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  • 1
    Keywords: Forschungsbericht ; Cookinseln ; Sonne ; Submariner Vulkanismus ; Trapp
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (20 Seiten, 927,12 KB) , Illustrationen, Diagramme
    Language: German
    Note: Förderkennzeichen BMBF 03G0225B. - Verbund-Nummer 01126005 , Autoren dem Berichtsblatt entnommen , Sprache der Zusammenfassung: Deutsch, Englisch
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  • 2
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    Unknown
    In:  [Paper] In: Statusseminar Meeresforschung mit FS SONNE 2015, 12.-13.02.2015, Bremen . Tagungsband Statusseminar Meeresforschung mit FS SONNE 2015 ; pp. 95-99 .
    Publication Date: 2019-09-23
    Type: Conference or Workshop Item , NonPeerReviewed
    Format: text
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  • 3
    Publication Date: 2024-03-22
    Description: Highlights • Re-organization of the West Pacific Warm Pool at ~ 1.7 – 1.35 Ma. • West Pacific Warm Pool and South Pacific Convergence Zone located further to the NE prior to ~ 1.5 Ma. • High amplitude variations at thermocline and deep thermocline depths after ~ 1.5 Ma. • West Pacific Warm Pool thermocline dynamics linked to southern-sourced mode waters. Abstract The internal development of the tropical West Pacific Warm Pool and its interaction with high latitude ocean regions on geological timescales is only poorly constrained. Based on two newly recovered sediment cores from the southeastern margin of the West Pacific Warm Pool (northern and southern Manihiki Plateau), we provide new aspects on the dynamically interacting ocean circulation at surface, subsurface, thermocline, and deep thermocline levels during the Pleistocene (~ 2.5–0.5 Ma). Notably, the variability of thermocline and deep thermocline (~ 150–400 m water depth) foraminiferal Mg/Ca-based temperatures with up to ~ 6 °C amplitude variations exceeds those at shallower depths (down to ~ 120 m) with only ~ 2–3 °C temperature variations. A major gradual reorganization of the West Pacific Warm Pool oceanography occurred during the transitional time period of ~ 1.7–1.35 Ma. Prior to ~ 1.7 Ma, pronounced meridional and latitudinal gradients in sea-surface to subsurface ocean properties point to the eastward displacement of the West Pacific Warm Pool boundaries, with the South Pacific Convergence Zone being shifted further northeastward across Manihiki Plateau. Simultaneously, the low amplitude variations of thermocline and deep thermocline temperatures refer to an overall deep and stable thermocline. The meridional and zonal gradients in sea-surface and subsurface ocean properties within the West Pacific Warm Pool reveal a pronounced change after 1.5 Ma, leading to a more southward position of the warm South Pacific Convergence Zone between ~ 1.35–0.9 Ma and ~ 0.75–0.5 Ma. Synchronous to the changes in the upper ocean, the deeper water masses experienced high amplitude variations in temperature, most prominently since ~ 1.5 Ma. This and the dynamically changing thermocline were most likely associated to the impact of southern-sourced mode waters, which might have developed coincidently with the emergence of the East Pacific Cold Tongue and high latitude sea-surface cooling.
