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Journal articles on the topic 'Southern tyrrhenian'

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Author: Grafiati

Published: 10 March 2023

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1

PSOMADAKIS, PETER NICK, STEFANO GIUSTINO, and MARINO VACCHI. "Mediterranean fish biodiversity: an updated inventory with focus on the Ligurian and Tyrrhenian seas." Zootaxa 3263, no. 1 (April 9, 2012): 1. http://dx.doi.org/10.11646/zootaxa.3263.1.1.

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In this paper we update the Mediterranean fish inventory, analyse the biogeographic features of this fauna and provideexhaustive biodiversity data for the Ligurian and Tyrrhenian seas. According to the data available in 2010, the Mediterraneanfish diversity can be summarized as follows: 602 (including sub-species) bony fish species (Osteichthyes), 79 cartilaginous fishspecies (Chondrichthyes) and 3 cyclostomes (Agnatha); making a total of 684 species belonging to 173 families (147Osteichthyes, 24 Chondrichthyes, 2 Agnatha). Most species 403 (58.9%) have an Atlantic origin, 128 (18.7%) species arecosmopolitan, 90 (13.2%) species are Indo-Pacific, and 63 (9.2%) are endemic to the Mediterranean. In the Ligurian Sea,northern Tyrrhenian and southern Tyrrhenian Sea, the richness can be estimated at 454, 426 and 447 species, respectively. Themost speciose families for the Mediterranean as a whole, but also for the three intra-mediterranean areas studied are theGobiidae, Sparidae, Labridae and Blenniidae; whereas Carangidae is a numerically important family mainly at theMediterranean level. The percentage of endemic fishes within the intra-mediterranean areas studied gradually decrease acrosslatitude from the Ligurian Sea (9.4%) to the northern (8.7%) and southern (8.0%) Tyrrhenian Sea. The updated fish inventorycontains 81 Lessepsian and 48 Atlantic immigrant species, which represent 11.8% and 7.0% of the whole Mediterranean fishcommunity, respectively. The Ligurian Sea (3.1%) houses a higher amount of immigrants with respect to the northern (1.6%)and southern (2.7%) Tyrrhenian sectors.Field observations made during this study indicate that both the Ligurian and Tyrrhenian seas are presently subjected toincreasing colonization events by thermophilic species spreading from the southern Mediterranean and to a lesser degree by the arrival of exotic species either of Atlantic or Indo-Pacific origin.

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2

Amelio, M., and E. Martorelli. "Seismo-stratigraphic characters of paleocontourites along the Calabro-Tyrrhenian margin (Southern Tyrrhenian Sea)." Marine Geology 252, no. 3-4 (July 2008): 141–49. http://dx.doi.org/10.1016/j.margeo.2008.03.011.

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3

Nicolosi, Agata, Nicola Sapone, Lorenzo Cortese, and Claudio Marcianò. "Fisheries-related Tourism in Southern Tyrrhenian Coastline." Procedia - Social and Behavioral Sciences 223 (June 2016): 416–21. http://dx.doi.org/10.1016/j.sbspro.2016.05.257.

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4

Casalbore, D., A. Bosman, C. Romagnoli, M. Di Filippo, and F. L. Chiocci. "Morphology of Lipari offshore (Southern Tyrrhenian Sea)." Journal of Maps 12, no. 1 (November 24, 2014): 77–86. http://dx.doi.org/10.1080/17445647.2014.980858.

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5

Casalbore, D., A. Bosman, C. Romagnoli, and F. L. Chiocci. "Morphology of Salina offshore (Southern Tyrrhenian Sea)." Journal of Maps 12, no. 5 (July 31, 2015): 725–30. http://dx.doi.org/10.1080/17445647.2015.1070300.

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6

De Luca, G., L. Filippi, D. Caccamo, G. Neri, and R. Scarpa. "Crustal structure and seismicity of southern Tyrrhenian basin." Physics of the Earth and Planetary Interiors 103, no. 1-2 (October 1997): 117–33. http://dx.doi.org/10.1016/s0031-9201(97)00026-5.

