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  • 2025-2025  (1)
  • 2005-2009  (13)
  • 2008  (13)
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  • 1
    Keywords: Forschungsbericht ; Reisebericht ; Meteor ; Forschungsreise
    Type of Medium: Book
    Series Statement: Meteor-Berichte ...
    Language: German
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  • 2
    Publication Date: 2018-03-08
    Description: New Mg/Ca, Sr/Ca, and published stable oxygen isotope and 87Sr/86Sr data obtained on ostracods from gravity cores located on the northwestern Black Sea slope were used to infer changes in the Black Sea hydrology and water chemistry for the period between 30 to 8 ka B.P. (calibrated radiocarbon years). The period prior to 16.5 ka B.P. was characterized by stable conditions in all records until a distinct drop in δ18O values combined with a sharp increase in 87Sr/86Sr occurred between 16.5 and 14.8 ka B.P. This event is attributed to an increased runoff from the northern drainage area of the Black Sea between Heinrich Event 1 and the onset of the Bølling warm period. While the Mg/Ca and Sr/Ca records remained rather unaffected by this inflow; they show an abrupt rise with the onset of the Bølling/Allerød warm period. This rise was caused by calcite precipitation in the surface water, which led to a sudden increase of the Sr/Ca and Mg/Ca ratios of the Black Sea water. The stable oxygen isotopes also start to increase around 15 ka B.P., although in a more gradual manner, due to isotopically enriched meteoric precipitation. While Sr/Ca remains constant during the following interval of the Younger Dryas cold period, a decrease in the Mg/Ca ratio implies that the intermediate water masses of the Black Sea temporarily cooled by 1–2°C during the Younger Dryas. The 87Sr/86Sr values drop after the cessation of the water inflow at 15 ka B.P. to a lower level until the Younger Dryas, where they reach values similar to those observed during the Last Glacial Maximum. This might point to a potential outflow to the Mediterranean Sea via the Sea of Marmara during this period. The inflow of Mediterranean water started around 9.3 ka B.P., which is clearly detectable in the abruptly increasing Mg/Ca, Sr/Ca, and 87Sr/86Sr values. The accompanying increase in the δ18O record is less pronounced and would fit to an inflow lasting ∼100 a.
    Type: Article , PeerReviewed
    Format: text
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  • 3
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    In:  EPIC3Symposium on Eastern Boundary Upwelling Ecosystems: integrative and comparative approaches. 2-6 June 2008, Las Palmas de Gran Canaria, Spain.
    Publication Date: 2019-07-16
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 4
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 5
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 6
    Publication Date: 2024-02-02
    Keywords: Age, 14C AMS; Age, 14C calibrated; Age, dated; Age, dated standard deviation; Age, maximum/old; Age, minimum/young; Argentine Basin; Center for Marine Environmental Sciences; DEPTH, sediment/rock; GeoB6211-2; Gravity corer (Kiel type); M46/2; MARUM; Meteor (1986); Sample code/label; SL
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 7
    Publication Date: 2024-06-25
    Keywords: Age model; Age model, SPECMAP chronology, Imbrie et al. (1984); Brazil Basin; Calcium carbonate; Calculated; Calculated from mass/volume; Carbon, organic, total; Cibicides wuellerstorfi, δ13C; Density, dry bulk; Depth, composite; DEPTH, sediment/rock; Element analyser CHN; Element analyser CHN, LECO; GeoB; GeoB1117-3; Geosciences, University of Bremen; Giant box corer; GKG; Grain size, sieving/settling tube; Intercore correlation; M9/4; Mass spectrometer Finnigan MAT 251; Meteor (1986); Sand; Sedimentation rate; SFB261; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; Water content, wet mass
    Type: Dataset
    Format: text/tab-separated-values, 87 data points
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  • 8
    Publication Date: 2024-06-26
    Description: Die an Bord von FS METEOR durchgeführten sedimentphysikalischen Analysen des M 16/1 Kernmaterials aus verschiedenen Arealen des Guinea-, Angola-und Brasil-Beckens umfassen im einzelnen folgende Arbeiten: -Messungen der Kompressionswellengeschwindigkeit, -Messungen der elektrischen Leitfahigkeit, -Messungen der magnetischen Suszeptibilitat, -Beprobungen für palao-und gesteinsmagnetische Untersuchungen. Erstmalig wurde auf diesem Fahrtabschnitt eine Methode zur Messung der elektrischen Leitfahigkeit getestet, mit der Zielsetzung ein schnelles und effizientes Verfahren zur Bestimmung von Porositats-und Dichteprofilen der Sedimentkerne zu entwickeln. Abbildung 30 zeigt das Blockschaltbild des MeBaufbaus. Zur Messung an den Halbschalen der geöffneten Kerne in Abstanden von in der Regel 5 cm wurde eine Wenner-Anordnung verwendet. AIs Elektroden dienen vier Platindrähte (ø 0,6 mm), die im Abstand von 4 mm in einen Kunststoffstab (16 x 4 x 100 mm) eingegossen sind; er ist zur besseren Ankopplung im unteren, ins Sediment eingefiihrten Teil auf einen etwa dreieckigen Querschnitt abgeschrägt. Der Strom wird über die beiden äußeren Elektroden eingespeist. AIs Stromquelle dienen ein Funktionsgenerator und ein Stromkonstanter, die einen Rechteck-Wechselstrom von 330 Hz und 400 µA erzeugen. Über die beiden inneren Elektroden wird der Spannungsabfall im Sediment bestimmt. Die wesentlichen Gerätekomponenten sind dabei ein Differentialverstärker, ein phasenempfindlicher Detektor und ein Voltmeter.