    Type: Article , PeerReviewed
    Format: text
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  • 4
    Publication Date: 2024-03-22
    Description: Highlights • First apparent calcification depth assessment of living foraminifera in the SE WPWP • Deep surface mixed layer causes deep apparent calcification depths. • Deep-dwelling G. hexagonus traces nutrient conditions in equatorial water masses. Abstract Insight into past changes of upper ocean stratification, circulation, and nutrient signatures rely on our knowledge of the apparent calcification depth (ACD) and ecology of planktonic foraminifera, which serve as archives for paleoceanographic relevant geochemical signals. The ACD of different species varies strongly between ocean basins, but also regionally. We constrained foraminiferal ACDs in the Western Pacific Warm Pool (Manihiki Plateau) by comparing stable oxygen and carbon isotopes (δ18Ocalite, δ13Ccalcite) as well as Mg/Ca ratios from living planktonic foraminifera to in-situ physical and chemical water mass properties (temperature, salinity, δ18Oseawater, δ13CDIC). Our analyses point to Globigerinoides ruber as the shallowest dweller, followed by Globigerinoides sacculifer, Neogloboquadrina dutertrei, Pulleniatina obliquiloculata and Globorotaloides hexagonus inhabiting increasing greater depths. These findings are consistent with other ocean basins; however, absolute ACDs differ from other studies. The uppermost mixed-layer species G. ruber and G. sacculifer denote mean calcification depths of ~ 95 m and ~ 120 m, respectively. These Western Pacific ACDs are much deeper than in most other studies and most likely relate to the thick surface mixed layer and the deep chlorophyll maximum in this region. Our results indicate that N. dutertrei appears to be influenced by mixing waters from the Pacific equatorial divergence, while P. obliquiloculata with an ACD of ~ 160 m is more suitable for thermocline reconstructions. ACDs of G. hexagonus reveal a deep calcification depth of ~ 450 m in oxygen-depleted, but nutrient-rich water masses, consistent to other studies. As the δ13C of G. hexagonus is in near-equilibrium with ambient seawater, we suggest this species is suitable for tracing nutrient conditions in equatorial water masses originating in extra-topical regions.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 5
    Publication Date: 2023-03-16
    Keywords: AWI_Paleo; Depth, bottom/max; Depth, top/min; DEPTH, water; Magnesium/Calcium ratio; Magnesium/Calcium ratio, standard deviation; MANIHIKI II; Mass spectrometry; MSN; Multiple opening/closing net; Number of species; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Size; SO225; SO225_21-3; Sonne; South Pacific Ocean; Species; δ13C, calcite; δ13C, standard deviation; δ18O, calcite; δ18O, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 331 data points
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  • 6
    Publication Date: 2023-03-16
    Keywords: AWI_Paleo; CTD; CTD/Rosette; CTD-RO; DEPTH, water; MANIHIKI II; Oxygen; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Salinity; SO225; SO225_21-1; Sonne; South Pacific Ocean; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 1467 data points
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  • 7
    Publication Date: 2023-03-16
    Keywords: AWI_Paleo; Comment; Depth, bottom/max; Depth, top/min; DEPTH, water; Foraminifera, planktic; Foraminifera, planktic, other; Globigerina bulloides; Globigerinella spp.; Globigerinita glutinata; Globigerinita minuta; Globigerinoides conglobatus; Globigerinoides ruber; Globigerinoides sacculifer; Globoquadrina conglomerata; Globorotalia crassaformis; Globorotalia menardii; Globorotalia spp.; Globorotalia truncatulinoides; Globorotalia tumida; Globorotaloides hexagonus; Globoturborotalita spp.; Hastigerina pelagica; MANIHIKI II; MSN; Multiple opening/closing net; Neogloboquadrina dutertrei; Orbulina universa; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Pulleniatina obliquiloculata; SO225; SO225_21-3; Sonne; South Pacific Ocean; Turborotalita spp.