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7

Maugeri, Teresa L., Giovanna Bianconi, Francesco Canganella, Roberto Danovaro, Concetta Gugliandolo, Francesco Italiano, Valeria Lentini, Elena Manini, and Barbara Nicolaus. "Shallow hydrothermal vents in the southern Tyrrhenian Sea." Chemistry and Ecology 26, sup1 (June 2010): 285–98. http://dx.doi.org/10.1080/02757541003693250.

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8

Carnevale, Alex, Francesco Luigi Leonetti, Gianni Giglio, Emilio Sperone, Sandro Tripepi, Concetta Milazzo, and Luca Lanteri. "Prvi dokumentirani zapis o Tetragonurus cuvieri Risso, 1810. (Perciformes, Stromatoidea) duž kalabrijskih obala (Južna Italija, Središnji Mediteran)." Acta Adriatica 62, no. 1 (July 26, 2021): 105–10. http://dx.doi.org/10.32582/aa.62.1.9.

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The first record of Tetragonurus cuvieri Risso, 1810 off Calabrian coast (Southern Italy, Central Mediterranean) is reported. The specimen, a male of 361 mm total length, was found at a depth of 7 m during a scientific visual census research activity, in March 2017. The sighting was located off the Tyrrhenian coast of Calabria (Paola: 39.355453N, 16.029192E). The present finding represents the 1st documented record for the Tyrrhenian coast of the Calabria region.

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9

ZAMMIT, P. P., C. LONGO, and P. J. SCHEMBRI. "Occurrence of Paraleucilla magna Klautau et al., 2004 (Porifera: Calcarea) in Malta." Mediterranean Marine Science 10, no. 2 (December 2, 2009): 135. http://dx.doi.org/10.12681/mms.114.

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The calcareous sponge Paraleucilla magna, first recorded from the Mediterranean in 2001 (southern Tyrrhenian, southern Adriatic and northwest Ionian coasts of Italy), is recorded from Malta (Central Mediterranean) where it was found forming part of the fouling community on small, surface marker-buoys around a fish-farm in Marsaxlokk Bay.

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10

D’Iglio, Claudio, Marco Albano, Francesco Tiralongo, Sergio Famulari, Paola Rinelli, Serena Savoca, Nunziacarla Spanò, and Gioele Capillo. "Biological and Ecological Aspects of the Blackmouth Catshark (Galeus melastomus Rafinesque, 1810) in the Southern Tyrrhenian Sea." Journal of Marine Science and Engineering 9, no. 9 (September 6, 2021): 967. http://dx.doi.org/10.3390/jmse9090967.

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Data on the biology and ecology of Galeus melastomus are old/absent for the Southern Tyrrhenian Sea, despite there being numerous studies in the wider area. A total of 127 specimens of G. melastomus from the southern Tyrrhenian Sea, collected in 2018–2019 using trawling nets, were analyzed to investigate size at sexual maturity, sex ratio, length–weight relationships, and feeding habits. To our best knowledge, this is the first time in which all these features were investigated in the Southern Tyrrhenian Sea for G. melastomus. The stomach content analysis showed that G. melastomus had intermediate feeding habits, preying on a great variety of species, especially Cephalopoda, Osteichthyes, and Crustacea. The Levin’s index value (Bi) was 0.53. Sex ratio was 0.92:1, with females slightly more abundant and bigger than males. The results also showed a decrease (33.7 cm for females, 31.1 cm for males) in length at 50% maturity (L50). This could be a result of anthropogenic stressors, such as overfishing and/or and environmental changes, which can induce physiological responses in several species. Our results highlighted the differences related to sexual maturity, growth, and feeding habits of the blackmouth catshark in the studied area, providing reference data to allow comparison with future studies on this species adaptations to this and other deep-sea areas in the Mediterranean Sea.

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11

Pasquale, V., M. Verdoya, and P. Chiozzi. "Thermal state and deep earthquakes in the Southern Tyrrhenian." Tectonophysics 306, no. 3-4 (June 1999): 435–48. http://dx.doi.org/10.1016/s0040-1951(99)00070-0.

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12

Pasquale, V., P. Chiozzi, and M. Verdoya. "Sedimentation rates and subsidence in the Southern Tyrrhenian Basin." Marine Geophysical Researches 27, no. 3 (September 20, 2006): 155–65. http://dx.doi.org/10.1007/s11001-005-4564-1.

