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  • International Association of Sedimentologists  (1)
  • Springer Berlin Heidelberg  (1)
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  • 1
    Publikationsdatum: 2023-08-17
    Beschreibung: Kepulauan Seribu is an isolated patch reef complex situated in the Java Sea (Indonesia) and is a typical example for a humid, equatorial carbonate system. We investigate the mineralogical and isotopic fingerprint of Panggang, one of the reef platforms of Kepulauan Seribu, to evaluate differences to other carbonate systems, using isotope in combination with XRD and SEM analysis. A characteristic property of shallow water (〈 20 m) sediments from Kepulauan Seribu is their increased LMC content (~ 10%) derived from some genera of rotaliid foraminifers and bivalves. The relative abundance of these faunal elements in shallow waters might be related to at least temporary turbid conditions caused by sediment-laden river runoff. This influence is also evidenced by the presence of low amounts of siliciclastic minerals below the regional wave base. Kepulauan Seribu carbonates are characterized by very low δ〈sup〉13〈/sup〉C and δ〈sup〉18〈/sup〉O values. This is related to the isotopically depleted riverine input. The δ〈sup〉13〈/sup〉C〈sub〉DIC〈/sub〉 in riverine water is reduced by the contribution of 〈sup〉12〈/sup〉C from riverside mangroves. Deep atmospheric convection and intensive rains contribute 〈sup〉18〈/sup〉O-depleted freshwater in the river catchments, finally reducing salinity in the Java Sea. The depleted δ〈sup〉13〈/sup〉C signature in carbonates is further enhanced by the lack of green algae and inorganic carbonates and abundance of coral debris. Low δ〈sup〉18〈/sup〉O values in carbonates are favored by the high water temperatures in the equatorial setting. Since equatorial carbonates in SE Asia, including the Java Sea, are typically influenced by high turbidity and/or river runoff, the observed distinctively low isotope values likely are characteristic for equatorial carbonate systems in the region.
    Beschreibung: Lembaga Pengelola Dana Pendidikan (ID)
    Beschreibung: Christian-Albrechts-Universität zu Kiel (3094)
    Schlagwort(e): ddc:552 ; Patch reefs ; Oxygen isotopes ; Carbon isotopes ; SE Asia ; Humid equatorial climate ; Maritime continent
    Sprache: Englisch
    Materialart: doc-type:article
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    facet.materialart.
    Unbekannt
    International Association of Sedimentologists
    In:  Sedimentology, 53 (4). pp. 849-866.
    Publikationsdatum: 2018-07-17
    Beschreibung: Organic biomarker and nannofossil assemblages are used in combination with sedimentary petrology to identify the role of diagenesis for the formation of a rhythmic calcareous succession. A record from the Early Pliocene of the Maldives (Ocean Drilling Program, ODP Leg 115) is presented containing precession and eccentricity cycles expressed as variable aragonite content. Additional sub-Milankovitch cycles are caused by rhythmic precipitation of calcite cement in the lower part of the interval. Comparison with palaeo-productivity indicators (nannofossils, chlorin, total organic carbon) suggests that cementation occurs preferentially in intervals characterized by increasing or decreasing productivity. The coupled variability in productivity and carbonate diagenesis is attributed to the effect of organic matter degradation in the sediment. The observed combination of primary and diagenetic factors hampers the interpretation of the cyclicity on Milankovitch and sub-Milankovitch scales. Diagenetically stable proxies for palaeo-productivity, such as nannofossil assemblage data, were used to distinguish between palaeoclimate and diagenetic influences.
    Materialart: Article , PeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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