scholarly journals On the conditions which determine the presence or absence of animal life on the deep sea bottom

1875 ◽  
Vol 4 (3) ◽  
pp. 176-202
Author(s):  
W.B. Carpenter
Keyword(s):  
Deep Sea ◽  
Nature ◽  
1870 ◽  
Vol 1 (21) ◽  
pp. 540-542
Author(s):  
W. B. CARPENTER
Keyword(s):  
Deep Sea ◽  

Author(s):  
A. H. Church

To the geologist, the mineralogist and the chemist, two of the observations made during the voyage of the Challenger are of especial interest. One of these observations is the occurrence over vast areas of the deep sea bottom of a peculiar red clay, containing silica, peroxide of iron, and alumina. The other discovery to which I refer has been described by Sir Wyville Thomson as the occurrence throughout this red clay of nodules of “nearly pure peroxide of manganese.” To these nodules, as well us to the red clay, an organic origin has been assigned. But the immediate source of so much manganese is hard to find, for this element is by no means an abundant constituent of animal or vegetable organisms. The difficulty is, however, somewhat lessened when the manganese nodules are submitted to a more minute chemical examination. From two correspondents I have received an ample supply of these curious concretions, accompanied by a suggestion that they should be submitted to chemical analysis.


2012 ◽  
Vol 131 (4) ◽  
pp. 3489-3489
Author(s):  
Xiaodong Liu ◽  
Weiqing Zhu ◽  
Fangsheng Zhang ◽  
Dongsheng Zhang ◽  
Gaofeng Xu
Keyword(s):  
Deep Sea ◽  

2008 ◽  
Vol 27 (2) ◽  
pp. 164-187 ◽  
Author(s):  
Torben Wolff

The Danish Ingolf Expedition took place in the summer months of 1895 and 1896, with C. F. Wandel as captain, a man with long experience in hydrographical work in the Arctic. The other scientific participants were the zoologists H. Jungersen, W. Lundbeck and H. J. Hansen during the 1895 cruise; C. Wesenberg-Lund replaced Hansen during the 1896 cruise. C. H. Ostenfeld was the botanist and M. Knudsen the hydrographer. The Ingolf (see Figure 1) was a naval cruiser. In both years the voyages were hindered by ice that had moved much further south than normal, even closing most of the Denmark Strait. In 1895, the best results were obtained south of Iceland and in the Davis Strait; in 1896 south and east of Iceland and as far north as Jan Mayen Island. A total of 144 stations were completed, all with soundings, trawlings and (for the first time) continuous hydrographical work associated with the deep-sea trawling (bottom measurements of temperature, salinity, chlorine contents and specific gravity). Eighty of the stations were deeper than 1,000 m. There were more than 800 hydrographical measurements, with about 3,300 registrations recordings added on the basis of the measurements. 138 gas analyses were performed on board with samples from the surface and the sea bottom. The main result of the expedition was the final demonstration of probably the most important threshold boundaries in the world: the Wyville Thompson Ridge from East Greenland to Scotland with maximum depths of 600 m, separating the fauna in the Norwegian and Polar Sea to the north, always with negative below-zero temperatures except close to the Norwegian coast, from the fundamentally different general Atlantic deep-sea fauna to the south of the ridge with positive temperatures. The results are published in the Ingolf Report, with fifteen volumes containing forty-three papers by nineteen Danish authors and fourteen papers by six foreign authors. The sieving technique was excellent—due to an apparatus designed by H. J. Hansen that kept the animals under water until preservation and using the finest silk for sieving. In this way, the expedition collected more smaller animals than had been acquired by previous deep-sea expeditions. Hansen's studies of the peracarid crustaceans and parasitic copepods and Lundbeck's report on the sponges were particularly noteworthy. The 130 photographs taken on board and on land by the ship's doctor William Thulstrup represent a cultural/historical treasure.


Author(s):  
H. Flügel

The question as to the existence of life at great depths was still a matter of controversy in the last century. In spite of the fact that the remains of living animals were recovered from several hundreds of metres, many marine biologists hesitated to believe that animal life could exist in deep-sea conditions. In 1841, Sir James Clark Ross, the leader of the British Antarctic Expedition, claimed:‘… and although contrary to the general belief of naturalists, I have no doubt that from however great a depth we may be able to bring the mud and stones of the bed of the ocean, we shall find them teeming with animal life; the extreme pressure at the greatest depth does not appear to affect these creatures; hitherto we have not been able to determine this point beyond a thousand fathoms, but from that depth several shellfish have been brought up with the mud’ (Murray 1895, p. 79). Edward Forbes, naturalist on H.M.S.S. Beacon, for instance, referred to the marine environment in excess of 550 m as the ‘azoic zone’. But the classical deep-sea expeditions in the second half of the nineteenth century, among others the famous voyage of the Challenger, produced overwhelming evidence for a more or less abundant abyssal fauna.


1988 ◽  
Vol 78 (3-4) ◽  
pp. 199-216 ◽  
Author(s):  
Christopher G. Fox ◽  
Kim Marie Murphy ◽  
Robert W. Embley

This sounding was obtained on a calm day, October 30, 1852, in the course of the passage of H. M. ship Herald, from Rio de Janeiro to the Cape of Good Hope. The sounding-line was 1/10 th of an inch in diameter, laid into one length, and weighing, when dry, lib . for every hundred fathoms. Captain Denham received from Commodore McKeever of the United States Navy, commanding the Congress Frigate, a present of 15,000 fathoms of this line, 10,000 fathoms on one reel, and 5000 on another; and considers it to have been admirably adapted for the purpose for which it was made and to which it was applied. The plummet weighed 91bs., and was 11­·5 inches in length, and 1·7 inch in diameter. When 7706 fathoms had run off the reel the sea-bottom was reached.


Author(s):  
P. Durán Muñoz ◽  
F.J. Murillo ◽  
M. Sayago-Gil ◽  
A. Serrano ◽  
M. Laporta ◽  
...  

The effects of deep-sea bottom longlining on fish communities and the benthic ecosystem, as well as the interactions between fishing and seabirds, were studied based on data collected from a joint collaboration between the Spanish Institute of Oceanography and a longliner, carried out on the Hatton Bank area (north-east Atlantic) in 2008. A total of 38 longline sets were distributed mainly along the rugged bottom of the rocky outcrop at depths ranging from 750 to 1500 m. Deep-water sharks and lotids were predominant in the catches contributing respectively 80.4% and 13.1% in terms of weight. Deep-water sharks were predominant in the discards. By-catch of cold-water corals and small glass sponges occurred along the western flank of the Hatton Bank, while large hexactinellids were found along the eastern flank. Longlines fished the adult fraction of vulnerable deep-water sharks and lotids. High catches per unit effort values for these species were obtained in coral areas. A combination of seabird-scaring streamer lines and other measures of preventing seabird by-catch were used. Only one fulmar was captured and it survived. Data on distribution of marine litter and derelict deep-sea gillnets are also presented.


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