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13

Di Bella, Marcella, Francesco Italiano, Giuseppe Sabatino, Alessandro Tripodo, Angela Baldanza, Sergio Casella, Paolo Pino, Riccardo Rasa’, and Selma Russo. "Pleistocene volcaniclastic units from North-Eastern Sicily (Italy): new evidence for calc-alkaline explosive volcanism in the Southern Tyrrhenian Sea." Geologica Carpathica 67, no. 4 (August 1, 2016): 371–89. http://dx.doi.org/10.1515/geoca-2016-0023.

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Abstract A well-preserved volcaniclastic sequence crops out in Pleistocene marine sediments along the Tyrrhenian coastline of the Calabrian-Peloritani arc (Sicily, Italy), testifying the occurrence of Lower-Middle Pleistocene volcanic activity in Southern Tyrrhenian Sea. The presence of dominant highly vesicular and minor blocky glassy particles indicates that the volcanic clasts were originated by explosive events related to the ascent and violent emission of volatile-rich magmas accompanied by and/or alternated with hydromagmatic fragmentation due to magma-sea water interaction. Field investigations and sedimentological features of the studied volcaniclastic units suggest a deposition from sediment-water density flows. The chemical classification of the pumice clasts indicates prevalent rhyolitic and dacitic compositions with calc-alkaline to high-K calc-alkaline affinity. The geochemical features of immobile trace elements together with the presence of orthopyroxene are indicative of a provenance from an arc-type environment. The age (from 980-910 to 589 ka), the chemical composition and the evidence of subaerial explosive volcanic activity constrain the origin nature and temporal evolution of the arc-type volcanism in the Southern Tyrrhenian domain. Finally, the new information here provided contribute to a better understanding of the temporal geodynamic evolution of this sector of the Mediterranean domain.

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14

Consoli, P., T. Romeo, G. Florio, F. Perdichizzi, S. Greco, M. Vacchi, and P. Rinelli. "First record of Carcharhinus plumbeus (Pisces: Carcharhinidae) from the southern Tyrrhenian Sea." Journal of the Marine Biological Association of the United Kingdom 84, no. 5 (October 2004): 1085–86. http://dx.doi.org/10.1017/s0025315404010471h.

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One juvenile specimen of the sandbar shark Carcharhinus plumbeus was recorded for the first time from the southern Tyrrhenian Sea. The specimen has been collected in an area of the Sicilian coast where trawling is banned except for scientific purposes. Morphometrics and meristics data are given.

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15

PINTO, CECILIA, GIOVANNI ROPPO VALENTE, NICOLA RASORE, EDOARDO OLMI, LUCA LANTERI, FULVIO GARIBALDI, CLAUDIO VIVA, et al. "Range expansion of the Atlantic fish Zenopsis conchifer (Lowe, 1852), family Zeidae, in the western Mediterranean Sea." Mediterranean Marine Science 24, no. 1 (January 30, 2023): 90–95. http://dx.doi.org/10.12681/mms.31409.

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Three specimens of Silver John dory, Zenopsis conchifer, (Lowe, 1852) were observed for the first time in the Ligurian Sea and northern Tyrrhenian Sea (western Mediterranean), one in 2020 and two in 2021. This is the fifth record (up to ten individuals) of Z. conchifer in the Mediterranean Sea, which occurred 11 years after the last observation in 2010 in the southern Tyrrhenian Sea. The present study reports the northernmost record of the species in the western Mediterranean Sea, indicating a potential range expansion of the distribution of this Atlantic species across the area. Morphometric, meristic and biological data of the three specimens are provided and compared with previous published records.

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16

Pola, L., C. Cerrano, D. Pica, V. Markantonatou, M. C. Gambi, and B. Calcinai. "Macrofaunal communities in the Gioia Canyon (Southern Tyrrhenian Sea, Italy)." European Zoological Journal 87, no. 1 (January 1, 2020): 122–30. http://dx.doi.org/10.1080/24750263.2020.1725665.

