A record of the trematode and cestode parasites of fishes from the Porcupine Bank, Irish Atlantic Slope and Irish Sea

Parasitology ◽  
1941 ◽  
Vol 33 (4) ◽  
pp. 390-396 ◽  
Author(s):  
Gwendolen Rees ◽  
Jack Llewellyn
Keyword(s):  
Coastal Waters ◽  
Deep Sea ◽  
Irish Sea ◽  
The West ◽  
The Past ◽  
Fresh Material ◽  
Junior Author ◽  
The Subject ◽  
The Irish Sea ◽  
West Of Ireland

The trematode and cestode parasites of fishes inhabiting British coastal waters have been the subject of several studies in the past, but the parasites of deep-sea fishes have received comparatively little attention due probably to the difficulty of obtaining fresh material. In order that such material might be obtained, excursions were made by the junior author in a commercial trawler to some of the deep-sea fishing grounds lying to the west of Ireland, namely, the Irish Atlantic Slope and the Porcupine Bank. Two excursions were made, the first in August 1938 and the second in July 1939, each extending over a period of about 12 days. In addition, a study has been made of the parasites of some fishes from the Irish Sea from 1936 to 1939. The results of both surveys are incorporated in this paper, and the areas investigated are indicated in Table 1.

A record of the nematode parasites of fishes from the Porcupine bank, Irish Atlantic Slope and Irish Sea

Parasitology ◽  
1946 ◽  
Vol 37 (1-2) ◽  
pp. 38-41 ◽  
Author(s):  
Gwendolen Rees
Keyword(s):  
Deep Sea ◽  
Irish Sea ◽  
The West ◽  
Nematode Parasites ◽  
The Irish Sea ◽  
West Of Ireland

The nematodes recorded in the present paper were obtained from fishes caught on some of the deep-sea fishing grounds to the west of Ireland, namely, the Porcupine Bank and Irish Atlantic Slope, and from the Irish Sea. The writer is indebted to Mr S. J. Hughes and Mr J. Llewellyn for the collection of material from the deep-sea fishing grounds, excursions having been made for the purpose in a commercial trawler in August 1938 and July 1939. The majority of the nematodes were collected by Mr S. J. Hughes during the 1939 excursion, the first excursion being devoted mainly to the collection of trematodes and cestodes. A record of the trematode and cestode parasites obtained during both years has already been published (Rees & Llewellyn, 1941). Nematodes from fishes in the Irish Sea have been obtained at intervals from 1936 onwards.

scholarly journals IV.—On the Drifts of the West and South Borders of the Lake District, and on the Three Great Granitic Dispersions

1871 ◽  
Vol 8 (85) ◽  
pp. 303-312 ◽  
Author(s):  
D. Mackintosh
Keyword(s):  
Small Area ◽  
Irish Sea ◽  
Lake District ◽  
The West ◽  
Boulder Clay ◽  
The Irish Sea ◽  
Sea Cliff

Boulder-scars.—From Maryport to Parkgate, the E. coast of the Irish Sea at intervals exhibits accumulations or concentrations of large boulders, which are locally called scars. They may be seen in all stages of formation, from the denudational area, where they are in course of being left by the washing away of the clayey matrix, to the depositional area, where they have become half-covered with recent sand and shingle. In many places (as between Seascale and near Silecroft) there are so many boulders within a small area as to show that a considerable thickness of the clay must have been removed. With the exception of having tumbled down as the cliffs were undermined and worn back by the sea, many of the boulders may still rest nearly in the positions they occupied in the clay, but (as is evidenced on the coast at Parkgate) others, up to a great diameter, may have been shifted horizontally. Some of the scars exist where the Boulder-clay would appear to have risen up into ridges or mounds, as no clay is now found opposite to them at the base of the sea-cliff. Others are clay and boulder plateaux, visibly connected with the cliff-line. Most of the scars, I believe, are remnants of the great Lower Brown Boulder-clay. The most conspicuous boulder in the scars S.W. of Bootle, is Eskdale-fell granite, accompanied by a little Criffell granite, and a great number of the usual felspathic erratics.

