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  • 2010-2014  (3)
  • 2000-2004  (7)
  • 1980-1984  (7)
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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Climatic changes. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (480 pages)
    Edition: 1st ed.
    ISBN: 9783662049655
    DDC: 551.69163/1
    Language: English
    Note: Climate Development and History of the North Atlantic Realm -- Copyright -- Preface -- Contents -- Climate History and the Great Geophysical Experiment -- Towards a History of Ideas on Anthropogenic Climate Change -- Climate Dynamics of the North Atlantic and NW-Europe: An Observation-Based Overview -- Holocene Climate Variability on Centennial-to-Millennial Time Scales: 1. Climate Records from the North-Atlantic Realm -- Holocene Climate Variability on Centennial-to-Millennial Time Scales: 2. Internal and Forced Oscillations as Possible Causes -- Solar Forcing of Climate Change in Recent Millennia -- Times of Quiet, Times of Agitation: Sverdrup's Conjecture and the Bermuda Coral Record -- A Case for Climate Cycles: Orbit, Sun and Moon -- Tracing Climate-Variability: The Search for Climate Dynamics on Decadal to Millennial Time Scales -- Holocene Climate and Past Volcanism: Greenland - Northern Europe -- Holocene Climate Evolution of the North Atlantic Ocean and the Nordic Seas - a Synthesis of New Results -- Holocene Climatic History of Northern Europe - the Evidence from Lake Deposits -- Climate Changes During the Holocene Recorded by Lakes from Europe -- The Post-Glacial Evolution of the Baltic Sea -- Holocene Climatic History of Northern Europe as Recorded by Vegetation Changes: Possible Influences Upon Human Activity -- Late Glacial and Holocene Glacier Fluctuations and Climatic Variations in Southern Norway -- Holocene Palaeoenvironmental Changes in North-West Europe: Climatic Implications and the Human Dimension -- Landscape Development and Occupation History Along the Southern North Sea Coast -- Climatic Change in Northern Europe Over the Last Two Thousand Years and its Possible Influence on Human Activity -- Human Stature and Climate: The Impact of Past Climate on Living Standards -- Malaria Around the North Sea: A Survey. , Patterns of Climate in Central Europe Since Viking Times -- On the Holocene Water Balance in Central Europe and Several Historical Consequences -- Narrowest-Ring" Events in the Irish Oak Chronology: Uncertainties in Reconstructing Cause and Effect in Prehistory -- The Pleistocene and Holocene Development of the Southeastern North Sea Basin and Adjacent Coastal Areas -- Effects of Climate and Human Interventions on the Evolution of the Wadden Sea Depositional System (Southern North Sea) -- Historic Storms in the North Sea Area, an Assessment of the Storm Data, the Present Position of Research and the Prospects for Future Research -- Climate Variability and Historical NW European Fisheries -- Changes in Coastal Zone Ecosystems -- The Impact of Harmful Algal Blooms in Natural and Human-Modified Systems of Northern Europe -- Climate and Human Induced Impacts on the Coastal Zone of the Southern North Sea.
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  • 2
    Keywords: CD-ROM ; Benguelastrom ; Aufschlussbohrung ; Geschichte 1997
    Type of Medium: Electronic Resource
    Pages: 1 CD-ROM , Booklet (XVII, 103, 44 S.), 2 Faltbl. (User guide; Tab.) , 12 cm
    Series Statement: Proceedings of the Ocean Drilling Program 175.1997
    Language: English
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  • 3
    Keywords: Kongreß ; Aufsatzsammlung ; Konferenzschrift ; Geologie ; Event ; Geochronologie ; Historische Geologie ; Event-Stratigraphie ; Event ; Impakt ; Tektonik ; Vulkanismus
    Type of Medium: Book
    Pages: X, 431 S. , Ill., graph. Darst.
    ISBN: 3540127496 , 0387127496
    Series Statement: Physical, chemical, and earth sciences research report 5
    DDC: 550
    RVK:
    RVK:
    Language: English
    Note: Literaturangaben. - Mit 4 Fotografien, 48 Abb. u. 12 Tab
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  • 4
    In: Expedition Erde, Bremen : MARUM - Zentrum für Marine Umweltwissenschaften, 2010, (2010), Seite 304-315, 9783000307720
    In: year:2010
    In: pages:304-315
    Type of Medium: Article
    Pages: zahlr. Ill. (farb.), graph. Darst., Kt.
