Hadrosauroid Dinosaurs from the Late Cretaceous of the Sultanate of Oman

Fragmentary post-cranial remains (femora, tibia, vertebrae) of ornithischian dinosaurs from the Late Cretaceous of the Sultanate of Oman are described and referred to hadrosauroids. The specimens come from the Al-Khod Conglomerate, of latest Campanian to Maastrichtian age, in the north-eastern part of the country. Although the fragmentary condition of the fossils precludes a precise identification, various characters, including the shape of the fourth trochanter of the femur and the morphology of its distal end, support an attribution to hadrosauroids. With the possible exception of a possible phalanx from Angola, this group of ornithopod dinosaurs, which apparently originated in Laurasia, was hitherto unreported from the Afro-Arabian plate. From a paleobiogeographical point of view, the presence of hadrosauroids in Oman in all likelihood is a result of trans-Tethys dispersal from Asia or Europe, probably by way of islands in the Tethys shown on all recent paleogeographical maps of that area. Whether hadrosauroids were widespread on the Afro-Arabian landmass in the latest Cretaceous, or where restricted to the « Oman island » shown on some paleogeographical maps, remains to be determined.     

Genetic characterization in four sciaenid species from the Arabian Sea

Four sciaenid species Johnieops dussumieri, Kathala axillaris, Pennahia macropthalmus and Otolithes ruber were analysed electrophoretically for genetic variation at 18 loci (16 in P. macropthalmus and O. ruber ). Twelve loci were polymorphic in J. dussumieri , 10 in K. axillaris , three in P. macropthalmus and 12 in O. ruber ( P <0·99). Average heterozygosity ranged from 0·033 ± 0·100 to 0·070 ± 0·122. The allele frequencies of 14 loci were used to estimate Nei's genetic distance (). The values ranged from 0·334 to 0·612. Three isozyme loci ( LDH-B*, MDH-2* and G3PDH-1* ) were found to be the most reliable species-specific markers.     

Spawning behavior and reproductive isolation of two species ofPseudolabrus

The reproductive behavior of two wrasses,Pseudolabrus eoethinus (Richardson, 1846) andP. sieboldi Mabuchi & Nakabo, 1997, was studied on a rocky coast in Shikoku, Japan, where the two species occur sympatrically. In the study area, individual males of each species established mating territories within which pair spawnings occurred. Pair spawnings were observed only between conspecifics, indicating that the two coexisting species were reproductively isolated. Both species usually spawned during the afternoon in early winter and had similar reproductive behavior. Although habitat, temporal and behavioral isolation mechanisms were not apparent, reproductive isolation seemed to occur via premating isolation through visual recognition of conspecific mates because the two species differed in body size and coloration. On one occasion a maleP. sieboldi was observed to perform streaking behavior to join a spawning pair ofP. eoethinus. Thus, postmating isolation between the two species is also discussed.     

An Artiodactyl Tracksite at Musandam Peninsula,Sultanate of Oman

Here we report an artiodactyl trackway from Musandam Peninsula, Sultanate of Oman. Epireliefs of the tracks are preserved in poorly consolidated aeolian deposits now making up the ceiling of a coastal cave. As an interesting morphological feature, the trackway documents the trackmaker negotiating a slippery dune slope at an angle.     

An initial assessment of mangrove resources and human activities at Mahout Island,Arabian Sea,Oman

This study was initiated to provide information on mangrove structure, communities, wildlife, socio-economics and human impacts on one of the most important areas of mangroves in Oman at Mahout Island, located on the Arabian Sea coast. The island is fringed with a luxuriant vegetation of mangroves formed by Avicennia marina (Forsk.) Vierh. Tree height, diameter at breast-height (dbh) and basal area (m²) show progressive increases from the upper to the lower level of the shore. Density (number of stems/0.1 ha) is variable, showing three peaks in transects across western and southern mangroves. The northern mangroves are the most developed, characterized by muddy substrate, followed by the western on a sandy bottom, and the southern surrounded by rock-flat. The mangroves support a large number of fishes, shrimps, crabs and molluscs. Wildlife are represented by shorebirds, waterfowls, turtles and dolphins.The Mahout population consists of bedouins, mostly supported by fishing. It is semi-settled with seasonal migration in summer to large towns. Fishing activities are usually between September and May. Shrimps and fish are the main natural resources. Human impacts were identified and qualitatively assessed: overutilization of mangroves by woodcutting or livestock grazing; litter and pollution; killing of turtle and other wildlife; removal of benthic marine organisms; the proposed construction of a fishery harbor; and the potential of mariculture and tourism. Management, based on sustainable development, should be undertaken to protect Mahout resources.     

