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  • Cooper, Rachel  (2)
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  • 1
    In: Marine and Freshwater Research, CSIRO Publishing, Vol. 67, No. 11 ( 2016), p. 1750-
    Abstract: The international literature highlights the importance of understanding the role and fate of terrestrial organic matter (OM) in the marine system, yet little is known about this on the oligotrophic east coast of South Africa. Within the Bight, three important processes make OM biologically available: (1) a topographically induced upwelling cell (north), (2) a Cyclonic Eddy (south), and (3) riverine input. We hypothesise that: (i) these OM sources differ substantially in their isotope ratios, and (ii) zooplankton at the inshore region has an isotope signature linked to localised fluvial fluxes. Particulate OM samples were collected at five locations along the Bight and in three main estuaries during austral summer and winter seasons in 2010 and subjected to isotopic and mixing model analysis. Riverine input played an important role in this ecosystem inshore during the wet season. Only marine OM played a role as a biological driver offshore and at all sites during the dry season. Although there were indications that the upwelling cell did occur, it was not confirmed as active in either season. The current study provides valuable insights into the Bight's biological functioning and principle insights into the fate of terrestrial organic carbon on the east coast of southern Africa.
    Type of Medium: Online Resource
    ISSN: 1323-1650
    Language: English
    Publisher: CSIRO Publishing
    Publication Date: 2016
    detail.hit.zdb_id: 1283028-8
    SSG: 12
    SSG: 21,3
    Location Call Number Limitation Availability
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  • 2
    In: Rapid Communications in Mass Spectrometry, Wiley, Vol. 25, No. 13 ( 2011-07-15), p. 1853-1861
    Abstract: Stable isotope measurements are an important tool for ecosystem trophic linkage studies. Ideally, fresh samples should be used for isotopic analysis, but in many cases organisms must be preserved and analysed later. In some cases dyes must be used to help distinguish organisms from detritus. Since preservatives and dyes are carbon‐based, their addition could influence isotopic readings. This study aims to improve understanding of the effects of sample storage method, dye addition and acidification on the δ 15 N and δ 13 C values of zooplankton ( Euphasia frigida and Undinula vulgaris ). Zooplankton was collected and preserved by freezing, or by the addition of 5% formalin, 70% ethanol, or 5% formalin with added Phloxine B or Rose Bengal, and stored for 1 month before processing. Samples in 5% formalin and 70% ethanol were also kept and processed after 3 and 9 months to study changes over time. Formalin caused the largest enrichment for δ 13 C and a slight enrichment for δ 15 N, while ethanol produced a slight depletion for δ 13 C, and different effects on δ 15 N depending on the species. In formalin, dyes depleted the δ 13 C values, but had variable effects on δ 15 N, relative to formalin alone. Acidification had no significant effect on δ 15 N or δ 13 C for either species. Long‐term storage showed that the effects of the preservatives were species‐dependent. Although the effects on δ 15 N varied, a relative enrichment in 13 C of samples occurred with time. This can have important consequences for the understanding of the organic flow within a food web and for trophic studies. Copyright © 2011 John Wiley & Sons, Ltd.
    Type of Medium: Online Resource
    ISSN: 0951-4198 , 1097-0231
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2011
    detail.hit.zdb_id: 2002158-6
    detail.hit.zdb_id: 58731-X
    SSG: 11
    Location Call Number Limitation Availability
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