    Type: Dataset
    Format: text/tab-separated-values, 386 data points
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Rippert, Nadine; Nürnberg, Dirk; Raddatz, Jacek; Maier, Edith; Hathorne, Ed C; Bijma, Jelle; Tiedemann, Ralf (2016): Constraining foraminiferal calcification depths in the western Pacific warm pool. Marine Micropaleontology, 128, 14-27, https://doi.org/10.1016/j.marmicro.2016.08.004
    Publication Date: 2023-03-16
    Description: Insight into past changes of upper ocean stratification, circulation, and nutrient signatures rely on our knowledge of the apparent calcification depth (ACD) and ecology of planktonic foraminifera, which serve as archives for paleoceanographic relevant geochemical signals. The ACD of different species varies strongly between ocean basins, but also regionally. We constrained foraminiferal ACDs in the western Pacific warm pool (Manihiki Plateau) by comparing stable oxygen and carbon isotopes (d18Ocalcite, d13Ccalcite) as well as Mg/Ca ratios from living planktonic foraminifera to in-situ physical and chemical water mass properties (temperature, salinity, d18Oseawater, d13CDIC). Our analyses point to Globigerinoides ruber as the shallowest dweller, followed by Globigerinoides sacculifer, Neogloboquadrina dutertrei, Pulleniatina obliquiloculata and Globotaloides hexagonus inhabiting increasingly greater depths. These findings are consistent with other ocean basins; however, absolute ACDs differ from other studies. The uppermost mixed-layer species G. ruber and G. sacculifer denote mean calcification depths of ~95 m and ~120 m, respectively. These Western Pacific ACDs are much deeper than in most other studies and most likely relate to the thick surface mixed layer and the deep chlorophyll maximum in this region. Our results indicate that N. dutertrei appears to be influenced by mixing waters from the Pacific equatorial divergence, while P. obliquiloculata with an ACD of ~160 m is more suitable for thermocline reconstructions. ACDs of G. hexagonus reveal a deep calcification depth of ~450 m in oxygen-depleted, but nutrient-rich water masses, consistent to other studies. As the d13C of G. hexagonus is in near-equilibrium with ambient seawater, we suggest this species is suitable for tracing nutrient conditions in equatorial water masses originating in extra-topical regions.
    Keywords: AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 9
    Publication Date: 2023-03-16
    Keywords: AWI_Paleo; CTD/Rosette; CTD-RO; DEPTH, water; MANIHIKI II; Mass spectrometry; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; SO225; SO225_21-1; Sonne; South Pacific Ocean; δ13C, dissolved inorganic carbon; δ13C, dissolved inorganic carbon, standard deviation; δ18O; δ18O, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 10
    Publication Date: 2023-01-30
    Description: The internal development of the tropicalWest Pacific Warm Pool and its interaction with high latitude ocean regions on geological timescales is only poorly constrained. Based on two newly recovered sediment cores fromthe southeastern margin of the West Pacific Warm Pool (northern and southern Manihiki Plateau), we provide new aspects on the dynamically interacting ocean circulation at surface, subsurface, thermocline, and deep thermocline levels during the Pleistocene (~2.5-0.5 Ma). Notably, the variability of thermocline and deep thermocline(~150-400 m water depth) foraminiferal Mg/Ca-based temperatures with up to ~6 °C amplitude variations exceeds those at shallower depths (down to ~120 m) with only ~2-3 °C temperature variations. A major gradual reorganization of the West Pacific Warm Pool oceanography occurred during the transitional timeperiod of ~1.7-1.35 Ma. Prior to ~1.7 Ma, pronounced meridional and latitudinal gradients in sea-surface to subsurface ocean properties point to the eastward displacement of the West Pacific Warm Pool boundaries, with the South Pacific Convergence Zone being shifted further northeastward across Manihiki Plateau. Simultaneously, the low amplitude variations of thermocline and deep thermocline temperatures refer to an overall deep and stable thermocline. The meridional and zonal gradients in sea-surface and subsurface ocean propertieswithin the West Pacific Warm Pool reveal a pronounced change after 1.5 Ma, leading to a more southward position of the warm South Pacific Convergence Zone between ~1.35-0.9 Ma and ~0.75-0.5 Ma. Synchronous to the changes in the upper ocean, the deeper water masses experienced high amplitude variations in temperature, most prominently since ~1.5 Ma. This and the dynamically changing thermocline were most likely associated to the impact of southern- sourced mode waters, which might have developed coincidently with the emergence of the East Pacific Cold Tongue and high latitude sea-surface cooling.
    Keywords: Manihiki Plateau; Mg/Ca ratios; Oxygen isotopes; West Pacific Warm Pool
    Type: Dataset
    Format: application/zip, 5 datasets
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