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  • 1
    Type of Medium: Book
    Pages: 173 S. , graph. Darst., Kt.
    Series Statement: Berichte zur Polarforschung 74
    DDC: 551.46/4
    Language: German
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  • 2
    Book
    Book
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    Keywords: Forschungsbericht ; Meeresgeologie ; Geophysik ; Polarstern
    Type of Medium: Book
    Pages: 133 S. , graph. Darst., Kt.
    Series Statement: Berichte zur Polarforschung 163
    DDC: 551.46/4
    Language: German , English
    Note: Beitr. teilw. dt., teilw. engl
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  • 3
    Keywords: Report ; Scotia Sea ; Meereskunde ; Polarstern ; Exkursion
    Type of Medium: Book
    Pages: 167 S. , graph. Darst., Kt.
    Series Statement: Berichte zur Polarforschung 131
    Language: German
    Note: Literaturverz. S. 109 - 112 , Intermediärsprache: Englisch
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  • 4
    Online Resource
    Online Resource
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    Keywords: Forschungsbericht ; Beringmeer ; Pazifischer Ozean Nord ; Biogeochemie ; Paläoozeanographie
    Type of Medium: Online Resource
    Pages: Online-Ressource
    Series Statement: Berichte zur Polar- und Meeresforschung 643
    Language: English
    Note: Förderkennzeichen BMBF 03G0202A
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  • 5
    Online Resource
    Online Resource
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    Description / Table of Contents: Schwerpunkt der Expedition ANT-XXVI/2, die Polarstern über eine Distanz von 9.757 nm zum ersten Mal über den gesamten polaren Südpazifik nach Neuseeland gebracht hat, sind marin-geowissenschaftliche Probennahmen, die entlang der gesamten Fahrtroute durch bathymetrische (HYDROSWEEP) und sedimentechographische (PARASOUND) Vermessungen über 9.273 nm begleitet worden sind...Neben paläozeanographisch orientierten Probennahmen galten die geowissenschaftlichen Arbeiten auch der weiteren Erkundung und Dokumentation des Eltanin-Asteroideneinschlages vor 2,5 Mio. Jahre im Bereich des Freeden Seamounts. Darüber hinaus konnten durch Kombination von Sedimentprobennahme mit seismischen, bathymetrischen und sedimentechographischen Surveys Voruntersuchungen (pre-site survey) durchgeführt werden, die für die weitere Beantragung des Bohrvorschlages 625 - full (Cenozoic Southern Ocean Pacific, CESOP) (Gersonde et al., 2008) im Rahmen von Integrated Ocean Drilling Program (IODP) benötigt werden...Die Auswertung des Daten- und Probenmaterials erfolgt in nationaler und internationaler Zusammenarbeit im Rahmen des AWI-Programms PACES, der Programme des DFG-Forschungszentrums The Ocean in the Earth System und der EU-ProjektesPast4Future, des Integrated Ocean Drilling Program (IODP) und einer Reihe von einzelnen nationalen (DFG) und internationalen Projekten.
    Type of Medium: Online Resource
    Pages: Online-Ressource
    Series Statement: Berichte zur Polar- und Meeresforschung 632
    Language: English
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  • 6
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    ELSEVIER SCIENCE BV
    In:  EPIC3Palaeogeography Palaeoclimatology Palaeoecology, ELSEVIER SCIENCE BV, 414, pp. 1-19, ISSN: 0031-0182
    Publication Date: 2014-09-04
    Description: Here we present an improvement of paleotemperature reconstructions for the Southern Ocean by combining new diatom data from the Pacific sector with published Atlantic and Indian sector reference data. The statistical analysis of 336 surface sediment samples recovered from a wide area of Southern Ocean environments defines a supra-regional reference data set for quantitative summer sea surface temperature (SSST) estimations. In situ temperature measurements covering the time span from approx. 1900 to 1991 were used as reference instead of more recent time series of satellite-derived data, possibly biased by ocean warming. Different transfer function (TF) models for the Imbrie and Kipp Method (IKM), the Modern Analog Technique (MAT), Weighted Averaging (WA), and Weighted Averaging Partial Least Squares (WAPLS) were tested. Best performance for IKM was obtained using the D336 set with 29 diatom taxa and three factors, resulting in root mean square error of prediction (RMSEP) of 0.833°C for SSST. MAT estimates were best with six analogs resulting in the lowest RMSEP of 0.812°C. WAPLS applied to D336 resulted in a RMSEP of 0.782°C. WA performed less well, expressed by a RMSEP of 0.974°C. Furthermore, two subsets for the Atlantic (D151) and the Pacific sectors (D107) were applied with IKM to test for the advantages of localized TFs. IKM-D151 and IKM-D107 performed comparably good as IKM-D336, with RMSEP of 0.71°C and 0.68°C, respectively. Application of the augmented reference data sets on two Pleistocene sediment records from the Atlantic (PS1768-8) and Pacific (PS58/271-1) sectors led to the best performance of IKM with D336, expressed by high overall communalities (〉0.75) and fewer (PS1768-8) to no (PS58/271-1) no-analogs, compared to the regional data sets, proving IKM-D336 to deal better with higher assemblage variability. SSST estimates for both cores exhibit similar glacial/interglacial patterns for all four applied D336-based TF methods, with the best concordance between IKM and WAPLS.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev , info:eu-repo/semantics/article
