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431 results for “Adriatic”
FIG. 1 in Three new species of Raphitoma Bellardi, 1847 (Mollusca, Gastropoda, Raphitomidae) from Croatian waters (NE Adriatic Sea)
FIG. 1. — Phylogenetic relationships (maximum likelihood topologies) among species of the genus Raphitoma (see Russini et al. 2020 for further details). Numbers at nodes are bootstrap supports after 1000 pseudoreplicates, and posterior probabilities after a Bayesian analysis on the same dataset; only values higher than 75% bootstrap support and 95% posterior probability are reported; black dots indicate nodes supported by 100% bootstrap and 1.0 posterior probability. A, ML analysis on the combined dataset (COI + 16S + 12S + ITS2); B, the histogram portraying the distribution of the pairwise genetic distances (K2p) among the COI sequences (red bars on the left are intraspecific comparisons, yellow bars on the right are interspecific comparisons); C, ML analysis on the ITS2 alignment.
FIG. 15 in Three new species of Raphitoma Bellardi, 1847 (Mollusca, Gastropoda, Raphitomidae) from Croatian waters (NE Adriatic Sea)
FIG. 15. — Murex echinatus Brocchi, 1814: A, lectotype, MCSNM i 5427; B, D, paralectotype, MCSNM i5428; C, E, paralectotype, MCSNM i5429. Photos courtesy: Martina Paolini (MCSNM).
Figure 7 in Adriatic species of Schizomavella (Bryozoa: Cheilostomata)
Figure 7. Schizomavella halimedae (MNCN 25.03/3904, St. 14, Hvar Island). (A) Group of ovicellate zooids with small avicularia; (B) autozooids with oral spines and spatulate avicularia.
Figure 2 in Adriatic species of Schizomavella (Bryozoa: Cheilostomata)
Figure 2. Schizomavella cornuta. (A, B) Autozooids with spatulate avicularia (MNCN 25.03/3888, St. 7, Kornati); (C) primary orifice with small suboral avicularium (MNCN 25.03/3898, St. 16, Korčula Island); (D) ovicellate zooid with spatulate avicularium (MNCN 25.03/3888, St. 7, Kornati).
Figure 3 in Adriatic species of Schizomavella (Bryozoa: Cheilostomata)
Figure 3. Schizomavella cornuta. (A) Ovicellate and non-ovicellate zooids (lectotype of Schizomavella cuspidata, NHMUK 1899.5.1.894); (B) (same) primary orifice; (C) a colony of S. cuspidata with spatulate avicularia, from Guernsey (NHMUK 1897.5.1.723); (D) Schizoporella auriculata var. leontiniensis, Taranto Bay (MM 3024); (E) type of Schizomavella cuspidata var. spathulata, Adriatic (NHMUK 1899.5.1.985) (F) type of Schizomavella auriculata var. ornata, Djerba (Tunisie).
Figure 4 in Adriatic species of Schizomavella (Bryozoa: Cheilostomata)
Figure 4. Schizomavella mystacea sp. nov. (A, B) Ovicellate and non-ovicellate autozooids with variably developed avicularia (CNHM Inv. br. 34, holotype, St. 8, Jabuka Shoal); (C) (same) lateral view of inclined avicularia and the calcified 'hood'; (D) autozooids with long oral spines (MNCN 25.03/3900, paratype, Algarve).
Figure 6 in Adriatic species of Schizomavella (Bryozoa: Cheilostomata)
Figure 6. Schizomavella rosae sp. nov. (CNHM Inv. br. 36, holotype, St. 8, Jabuka Shoal). (A) Group of zooids; (B) development of oral spines; (C, D) primary orifices; (E) autozooids and a kenozooid with adventitious avicularium.
Figure 1. Adriatic Sea localities where Schizomavella species were found. 1 in Adriatic species of Schizomavella (Bryozoa: Cheilostomata)
Figure 1. Adriatic Sea localities where Schizomavella species were found. 1 – Ždralova Bay (Velebit Channel); 2 – Ćutin Islet (Cres); 3 – Silba; 4 – Dugi otok (North); 5 – Iž Island; 6 – Dugi otok Vele stijene; 7 – Kornati; 8 – Jabuka Shoal; 9 – Jabuka Islet; 10 – Brusnik; 11 – Biševo; 12 – Vis (Komiža); 13 – Sušac; 14 – Hvar (Kozja); 15 – Lastovo; 16 – Korčula; 17 – Pelješac; 18 – Mljet.