From midden to megalith? The Mesolithic-Neolithic transition in western Britain

2007 ◽  
Author(s):  
Vicki Cummings
Keyword(s):  
Transition Process ◽  
The Other ◽  
Irish Sea ◽  
Technological Transformation ◽  
Neolithic Transition ◽  
Isle Of Man ◽  
The Past ◽  
Hunting And Gathering ◽  
The Irish Sea

The transition from the Mesolithic to the Neolithic in Britain and Ireland remains one of the most debated and contested transitions of prehistory. Much more complex than a simple transition from hunting and gathering to farming, the Mesolithic–Neolithic transition in Britain has been discussed not only as an economic and technological transformation, but also as an ideological one. In western Britain in particular, with its wealth of Neolithic monuments, considerable emphasis has been placed on the role of monumentality in the transition process. Over the past decade the author‧s research has concentrated on the early Neolithic monumental traditions of western Britain, a deliberate focus on areas outside the more ‘luminous’ centres of Wessex, the Cotswold–Severn region, and Orkney. This chapter discusses the transition in western Britain, with an emphasis on the monuments of this region. In particular, it discusses the areas around the Irish Sea – west Wales, the Isle of Man, south-west and western Scotland – as well as referring to the sequence on the other side of the Irish Sea, specifically eastern Ireland.

XI.—The Glaciation of Holyhead Mountain

1904 ◽  
Vol 1 (10) ◽  
pp. 504-505
Author(s):  
Edward Greenly
Keyword(s):  
Irish Sea ◽  
General Level ◽  
The South ◽  
The West ◽  
Scottish Highlands ◽  
The North ◽  
The Irish Sea ◽  
North And South ◽  
Sea Cliffs

The bare and rocky hill known as Holyhead Mountain is of considerable interest in connection with recent geological events, standing as it does some thirty miles out from the highlands of Carnarvonshire into the Irish Sea Basin; and in such remarkable isolation, for it is much the highest of the five hills which rise above the general level of the platform of Anglesey.Its height is only 721 feet, but so strongly featured is it, especially towards the west, that one feels the term ‘mountain’ to be no misnomer, and can hardly believe it to be really lower than many of our smooth wolds and downs of Oolite and Chalk. Being composed, moreover, of white quartzite (or more properly of quartzite-schist), and being so bare of vegetation, it recalls much more vividly certain types of scenery in the Scottish Highlands than anything in those Welsh mountains that one sees from its sides. Towards the east it slopes at a moderate angle, but a little west of the summit it is traversed by a very strong feature, due to a fault, running nearly north and south, along which is a line of great crags, facing west, and prolonged northwards into the still greater sea cliffs towards the North Stack. Beyond this the land still remains high, but is smoother in outline, a somewhat softer series of rocks extending from the fault to the South Stack, where the high moors end off in great cliffs above the sea.

Population dispersal in the brittle-star Ophiocomina nigra (Abildgaard) (Echinodermata: Ophiuroidea)

1977 ◽  
Vol 57 (2) ◽  
pp. 405-439 ◽  
Author(s):  
J. B. Wilson ◽  
N. A. Holme ◽  
R. L. Barrett
Keyword(s):  
West Coast ◽  
Personal Communication ◽  
Irish Sea ◽  
English Channel ◽  
The West ◽  
The North ◽  
Sea Bed ◽  
Cook Strait ◽  
The North Sea ◽  
The Irish Sea

A number of species of ophiuroid are known to occur in dense clusters on the sea-bed. Aggregations of Ophiothrix fragilis (Abildgaard) have been recorded from the English Channel by Allen (1899), Vevers (1951, 1952), Barnes (1955), Ancellin (1957), Cabioch (1961, 1967, 1968), Holme (1966), Warner (1969, 1971), and by Allain (1974). Beds of the same species have been found in the Irish Sea by Jones (1951) and by Brun (1969), on the west coast of Ireland by Könnecker & Keegan (1973) and Keegan (1974), and on the west coast of Scotland, where it is widespread in sea lochs and elsewhere around the coast (McIntyre, 1956, and personal communication, 1975). Records of Ophiothrix fragilis from the North Sea have been summarized by Ursin (1960). In the Mediterranean, aggregations of Ophiothrix quinquemaculata (D.Ch.) have been described by Guille (1964, 1965) from off the south coast of France, and by Czihak (1959) from the Adriatic. Hurley (1959) gives underwater photographs of Ophiocomina bollonsi Farquhar from the Cook Strait, New Zealand. Further examples of aggregation in ophiuroids and other echinoderms are cited by Reese (1966), Mileykovskiy (1967) and by Warner (1978).