Biology of the kingsoldier bream (Argyrops spinifer, Forsskål 1775; Sparidae), from the Arabian Sea, Oman

It is recognized by the FAO that management of fish resources in the western Indian Ocean is complicated by the lack of data on the basic biology and landing statistics for exploited fish species. In this paper data are presented on the population biology of kingsoldier bream, Argyrops spinifer (Forsskål 1775), in the Arabian Sea with a view to contributing towards the development of management plans for its sustainable exploitation. Samples were obtained from the Omani artisanal hand‐line fishery catch, January 2001–December 2002. Total length (L_T) of fish sampled ranged from 20 to 68 cm (males) and 25 to 70 cm (females). The male : female ratio was similar up to 55 cm L_T but the larger size‐classes were composed predominately of male fish. L_T/carcass weight (W_C) relations for male and female fish were similar and the combined data produced an equation W_C = 0.00005 × L_T^2.67. Marginal increment analysis indicated an annual cycle of opaque and translucent ring formation in otoliths that was related to the change in surface water temperature during the annual monsoon period. The opaque zone was completed in May and the translucent zone began to form in June. Female and male fish age ranged between 2 and 25 years. Both males and females exhibited similar asymptotic growth patterns; the combined von Bertalanffy growth function was L_t = 64.6(1 ? e^{[?0.142(t + 0.489)]}). Gonadosomatic indices and gonad condition of male and female fish indicated that the spawning season occurred between September and January. Size (L₅₀) and age at first maturity (A₅₀) were estimated to be 36.5 cm L_T and 5.0 years for males and 37.2 cm L_T and 5.6 years females, respectively. The results of this study provide fundamental information on the biology and population dynamics of A. spinifer in the Arabian Sea that can be used in management models for the continued sustainable exploitation of this species in the Omani demersal coastal fisheries.     

Fungi and aflatoxins associated with spices in the Sultanate of Oman

One hundred and five samples of seven spices (cumin, cinnamon, clove, black pepper, cardamom, ginger, and coriander) were purchased from five popular companies in the Sultanate of Oman. The spices were surveyed for the mycoflora and aflatoxins. Twenty fungal species were isolated in which Aspergillus flavus , A. niger . Penicillium , Rhizopus , and Syncephalastrum racemosum were the most dominant. When colony forming units per gm (cfu/gm) of fungi were compared, significant differences were found among spices and companies. Of the seven spices studied, clove was found to be the least contaminated, while cumin was the most contaminated. None of the 15 selected samples of the spices contaminated by A. flavus were found to contain aflatoxins. Nevertheless, nine isolates (45%) of the twenty A. flavus strains screened for aflatoxins were aflatoxigenic. The moisture content of most of the spices was below the maximum standard limit. The results showed that the spices were contaminated by some fungi that might constitute health hazards for humans. This revised version was published online in June 2006 with corrections to the Cover Date.     

New radiolarians from the earliest Cretaceous of the Sultanate of Oman (Wahrah Formation,Jebel Buwaydah)

In a section from the central Oman Mountains (Wahrah Formation, Jebel Buwaydah) well preserved radiolarians were extracted. Stratigraphically they represent typical earliest Cretaceous species (Bernasian). Besides well known Tethyan species allowing an exact age determination, unknown morphotypes are common in some samples. Some of these represent new species, which are described herein. The composition and diversity of the faunas hints to a depositional environment in the lower bathyal.     

Fishing pattern and management scenarios of Epinephelus gabriellae (Randall and Heemstra, 1991) fisheries in the Arabian Sea,Oman

Management of fish resources in the Western Indian Ocean is complicated due to the lack of data on the basic biology and landing statistics for exploited fish species. In this paper, a database including biological parameters, length frequency distributions and catches of Epinephelus gabriellae in Oman according to fleet components has been established to develop a management plan for its sustainable exploitation. Length cohort analyses and yield per recruit were examined by simulating changes in fishing effort in length at first capture and by introducing a seasonal ban for trawlers. The results showed a high sensitivity to the applied value of natural mortality (M). (i) With M = 0.40, a healthy status of the stock is observed; however, with M values of 0.20 and 0.15 the stock appears slightly overexploited, and actual F exceeds 10 and 30% of the F₀₁ level, respectively. (ii) A moderate increase of length at first capture would not significantly affect the long‐term yield or stock spawning biomass; however, a substantial length increase would in the long‐term lead to a decrease in yields for the artisanal fleet using traps. (iii) A seasonal ban regulation for trawlers would not have a significant effect on the sustainable yield, but if the fishing effort were to increase considerably, a significant long‐term gain in yield would be obtained with a closed season from April‐September.     

Miocene phosphorites from the Murray Ridge, northwestern Arabian Sea

Phosphorites from the Murray Ridge, NW Arabian Sea comprise nodules, bioclasts, and bone fragments. The nodules are made up of a homogeneous, light-colored phosphate nucleus consisting of Rivulariacean filamentous cyanobacteria and a thin dark-grey colored phosphate cortex showing abundant microbial filaments and microborings. The bioclasts comprise of  14–14.5 Ma old planktonic foraminifers, accepted as the time of deposition. Spherical to ovoid-shaped apatite microparticles resembling fossil bacteria are distinct components in the bioclasts. Bone fragments exhibit apatite fillings. The nodules and bone fragments consist entirely of carbonate fluorapatite (CFA) with low Al, K, and Th concentrations suggesting absence of continental detritus. Shale-normalized REE patterns of the samples support a seawater-derived composition. The highly uniform initial _Nd values of − 4.8 to − 5.1 are interpreted as the seawater value at the onset of phosphatization  14 Ma ago. In contrast, ⁸⁷Sr/⁸⁶Sr ratios show a large range of 0.709055 to 0.709124 corresponding to unusually young stratigraphic ages of  1 to 3 Ma. The data are interpreted as evidence for post-depositional Sr exchange of the recrystallizing phosphorites with fluids isotopically not much different from modern seawater. It is concluded that the phosphorites formed under oxic, shallow-water conditions where microbial populations assimilated phosphorus primarily from seawater and mediated precipitation of CFA during early diagenesis at the sediment–water interface on different substrates.     

