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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
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  • 2
    Publikationsdatum: 2019-09-23
    Beschreibung: Pliocene d18O records of shallow and deep dwelling planktonic foraminifers from the Caribbean (Ocean Drilling Program sites 999 and 1000), the tropical east Pacific (sites 1241 and 851), and the Atlantic (site 925, Ceara Rise, and site 1006, western Great Bahama Bank) were used to examine Atlantic-Caribbean-Pacific atmospheric and oceanic linkages associated with the progressive closure of the Central American Seaway (5.5–3 Ma). Comparisons indicate the development of an inner-Caribbean salinity gradient in the mixed layer and salinity changes on precessional periodicities after 4.4 Ma (site 1000), when the Pacific-Caribbean throughflow became significantly restricted. The high-amplitude variability in salinity is also observed at site 1006, monitoring the Caribbean outflow into the Atlantic. Comparisons of Caribbean and Atlantic planktonic d18O records suggest the North Atlantic subtropical gyre as a major source for high-salinity surface waters. Precession-induced variations in the volume transport of Pacific surface water masses through the Panamanian Seaway are considered a main factor to explain the Caribbean salinity minima. Results from a coupled climate model point to changes in the El Nin˜o–Southern Oscillation state as a potential trigger for changes in the amount of Pacific inflow into the Caribbean.
    Materialart: Article , PeerReviewed
    Format: text
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  • 3
    Publikationsdatum: 2018-03-07
    Beschreibung: We constructed a high-resolution Mg/Ca record on the planktonic foraminifer Globigerinoides sacculifer in order to explore the change in sea surface temperature (SST) due to the shoaling of the Isthmus of Panama as well as the impact of secondary factors like diagenesis and large salinity fluctuations. The study covers the latest Miocene and the early Pliocene (5.6–3.9 Ma) and was combined with δ18O to isolate changes in sea surface salinity (SSS). Before 4.5 Ma, SSTMg/Ca and SSS show moderate fluctuations, indicating a free exchange of surface ocean water masses between the Pacific and the Atlantic. The increase in δ18O after 4.5 Ma represents increasing salinities in the Caribbean due to the progressive closure of the Panamanian Gateway. The increase in Mg/Ca toward values of maximum 7 mmol/mol suggests that secondary influences have played a significant role. Evidence of crystalline overgrowths on the foraminiferal tests in correlation with aragonite, Sr/Ca, and productivity cyclicities indicates a diagenetic overprint on the foraminiferal tests. Laser ablation inductively coupled plasma–mass spectrometry analyses, however, do not show significantly increased Mg/Ca ratios in the crystalline overgrowths, and neither do calculations based on pore water data conclusively result in significantly elevated Mg/Ca ratios in the crystalline overgrowths. Alternatively, the elevated Mg/Ca ratios might have been caused by salinity as the δ18O record of Site 1000 has been interpreted to represent large fluctuations in SSS, and cultivating experiments have shown an increase in Mg/Ca with increasing salinity. We conclude that the Mg/Ca record 〈4.5 Ma can only reliably be considered for paleoceanographical purposes when the minimum values, not showing any evidence of secondary influences, are used, resulting in a warming of central Caribbean surface water masses after 4.5 Ma of ∼2°C.
    Materialart: Article , PeerReviewed
    Format: text
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  • 4
    facet.materialart.
    Unbekannt
    In:  (PhD/ Doctoral thesis), Christian-Albrechts-Universität, Kiel, 114 pp
    Publikationsdatum: 2012-02-23
    Materialart: Thesis , NonPeerReviewed
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
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    Unbekannt
    AGU (American Geophysical Union)
    In:  Paleoceanography, 21 (PA1017).
