Mating behaviour of the newly-established ornate wrasse Thalassomapavo (Osteichthyes: Labridae) in the Ligurian Sea (north-western Mediterranean)

Author(s):  
Giampietro Sara ◽  
Carlo Nike Bianchi ◽  
Carla Morri

Reproduction of newly established populations of the warm-water Atlantic Mediterranean wrasse Thalassoma pavo is here reported for the first time in the Ligurian Sea, and mating behaviour is described in detail. The reproductive season (May to October) may be divided in three stages: (1) pre-mating (mid-May to the end of June), during which terminal-phase (TP) males establish territories and start courting females; (2) mating (end of June to the end of August), with a mean frequency of up to one spawning event ind−1 h−1; and (3) post-mating (September to mid-October), when TP males remained inside territories but no spawning events were recorded. Mating followed two distinct modalities: pair spawning and group spawning, the latter replacing the former when population density exceeded 10 ind 100 m−2. Four phases have been distinguished in both modalities: (1) approach (pair) or gathering (group), to establish the contact between potential partners; (2) acceptance (pair) or priming (group), in which partners establish a common behavioural pattern; (3) ascent to near the sea surface; and (4) spawning. The saddled sea-bream Oblada melanura has been seen to predate intensively on the large cloud of sexual products released by groups.

2018 ◽  
Vol 135 ◽  
pp. 303-310 ◽  
Author(s):  
Ilaria Bernardini ◽  
Fulvio Garibaldi ◽  
Laura Canesi ◽  
Maria Cristina Fossi ◽  
Matteo Baini

2019 ◽  
Vol 51 (1) ◽  
pp. 51-54
Author(s):  
Ignacio Ribera ◽  
Carles Hernando

Ochthebius (Ochthebius) lobiccoastal habitatsollis Rey, 1885 is recorded for the first time from the Iberian Peninsula (Girona) and the island of Corsica; new records are also given for the islands of Menorca and Sardinia. The species is known only from coastal habitats through the Gulf of Lion and the Ligurian and Balearic seas, typically living in rockpools of different salinity or small trickles or freshwater runoffs. Genetic data of the cytochrome oxidase 1 gene from Iberian, Menorcan and Sardinian specimens shows less than 1% divergence, suggesting lack of isolation between populations.


1989 ◽  
Vol 59 (4) ◽  
pp. 243-249 ◽  
Author(s):  
Rony Huys

The new genus and species, Dicrotrichura tricincta, is described from deep mud (1220 m) in the Ligurian Sea (western Mediterranean). It is the first tantulocaridan not found to be attached to a crustacean host but free living in the sediment. It is assigned to the Deoterthridae on the basis of the absence of a rostrum, the abdominal segmentation and the characteristic cephalic pore pattern. It can be distinguished from all known tantulocaridans in the presence of peculiar, bi-articulated caudal setae and the difference in thoracopodal setation between leg 2 and legs 3–5. Some new structures located on the attachment disc are described for the first time. D. tricincta is the second tantulocaridan to be recorded from the Mediterranean.


2010 ◽  
Vol 74 (19) ◽  
pp. 5549-5559 ◽  
Author(s):  
Lars-Eric Heimbürger ◽  
Daniel Cossa ◽  
Jean-Claude Marty ◽  
Christophe Migon ◽  
Bernard Averty ◽  
...  

2006 ◽  
Vol 24 (2) ◽  
pp. 443-452 ◽  
Author(s):  
S. Sparnocchia ◽  
M. E. Schiano ◽  
P. Picco ◽  
R. Bozzano ◽  
A. Cappelletti

Abstract. Meteorological and sea temperature data from the ODAS Italia 1 buoy (Ligurian Sea, Western Mediterranean) are used to study the anomalous warming of summer 2003 at sea. The event was related to the record heat wave that interested much of Europe from June to September of that year. The data show that the anomalous warming was prevalently confined to within a few meters below the sea surface. On the contrary, the temperatures in the underlying layers were lower than usual. The limited vertical propagation of heat is ascribed to the high temperature difference that arose between the surface and the deeper layers due to protracted calm weather conditions. The degree of penetration of heat deduced from the observations is consistent with that computed on the basis of an energetic argument, wherein the wind constitutes the sole supply of kinetic energy, while the heating is viewed as the source of potential energy that must be "subtracted" by mixing. The results support the hypothesis that the scanty energy from the wind is mainly responsible for the development of the temperature anomaly at the sea surface.


2019 ◽  
Vol 86 (1) ◽  
pp. 343-353
Author(s):  
F. Betti ◽  
M. Bo ◽  
F. Enrichetti ◽  
M. Manuele ◽  
R. Cattaneo-Vietti ◽  
...  

2000 ◽  
Vol 3 (4) ◽  
pp. 284-293 ◽  
Author(s):  
C. Cerrano ◽  
G. Bavestrello ◽  
C.N. Bianchi ◽  
R. Cattaneo-vietti ◽  
S. Bava ◽  
...  

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