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17

Trua, Teresa, Giancarlo Serri, Michael Marani, Alberto Renzulli, and Fabiano Gamberi. "Volcanological and petrological evolution of Marsili Seamount (southern Tyrrhenian Sea)." Journal of Volcanology and Geothermal Research 114, no. 3-4 (May 2002): 441–64. http://dx.doi.org/10.1016/s0377-0273(01)00300-6.

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18

Cuffaro, Marco, Federica Riguzzi, Davide Scrocca, and Carlo Doglioni. "Coexisting tectonic settings: the example of the southern Tyrrhenian Sea." International Journal of Earth Sciences 100, no. 8 (January 20, 2011): 1915–24. http://dx.doi.org/10.1007/s00531-010-0625-z.

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19

Piangiamore, G. L., O. Faggioni, and M. S. Barbano. "Crustal magnetism of the Southern Tyrrhenian Sea from aeromagnetic surveys." Geological Society, London, Special Publications 262, no. 1 (2006): 337–48. http://dx.doi.org/10.1144/gsl.sp.2006.262.01.20.

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20

Pondrelli, S., C. Piromallo, and E. Serpelloni. "Convergence vs. retreat in Southern Tyrrhenian Sea: Insights from kinematics." Geophysical Research Letters 31, no. 6 (March 2004): n/a. http://dx.doi.org/10.1029/2003gl019223.

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21

Neri, G., D. Caccamo, O. Cocina, and A. Montalto. "Geodynamic implications of earthquake data in the southern Tyrrhenian sea." Tectonophysics 258, no. 1-4 (June 1996): 233–49. http://dx.doi.org/10.1016/0040-1951(95)00202-2.

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22

Pasquale, V., P. Chiozzi, and M. Verdoya. "Isostasy and paleotemperatures in the Southern Tyrrhenian Basin, Mediterranean Sea." Marine Geophysical Researches 28, no. 2 (June 5, 2007): 139–51. http://dx.doi.org/10.1007/s11001-007-9021-x.

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23

Iannace, Pietro, Maurizio M. Torrente, and Alfonsa Milia. "Tectono-stratigraphic evolution of the Southern Campania Margin: a key area for the evolution of the Tyrrhenian-Apennine system." Oil & Gas Science and Technology – Revue d’IFP Energies nouvelles 73 (2018): 39. http://dx.doi.org/10.2516/ogst/2018035.

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The Southern Campania Margin (SCM) represents a key area of the Central Mediterranean because it records all the rifting stages of the Tyrrhenian Sea. The interpretation of a seismic dataset calibrated with deep wells and outcrops, using seismic stratigraphy and structural geology methods in a dedicated Geographic Information System (GIS) environment, the seismic depth conversion, the generation of 2-D and 3-D models led to the reconstruction of a polyphased tectono-stratigraphic evolution of the SCM. During the early stage of Tyrrhenian opening a terrigenous transtensional Basin (Langhian-Tortonian Cilento Basin) formed on the Liguride accretionary prism adjacent to the Calabria crystalline terrane. In the SCM the Liguride thrust sheets tectonically overly the Apennine Platform units and both these nappes have been dismembered by Quaternary faults. Three rifting stages, not homogeneously distributed, affected the region since the Lower Pleistocene. They are associated to the deposition of a thick Quaternary succession (A, B and C units). During these Pleistocene stages there was an abrupt change of the extension direction (from NE-SW to NW-SE) accompanying a change of the nappe transport direction of the Southern Apennines. The construction of balanced sections using dedicated software, permitted us to recognize the true geometry of the faults and compute the amount of Quaternary extension of the SCM that results comparable to those calculated for other sectors of the Tyrrhenian margin and further extensional regions worldwide.

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24

PROSSER, GIACOMO, MARIO BENTIVENGA, MARINELLA A. LAURENZI, ALFREDO CAGGIANELLI, PIERFRANCESCO DELLINO, and DOMENICO DORONZO. "Late Pliocene volcaniclastic products from Southern Apennines: distal witness of early explosive volcanism in the central Tyrrhenian Sea." Geological Magazine 145, no. 4 (April 11, 2008): 521–36. http://dx.doi.org/10.1017/s0016756808004512.

