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  • IUGG Secretariat, CIRES Cooperative Institute for Research in Environmental Sciences, University of Colorado  (4)
  • Deutsches GeoForschungsZentrum GFZ  (3)
  • Fisheries Centre Research Reports  (1)
  • National Museum of Natural History, Leiden
  • 2000-2004  (9)
  • 2004  (6)
  • 2003  (3)
Document type
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  • 2000-2004  (9)
Year
  • 1
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    IUGG Secretariat, CIRES Cooperative Institute for Research in Environmental Sciences, University of Colorado
    Publication Date: 2020-02-12
    Language: English
    Type: info:eu-repo/semantics/other
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  • 2
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    IUGG Secretariat, CIRES Cooperative Institute for Research in Environmental Sciences, University of Colorado
    Publication Date: 2020-02-12
    Language: English
    Type: info:eu-repo/semantics/other
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  • 3
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    Fisheries Centre Research Reports
    In:  In: Seamounts: biodiversity and fisheries. , ed. by Morato, T. and Pauly, D. Fisheries Centre Research Reports, Vancouver, Canada, pp. 25-31. ISBN 1198-6727
    Publication Date: 2012-07-06
    Type: Book chapter , PeerReviewed
    Format: text
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  • 4
    Publication Date: 2024-01-12
    Description: The coastal waters of East Kalimantan are part of the western boundary of the Indo-West Pacific centre of maximum marine biodiversity. During the pilot phase of the East Kalimantan Program (EKP) this has been tested by various specialists who used model taxa to test this hypothesis. Emphasis has been put on the species-rich coral reefs and islands that show reef communities in association with mangroves, seagrass, and algae. A range of habitats has been surveyed, varying in distance offshore (with decreasing salinity, turbidity, sedimentation and nutrient load): fringing reefs along the mainland shore, offshore patch reefs, delta-front barrier reefs, and uplifted atolls. The atolls consist of limestone rock and contain shallow enclosed marine lakes with a unique marine biota. The various marine environments at NE Kalimantan have enabled the selection of taxa and sites that can be used for future research on climate change records (e.g. corals, sponges and molluscs), molecular (genetic) divergence within species between separated populations, and environmental effects on species diversity. The biodiversity data will be important for the design of Marine Protected Areas (MPAs) and as an instrument in raising public awareness regarding the sustainable use of the natural resources, such as through fisheries and diving tourism.
    Keywords: Marine biodiversity ; Berau region ; Kalimantan ; Indonesia
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/other
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  • 5
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    IUGG Secretariat, CIRES Cooperative Institute for Research in Environmental Sciences, University of Colorado
    In:  IUGG Annual Report
    Publication Date: 2023-03-02
    Language: English
    Type: info:eu-repo/semantics/report
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  • 6
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    IUGG Secretariat, CIRES Cooperative Institute for Research in Environmental Sciences, University of Colorado
    In:  IUGG Annual Report
    Publication Date: 2023-03-02
    Language: English
    Type: info:eu-repo/semantics/report
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  • 7
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    Deutsches GeoForschungsZentrum GFZ
    In:  Scientific Technical Report STR
    Publication Date: 2020-02-12
    Description: Late Miocene to Quaternary volcanic rocks from the frontal arc to the back-arc region of the Central Volcanic Zone in the Andes show a wide range of delta 11B values (+4 to -7 ‰) and boron concentrations (6 to 60 ppm). Positive delta 11B values of samples from the volcanic front indicate involvement of a 11B-enriched slab component, most likely derived from altered oceanic crust, despite the thick Andean continental lithosphere, and rule out a pure crust-mantle origin for these lavas. The delta 11B values and B concentrations in the lavas decrease systematically with increasing depth of the Wadati-Benioff Zone. This across-arc variation in delta 11B values and decreasing B/Nb ratios from the arc to the back-arc samples are attributed to the combined effects of B-isotope fractionation during progressive dehydration in the slab and a steady decrease in slab-fluid flux towards the back arc, coupled with a relatively constant degree of crustal contamination as indicated by similar Sr, Nd and Pb isotope ratios in all samples. Modelling of fluid-mineral B-isotope fractionation as a function of temperature fits the across-arc variation in delta 11B and we conclude that the B-isotope composition of arc volcanics is dominated by changing delta 11B composition of B-rich slab-fluids during progressive dehydration. Crustal contamination becomes more important towards the back-arc due to the decrease in slab-derived fluid flux. Because of this isotope fractionation effect, high delta 11B signatures in volcanic arcs need not necessarily reflect differences in the initial composition of the subducting slab. Three-component mixing calculations for slab-derived fluid, the mantle wedge and the continental crust based on B, Sr and Nd isotope data indicate that the slab-fluid component dominates the B composition of the fertile mantle and that the primary arc magmas were contaminated by an average addition of 15 to 30 % crustal material.
    Language: English
    Type: info:eu-repo/semantics/doctoralThesis
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  • 8
    Publication Date: 2021-08-07
    Language: German
    Type: info:eu-repo/semantics/report
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  • 9
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    Deutsches GeoForschungsZentrum GFZ
    In:  Scientific Technical Report STR
    Publication Date: 2021-08-08
    Language: German
    Type: info:eu-repo/semantics/doctoralThesis
    Format: application/pdf
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