The transmission of pathogenic Micro-Organisms by Flies in Saint Lucia

1912 ◽  
Vol 3 (1) ◽  
pp. 81-88 ◽  
Author(s):  
Lucius Nicholls

The mechanical conveyance of germs by flies and other insects is of importance not only to the sanitary officer, but to the agriculturist and even to the merchant, for the more the matter is enquired into, the more numerous become the cases in which the origin of fermentation or disease in plants and animals can be traced primarily to this agency. Whatever may be the significance of this question in temperate climates, it is obviously of far greater importance in the tropics, where insects are present in greater profusion throughout all seasons of the year. The subject certainly merits more attention than has yet been bestowed upon it.

SCOPE, the Scientific Committee on Problems of the Environment, analyses such problems by means of programmes leading to published reports on the state of knowledge. The meeting reported here was the major British contribution to the SCOPE Programme on the Ecology of Biological Invasions. It is a slightly unusual programme for SCOPE in that the subject is an entirely biological one, and also in that, although most of the problems are caused by invasions induced by man, some can arise as a result of natural extensions of range. Such effects are often acute in ecosystems with a mediterranean climate away from the Mediterranean itself, that is to say in California, South Africa and Australia. These mediterranean zones are in different biogeographical regions, so the organisms native and introduced to them have, in general, no evolutionary experience of each other. Species introduced from one such region to another have frequently spread in semi-natural and natural ecosystems. The SCOPE programme arises from concern about the impact and management of such pests in particular. The preamble to the programme (Anon. 1985) therefore talks about ‘ the introduction of plants, animals and micro-organisms to regions remote from their centres of origin. ’ It goes on to say that the ‘ areas include a wide variety of non-agricultural, non-urban land such as native forests and rangelands, and protected areas like National Parks and Ecological Reserves.’


1955 ◽  
Vol 143 (911) ◽  
pp. 159-178 ◽  

It is a signal honour to be invited to give the Leeuwenhoek Lecture, and I would like to thank the authorities of the Royal Society for their invitation to me to give this lecture on the chemical aspects of soil microbiology. Leeuwenhoek clearly perceived from his pioneer work that a vast world of micro-organisms lies in the soil. The importance of its study, both in the purely scientific domain and in the practical fields of agriculture and medicine, is only now being realized. I will try in this lecture to give a short description of some recent studies of the chemical aspects of soil microbiology with a few observations on their practical implications. Some conception of the enormous population of micro-organisms in soil is provided by the fact that there may be as many as 5000 million bacteria per gram of soil. This corresponds to a weight of over 4 tons of bacterial substance per acre of soil. The numbers of bacteria fluctuate very greatly depending on availability of food supply, moisture, aeration conditions, temperature, hydrogen-ion concentration of the soil, and other factors. Protozoa may reach figures of the order of 1 million per gram of soil and algae may exceed a hundred thousand per gram. Actinomycetes and fungi, the exact numbers of which are difficult to estimate, may have a combined weight in the soil equal to that of the bacteria. Kluyver (1953) makes a comment in his recent Leeuwenhoek Lecture that the weight of microbial protoplasm on earth surpasses that of animal protoplasm by almost twenty times. It is obvious, therefore, that in dealing with the subject of soil metabolism we are dealing with the metabolism of vast numbers of living cells, greatly exceeding the number of cells found in animal life. The organisms of soil do not develop in an unrestricted chaotic manner. They are, on the other hand, greatly dependent on each other, sharing many factors in common. Soil may be considered to be a complex biological system in which hosts of organisms compete with each other often for a limited supply of nutritional material. They exercise profound effects on each others’ development and chemical activities, and they establish between themselves a dynamic equilibrium which continually changes with the changes in the physical and chemical environment of the soil.


Metchnikoff, and his school, in the face of much opposition, lasting many years, have offered convincing proofs of the importance of phagocytosis in the protection of the animal body against bacterial invasion. The main theses of the Metchnikovian theory are now almost universally accepted, but the exact mechanism of the processes involved is even now the subject of keen controversy. If a highly virulent organism is injected into a susceptible animal, the leucocytes appear to be repelled, and to be unable to deal with the microbe, which multiplies and causes the death of the animal. If, however, the suitable immune serum is injected into the animal before inoculation, the phagocytes attack and devour the invading micro-organisms. Much discussion has centred round the interpretation of such experiments. The early work of Nuttall and others on the bactericidal action of normal serum, and Pfeiffer’s demonstration of the bacteriolysis of cholera and typhoid bacilli by immune sera in the absence of cells, formed the chief basis on which rested the humoral theory, which attributed the protection in such cases to the destructive action of the serum on the microbes. Flügge graphically illustrated the view of the humoralists by likening the phagocytes to the trenches made ready behind the fighting line to receive the conquered dead.