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  • 7
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 8
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    ELSEVIER SCIENCE BV
    In:  EPIC3Earth and Planetary Science Letters, ELSEVIER SCIENCE BV, 369-37, pp. 86-97, ISSN: 0012-821X
    Publication Date: 2019-07-17
    Description: Boundary scavenging, or the enhanced removal of adsorption-prone elements from the ocean in areas of high particle flux, is an often cited, though not well-quantified, concept used to understand the oceanic distribution of many trace metals. Because 230Th and 231Pa are produced uniformly from uranium decay and removed differentially by scavenging, the process of boundary scavenging can bee lucidated by a more detailed knowledge of their water column distributions. To this end, filtered seawater was collected across the gradients in particle flux which span the subarctic Pacific: in the west during the Innovative North Pacific Experiment (INOPEX) and in the east along LineP. Lateral concentration gradients of dissolved 230Th are small throughout the subarcticPacific at 12 sites of variable particle flux. This contradicts the prediction of the traditional boundary scavenging model. A compilation of water column data from throughout the North Pacific reveals much larger lateral concentration gradients for 230Th between the subarctic North Pacific and subtropical gyre, over lateral gradients in scavenging intensity similar to those found within the subarctic. This reflects a biogeochemical-province aspect to scavenging. Upper water column distributions of 231Pa and 231Pa/230Th ratio are consistent with the influence of scavenging by biogenic opal, while deep waters (〉2.5 km) reveal an additional 231Pa sink possibly related to manganese oxides produced at continental margins or ridge crests.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 9
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    ELSEVIER SCIENCE BV
    In:  EPIC3Earth and Planetary Science Letters, ELSEVIER SCIENCE BV, 383, pp. 16-25, ISSN: 0012-821X
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 10
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    ELSEVIER SCIENCE BV
    In:  EPIC3Palaeogeography Palaeoclimatology Palaeoecology, ELSEVIER SCIENCE BV, 402, pp. 81-103, ISSN: 0031-0182
    Publication Date: 2014-05-08
    Description: In order to map the modern distribution of diatoms and to establish a reliable reference data set for paleoenvironmental reconstruction in the northern North Pacific, a new data set including the relative abundance of diatom species preserved in a total of 422 surface sediments was generated, which covers a broad range of environmental variables characteristic of the subarctic North Pacific, the Sea of Okhotsk and the Bering Sea between 30° and 70°N. The biogeographic distribution patterns as well as the preferences in sea surface temperature of 38 diatom species and species groups are documented. A Q-mode factor analysis yields a three-factor model representing assemblages associated with the Arctic, Subarctic and Subtropical water mass, indicating a close relationship between the diatom composition and the sea surface temperatures. The relative abundance pattern of 38 diatom species and species groups was statistically compared with nine environmental variables, i.e. the summer sea surface temperature and salinity, annual surface nutrient concentration (nitrate, phosphate, silicate), summer and winter mixed layer depth and summer and winter sea ice concentrations. Canonical Correspondence Analysis (CCA) and other analyses indicate 32 species and species groups have strong correspondence with the pattern of summer sea surface temperature. In addition, the total diatom flux data compiled from ten sediment traps reveal that the seasonal signals preserved in the surface sediments are mostly from spring through autumn. This close relationship between diatom composition and the summer sea surface temperature will be useful in deriving a transfer function in the subarctic North Pacific for the quantitative paleoceanographic and paleoenvironmental studies. The relative abundance of the sea ice indicator diatoms Fragilariopsis cylindrus and F. oceanica of 〉 20% in the diatom composition is used to represent the winter sea ice edge in the Bering Sea. The northern boundary of the distribution of F. doliolus in the open ocean is suggested to be an indicator of the Subarctic Front, while the abundance of Chaetoceros resting spores may indicate iron input from nearby continents and shelves and induced productivity events in the study area.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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