Allozyme and mitochondrial DNA analysis of the tropical saddle-tail sea perch, Lutjanus malabaricus (Schneider), from Australian waters

1996 ◽  
Vol 47 (7) ◽  
pp. 869 ◽  
Author(s):  
NG Elliott

Samples of Lutjanus malabaricus from four localities were examined for genetic variability at 10 polymorphic allozyme loci and, after restriction fragment analysis with five enzymes detecting polymorphic cut sites, in mitochondrial DNA (mtDNA). Twenty composite mtDNA haplotypes were found, with three common haplotypes occurring in 84% of individuals examined. Significant differentiation in haplotype frequencies between individuals sampled from the east coast of Queensland and those from the Gulf of Carpentaria and the North West Shelf suggests little, if any, movement of genes through the Torres Strait since its opening about 8000 years ago. Allozyme allele frequencies differed at one locus (PGM-1*) between samples from the North West Shelf and those from the Gulf of Carpentaria. These results are consistent with a recolonization, after the last ice age, of the more northern waters of Australia from a stock off the west coast. The observation of more nuclear than mitochondrial DNA differentiation may be partly a consequence of a female bias in sex ratios. The suggested presence of multiple stocks (North West Shelf, Gulf of Carpentaria, east coast of Queensland) of L. malabaricus, a dominant component of the northern Australian finfish fishery, should be considered in future management plans.


2017 ◽  
Vol 57 (2) ◽  
pp. 363
Author(s):  
Frankie Cullen

In 2016, sustained depressed and volatile oil prices led companies to continue cost reduction strategies. Proposed developments have seen delays and reductions in scope as a result. Australian oil production declined by around 10%. However, new and continued liquefied natural gas (LNG) production bolstered both Australian and global gas supply. Australia was the strongest contributor to global LNG growth in 2016, showing the biggest year-on-year increase. In the first half of 2016, 20% of global LNG came from Australia, second only to Qatar with 29% of the market share. Australia remains on track to become the world’s largest LNG producer in the next 3–5 years. 2016 saw the start-up of Gorgon LNG in March, the first of Chevron’s two North West Shelf LNG projects and the third of several producing, developing and proposed LNG projects within the North Carnarvon Basin – already Australia’s most prolific producing basin. On the east coast, development of the coalbed methane (CBM) to LNG projects continued with an additional train brought onstream at each of the Origin/ConocoPhillips-operated APLNG Project and Santos’ GLNG Project. This further increased production in the Bowen–Surat Basins and drove discussions around the ability of east coast gas to meet both the demands of the LNG projects and ensure continued domestic gas reliability. Additional gas may be required for both, opening opportunities for production from other basins. Gas production continues to drive the Australian industry, with substantial inputs from LNG and unconventional operations. The next phase, in all sectors, will be key to Australia’s future in the global energy market. Will it be able to overcome the expected challenges of global oversupply, continued price volatility and domestic reliability concerns to fulfil its potential?



1960 ◽  
Vol 67 (4) ◽  
pp. 351-362 ◽  
Author(s):  
A. D. McIntyre

SynopsisFrom a faunistic survey in Scottish waters, concentrated mainly in the sea lochs of the north-west coast and in the deep water in the North Sea off the east coast, thirty-two species of polychætes are listed which have not previously been recorded from these areas. Seven of the species are new records for British coastal waters or for the North Sea.



2021 ◽  
pp. jgs2020-106
Author(s):  
L. Manifold ◽  
P. del Strother ◽  
D.P. Gold ◽  
P. Burgess ◽  
C. Hollis

The Mississippian Derbyshire and North Wales carbonate platforms were formed in similar tectonic settings within the Pennine and East Irish Sea Basin, respectively. The Derbyshire Platform was surrounded by sub-basins to the north, west, and south whilst the North Wales Platform, 130 km west, had a simpler land-attached geometry. Comparison of these age-equivalent platforms allows the controls on sedimentation, at an important juncture in Earth history, to be evaluated. Both platforms are dominated by moderate-to-high-energy, laterally discontinuous facies, with weak evidence for facies cyclicity, suggesting multiple controls on deposition. Influx of siliciclastic mud on the North Wales Platform led to perturbations in carbonate accumulation; along with abundant palaeosols and coal beds this implies a more humid climate, or shallower water depths compared to the Derbyshire Platform. On both platforms, exposure surfaces can rarely be correlated over >500 metres except for a regionally correlative palaeokarstic surface at the Asbian-Brigantian boundary. This exposure event appears to coincide with a significant regional facies change. Given the lack of evidence for ordering and cyclicity within the strata, the Asbian-Brigantian boundary may mark a significant event that could reflect onset of a transitional climate, prior to the second glaciation event in the Late Palaeozoic Ice Age.