2015 ◽  
Vol 1130 ◽  
pp. 197-200 ◽  
Author(s):  
Mariekie Gericke

The tank bioleaching of metal sulphides is an established technology. Commercial success started with the treatment of refractory gold concentrates using mesophilic micro-organisms, followed by the development of tank bioleaching processes for the treatment of base metal concentrates. This was initially a mesophilic process treating secondary copper sulphides, pentlandite and cobaltiferous pyrite. There was though limited potential for recovery of copper from chalcopyrite concentrates due to low copper extractions. Over the past decades the optimization of bioleaching processes for the treatment of chalcopyrite ores and concentrates has been the subject of numerous research programmes. The use of bioleaching for the treatment of pure chalcopyrite concentrates has, however, not found commercial application mainly due to competitive smelter prices. With this in mind, Mintek’s base metal bioleaching development over the past few years focused on the treatment of complex polymetallic concentrates containing contaminants such as As, Bi, Pb and Sb as a niche application for tank bioleaching processes. These contaminants pose problems when processed via the smelting route. This paper reviews Mintek’s involvement in the development of base metal tank bioleaching processes for the treatment of chalcopyrite and polymetallic concentrates. Examples of laboratory-scale test work as well as larger scale demonstration and commercialization of the technology are highlighted.


1909 ◽  
Vol 6 (8) ◽  
pp. 350-352 ◽  
Author(s):  
F. P. Mennell

A number of communications dealing with the origin and composition of the material commonly known as laterite have appeared in the Geological Magazine during the past few years. That of Dr. Maclaren is an especially valuable contribution to the literature of the subject, and I think few workers in the Tropics will be disposed to question the substantial accuracy of his conclusions. I shall not attempt, therefore, to discuss the general problem presented by the widespread occurrence of laterite deposits in tropical regions. The object of the present brief communication is merely to place on record a few observations made in another area.


1926 ◽  
Vol 16 (3) ◽  
pp. 443-450
Author(s):  
F Procter
Keyword(s):  

It is of great importance that milk should possess a pleasant flavour, but in spite of much trouble which is devoted by farmers and dairymen to this aspect of dairying, it happens from time to time that mishaps do occur. Taints and flavours in milk are due chiefly to the following three causes:1. The activity of contaminating micro-organisms.2. The action of milk on metals.3. The influence of the foods eaten on the milk produced.It must be admitted that we have very little knowledge of the subject of milk flavours and taints, and there seems little doubt but that the blame for many taints caused by micro-organisms has been associated wrongly with foods and sometimes with manures.


1891 ◽  
Vol 17 ◽  
pp. 257-270
Author(s):  
A. B Griffiths

Dr P. W. Latham, in the Harveian oration at the Koyal College of Physicians, on October 17, 1888, supported my own researches (which have already been published in the Proc. Roy. Soc. Edin., vol. xiv. pp. 97–106, and vol. xv. pp. 33–63), on the subject of “disease germs.” He says:—” “We might hope to find that the action and growth of the bacilli [of phthisis] might be inhibited by certain substances, and then, by injecting these substances into the blood, disease might be prevented, or if disease existed it might be arrested or cured.”


