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  • 1
    Publication Date: 2019
    Description: 〈div data-abstract-type="normal"〉〈p〉A survey of Antarctic toothfish (〈span〉Dissostichus mawsoni〈/span〉) was conducted in the northern Ross Sea region during the winter of 2016 to document the timing and location of spawning activity, to collect biological information about reproductive status during the spawning season and to look for temporal signals in biological data from 〈span〉D. mawsoni〈/span〉 that may indicate a spawning migration of mature toothfish from the continental slope region to the northern Ross Sea region. The 58 day survey showed that spawning of 〈span〉D. mawsoni〈/span〉 began on some seamounts by early July. No changes were detected between winter and summer in length, age, sex ratio or condition factor distributions for 〈span〉D. mawsoni〈/span〉 in the northern Ross Sea as hypothesized following a spawning migration from the slope to the northern Ross Sea region. These results suggest that the distribution of 〈span〉D. mawsoni〈/span〉 in the Ross Sea is mainly accomplished through ontogenetic migration and not annual return spawning migrations.〈/p〉〈/div〉
    Print ISSN: 0954-1020
    Electronic ISSN: 1365-2079
    Topics: Biology , Geography , Geosciences
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  • 2
    Publication Date: 2004-09-01
    Description: Sedimentological, malacological, and pollen analyses from 14C-dated alluvial sections from the Luján River provide a detailed record of environmental changes during the Holocene in the northeastern Pampas of Argentina. From 11,200 to 9000 14C yr B.P., both sedimentary and biological components suggest that the depositional environment was eutrophic, alkaline, and freshwater to brackish shallow water bodies without significant water circulation. During this time, bioclastic sedimentation was dominant and the shallow water bodies reached maximum development as the climate became more humid, suggesting an increase in precipitation. Short-term fluctuations in climate during the last stage of this interval may have been sufficient to initiate changes in the water bodies, as reduction of the volume alternated with periods of flooding. The beginning of the evolution of shallow swamps in the wide floodplain or huge wetlands was contemporaneous with a sea level lower than the present one. From 9000 and 7000 14C yr B.P., mesotrophic, alkaline, brackish, probably anoxic swamps existed. Between 7000 and 3000 14C yr B.P., anoxic calcareous swamps were formed, with subaerial exposure and development of the Puesto Berrondo Soil (3500–2900 14C yr B.P.). A trend to a reduction of water bodies is recorded from 9000 to ca. 3000 14C yr B.P., with a significant reduction after ca. 7000 14C yr B.P. A shift to subhumid–dry climate after 7000 14C yr B.P. appears to be the main cause. During this time, an additional external forcing toward higher groundwater levels was caused by Holocene marine transgression causing changes in the water bodies levels. The climate became drier during the late Holocene (ca. 3000 yr B.P.), when clastic sedimentation increased, under subhumid–dry conditions. Flood events increased in frequency during this time. From ca. A.D. 1790 to present, the pollen record reflects widespread disturbance of the vegetation during the European settlement.
    Print ISSN: 0033-5894
    Electronic ISSN: 1096-0287
    Topics: Geography , Geosciences
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  • 3
    Publication Date: 2019-08-01
    Description: A survey of Antarctic toothfish (Dissostichus mawsoni) was conducted in the northern Ross Sea region during the winter of 2016 to document the timing and location of spawning activity, to collect biological information about reproductive status during the spawning season and to look for temporal signals in biological data from D. mawsoni that may indicate a spawning migration of mature toothfish from the continental slope region to the northern Ross Sea region. The 58 day survey showed that spawning of D. mawsoni began on some seamounts by early July. No changes were detected between winter and summer in length, age, sex ratio or condition factor distributions for D. mawsoni in the northern Ross Sea as hypothesized following a spawning migration from the slope to the northern Ross Sea region. These results suggest that the distribution of D. mawsoni in the Ross Sea is mainly accomplished through ontogenetic migration and not annual return spawning migrations.
    Print ISSN: 0954-1020
    Electronic ISSN: 1365-2079
    Topics: Biology , Geography , Geosciences
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  • 4
    Publication Date: 2020-11-04
    Description: Chinese immigration to the Philippines has traditionally been studied in relation to commercial activities. But between 1850 and 1898, there was an unparalleled influx of Chinese labourers, which raised the number of Chinese residents to 100,000. This influx was fuelled by the abundant profits obtained by Chinese brokers and foremen, Spanish institutions and authorities in Manila, consuls in China, and Spanish and British ship captains, all of whom extracted excessive fees and taxes from the labourers. The trade in and the exploitation of Chinese labourers in the Philippines have yet to be thoroughly researched. This article shows that the import and abuse of Chinese labourers in and to the Philippines continued throughout the second half of the nineteenth century, and that, despite some anti-Chinese Spanish colonial rhetoric, a wide range of actors and institutions, both in China and in the Philippines, took advantage of this unprecedented inflow of immigrants.
    Print ISSN: 0022-4634
    Electronic ISSN: 1474-0680
    Topics: Geosciences , Political Science
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