1980 ◽  
Vol 100 ◽  
pp. 83-86
Author(s):  
A. B Armour-Brown ◽  
T Tukiainen ◽  
B Wallin

The SYDURAN project completed the airborne gamma-spectrometer and geochemical sampling survey over some 14 000 km2 of south-west Greenland from the fjord Sermiligarssuk in the north-west to Kap Farvel in the south and up the east coast as far as the southern shore of Lindenows Fjord. This covered all the Ketilidian structural zones and a small area of Archaean as classified by Allaart (1976) (fig. 29). Geological field work and prospecting of a more detailed nature was carried out in five areas where previous work indicated possibie uranium mineralisation.



Britannia ◽  
2019 ◽  
Vol 50 ◽  
pp. 203-224 ◽  
Author(s):  
Trudi Buck ◽  
Elizabeth M. Greene ◽  
Alexander Meyer ◽  
Victoria Barlow ◽  
Eleanor Graham

ABSTRACTDisarticulated human remains were recovered from a first-century fort ditch at Vindolanda on the north-west frontier of the Roman Empire. Ancient DNA analysis revealed the skeleton to be that of a male individual and forensic taphonomic analysis suggested a primary deposition of the body in a waterlogged environment with no obvious evidence of formal burial. Occurrences of disarticulated human remains outside a cemetery context are often overlooked in Roman bioarchaeology. This discovery adds to the growing body of literature regarding alternative funerary practice in the Empire, highlighting that the concept of burial and disposal of the dead is more complex than ancient historical sources suggest. Details of the DNA analysis are provided in the Supplementary Material available at https://doi.org/10.1017/S0068113X1900014X.



Author(s):  
D. J. Crisp

Material collected prior to 1940 indicates that Elminius modestus was not present on British coasts at that time.Elminius increased in abundance in south-east England from 1946 to 1950 and extended its range as far as the Humber, where it halted.Its advance westwards along the south coast was similarly halted at Portland, but by 1948 independent colonies had been established in several of the river systems of Devon and Cornwall, in Milford Haven, and in the Bristol Channel.The first populations in the Irish Sea were in Morecambe Bay. From there Elminius spread rapidly south and west along the north coast of Wales, and more slowly north and west towards Galloway, eventually bridging the sea to the Isle of Man.Detailed observations showed that Elminius advanced along the uniformly favourable north coast of Wales as a definite front moving at a rate of approximately 20–30 km per year. Around Anglesey where tidal currents were stronger it appeared simultaneously in many scattered centres.A distinction is drawn between marginal dispersal taking place under the influence of normal agencies at the boundary of an existing population, and remote dispersal due to an artificial or freak transport over a long distance. In the case of Elminius the maximum distance that is likely to be bridged by marginal dispersal in the absence of strong residual drifts is about 30 miles.Elminius probably first appeared near Southampton, and was introduced into the Thames estuary area probably by remote dispersal. Thence it spread along the east coast and was transported to Holland. Its extension into south Devon, the Bristol Channel, the Irish Sea, and to the French coast must also be attributed to remote dispersal.The main ecological effects of Elminius result from competition for space with Balanus balanoides. Since Elminius breeds in summer, its dominance has a profound effect on the composition of the summer plankton, greatly increasing the number of barnacle nauplii, presumably at the expense of other larvae.



Radiocarbon ◽  
2007 ◽  
Vol 49 (2) ◽  
pp. 625-637 ◽  
Author(s):  
Danuta Michalska Nawrocka ◽  
Danuta Joanna Michczyńska ◽  
Anna Pazdur ◽  
Justyna Czernik

