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  • 1
    Book
    Book
    Kingston : Univ. of the West Indies Publ.
    Keywords: geology ; Caribbean Region ; Karibik ; Geologie
    Type of Medium: Book
    Pages: III; 289 S , graph. Darst., Kt
    ISBN: 9764100333
    Language: English
    Note: Order from: Dr. T. A. Jackson, Department of Geology, University of the West Indies, Kingston 7, Jamaica
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 41 (1994), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The only reported occurrence of quartz-rich sands in Jamaica is on the plains of Black River, St Elizabeth, where they outcrop in isolated pockets. The sands overlie limestones of the White Limestone Supergroup and the Coastal Group, and partly underlie Holocene peat deposits.Monocrystalline quartz, containing fluid and mineral inclusions, is the dominant mineral of the sands, with the heavy minerals. magnetite, haematite, epidote, rutile, anatase, zircon and tourmaline, occurring in minor amounts. Grain surface texture studies of the quartz grains have identified a series of mechanical and chemical features. Microtextures depicting marine, aeolian and pedological environments have been retained on the grains and represent the last three stages in the history of the grains.The petrography of the sands indicates an igneous provenance, with the major source of the detrital minerals being the Cretaceous granitoids that outcrop in the eastern half of the island. These rocks were unroofed during the uplift of Jamaica in the Late Tertiary and were subjected to extensive chemical weathering, which accounted for the breakdown of the majority of their primary silicate minerals. Fluvial transportation and deposition of detritus onto the shelf of the south coast commenced during this period and continued into the Pleistocene, providing terrigenous sand that was modified along the coast to quartz arenite by moderate to high energy marine conditions. Tidal currents, east-west longshore currents and weathering contributed to the maturity of the sand by the time it had been transported along the shelf to the vicinity of Black River. During low sea level stands in the Pleistocene, some of this sediment that became trapped on the shelf was blown inland by south-east winds.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1570-7458
    Keywords: Serratia marcescens ; Listronotus maculicollis ; Listronotus bonariensis ; Microctonus hyperodae ; parasitoid-bacteria transmission ; host-specificity testing
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Listronotus maculicollis (Dietz) (Coleoptera: Curculionidae) is a potential novel host of the braconid parasitoid Microctonus hyperodae Loan, but initial studies have shown that levels of parasitism are lower than in the natural host L. bonariensis (Kuschel). A novel bacterial indicator test was used to determine whether the lower level of parasitism was due to behavioural factors, lack of oviposition, or host resistance. The incidence of ovipositor penetration by the parasitoid M. hyperodae into adult L. maculicollis was measured by immersing the ovipositor of the parasitoid in the facultative pathogen, Serratia marcescens Bizio. Adult weevils were then exposed to parasitoids for up to 72 h and rapid mortality used as an indicator of oviposition penetration. Survival was assessed after six days and surviving weevils were dissected and examined for parasitoid larvae. Mortality among L. maculicolis exposed to parasitoids treated with S. marcescens was significantly higher (P〈0.001) than the controls but significantly lower (P〈0.001) than in the natural host, L. bonariensis. Dissection of weevils exposed to uncontaminated parasitoids revealed that parasitism in L. maculicolis was significantly (P〈0.001) less than parasitism in L. bonariensis. Serratia marcescens-induced mortality plus parasitism of surviving weevils in the parasitoid plus bacteria treatments produced a similar overall effect. Application of bacteria to the parasitoid ovipositor provided a rapid, simple test for ovipositor penetration, which shows potential for separation of behavioural and physiological defence mechanisms in parasitoid/host range studies.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Integrated pest management reviews 4 (1999), S. 281-285 
    ISSN: 1572-9745
    Keywords: microbial control ; soil pests ; persistence ; specificity
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract The soil, being rich in microbes, should be an ideal environment in which to practise microbial control of insect pests, but relatively few organisms have been developed into successful microbial control agents for soil pests. Difficulty arises in implementation of microbial control, as the soil is a highly complex, competitive environment where survival of applied microbes is by no means assured. In addition, soil dwelling pests appear to show a high level of resistance to broad spectrum pathogens and microbial toxins. However, some significant successes have been achieved with bacteria, fungi and nematodes for control of a range of soil inhabiting pest species. The successful microbial controls are based on highly specific microbial/insect interactions where co-evolved pathogens can overcome the host's defences. These agents also have the ability to persist in the soil, either through the inherent stability of the organism or from recycling through the host population. While strain selection for high levels of pathogenicity and environmental competence is the essential first step in microbial control of soil dwelling pests, it must be followed by development of efficient production systems and quality control measures to ensure application of standardised, high quality products. Success in microbial control of soil dwelling pests depends on an appropriate combination of these factors, with failure likely to occur if any one of these essential components is overlooked.
    Type of Medium: Electronic Resource
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  • 5
    Publication Date: 2021-04-25
    Description: The first starfish bed to be recognized from the Antilles is a lensoid body in the middle Miocene Grand Bay Formation of Carriacou, The Grenadines (West Indies). This unit was deposited in a turbidite basin in a region of active volcanism fed from one centre and preserves common deep-water taxa more typical of the Palaeozoic, such as crinoids and brachiopods. The starfish bed is a channel-fill deposit laid down in at least 150–200 m water depth, although the specimens may have been derived from shallower water. A goniasterid asteroid and an ophiacanthid ophiuroid have been recognized. The first articulated asteroid from the Antillean fossil record is Paragonaster(?) haldixoni sp. nov. In all skeletal features it appears close to the extant Atlantic species Paragonaster grandis H. L. Clark and P. subtilis (Perrier), but differs in having a single row of rectangular abactinal ossicles extending to the arm tip; these are longer than wide. The brittlestar, Ophiocamax ventosa sp. nov., is described on the basis of a fragmentary disc and arms from this deposit. The closest similarities are with the extant tropical western Atlantic species Ophiocamax hystrix Lyman and O. austera Verrill. However, the new species has thorns covering the entire surface of dorsal arm plates, while arm spines have a multitude of small thorns, loosely arranged in numerous rows and dorsal arm plate shape differs markedly. The occurrence of O. ventosa sp. nov. suggests that Ophiocamax has been a deep-sea taxon at least since the Miocene.
    Keywords: Asteroidea; Goniasteridae; Ophiuroidea; Ophiocanthidae; deep water ; 551
    Language: German
    Type: article , publishedVersion
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