    Keywords: Cardno Seamount; East Brazil Basin; GeoB; GeoB1405-6; GeoB1407-5; GeoB1408-2; GeoB1412-1; GeoB1413-4; GeoB1414-1; GeoB1415-2; GeoB1417-1; GeoB1419-2; GeoB1420-2; Geosciences, University of Bremen; Gravity corer (Kiel type); M16/1; Meteor (1986); Mid Atlantic Ridge; Northern Guinea Basin; SL; Southwest Guinea Basin; West Angola Basin
    Type: Dataset
    Format: application/zip, 10 datasets
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  • 9
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    PANGAEA
    In:  Supplement to: Salgueiro, Emilia; Voelker, Antje H L; Abrantes, Fatima F; Meggers, Helge; Pflaumann, Uwe; Loncaric, Neven; González-Álvarez, Raquel; Oliveira, Paulo; Bartels-Jonsdottir, Helga B; Moreno, João; Wefer, Gerold (2008): Planktonic foraminifera from modern sediments reflect upwelling patterns off Iberia: Insights from a regional transfer function. Marine Micropaleontology, 66(3-4), 135-164, https://doi.org/10.1016/j.marmicro.2007.09.003
    Publication Date: 2024-06-26
    Description: Quantitative and qualitative analyses of planktonic foraminiferal assemblages from 134 core-top sediment samples collected along the western Iberian margin were used to assess the latitudinal and longitudinal changes in surface water conditions and to calibrate a Sea Surface Temperature (SST) transfer function for this seasonal coastal upwelling region. Q-mode factor analysis performed on relative abundances yielded three factors that explain 96% of the total variance: factor 1 (50%) is exclusively defined by Globigerina bulloides, the most abundant and widespread species, and reflects the modern seasonal (May to September) coastal upwelling areas; factor 2 (32%) is dominated by Neogloboquadrina pachyderma (dextral) and Globorotalia inflata and seems to be associated with the Portugal Current, the descending branch of the North Atlantic Drift; factor 3 (14%) is defined by the tropical-sub-tropical species Globigerinoides ruber (white), Globigerinoides trilobus trilobus, and G. inflata and mirrors the influence of the winter-time eastern branch of the Azores Current. In conjunction with satellite-derived SST for summer and winter seasons integrated over an 18 year period the regional foraminiferal data set is used to calibrate a SST transfer function using Imbrie & Kipp, MAT and SIMMAX(ndw) techniques. Similar predicted errors (RMSEP), correlation coefficients, and residuals' deviation from SST estimated for both techniques were observed for both seasons. All techniques appear to underestimate SST off the southern Iberia margin, an area mainly occupied by warm waters where upwelling occurs only occasionally, and overestimate SST on the northern part of the west coast of the Iberia margin, where cold waters are present nearly all year round. The comparison of these regional calibrations with former Atlantic and North Atlantic calibrations for two cores, one of which is influenced by upwelling, reveals that the regional one attests more robust paleo-SSTs than for the other approaches.
    Keywords: BC; BCR; Box corer; Box corer (Reineck); GAP; GeoB9014-1; Giant box corer; GKG; Gravity corer (Kiel type); M39/1; M39/1_02-3; M39/1_03-2; M39/1_04-2; M39/1_16-2; M39/1_17-4; M39/1_21-5; M39/1_22-1; M39/1_22-3; M39/1_23-3; M39/1_29-6; M39/1_35-3; M39/1_58-1; M39/1_59-2; M39/1_70-1; M39/1_72-1; M39021-5; M39022-1; M39058-1; M39059-2; M39070-1; M39072-1; MARFLUX; Meteor (1986); MUC; MultiCorer; Multicorer with television; North Atlantic; off Portugal; PALEO 1; Portuguese Margin; POS200/10; POS200/10_1-2; POS200/10_3-1; POS200/10_5-1; POS200/10_5-2; POS287; POS287_05-1B; POS287_08-1B; POS287_13-1B; POS287_15-1B; POS287_19-1B; POS287_21-1B; POS287_26-1B; POS287_27-1B; POS287_28-1B; POS287_33-1B; POS287_34-1B; POS287_40-1B; POS287_41-1B; Poseidon; SL; SO10GK; SO11GK; SO175; SO75/3; SO75/3_13KG; SO75/3_15KG; SO75/3_25KG; SO75/3_30KG; SO75/3_33KG; SO75/3_9KG; SO7GK; SO83; SO83_10GK; SO83_11GK; SO83_7GK; SO83_9GK; SO9GK; Sonne; TVMUC
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 10
    Publication Date: 2024-06-26
    Keywords: Calculated from stable oxygen isotopes; Communality; DEPTH, sediment/rock; Dissimilarity index; Giant box corer; GKG; Globigerina bulloides, δ18O; Globigerinoides ruber white, δ18O; Globorotalia inflata, δ18O; M39/1; M39/1_22-1; M39022-1; Mass spectrometer Finnigan MAT 252; Meteor (1986); Modern analog technique (MAT); Modern analog technique (MAT), SIMMAX28, non-distance-weighted; Sea surface temperature, annual mean; Sea surface temperature, summer; Sea surface temperature, winter; Similarity index; Transfer function (Imbrie & Kipp, 1971, in Turekian, Yale Univ Press)
    Type: Dataset
    Format: text/tab-separated-values, 611 data points
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