Carbonate binders from mortars and plasters as well as charcoal fragments sampled at the ancient settlement of Hippos (Sussita) have been subjected to radiocarbon dating by gas proportional counting (GPC) and accelerator mass spectrometry (AMS). Hippos is situated on the east coast of the Sea of Galilee (32°46′N, 35°39′E) at the top of a hill in the Golan Heights area, Israel. According to historical-archaeological data, the town had functioned since the 3rd century BC until AD 749, when it eventually crumbled into ruins after an earthquake. The appropriate sample selection and preparation based on the results of petrographic observations permitted us to distinguish different phases involved in the expansion of the settlement. More than 200 samples were taken from the settlement and subjected to petrographic and chemical analyses. Of the 200 total samples, about 20 were selected for dating. Here, we present the first 10 results of 14C dating carried out for Hippos. The oldest sample dated thus far gave an age corresponding with the 2nd century BC to 1st century AD—probably indicating an old Roman temple, on the base of which the North-West church (NWC) was later erected. The next dates extend up to the 8th century AD, the age related to the last phase of settlement inhabitation. Research is continuing as new excavations take place.



1995 ◽  
Vol 46 (6) ◽  
pp. 921 ◽  
Author(s):  
RD Ward ◽  
NG Elliott ◽  
PM Grewe

Northern and southern bluefin tunas are morphologically similar and can be misidentified, posing problems for fishery management and marketing. Allozyme variation and restriction-site variation in mitochondrial DNA (mtDNA) were used to distinguish between the two species. A survey of 36 allozyme loci active in white muscle and liver tissue showed that the genetic identity between the species was high (Nei's I = 0.907). One diagnostic locus (sAH*) and two nearly diagnostic loci (ADA* and GDA*) were found, and four loci showed highly significant allele frequency differences (FH*, GPI-A*, PGDH* and sSOD*). A survey of the mtDNA genome, using 15 restriction enzymes and southern blotting, revealed five restriction enzymes that gave species-diagnostic restriction digest profiles (Ban I, Bcl I, Dra I, Pvu II, Xba I) and a further three enzymes (Pst I, Barn HI and Nco I) with large haplotype frequency differences. Mitochondrial DNA analysis provided more reliable discrimination of specimens than did allozyme analysis, although the more rapid allozyme identification will be accurate for most specimens. The two biochemical genetic methods were then used to identify Australian-caught fish of uncertain identity. Six of 12 tuna originally considered to be northern bluefin tuna were confirmed as northern bluefin and six were identified as southern bluefin. The presence of northern bluefin tuna as far south as south-western Tasmania was confirmed.



1971 ◽  
Vol 35 ◽  
pp. 11-13
Author(s):  
N Hald

Hareøen is an island north-west of Disko in western Greenland. It has the form of a plateau, whose highest point - 512 metres - is found near the south coast. Like the neighbouring parts of Nugssuaq and Disko, Hareøen consists chiefly of Tertiary basaltic lavas. The island first attracted attention on account of the presence of interbasaltic, coal-bearing sediments on the north-east coast. These were already examined by Giesecke in 1811 (Giesecke, 1910) and later among others by Steenstrup (1874) and B.E. Koch (1959). A petrographie investigation of the basalts was first undertaken by Holmes (1919), who described loose fragments rich in K2O. Lavas from the south coast, colleeted and analysed by Pedersen (1970), also have a high content of potash. V. Miinther in the years 1948-49 untertook geological mapping of the island, on which the present investigation is supported (Miinther, in press).



1991 ◽  
Vol 31 (1) ◽  
pp. 423
Author(s):  
Ian LeProvost

Environmentally safe management of hydrocarbon exploration and production activities is becoming increasingly important, particularly in sensitive marine areas. LeProvost Environmental Consultants have been working closely with Hadson Energy Limited, Western Mining Corporation Ltd and West Australian Petroleum Pty Ltd to produce environmental impact assessments, environmental management plans and monitoring programs for oilfields recently developed on the North West Shelf. Many of the well sites are located in areas with sensitive ecological habitats, including coral reefs, seagrass beds, mangroves and prawn spawning and fishing grounds. Consequently, operators in these areas have been required to produce comprehensive Environmental Management Plans and Oil Spill Contingency Plans, to gain development and operating approvals from the Western Australian Government.Formulation of these plans begins with baseline surveys of the biological, physical and social characteristics of the study area. Hydrodynamic modelling of the metocean conditions produces oil spill prediction envelopes to highlight the areas that may potentially be affected by an oil spill, if one should occur. Site-specific oil spill response procedures are then designed to cater for the sensitive marine habitats of the area, using the resources that are available in the region to deal with an oil spill.Results to date from the Marine Biological Monitoring Programs for three oilfields have supported predictions that no significant adverse impacts on the environment would result from the development and operation of the oilfields.



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