perturbations. To perform this study, we selected OAE 2 as a target event and we focused on two species, Rotalipora cushmani (Morrow, 1934) and Whiteinella brittonensis (Loeblich & Tappan, 1961), commonly occurring in the assemblages and likely having different palaeoecological preferences. Specimens analysed are from Eastbourne (England), Clot Chevalier (SE France), and Tarfaya (core S57, Morocco). For both species, we measured selected shell parameters (i.e., the number of chambers in the last whorl, the maximum diameter and the height of the test).
Our study suggests that the maximum diameter across the first chamber of the inner whorl visible in spiral view is the simplest and most objective methodology to estimate shell size variation in trochospiral planktonic foraminifera, and that this morphometric parameter is likely the most sensitive to the Cenomanian-Turonian environmental disturbances, and thus its variability through time appears worth investigating across other key-stratigraphic intervals. Moreover, this study indicates that the acquisition of morphometric data is required to accurately reconstruct planktonic foraminiferal response to environmental perturbations, because specimen dimensions show high inter-sample variability and based on the data collected in this study they do not experience the predicted size reduction
Reassessing planktonic foraminiferal biostratigraphy across the Cenomanian–Turonian boundary interval (middle Cretaceous)
Age and synchronicity of planktonic foraminiferal bioevents across the Cenomanian–Turonian boundary interval (Late Cretaceous)
The upper Cenomanian \u2013 lower Turonian is a key-stratigraphic interval, as it encompasses the
Late Cretaceous supergreenhouse and a major perturbation of the global carbon cycle (i. e., Oceanic Anoxic
Event 2) as evidenced by a global positive carbon isotope excursion and by the nearly world-wide deposition
of organic-rich marine facies. A turnover in planktonic foraminiferal assemblages and in other marine organisms
is documented across this stratigraphic interval, but reconstruction of the timing and identification of
the cause and effect relationships between environmental perturbations and organism response require a highly-
resolved stratigraphic framework. The appearance and extinction levels of planktonic foraminiferal species
generally allow accurate intra- and supra-basinal correlations. However, bioevents cannot be assumed to be
globally synchronous, because the stratigraphic and geographic distribution of species is modulated by ecological
preferences exhibited by each taxon and controlled by oceanic circulation, often resulting in earlier
or delayed events in certain geographic areas (i. e., diachronous datums). The aim of this study is to test the
synchronicity of the planktonic foraminiferal bioevents recognized across the C/T boundary and to provide
the most reliable sequence of events for correlation of low to mid-latitude localities. For this purpose, we have
compiled a highly-resolved biostratigraphic analysis of the European reference section for the C/T boundary
at Eastbourne, Gun Gardens (UK), and core S57 (Tarfaya, Morocco), and correlated the sequence of bioevents
identified with those recorded in other coeval sections available in the literature, including the GSSP section
for the base of the Turonian Stage at Rock Canyon, Pueblo (Colorado), where we calculated reliable estimates
of planktonic foraminiferal events that are well-constrained by radioisotopically and astrochronologically
dated bentonite layers. Results indicate that the extinctions of Thalmanninella deeckei, Thalmanninella
greenhornensis, Rotalipora cushmani and \u201cGlobigerinelloides\u201d bentonensis in the latest Cenomanian are
reliable bioevents for correlation. In addition, our analysis highlights other promising lowest occurrences
(LOs) that need to be better constrained by bio- and chemostratigraphy, including the LO of Marginotruncana
schneegansi falling close to the C/T boundary. By contrast, the appearance of Helvetoglobotruncana helvetica
and of some Dicarinella species, the extinction of anaticinellids and the onset of the \u201cHeterohelix\u201d shift are
likely diachronous across low to mid-latitude localities. Finally, our study suggests that different species concepts
among authors, different sample size and sampling resolution, as well as species paleoecology are important
factors that control the stratigraphic position at which bioevents are identified
P2 receptors in macrophage fusion and osteoclast formation
Cells of the mononuclear phagocyte lineage fuse to form multinucleated giant cells and osteoclasts. Several lines of evidence suggest that P2 receptors, in particular P2X7, are involved in this process, although P2X7 is not absolutely required for fusion because P2X7-null mice form multinucleated osteoclasts. Extracellular ATP may be an important regulator of macrophage fusion
Analysis of the humoral and cellular immune response after a full course of BNT162b2 anti-SARS-CoV-2 vaccine in cancer patients treated with PD-1/PD-L1 inhibitors with or without chemotherapy: an update after 6 months of follow-up
Background: The durability of immunogenicity of SARS-CoV-2 vaccination in cancer patients remains to be elucidated. We prospectively evaluated the immunogenicity of the vaccine in triggering both the humoral and the cell-mediated immune response in cancer patients treated with anti-programmed cell death protein 1/programmed death-ligand 1 with or without chemotherapy 6 months after BNT162b2 vaccine. Patients and methods: In the previous study, 88 patients were enrolled, whereas the analyses below refer to the 60 patients still on immunotherapy at the time of the follow-up. According to previous SARS-CoV-2 exposure, patients were classified as SARS-CoV-2-naive (without previous SARS-CoV-2 exposure) and SARS-CoV-2-experienced (with previous SARS-CoV-2 infection). Neutralizing antibody (NT Ab) titer against the B.1.1 strain and total anti-spike immunoglobulin G concentration were quantified in serum samples. The enzyme-linked immunosorbent spot assay was used for quantification of anti-spike interferon-Îł (IFN-Îł)-producing cells/106 peripheral blood mononuclear cells. Fifty patients (83.0%) were on immunotherapy alone, whereas 10 patients (7%) were on chemo-immunotherapy. We analyzed separately patients on immunotherapy and patients on chemo-immunotherapy. Results: The median T-cell response at 6 months was significantly lower than that measured at 3 weeks after vaccination [50 interquartile range (IQR) 20-118.8 versus 175 IQR 67.5-371.3 IFN-Îł-producing cells/106 peripheral blood mononuclear cells; P < 0.0001]. The median reduction of immunoglobulin G concentration was 88% in SARS-CoV-2-naive subjects and 2.1% in SARS-CoV-2-experienced subjects. SARS-CoV-2 NT Ab titer was maintained in SARS-CoV-2-experienced subjects, whereas a significant decrease was observed in SARS-CoV-2-naive subjects (from median 1 : 160, IQR 1 : 40-1 : 640 to median 1 : 20, IQR 1 : 10-1 : 40; P < 0.0001). A weak correlation was observed between SARS-CoV-2 NT Ab titer and spike-specific IFN-Îł-producing cells at both 6 months and 3 weeks after vaccination (r = 0.467; P = 0.0002 and r = 0.428; P = 0.0006, respectively). Conclusions: Our work highlights a reduction in the immune response in cancer patients, particularly in SARS-CoV-2-naive subjects. Our data support administering a third dose of COVID-19 vaccine to cancer patients treated with programmed cell death protein 1/programmed death-ligand 1 inhibitors
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