A great part of this paper was written in the spring of 1886, but its completion was unavoidably delayed. This has, however, not been altogether without advantage. Thus, in the first place, at the Naturforscher-Versammlung , held in Berlin, in September, 1886, the greater part of the sittings of two days was devoted, in the Section of Landwirthschaftliches Versuchs- Wesen , to the discussion of the subject from various points of view, one of ourselves taking part; and as it seemed desirable that the results and conclusions then brought forward by others should be considered, we have waited for the publication of the exact figures in some cases. Again, since the Berlin meeting, M. Berthelot has published some further results, to which reference should be made. And lastly, we are now enabled to give further new results of our own. In Part 2 of the ‘Philosophical Transactions’ for 1861, a paper was given, by ourselves and the late Dr. Pugh, “ On the Sources of the Nitrogen of Vegetation, with special reference to the question whether plants assimilate free or uncombined Nitrogen .” Since that time, the question of the sources of the nitrogen of vegetation has continued to be the subject of much discussion, and also of much experimental enquiry, both at Rothamsted and elsewhere. Until quite recently, the controversy has chiefly been as to whether plants directly assimilate the free nitrogen of the atmosphere; but, during the last few years, the discussion has assumed a somewhat different aspect. The question still is whether the free nitrogen of the air is an important source of the nitrogen of vegetation; but whilst few now adhere to the view that the higher chlorophyllous plants directly assimilate free nitrogen, it is, nevertheless, assumed to be brought under contribution in various ways—coming into combination within the soil, under the influence of electricity, or of micro-organisms, or of other low forms, and so indirectly serving as an important source of the nitrogen of plants of a higher order. Several of the more important of the investigations in the lines here indicated seem to have been instigated by the assumption that compensation must be found for the losses of combined nitrogen which the soil sustains by the removal of crops, and also for the losses which result from the liberation of nitrogen from its combinations under various circumstances.


2020 ◽  
Vol 7 (1) ◽  
pp. 39-49
Author(s):  
Mary Kensa V ◽  
Anju M

Fish is one of the most important sources of animal protein available in the tropics and has been widely accepted as a good source of protein and other elements for the maintenance of healthy body. Salting and drying is an ancient and simple method to preserve fish and in India about 17% of the total catch is beingused for salting and drying. The present investigation was aimed to analyse the presence of osmotolerant microbes in the dry fishes. The commercially important marine edible salted dry fishes were collected from the study area Pallam. Four common edible dry fishes like (Nethili, Sardines, Ribbon fish and Prawn) wereselected for the screening of microbial population. The highest TFC value was reported in Sardine and Ribbon fish (5103) than the other fishes like Netthili and Prawn (4103 and 2103). The moisture content was higher (45%) in Prawn followed by Ribbon fish (40%), Sardines (29%), Netthili (26%). In this study,Prawn had high moisture content (45%) and high microbial load (5.3104 cfu/g). Total five fungal species were isolated from the selected dried fishes. The result of isolation of human pathogens such as Salmonella and Vibrio identified from the selected dry fish samples. The nutritive value of raw fish in found to be good.The sensory characteristics such as colour, odor, texture, insect infestation showed that the Sardine and Prawn was good in quality, while the netthili had decreased the quality. The study showed that salted and sundried fishes sold in study area are contaminated with pathogenic bacteria and fungal agents. Spoilage ofdried fish products was found and this might be due to unhygienic handling of the fisher folks, improper processing and unhygienic vendors and vending areas.


1938 ◽  
Vol 19 (2) ◽  
pp. 59-66
Author(s):  
E. Gherzi

The question of frontology and modern synoptic analysis of tropical cyclones has come to the fore rapidly in the last decade owing to the influence of the Norwegian School and the improvement in collecting synoptic information in the tropics; Fr. Gherzi has been a cogent critic of typhoon frontology ever since the Indian and Japanese meteorologists first put fronts on typhoon maps. He has already expressed some of his views on the question in Gerlands Beitr., bd. 29, p. 344, Q. Jn. R. Met. Soc., 1932, p. 303, Met. Zts., March 1937, and in “Typhoons in 1933”, Zikawei, 1934 ; and is an authority on the subject with years of study and forecasting experience in the Far Eastern region. While many meteorologists will agree with some of his criticisms, in regard to Fr. Deppermann's work we think he may have misread him as the latter in his texts specifically denies that the fronts always extend right into the center of the typhoon even though his maps seem to show them that way, and also he does not claim the fronts in themselves are dynamically necessary for a typhoon; Deppermann does, however, seem to believe that as far as the Philippine region is concerned the typhoons do not form totally within a single homogeneous air mass and that the greater convergence in the SW Monsoon sector is somehow an important dynamic factor. It is with these points that Gherzi is really in disagreement. One of Deppermann's maps is reproduced here in order that the reader may see what is referred to, and in a coming issue of the Bulletin some of Fr. Deppermann's views will be quoted by way of rebuttal.—R. G .S.


Sign in / Sign up

Export Citation Format

Share Document