Cast Away in the Adriatic: Low Degree of Parallel Genetic Differentiation in Three-Spined Sticklebacks
<p>This repository incorporates data and scripts associated with the paper "Cast Away in the Adriatic: Low Degree of Parallel Genetic Divergence in Three-Spined Sticklebacks".</p> <p>Included in the repository are the following compressed folders: </p> <ul> <li>Moments_models&data.zip: two-population demographic models and SFS to run in <em>moments.</em></li> <li>Stairwayplot.zip: blueprint files for multiple mutation rates and results for StairwayPlots.</li> <li>TreeMix.zip: pipeline to infer population splits and mixture events from allele frequency data using TreeMix, including input files.</li> <li>VCF.zip: a filtered VCF file for all three-spined stickleback samples.</li> </ul> <p>The scripts for TreeMix and demographic analyses in <em>moments</em> are also available on <a href="https://github.com/carolindahms">GitHub</a>.</p>
Chemical composition and sources of organic aerosol on the Adriatic coast in Croatia
<p>Air pollution studies are still scarce in some areas in Europe like around the Adriatic Sea. Source apportionment of the fine particulate (PM<sub>2.5</sub>) organic aerosol (OA) was conducted near Rogoznica, a small touristic settlement on the Eastern Adriatic coast of Croatia, near Lake Rogoznica (43.53° N, 15.95° E). Filter-based offline analyses of PM by a high resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) and an extractive electrospray ionization time-of-flight mass spectrometer (EESI-TOF) were used to apportion OA to its sources. We quantified the contributions of fresh biomass burning OA (BBOA) and three oxygenated OA (OOA), denoted as background OOA (bkgOOA), summer OOA (SOOA), and sulfur-containing OOA (SC-OOA). The bkgOOA component correlates with anthropogenically influenced secondary inorganic aerosol constituents (e.g. sulfate) and dominates OA both during the warm and cold seasons (44%). It exhibits characteristics of regional SOA and there are indications that during the warm season SOA from wildfires could be substantial contributors. EESI-TOF measurements of the levoglucosan related ion showed a high correlation with the BBOA factor. Secondary OA has a similar molecular composition during the cold and warm seasons – in line with the large contribution of bkgOOA throughout the investigated seasons. SOOA comprises 19% of total OA and increases exponentially with the local temperature, consistent with SOA production by oxidation of biogenic emissions. In addition to biogenic precursors, other precursors (alkanes and aromatic) plausibly also contribute to the SOOA enhancement during the warm season. SC-OOA is a minor contributor to OA (6%) and is most likely linked to emissions from a close-by marine lake.</p>
AdriE ocean climate model ensemble for the Adriatic Sea - monthly fields
<p>This dataset contains the monthly-averaged fields of the key physical oceanographic quantities from the AdriE ocean model ensemble. The model runs were carried out by using the ROMS modelling system (Haidvogel et al., 2008) forced by the SMHI-RCA4 Regional Climate Model (Samuelsson et al., 2021), in turn driven by different General Circulation Models. The period is 1987-2099 in the severe RCP8.5 scenario for the climate simulations, whereas the evaluation runs span the period 1987-2010. Each file contains the results for one run.</p> <p>The model implementation and its validation are fully described in a manuscript recently submitted to Ocean Science (Bonaldo, D., Carniel, S., Colucci, R. R., Denamiel, C., Pranic, P., Raicich, F., Ricchi, A., Sangelantoni, L., Vilibic, I., and Vitelletti, M. L.: AdriE: a high-resolution ocean model ensemble for the Adriatic Sea under severe climate change conditions, EGUsphere [preprint], https://doi.org/10.5194/egusphere-2024-1468, 2024).</p>
Fig. 1 in Seasonal residency of loggerhead turtles Caretta caretta tracked from the Gulf of Manfredonia, South Adriatic Abstract
Fig. 1: Positions and paths of four loggerhead turtles (A, B, D, E) which remained in the Gulf of Manfredonia during the monitored period. The grey areas represent KDE 50%. Isobaths are shown (10, 20, 50 m).