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AbstractTwo volcaniclastic successions intercalated in Pliocene basinal clays from the Southern Apennines have been analysed to determine their provenance and their relationship with the geodynamic evolution of the Western Mediterranean. The studied deposits are exclusively made up of ashy pyroclasts, dominated by fresh acidic to intermediate glass, mostly in the form of shards, pumice fragments and groundmass fragments with vitrophyric texture. Crystals include Pl, Opx, Cpx, Hbl and rare Bt. Sedimentological features suggest that the volcanic material accumulated near the basin margin by primary fallout processes and was later remobilized by density currents. 40Ar–39Ar geochronology allowed dating of one succession at 2.24±0.06 Ma, corresponding to the Late Pliocene. Composition of the volcaniclastic material is typical of a transitional high-K calc-alkaline series. The age and chemical composition constrain the provenance of the volcaniclastic rocks from the Southern Tyrrhenian domain. Here, volcanic centres were active during Pliocene time, approximately at the northern end of a volcanic arc formed before the opening of the southernmost part of the sea. This paper shows that a detailed study of volcaniclastic products from the southern Apennines and Calabria can be very useful in collecting new pieces of information on the eruption history of the southern Tyrrhenian domain, since they record additional data not available from the study of exposed volcanic edifices.

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25

Argnani, Andrea. "Evolution of the southern Tyrrhenian slab tear and active tectonics along the western edge of the Tyrrhenian subducted slab." Geological Society, London, Special Publications 311, no. 1 (2009): 193–212. http://dx.doi.org/10.1144/sp311.7.

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26

De Ritis, R., G. Ventura, M. Chiappini, R. Carluccio, and R. von Frese. "Regional magnetic and gravity anomaly correlations of the Southern Tyrrhenian Sea." Physics of the Earth and Planetary Interiors 181, no. 1-2 (July 2010): 27–41. http://dx.doi.org/10.1016/j.pepi.2010.04.003.

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27

Mazzola, A., E. Favaloro, and G. Sarà. "Experiences of integrated mariculture in a southern Tyrrhenian area (Mediterranean Sea)." Aquaculture Research 30, no. 10 (October 1999): 773–80. http://dx.doi.org/10.1046/j.1365-2109.1999.00406.x.

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28

Bonomo, S., F. Placenti, E. M. Quinci, A. Cuttitta, S. Genovese, S. Mazzola, and A. Bonanno. "Living coccolithophores community from Southern Tyrrhenian Sea (Central Mediterranean — Summer 2009)." Marine Micropaleontology 131 (March 2017): 10–24. http://dx.doi.org/10.1016/j.marmicro.2017.02.002.

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29

Falco, I. De, A. Iazzetta, and G. Luongo, A. Mazzarella, E. Tarantino. "The Seismicity in the Southern Tyrrhenian Area and its Neural Forecasting." Pure and Applied Geophysics 157, no. 3 (March 1, 2000): 343–55. http://dx.doi.org/10.1007/s000240050003.

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30

Menna, Milena, Pierre-Marie Poulain, Daniele Ciani, Andrea Doglioli, Giulio Notarstefano, Riccardo Gerin, Marie-Helene Rio, Rosalia Santoleri, Adam Gauci, and Aldo Drago. "New Insights of the Sicily Channel and Southern Tyrrhenian Sea Variability." Water 11, no. 7 (June 29, 2019): 1355. http://dx.doi.org/10.3390/w11071355.

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The dynamics of the Sicily Channel and the southern Tyrrhenian Sea are highly influenced by the seasonal variability of the Mediterranean basin-wide circulation, by the interannual variability of the numerous mesoscale structures present in the Channel, and by the decadal variability of the adjacent Ionian Sea. In the present study, all these aspects are investigated using in-situ (Lagrangian drifter trajectories and Argo float profiles) and satellite data (Absolute Dynamic Topography, Sea Level Anomaly, Sea Surface Temperature, wind products) over the period from 1993 to 2018. The availability of long time series of data and high-resolution multi-sensor surface currents allow us to add new details on the circulation features and on their driving mechanisms and to detect new permanent eddies not yet described in literature. The structures prevailing in winter are mainly driven by wind, whereas those prevailing in summer are regulated by topographical forcing on surface currents. The strength of the surface structures located at the western entrance of the Ionian Sea and of the mesoscale activity along the northern Sicily coast is modulated by the large-scale internal variability. The vertical hydrological characteristics of these mesoscale eddies are delineated using the Argo float profiles inside these structures.