Fungi associated with black tea and tea quality in the Sultanate of Oman

Forty-eight samples of four popular commercial brands of black tea ( Camellia sinensis L.) were purchased from the local markets in Muscat area, Sultanate of Oman. Tea leaves were surveyed for mycoflora. Five fungal species were isolated with A. niger as the most dominant in all the brands having percentage contamination ranging between 0.66% and 30.34%. Other fungi isolated were Aspergillus flavus, Penicillium spp. and Pacelomyces spp. but having average percentages of 0.6%, 0.84% and 0.21% respectively. Significant differences were found among the batches contaminated by A. niger. None of the 25 A. flavus strains screened for aflatoxins were found aflatoxigenic. The total ash, water-soluble ash, and mineral concentration of the samples were within the British standards and were not affected by fungal contamination. The results showed that black tea is contaminated by fungi that might constitute health hazards for humans. The post harvest contamination of tea could be eliminated or reduced if processing is conducted under more hygienic conditions. This revised version was published online in June 2006 with corrections to the Cover Date.     

Emericella omanensis,a new species from Oman soil

A new species ofEmericella isolated from forest soil in the Oman,E. omanensis, is described and illustrated. It differs from the other known species of the genus in having bivalvate ascospores with a tuberculate or verruculose convex wall. The new species is compared with the closely related speciesE. desertorum andE. echinulata.     

<Emphasis Type=Italic>Trichodesma dhofaricum</Emphasis> (Boraginaceae), a new species from the Sultanate of Oman

A new species of Trichodesma (Boraginaceae) is described from the southern region of Oman.     

Increased Markers of Oxidative Stress in Autistic Children of the Sultanate of Oman

Autism spectrum disorder (ASD) is a neurodevelopmental disorder of early childhood, and an enumeration about its etiology and consequences is still limited. Oxidative stress-induced mechanisms are believed to be the major cause for ASD. In this study 19 autistic and 19 age-matched normal Omani children were recruited to analyze their degree of redox status and a prewritten consent was obtained. Blood was withdrawn from subjects in heparin-coated tube, and plasma was separated. Plasma oxidative stress indicators such as nitric oxide (NO), malondialdehyde (MDA), protein carbonyl, and lactate to pyruvate ratio were quantified using commercially available kits. A significant elevation was observed in the levels of NO, MDA, protein carbonyl, and lactate to pyruvate ratio in the plasma of Omani autistic children as compared to their age-matched controls. These oxidative stress markers are strongly associated with major cellular injury and manifest severe mitochondrial dysfunction in autistic pathology. Our results also suggest that oxidative stress might be involved in the pathogenesis of ASD, and these parameters could be considered as diagnostic markers to ensure the prevalence of ASD in Omani children. However, the oxidative stress-induced molecular mechanisms in ASD should be studied in detail.     

High rates of denitrification and nitrous oxide emission in arid biological soil crusts from the Sultanate of Oman

Using a combination of process rate determination, microsensor profiling and molecular techniques, we demonstrated that denitrification, and not anaerobic ammonium oxidation (anammox), is the major nitrogen loss process in biological soil crusts from Oman. Potential denitrification rates were 584±101 and 58±20 μmol N m⁻² h⁻¹ for cyanobacterial and lichen crust, respectively. Complete denitrification to N₂ was further confirmed by an ¹⁵NO₃⁻ tracer experiment with intact crust pieces that proceeded at rates of 103±19 and 27±8 μmol N m⁻² h⁻¹ for cyanobacterial and lichen crust, respectively. Strikingly, N₂O gas was emitted at very high potential rates of 387±143 and 31±6 μmol N m⁻² h⁻¹ from the cyanobacterial and lichen crust, respectively, with N₂O accounting for 53–66% of the total emission of nitrogenous gases. Microsensor measurements revealed that N₂O was produced in the anoxic layer and thus apparently originated from incomplete denitrification. Using quantitative PCR, denitrification genes were detected in both the crusts and were expressed either in comparable (nirS) or slightly higher (narG) numbers in the cyanobacterial crusts. Although 99% of the nirS sequences in the cyanobacterial crust were affiliated to an uncultured denitrifying bacterium, 94% of these sequences were most closely affiliated to Paracoccus denitrificans in the lichen crust. Sequences of nosZ gene formed a distinct cluster that did not branch with known denitrifying bacteria. Our results demonstrate that nitrogen loss via denitrification is a dominant process in crusts from Oman, which leads to N₂O gas emission and potentially reduces desert soil fertility.