Fig. 2 in Seasonal residency of loggerhead turtles Caretta caretta tracked from the Gulf of Manfredonia, South Adriatic Abstract
Fig. 2: Turtle C. (a) entire path.(b) coastal subarea of the periods 4 Jul-11 Nov 2012 and 3 May-27 Jun 2013, where the grey area represents KDE 50% for aggregated data. (c)the same subarea with separate KDE 50% for the period 2012 (grey area) and 2013 (ellipse). AL: Albania; BA: Bosnia and Herzegovina; HR: Croatia; ME: Montenegro. Isobaths 200m (a) and 20 m (b and c) are shown.
Fig. 4 in Mollusc fauna associated with the Cystoseira algal associations in the Gulf of Trieste (Northern Adriatic Sea)
Fig. 4: Comparison of mean mollusc richness (S) and abundance (N) per 400 cm2 in logarithmic scale with standard error bars (±SE) in different algal species (A) and at different depths (B) at sites investigated in 2012. Samples with C. barbata were: MBP1-5, PI4, PA1-5, STR1-4, FI1-2; with C. compressa were PI1-3.5, CM1-3, PO1-3, with C. corniculata were RR1-5; with H. incurva DR 1-5. Samples collected between 1 and 1.9 m were: DR3-4, MBP-1, PI1-4, PA3-5; between 2 and 2.9 m were: DR1- 2, 5, MBP2-5; PI2-3.5, PA1-2; STR 1-4, FI1-2; CM1-3, PO1-3, more than 3m were RR 1-5.
Fig. 1 in Mollusc fauna associated with the Cystoseira algal associations in the Gulf of Trieste (Northern Adriatic Sea)
Fig. 1: The study area with sampling sites. Five sites were sampled in 2012 [DR Debeli rtič], RR (Cape Ronek), PA (Pacug), MBP (Marine Biology Station), and PI (Piranček)). Four sites were sampled in 2008 (STR (Natural Reserve Strunjan), FI (Fiesa), CM (Cape Madona Natural Monument) and PO Izola)].
Fig. 3 in Mollusc fauna associated with the Cystoseira algal associations in the Gulf of Trieste (Northern Adriatic Sea)
Fig. 3: Comparison of the proportions of mollusc feeding guilds among sampling sites investigated in 2012, in terms of mean abundance (A) and richness (B) per 400 cm2.
Fig. 2 in Mollusc fauna associated with the Cystoseira algal associations in the Gulf of Trieste (Northern Adriatic Sea)
Fig. 2: K-dominance curve for sampling sites investigated in 2012. The graph shows the distribution of species abundances in the assemblage, plotted as a percentage of cumulative abundance (y axis) as a function of rank (x axis). Curves with low initial dominance reaching the asymptote slowly represent assemblages with homogeneous abundances and with high diversity.
Fig. 5 in Mollusc fauna associated with the Cystoseira algal associations in the Gulf of Trieste (Northern Adriatic Sea)
Fig. 5: Cluster of samples associated with four canopy-forming algal species (H_inc=H. incurva; C_corn=C. corniculata; C_ bar=C. barbata; C_comp=C. compressa), based on mollusc abundance data. Groups were formed with a cut at 20% of similarity.
Fig. 6 in Seasonal response of benthic foraminifera to anthropogenic pressure in two stations of the Gulf of Trieste (northern Adriatic Sea, Italy): the marine protected area of Miramare versus the Servola water sewage outfall
Fig. 6: Rank-frequency diagram for the Ser(a) and Res(b) stations using the cumulative abundance (as relative frequency) for y-axe and the decreasing rank order for x-axe of each species for each sample. Both axes are on logarithmic scale.
Fig. 4 in Seasonal response of benthic foraminifera to anthropogenic pressure in two stations of the Gulf of Trieste (northern Adriatic Sea, Italy): the marine protected area of Miramare versus the Servola water sewage outfall
Fig. 4: Foraminiferal data for Ser and Res stations using the complete living assemblage of the 0-2 cm level: a) Foraminiferal density (FD) as the number of specimens normalised to 50 cc of sediments and species richness; b) Dominance index; c) bias corrected Shannon (H' bc) and the exponential function Exp(H' ) indexes.
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Allen Brain Atlas
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International Brain Laboratory public data
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OpenNeuro
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