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31

Perri, Edoardo, Maria Pia Bernasconi, and Massimo Cefalà. "Quaternary carbonate deposition and climate variation (Tyrrhenian coast, Calabria, Southern Italy)." Rendiconti Online della Società Geologica Italiana 38 (February 2016): 73–76. http://dx.doi.org/10.3301/rol.2016.21.

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32

Crocetta, Fabio, Ottavio Soppelsa, and Carlo Pipitone. "Maja goltziana d'oliveira, 1888 (Decapoda, Brachyura, Majidae) in the southern Tyrrhenian Sea." Crustaceana 78, no. 1 (2005): 121–24. http://dx.doi.org/10.1163/1568540054024529.

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33

Giordano, Daniela, Adriana Profeta, Barbara Busalacchi, Roberta Minutoli, Letterio Guglielmo, Alessandro Bergamasco, and Antonia Granata. "Summer larval fish assemblages in the Southern Tyrrhenian Sea (Western Mediterranean Sea)." Marine Ecology 36, no. 1 (April 7, 2014): 104–17. http://dx.doi.org/10.1111/maec.12123.

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34

Selvaggi, G., and C. Chiarabba. "Seismicity and P-wave velocity image of the Southern Tyrrhenian subduction zone." Geophysical Journal International 121, no. 3 (June 1995): 818–26. http://dx.doi.org/10.1111/j.1365-246x.1995.tb06441.x.

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35

Etiope, G., P. Beneduce, M. Calcara, P. Favali, F. Frugoni, M. Schiattarella, and G. Smriglio. "Structural pattern and CO2–CH4 degassing of Ustica Island, Southern Tyrrhenian basin." Journal of Volcanology and Geothermal Research 88, no. 4 (March 1999): 291–304. http://dx.doi.org/10.1016/s0377-0273(99)00010-4.

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36

Italiano, Francesco, Angelo De Santis, Paolo Favali, Mario Rainone, Sergio Rusi, and Patrizio Signanini. "The Marsili Volcanic Seamount (Southern Tyrrhenian Sea): A Potential Offshore Geothermal Resource." Energies 7, no. 7 (June 26, 2014): 4068–86. http://dx.doi.org/10.3390/en7074068.

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37

Pepe, Fabrizio, Giovanni Bertotti, and Sierd Cloetingh. "Tectono-stratigraphic modelling of the North Sicily continental margin (southern Tyrrhenian Sea)." Tectonophysics 384, no. 1-4 (June 2004): 257–73. http://dx.doi.org/10.1016/j.tecto.2004.04.002.

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38

Chiozzi, P., V. Pasquale, M. Verdoya, and S. Minato. "Gamma-ray activity in the volcanic islands of the Southern Tyrrhenian Sea." Journal of Environmental Radioactivity 67, no. 3 (January 2003): 235–46. http://dx.doi.org/10.1016/s0265-931x(03)00026-2.

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39

Milia, Alfonsa, and Maurizio M. Torrente. "Early-stage rifting of the Southern Tyrrhenian region: The Calabria–Sardinia breakup." Journal of Geodynamics 81 (November 2014): 17–29. http://dx.doi.org/10.1016/j.jog.2014.06.001.

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40

Spinelli, Andrea, and Luca Castriota. "A new record of Gymnothorax unicolor (Muraenidae) in the southern Tyrrhenian Sea." Marine Biodiversity 47, no. 3 (May 27, 2016): 785–86. http://dx.doi.org/10.1007/s12526-016-0512-3.

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41

Busalacchi, B., P. Rinelli, F. De Domenico, A. Profeta, F. Perdichizzi, and T. Bottari. "Analysis of demersal fish assemblages off the Southern Tyrrhenian Sea (central Mediterranean)." Hydrobiologia 654, no. 1 (July 13, 2010): 111–24. http://dx.doi.org/10.1007/s10750-010-0374-9.

