scholarly journals Morphological and cytological ontogenesis of the ampullae of Lorenzini and lateral line canals in the Oman shark,Iago omanensis Norman 1939 (Triakidae), from the Gulf of Aqaba, Red Sea

1998 ◽  
Vol 252 (4) ◽  
pp. 532-545 ◽  
Author(s):  
Lev Fishelson ◽  
Avi Baranes
Keyword(s):  
Red Sea ◽  
Lateral Line ◽  
Gulf Of Aqaba ◽  
Ampullae Of Lorenzini

scholarly journals Saurida golanii, a new deep water lizardfish (Pisces: Synodontidae) from the Gulf of Aqaba, northern Red Sea

Zootaxa ◽  
2011 ◽  
Vol 3098 (1) ◽  
pp. 21 ◽  
Author(s):  
BARRY C. RUSSELL
Keyword(s):  
New Species ◽  
Red Sea ◽  
Lateral Line ◽  
Deep Water ◽  
Gulf Of Aqaba ◽  
Caudal Peduncle ◽  
Pectoral Fins ◽  
Dorsal Fin ◽  
Transverse Scale ◽  
Northern Red Sea

Saurida golanii sp.nov. is described on the basis of eight specimens collected from bottom-set trammel nets in deep water (200–500 m) off Eilat, in the Gulf of Aqaba, northern Red Sea. The new species is characterised by the following combination of characters: lateral-line scales 53–56; transverse scale rows 4½/5½; long pectoral fins (extending beyond a line from origin of pelvic fins to origin of dorsal fin); caudal peduncle compressed (depth greater than width); and pelvic fins unpigmented.

Shrimp-gobies in the southern Gulf of Aqaba (Red Sea)

2012 ◽  
Vol 55 (1) ◽  
pp. 41-46 ◽  
Author(s):  
Mario Freinschlag ◽  
Robert A. Patzner
Keyword(s):  
Red Sea ◽  
Gulf Of Aqaba

Iron and sulphur speciation and cycling in the sediments of marine systems located in the arid environment: Case of the northern Red Sea

2021 ◽  
pp. jgs2021-027
Author(s):  
Valeria Boyko ◽  
Jürgen Pätzold ◽  
Alexey Kamyshny
Keyword(s):  
Red Sea ◽  
Water Depth ◽  
Iron Content ◽  
Gulf Of Aqaba ◽  
Earth System ◽  
Content Type ◽  
Reactive Iron ◽  
The Earth ◽  
Sulphur Cycle ◽  
Supplementary Material

High fluxes of iron minerals associated with aeolian dry deposition may result in anomalously high reactive iron content and fast reoxidation of hydrogen sulphide in the sediments that prevents pyrite formation and results in “cryptic” sulphur cycle. In this work, we studied cycling of iron and sulphur in the deep-water (> 800 m water depth) sediments of the Red Sea and its northern extension, Gulf of Aqaba. We found that reactive iron content in the surface sediments of the Gulf of Aqaba and the Red Sea is high, while the content of sulphur-bound iron is very low and decreases with water depth. The presence of pyrite traces and zero-valent sulfur as well as isotopic compositions of sulphate and pyrite, which are consistent with sulphate reduction under substrate-limiting conditions, suggest that cryptic sulfur cycling is likely to be a result of fast reoxidation of hydrogen sulfide rather than microbial sulfate reduction suppression. In the sediments of Shaban Deep, which are overlain with hyper-saline hydrothermal brine, low reactive iron and high organic carbon contents result in a non-cryptic sulphur cycle characterized by preservation of pyrite in the sediments.Thematic collection: This article is part of the Sulfur in the Earth system collection available at: https://www.lyellcollection.org/cc/sulfur-in-the-earth-systemSupplementary material:https://doi.org/10.6084/m9.figshare.c.5508155

Checklist of the Red Sea Fishes with delineation of the Gulf of Suez, Gulf of Aqaba, endemism and Lessepsian migrants

Zootaxa ◽  
2018 ◽  
Vol 4509 (1) ◽  
pp. 1 ◽  
Author(s):  
DANIEL GOLANI ◽  
RONALD FRICKE
Keyword(s):  
Red Sea ◽  
Endemic Species ◽  
Gulf Of Aqaba ◽  
Gulf Of Suez ◽  
Actual Number ◽  
Suez Gulf ◽  
Number Of Species ◽  
Main Basin ◽  
Lessepsian Migrants ◽  
Current List

The current checklist provides for each species of the Red Sea its records in the Gulf of Suez, Gulf of Aqaba, Red Sea main basin and its general distribution.This new checklist of Red Sea fishes enumerates 1207 species, representing 164 families. Of these, 797 species were recorded from the Gulf of Aqaba and 339 from the Gulf of Suez. The number of species from the Gulf of Suez is evidently lower than the actual number not including 27 Lessepsian (Red Sea) migrants to the Mediterranean that most likely occur in the Gulf. The current list includes 73 species that were newly described for science since the last checklist of 2010. The most specious Osteichthyes families are: Gobiidae (134 species), Labridae (66), Apogonidae (59), Serranidae (including Anthiadinae) (44), Blenniidae (42), Carangidae (38), Muraenidae (36), Pomacentridae (35), Syngnathidae (34), Scorpaenidae (24) and Lutjanidae (23). Among the families of Chondrichthyes, the most specious families are the Carcharhinidae (18 species) and Dasyatidae (11). The total number of endemic species in the Red Sea is 174 species, of these, 34 species are endemic to the Gulf of Aqaba and 8 to the Gulf of Suez. 

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