scholarly journals Exploring the clumped and bulk isotopic systematic of carbonates near two deep-water cold seeps offshore Nova Scotia, Canada

2021 ◽  
Author(s):  
Josué Jautzy ◽  
Martine Savard ◽  
Calvin Campbell ◽  
Adam MacDonald
1958 ◽  
Vol 15 (6) ◽  
pp. 1269-1311 ◽  
Author(s):  
F. D. McCracken

Exploratory fishing in the northern Gulf of St. Lawrence in 1945 and 1946 and off western Nova Scotia in 1947 caught 739 halibut, of which 229 were tagged and released. About 590 fish from the commercial fishery of the two regions were also examined.Larger, older halibut were caught in the northern part of the Gulf of St. Lawrence than off western Nova Scotia. Tagged halibut recaptures, size and age composition of commercial landings, and differences in rate of growth suggest generally separate stocks in the two regions.Younger, immature halibut were most available in shallower water; larger, mature fish usually in deep water. Most halibut were caught at temperatures between about 3° and 9 °C. Seasonal, inshore, relatively shallow water halibut fisheries in the northern part of the Gulf of St. Lawrence and off western Nova Scotia occur as the bottom water warms. Large female halibut predominate in such catches.Mature halibut, about 9 to 11 years and older, must spawn in late winter and early spring, probably along the deep-water edge of the banks. Mature halibut grow slowly though the females exceed the mature males and reach a much larger size. The faster-growing, immature halibut of both sexes grow at about the same rate.Halibut landings from ICNAF Subareas 3 and 4 which were at a low level between 1940 to 1948 increased sharply to about 13 million pounds in 1950. More recent landings approximate the long-term annual average of about 5 million pounds. Changes in the level of landings are related to changes in the magnitude of the Canadian fishery which, since 1940, has produced most of the halibut from Subareas 3 and 4.Offshore and inshore fisheries specifically for large halibut produce most of the landings. Catches of halibut taken incidentally in other fisheries contribute little by weight but take large numbers of small, faster-growing individuals. With a continuation of present fishing practices and intensities an annual yield of about 5 million pounds may be expected to continue, but some increased yield might result from controlling the incidental catches of younger halibut. Ways and means of effecting such control should be explored.


1970 ◽  
Vol 7 (5) ◽  
pp. 1349-1352 ◽  
Author(s):  
Robert Evans

Recent work on the carbonates and sulfates of the Mississippian Windsorian rocks of the Maritime Provinces has led to the idea that the widespread evaporites in the area are the product of sedimentation in supratidal fiats and in depressions in those flats. The tectonic setting and lithologic features of the more soluble evaporites, however, suggest a comparison with the Plio-Pleistocene sediments of the Dead Sea Graben, and it is proposed that the great thicknesses of chlorides known to exist in Nova Scotia and New Brunswick are the result of rapid sedimentation in possibly deep water within the Fundy Rift formed at the end of the Acadian Orogeny.


2011 ◽  
Vol 437 ◽  
pp. 175-181 ◽  
Author(s):  
T Treude ◽  
S Kiel ◽  
P Linke ◽  
J Peckmann ◽  
JL Goedert
Keyword(s):  

2007 ◽  
Vol 87 (5) ◽  
pp. 1175-1180 ◽  
Author(s):  
Jacopo Aguzzi ◽  
Eva Ramirez-Llodra ◽  
Guy Telesnicki ◽  
Mercedes Camps

The activity rhythm of the cold seep shrimp Alvinocaris stactophila from the Gulf of Mexico slope (650 m depth) was investigated in the laboratory in relation to an artificial 12 h light-dark regime. Animals were sampled with a submersible and transferred into individual aquaria where their activity was monitored for 5 d by taking digital video snapshots every 30 s. An observer analysed the footage by counting the number of times an animal crossed two perpendicular lines drawn on a PC screen per 30 min interval. Resulting time series were represented over consecutive days and the waveform analysis was used to precisely assess the phase (i.e. the peak timing) and its limits (i.e. onset and offset) in relation to light ON and OFF. The majority (73%) of animals showed a marked nocturnal pattern of activity with number of movements close to zero during the photophase. Waveform analysis showed that the behavioural transition from activity to inactivity after light ON occurred within approximately 1 h. Considering the general lack of knowledge on the regulation of activity rhythms of crustaceans from subtidal areas, the present data provide a new insight on the role played by light in the regulation of animal activity rhythm in deep-water environments such as those of the cold seeps in the Gulf of Mexico.


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