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42

De Astis, Gianfilippo, Luigi La Volpe, Angelo Peccerillo, and Lucia Civetta. "Volcanological and petrological evolution of Vulcano island (Aeolian Arc, southern Tyrrhenian Sea)." Journal of Geophysical Research: Solid Earth 102, B4 (April 10, 1997): 8021–50. http://dx.doi.org/10.1029/96jb03735.

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43

Ferraro, Luciana, Ines Alberico, Fabrizio Lirer, and Mattia Vallefuoco. "Distribution of benthic foraminifera from the southern Tyrrhenian continental shelf (South Italy)." Rendiconti Lincei 23, no. 1 (January 12, 2012): 103–19. http://dx.doi.org/10.1007/s12210-011-0160-2.

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44

Chiarabba, Claudio, Pasquale De Gori, and Fabio Speranza. "The southern Tyrrhenian subduction zone: Deep geometry, magmatism and Plio-Pleistocene evolution." Earth and Planetary Science Letters 268, no. 3-4 (April 2008): 408–23. http://dx.doi.org/10.1016/j.epsl.2008.01.036.

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45

ROMEO, T., L. CASTRIOTA, P. CONSOLI, M. FALAUTANO, G. FLORIO, F. PERDICHIZZI, M. G. FINOIA, F. ANDALORO, and P. RINELLI. "Bathymetric and longitudinal distribution analyysis of the rockfish Helicolenus Dactylopterus (Delaroche, 1809) in the southern Tyrrhenian Sea (central Mediterranean)." Mediterranean Marine Science 10, no. 1 (June 1, 2009): 73. http://dx.doi.org/10.12681/mms.123.

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This study provides information on bathymetric and longitudinal distribution heterogeneity of the rockfish Helicolenus dactylopterus in the southern Tyrrhenian Sea. Data were drawn from experimental bottom trawl (1996-2002) plus bottom trap (2001-02) surveys. The frequency of occurrence and mean relative density (N/km2) and biomass (kg/km2) indexes were calculated for two survey seasons (spring and autumn), four geographic sectors and three depth strata. MANOVA was used to test fish abundance among years, sectors and strata. Analysis of the length-frequency distributions was carried out by two-way (gears and depths) ANOVA, post hoc multiple comparisons for testing differences among depths and Student’s t test for testing differences between gears. Length-weight relationship was also estimated and the allometric coefficient was tested with the Student’s t test. The results showed a significant positive bathymetric gradient of sizes both for trawl and trap surveys; at same depths, fish caught by traps were significantly longer than those caught by trawl. In spring surveys, significant differences were found among strata for both abundance indexes; in autumn surveys, significant differences between depth strata were found only for density indices. The distribution and abundance patterns of H. dactylopterus along the southern Tyrrhenian Sea was homogeneous among sectors. Length-weight relationship showed a significant positive allometric growth.

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46

Komar, Paulina. "Aegean Enigma: The Rise and Fall of Vineyards during Antiquity." Electrum 27 (2020): 33–43. http://dx.doi.org/10.4467/20800909el.20.002.12792.

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This paper argues that the rise and fall of north and central Aegean wine exportations was caused by economic factors, such as changes in wine supply. It demonstrates that these wines disappeared from southern Gaul and central Tyrrhenian Italy when these areas started to locally produce their own wine. At the same time, north and central Aegean wines were also ousted from the Black Sea region by both local products and cheaper imports from the southern Aegean. This shows that supply and demand governed commercial activities during the Classical and Hellenistic periods, which provides new evidence regarding the nature of the ancient Greek economy.

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Pipitone, Carlo, Arturo Zenone, Fabio Badalamenti, and Giovanni D'Anna. "First record of the blue crab Callinectes sapidus (Crustacea, Decapoda, Portunidae), a non-indigenous species in the central/southern Tyrrhenian Sea." Acta Adriatica 61, no. 1 (June 29, 2020): 101–6. http://dx.doi.org/10.32582/aa.61.1.8.

