Distribution of external parasites indicates boundaries to dispersal of sillaginid fishes in the Indo-West Pacific

1997 ◽  
Vol 48 (5) ◽  
pp. 391 ◽  
Author(s):  
Craig J. Hayward

The distribution of sillaginid-specific ectoparasites permits the distinction of two provinces with high parasite diversity: one on the continental shelf of Australia, and one on the shelf of Asia. The Australian province has 15 endemics (five monogeneans, one leech and nine copepods), and the Asian province has 14 endemics (two monogeneans and 12 copepods). These provinces are separated by a region with coastlines that descend very steeply to the ocean floor and by deep ocean waters that largely inhibit sillaginid movements. Some sillaginids must have dispersed across eastern Indonesia, however, leading to the occurrence of four parasites in both provinces. Three Australian parasites also appear to be presently encroaching onto the southern periphery of the Asian shelf. At least one less-recent invasion of Australian waters by Asian sillaginids would account for the occurrence of six pairs of copepod congeners that have one member in each province. The most widespread sillaginid, Sillago sihama, seems to have dispersed to African shores from the Arabian Sea as planktonic larvae only (no Asian parasites were present in samples of 29 hosts) and relatively recently (only one locally endemic parasite appears to have been acquired).

1971 ◽  
Vol 11 (1) ◽  
pp. 27
Author(s):  
J. B. R. Livermore

For countless centuries the activities of man were bounded, in the main, by the limits of the dry land on which he lived. Some of the more intrepid ventured out upon the seas and oceans — to fish, to explore, to trade, or to fight. In the twentieth century man has conquered the air and circled the globe in space.Now the world looks to another new frontier — the field of exploration of the seabed beneath the oceans. In recent decades there has been an awakening to the existence of natural resources in the seabed and ocean floor.Tliis prospect of discoiering, and more importantly producing, minerals from the deep ocean floor, appears to offer the potential of expanding the resource base of modern civilisation at a time when a growing world population, coupled with rising standards of living, are throwing increased demands on the world's known stock of natural resources.For three years the United Nations, following an initiative by the island state of Malta, has been discussing the reservation, exclusively for peaceful purposes, of the seabed and ocean floor beyond the limits of national jurisdiction, and the use of the resources of this area, in the interests of mankind as a whole.During these discussions diverse points of view have emerged: some would restrict the jurisdiction of a coastal state severely; others argue for extensive coastal state jurisdiction. Some want elaborate and comprehensive international machinery to control all activities on the seabed in accordance with a regime agreed internationally; others support more modest arrangements arguing that elaborate machinery would swallow up the financial benefits and leave little or nothing for the world community; still others contend that the regime and machinery should, initially at least, be resource oriented.The Australian delegation has put the view that any international arrangements for the deep seabed must be effective, credible and impartial. Such arrangements must not only command the support of the nations of the world regardless of geographical location or political system, they must also instil confidence in the minds of operators that rights granted can, and will, be upheld.Moves are developing for a further comprehensive law of the sea conference — perhaps within two or three years - which will tackle several outstanding matters including, importantly, that of a suitable regime and administrative machinery for the seabed and ocean floor beyond national jurisdiction. Inevitably this will involve consideration of the imprecision of the limits of the continental shelf as presently defined by the Geneva Convention of 1958. Other subjects requiring attention are the breadth of the territorial sea, rights of passage through straits and fisheries matters.Australia, an island continent with a long coastline and an extensive continental shelf, has a vital interest in the course of these deliberations.


2015 ◽  
Vol 106 ◽  
pp. 70-84 ◽  
Author(s):  
Shiba Shankar Acharya ◽  
Mruganka K. Panigrahi ◽  
Anil K. Gupta ◽  
Subhasish Tripathy

2010 ◽  
Vol 7 (1) ◽  
pp. 177-205
Author(s):  
K. Fennel

Abstract. Continental shelves play a key role in the cycling of nitrogen and carbon. Here the physical transport and biogeochemical transformation processes affecting the fluxes into and out of continental shelf systems are reviewed, and their role in the global cycling of both elements is discussed. Uncertainties in observation-based estimates of nitrogen and carbon fluxes mostly result from uncertainties in the shelf-open ocean exchange of organic and inorganic matter, which is hard to quantify based on observations alone, but can be inferred from biogeochemical models. Model-based nitrogen and carbon budgets are presented for the Northwestern North Atlantic continental shelf. Results indicate that shelves are an important sink for fixed nitrogen and a source of alkalinity, but are not much more efficient in exporting organic carbon to the deep ocean than the adjacent open ocean for the shelf region considered.