    Publikationsdatum: 2017-05-10
    Beschreibung: High-resolution bulk sediment (magnetic susceptibility and aragonite content) and δ18O records from two different planktonic foraminifera species were analyzed in an early Pliocene core interval from the Straits of Florida (Ocean Drilling Program site 1006). The δ18O record of the shallow-dwelling foraminifera G. sacculifer and the aragonite content are dominated by sub-Milankovitch variability. In contrast, magnetic susceptibility and the δ18O record of the deeper-dwelling foraminifera G. menardii show precession cycles. The relationship between the aragonite and the paleoproxy data suggests that the export of sediment from the adjacent Great Bahama Bank was triggered directly by atmospheric processes rather than by sea level change. We propose a climate mechanism that bears similarities with the semiannual cycle component of eastern equatorial Pacific sea surface temperatures under present-day conditions.
    Materialart: Article , PeerReviewed
    Format: text
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  • 6
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    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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  • 7
    facet.materialart.
    Unbekannt
    Elsevier
    In:  Marine Geology, 185 . pp. 121-142.
    Publikationsdatum: 2020-03-24
    Beschreibung: Numerous small-scale depositional cycles are present in the Miocene sediments of seismic sequence along the margin of Great Bahama Bank (ODP Leg 166). These cycles consist of decimetre- to metre-scale alternations between light-grey and dark-grey/black wackestones/packstones. The light-grey layers are well cemented and nearly uncompacted. They contain planktonic and benthic foraminifera, and bioclasts. Bioturbation in these layers is moderate. The dark-grey wackestones/packstones are uncemented, strongly compacted and normally strongly bioturbated. The main components are planktonic foraminifera and fine-grained bioclasts. The dark layers are rich in aragonite and organic carbon and contain around 80% carbonate. The light layers show low aragonite and organic carbon contents combined with carbonate values of up to 97.5%. Light δ13C and slightly negative δ18O values were observed in the dark uncemented layers while the cemented intervals show heavy δ13C values and slightly more positive δ18O values. The carbon isotope signal between the dark and the light layers shows variations of up to 1.45‰. Both δ13C and δ18O co-vary with carbonate content. The Formation MicroScanner images reflect the changes in carbonate mineralogy. The Natural Gamma-Ray Tool shows that variations in siliciclastic content of the examined succession displays a different frequency than the cyclic alternations in carbonate mineralogy. The internal stacking pattern of the cycles is closely tied to sea level. The dark layers are deposited during rising sea level, while the light layers reflect sediment production and export during highstand and falling sea level. These cycles thus represent a rather continuous sediment shedding pattern that is clearly related to the ramp morphology and differs from the highstand shedding pattern typical for rimmed flat-topped platforms. Most measured parameters suggest that primary sediment composition played an important role in the cementation process. The primary differences in composition were enhanced during shallow burial diagenesis. The initially high content of metastable carbonate phases in the periplatform sediments triggered rapid cementation of the primary aragonite-rich layers leading to the formation of the light beds. Dissolution of metastable high-Mg calcite and aragonite was followed by in situ precipitation of more stable dolomite and calcite. Diagenesis was enhanced by the coarse grain size of the primary aragonite-rich layers. In contrast the more pelagic, dark calcite-rich layers were only slightly affected by diagenesis and could preserve their aragonite content. The uncemented layers subsequently were subject to strong mechanical compaction, whereas the cemented beds stayed nearly uncompacted.
    Materialart: Article , PeerReviewed
    Format: text
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  • 8
    Publikationsdatum: 2018-07-19
    Beschreibung: In a sediment core from the leeward side of the Great Bahama Bank (Ocean Drilling Program ODP-Leg 166, 1006A-24H, early Pliocene) several paleoceanographic proxies were compared with carbonate mineralogy. The proxies measured on the planktonic foraminifera species Globigerinoides sacculifer are Mg/Ca and Sr/Ca elemental ratios, and δ18O values. These proxies are widely used in pelagic sediments to derive parameters of water masses, such as paleo-temperature and -salinity. To produce quantitative estimates it is necessary to verify that the primary shell mineralogy of the foraminifera was not altered diagenetically. Diagenetic alteration can be rapid in periplatform settings relative to pelagic deep-sea sediments, since the meta-stable carbonate phases provide an additional driving force for recrystallisation. We show that the Sr/Ca ratio of foraminiferal calcite can be used to assess the degree of diagenetic alteration of their shell chemistry. Using this method, we demonstrate that the primary signal in the oxygen-isotope ratios is preserved in the studied core. In the Mg/Ca record, the relative change of foraminiferal Mg/Ca ratios seems to be preserved, but absolute values are influenced by diagenesis. The second set of proxies comprises δ13C and C/N ratios of organic carbon. These are used in pelagic sediments in order to assess the origin of organic carbon (terrestrial or marine phytoplankton). It is demonstrated here that a simple two-end mixing model cannot explain the observed co-occurrence of relatively high δ13Corg and C/N values. As the δ13Corg values co-vary with the aragonite content, we attribute this signature to varying contribution of organic carbon from benthic algae, which are also the major aragonite producers on the platform top.