scholarly journals Certain Effects of Glacial Events in the Vale of Glamorgan, South Wales

1966 ◽  
Vol 6 (44) ◽  
pp. 261-266
Author(s):  
C. B. Crampton
Keyword(s):  
Mediterranean Climate ◽  
Irish Sea ◽  
The West ◽  
South Wales ◽  
Melt Water ◽  
The Irish Sea ◽  
Two Phases ◽  
Carboniferous Limestone

AbstractIn South Wales there is evidence for two phases of intense glaciation and an interglacial phase during the Pleistocene. During the closing stages of the earlier glaciation in the west of the Vale of Glamorgan two overflow channels were cut by melt water from an ice lobe off the Glamorgan upland, abutting against ice from the Irish Sea. During retreat, ice from the Irish Sea and local ice deposited material on the Lower Lias outcrop on which two contrasting soils developed. Soils normally associated with a Mediterranean climate developed locally on the outcrop of the Carboniferous Limestone during the interglacial phase.

scholarly journals VI.—On the Millstone Grit of the North Wales Border

1870 ◽  
Vol 7 (68) ◽  
pp. 68-73
Author(s):  
D. C. Davies
Keyword(s):  
Irish Sea ◽  
Eastern Slope ◽  
Natural Boundary ◽  
The West ◽  
The North ◽  
The People ◽  
North Wales ◽  
Great Western Railway ◽  
The Irish Sea ◽  
Carboniferous Limestone

The Millstone Grit of the North Wales Border follows the eastern slope of the Carboniferous Limestone, from Crickheath and Sweeney, South of Oswestry, to the shores of the Irish Sea; it is also thrown up into the range of hills which the traveller by the Great Western Railway may see to the west of the line between Oswestry and Chester. This range serves as a natural boundary between this part of England and Wales, and forms a second line of natural fortification, strengthened on the English side by numerous outposts of low hills of clay, gravel, and sand, which give place, upon the Welsh side, to precipitous escarpments of Mountain Limestone, beyond which the change in the language, dress, and manners of the people is marked and sudden.

scholarly journals Persophilia

2016 ◽  
Vol 33 (3) ◽  
pp. 119-123
Author(s):  
Negar Davari
Keyword(s):  
Eighteenth Century ◽  
Public Space ◽  
World History ◽  
National Level ◽  
Space Theory ◽  
The West ◽  
The Past ◽  
The Subject ◽  
And Shifts

Academic investigation of the mutual influences of the West and the Easthas been the subject of few studies during the past decades. In this category,Hamid Dabashi’s work on the mutual effects of the Persianate Orient and theWest is impressive. The book traces evidences of the West’s Persophiliathroughout world history from Biblical and ancient texts to contemporarytexts under the influence of the Romanticism, Transcendentalism, mysticism,fascism, and pan-Islamism approaches. It provides thoughtful commentaryon the roots of western Persophilia, its outcome for the West and the Persianaiteworld, and the overall picture of Persophilic knowledge productionand transfer.As such, Dabashi’s work contributes to the socio-historical hermeneuticsof Persian and western culture by mapping their inter-related texts. He considersPersophilia a sub-category of Orientalism, through which he challengescolonial-based Orientalism. By relying on Jürgen Habermas’ theory of bourgeoispublic space, Dabashi criticizes Raymond Schwab and Edward Said’sviews as introducing a one-directional influence of the West upon the East. Hiswork suggests that there is a cyclic relation of influences between them. Tofurther this point, Dabashi expands Habermas’ public space theory beyond“bourgeois” and shifts it from a limited national level into a transnational scenethat emphasizes the role of Persophilia in the circulation and production ofknowledge worldwide. The book deems the emergence of Persophilia duringthe eighteenth century and its continuation to the present time as an influential ...

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