1971 ◽  
Vol 8 (02) ◽  
pp. 145-158
Author(s):  
Raymond Kaufman

The paper discusses the latest techniques proposed for mining minerals from the deep ocean. Deep ocean is defined as the sea beyond the continental shelf, particularly areas of the sea floor exceeding 1200 ft in depth. The three principal deep-ocean minerals having economic potential in the immediate future are identified. Four recently proposed advanced deep-ocean mining concepts are presented. Use of the air-lift pump as a viable mining method is discussed and a large-scale air-lift pump experiment conducted in an abandoned mine shaft at Galax, Virginia is described. The principal features of the conversion of a small C1-M-AV1 type cargo ship to a deep-ocean mining prototype vessel, RV Deepsea Miner, is outlined.


Author(s):  
Steinar Løve Ellefmo ◽  
Thomas Kuhn

AbstractMinerals and metals are of uttermost importance in our society, and mineral resources on and beneath the deep ocean floor represent a huge potential. Deciding whether mining from the deep ocean floor is financially, environmentally and technologically feasible requires information. Due to great depths and harsh conditions, this information is expensive and time and resource consuming to obtain. It is therefore important to use every piece of data in an optimum way. In this study, data retrieved from images and expert knowledge were used to estimate minimum and maximum nodule abundances at image locations from an area in the Clarion-Clipperton-Zone of the equatorial North East Pacific. From the minimum and maximum values, box cores and the spatial correlation quantified through variogram, a conditional expectation and associated uncertainty were obtained through the Gibbs sampler. The conditional expectation and the uncertainty were used with the assumed certain abundance data from the box cores in a kriging exercise to obtain better informed estimates of the block by block abundance. The quality assessment of the estimations was done based on distance criterion and on kriging quality indicators like the slope of regression and the weight of the mean. From the original image locations, alternative image configurations were tested, and it was shown that such alternatives produce better estimates, without extra costs. Future improvements will focus on improving the estimation of the minimum and the maximum values at image locations.


2004 ◽  
Vol 89 (516) ◽  
pp. 437-440 ◽  
Author(s):  
Maurice N. Brearley

A tsunami usually starts on deep ocean water as a result of a submarine earthquake. A tsunami wave is very long, even as much as tens of kilometres, but of only very small amplitude, typically less than half a metre (Bascom [1]). In mid-ocean, the passage of a tsunami is imperceptible, but on reaching a shore it can achieve great heights and can deliver massive surges of water. Before the arrival of the first surge, and between subsequent surges, the water at a shore line usually retracts for a long distance, leaving bare large areas of ocean floor that are normally under water. This paper analyses the behaviour of a tsunami, and explains how its mid-ocean character is transformed to produce such massive surges of water at a shore line.


Ocean Science ◽  
2010 ◽  
Vol 6 (2) ◽  
pp. 539-548 ◽  
Author(s):  
K. Fennel

Abstract. Continental shelves play a key role in the cycling of nitrogen and carbon. Here the physical transport and biogeochemical transformation processes affecting the fluxes into and out of continental shelf systems are reviewed, and their role in the global cycling of both elements is discussed. Uncertainties in the magnitude of organic and inorganic matter exchange between shelves and the open ocean is a major source of uncertainty in observation-based estimates of nitrogen and carbon fluxes. The shelf-open ocean exchange is hard to quantify based on observations alone, but can be inferred from biogeochemical models. Model-based nitrogen and carbon budgets are presented for the Northwestern North Atlantic continental shelf. Results indicate that shelves are an important sink for fixed nitrogen and a source of alkalinity, but are not much more efficient in exporting organic carbon to the deep ocean than the adjacent open ocean for the shelf region considered.


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