    Materialart: Article , PeerReviewed
    Format: text
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  • 9
    Publikationsdatum: 2024-02-07
    Beschreibung: We present two 40 year records of monthly coral Sr/Ca ratios from the eastern pole of the Indian Ocean Dipole. A modern coral covers the period from 1968 to 2007. A sub-fossil coral derives from the medieval climate anomaly (MCA) and spans 1100–1140 ad. The modern coral records SST variability in the eastern pole of the Indian Ocean Dipole. A strong correlation is also found between coral Sr/Ca and the IOD index. The correlation with ENSO is asymmetric: the coral shows a moderate correlation with El Niño and a weak correlation with La Niña. The modern coral shows large interannual variability. Extreme IOD events cause cooling 〉 3 °C (1994, 1997) or ~ 2 °C (2006). In total, the modern coral indicates 32 warm/cool events, with 16 cool and 16 warm events. The MCA coral shows 24 warm/cool events, with 14 cool and 10 warm events. Only one cool event could be comparable to the positive Indian Ocean Dipole in 2006. The seasonal cycle of the MCA coral is reduced (〈 50% of to the modern) and the skewness of the Sr/Ca data is lower. This suggests a deeper thermocline in the eastern Indian Ocean associated with a La Niña-like mean state in the Indo-Pacific during the MCA.
    Materialart: Article , PeerReviewed
    Format: text
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  • 10
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    Unbekannt
    PANGAEA
    In:  Supplement to: Hallenberger, Maximilian; Reuning, Lars; Gallagher, Stephen John; Back, Stefan; Ishiwa, Takeshige; Christensen, Beth A; Bogus, Kara A (2019): Increased fluvial runoff terminated inorganic aragonite precipitation on the Northwest Shelf of Australia during the early Holocene. Scientific Reports, 9(1), https://doi.org/10.1038/s41598-019-54981-7
    Publikationsdatum: 2023-02-24
    Beschreibung: Inorganic precipitation of aragonite is a common process within tropical carbonate environments. Across the Northwest Shelf of Australia (NWS) such precipitates were abundant in the late Pleistocene, whereas present-day sedimentation is dominated by calcitic bioclasts. This study presents sedimentological and geochemical analyses of core data retrieved from the upper 13 meters of IODP Site U1461 that provide a high-resolution sedimentary record of the last ~15 thousand years. Sediments that formed from 15 to 10.1 ka BP are aragonitic and characterised by small needles (〈5 µm) and ooids. XRF elemental proxy data indicate that these sediments developed under arid conditions in which high marine alkalinity favoured carbonate precipitation. A pronounced change of XRF-proxy values around 10.1 ka BP indicates a transition to a more humid climate and elevated fluvial runoff. This climatic change coincides with a shelf-wide cessation of inorganic aragonite production and a switch to carbonate sedimentation dominated by skeletal calcite. High ocean water alkalinity due to an arid climate and low fluvial runoff therefore seems to be a prerequisite for the formation of shallow water aragonite-rich sediments on the NWS. These conditions are not necessarily synchronous to interglacial periods, but are linked to the regional hydrological cycle.
    Schlagwort(e): Carbonate Sedimentology; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Northwest Shelf of Australia; palaeoclimate
    Materialart: Dataset
    Format: application/zip, 4 datasets
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