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Four individuals of the non-indigenous blue crab, Callinectes sapidus Rathbun, 1896 (Crustacea, Decapoda, Portunidae) were collected during commercial trammel net operations in fall 2019 and winter 2020 along the coast of NW Sicily. The crabs were collected in very shallow waters on a sandy bottom close to the coast. Although blue crabs are now widespread along most eastern, western and northern Mediterranean coasts, this is the first record of this species from the central and southern Tyrrhenian Sea

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Longo, Caterina. "Leucosolenia microspinata sp. nov. (Porifera: Calcarea), a new species from the Mediterranean Sea." Journal of the Marine Biological Association of the United Kingdom 89, no. 8 (June 23, 2009): 1663–69. http://dx.doi.org/10.1017/s0025315409990440.

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A new species of Leucosoleniidae, Leucosolenia microspinata sp. nov., from the southern Tyrrhenian Sea (Porto Vecchio pond, Marinello Marine Reserve, Messina) is here described. The species consists of a dense reticulation of ascon tubes having a colour ranging from white-cream to light-brown. Its spiculation consists of diactines sometimes serrated or microspined, not separable into size-classes, triactines of four types and tetractines with microspined apical actine. The comparison with other Mediterranean Leucosolenia is reported.

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Montuori, A., P. de Ruggiero, M. Migliaccio, S. Pierini, and G. Spezie. "X-band COSMO-SkyMed wind field retrieval, with application to coastal circulation modeling." Ocean Science 9, no. 1 (February 14, 2013): 121–32. http://dx.doi.org/10.5194/os-9-121-2013.

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Abstract. In this paper, X-band COSMO-SkyMed© synthetic aperture radar (SAR) wind field retrieval is investigated, and the obtained data are used to force a coastal ocean circulation model. The SAR data set consists of 60 X-band Level 1B Multi-Look Ground Detected ScanSAR Huge Region COSMO-SkyMed© SAR data, gathered in the southern Tyrrhenian Sea during the summer and winter seasons of 2010. The SAR-based wind vector field estimation is accomplished by resolving both the SAR-based wind speed and wind direction retrieval problems independently. The sea surface wind speed is retrieved by means of a SAR wind speed algorithm based on the azimuth cut-off procedure, while the sea surface wind direction is provided by means of a SAR wind direction algorithm based on the discrete wavelet transform multi-resolution analysis. The obtained wind fields are compared with ground truth data provided by both ASCAT scatterometer and ECMWF model wind fields. SAR-derived wind vector fields and ECMWF model wind data are used to construct a blended wind product regularly sampled in both space and time, which is then used to force a coastal circulation model of a southern Tyrrhenian coastal area to simulate wind-driven circulation processes. The modeling results show that X-band COSMO-SkyMed© SAR data can be valuable in providing effective wind fields for coastal circulation modeling.

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Montuori, A., P. de Ruggiero, M. Migliaccio, S. Pierini, and G. Spezie. "X-band COSMO-SkyMed wind field retrieval, with application to coastal circulation modeling." Ocean Science Discussions 9, no. 5 (October 16, 2012): 3251–79. http://dx.doi.org/10.5194/osd-9-3251-2012.

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Abstract. In this paper, X-band COSMO-SkyMed© SAR wind field retrieval is investigated to force coastal circulation modeling. The SAR data set consists of 60 X-band Level 1B Multi-Look Ground Detected ScanSAR Huge Region COSMO-SkyMed© SAR data, gathered in the Southern Tyrrhenian Sea during the Summer and Winter seasons of 2010. The SAR-based wind vector field estimation is accomplished by resolving both the SAR-based wind speed and wind direction retrieval problems independently. The sea surface wind speed is retrieved by means of a SAR wind speed algorithm based on the Azimuth cut-off procedure, while the sea surface wind direction is provided by means of a SAR wind direction algorithm based on the Discrete Wavelet Transform Multi-Resolution Analysis. The obtained wind fields are compared with ground truth data provided by both ASCAT scatterometer and ECMWF model wind fields. SAR-derived wind vector fields and ECMWF model wind data are used to construct a blended wind product regularly sampled in both space and time, which is then used to force a coastal circulation model of a Southern Tyrrhenian coastal area to simulate wind-driven circulation processes. The modeling results clearly show that X-band COSMO-SkyMed© SAR data can be valuable in providing effective wind fields for coastal circulation modeling.

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