    Language: German
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  • 5
    In: Expedition Erde, Bremen : MARUM - Zentrum für Marine Umweltwissenschaften, 2010, (2010), Seite 316-325, 9783000307720
    In: year:2010
    In: pages:316-325
    Type of Medium: Article
    Pages: zahlr. Ill. (farb.), graph. Darst., Kt.
    Language: German
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  • 6
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    PANGAEA
    In:  Supplement to: Berger, Wolfgang H; Killingley, John S (1982): Box cores from the equatorial Pacific: 14C sedimentation rates and benthic mixing. Marine Geology, 45(1-2), 93-125, https://doi.org/10.1016/0025-3227(82)90182-7
    Publication Date: 2024-07-19
    Description: Carbon-14 determinations on box cores of calcareous ooze from the western and eastern equatorial Pacific suggest that patterns of mixed-layer ages, sedimentation rates, and mixed-layer thicknesses are controlled by gradients of carbonate dissolution and fertility, and by small-scale redeposition processes. Mixed-layer ages range from 3000 to 7000 years, with a mode between 4000 and 5000 years. Sedimentation rates range from 0.8 to 2.4 cm/1000 years. Mixed-layer depths, calculated according to the box model of mixing, range from 7 cm to 16 cm. Observed thicknesses are about one-fourth smaller than calculated ones.
    Type: dataset publication series
    Format: application/zip, 3 datasets
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  • 7
    Publication Date: 2024-07-19
    Description: An important discovery during Ocean Drilling Program Leg 175, when investigating the record of upwelling off Namibia, was the finding of a distinct Late Pliocene diatom maximum spanning the lower half of the Matuyama reversed polarity chron (MDM, Matuyama Diatom Maximum) and centered around 2.6-2.0 Ma. This maximum was observed at all sites off southwestern Africa between 20°S and 30°S, and is most strongly represented in sediments of Site 1084, off Lüderitz, Namibia. The MDM is characterized by high biogenic opal content, high numbers of diatom valves, and a diatom flora rich in Southern Ocean representatives (with Thalassiothrix antarctica forming diatom mats) as well as coastal upwelling components. Before MDM time, diatoms are rare until ca. 3.6 Ma. After the MDM, in the Pleistocene, the composition of the diatom flora points to increased importance of coastal upwelling toward the present, but is accompanied by a general decrease in opal and diatom deposition. Here we present a simple conceptual model as a first step in formalizing a possible forcing mechanism responsible for the record of opal deposition in the upwelling system off Namibia. The model takes into account Southern Ocean oceanography, and a link with deepwater circulation and deepwater nutrient chemistry which, in turn, are coupled to the evolution of North Atlantic Deep Water (NADW). The model proposes that between the MDM and the Mid-Pleistocene climate revolution, opal deposition off Namibia is not directly tied to glacial-interglacial fluctuations (as seen in the global d18O record), but that, instead, a strong deepwater link exists with increased NADW production (as seen in the deepwater d13C record) accounting for higher supply of silicate to the thermocline waters that feed the upwelling process. The opal record of Site 1084 shows affinity to eccentricity on the 400-kyr scale but not for the 100-kyr scale. This points toward long-term geologic processes for delivery of silica to the ocean.
    Keywords: 175-1084; Abundance estimate; AGE; Age, maximum/old; Age, minimum/young; Benguela Current, South Atlantic Ocean; Calculated, see reference(s); COMPCORE; Composite Core; Diatom abundance index; Index; Joides Resolution; Leg175; Ocean Drilling Program; ODP
    Type: dataset
    Format: text/tab-separated-values, 36 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Bonneau, M-C; Vergnaud-Grazzini, Colette; Berger, Wolfgang H (1980): Stable isotope fractionation and differential dissolution in recent planktonic foraminifera from Pacific box-cores. Oceanologica Acta, 3(3), 377-381
    Publication Date: 2024-07-23
    Description: Stable isotope analyses and scanning electron micrographs have been carried out on six planktonic forminifera species, Pulleniatina obliquiloculata, Globorotalia tumida, Sphaeroidinella dehiscens, Globigerinoides ruber, Globigerinoides sacculifer and Globigerinoides quadrilobatus from eleven box-cores taken at increasing depths in the equatorial Ontong-Java Plateau (Pacific). This allows us to describe the way dissolution affects the microstructures of the tests of the different species and to quantify the changes of isotopic composition. We may conclude that: 1) dissolution effects on test morphology and stable isotope compositions are species dependent, species with a similar habitat showing a similar trend; 2) the shallow water, thin-shelled species are the first to disappear: scanning electron microscope (SEM) work shows alteration of outer layers. Deep water, thick-shelled species are present in all samples: SEM work shows breakdown and disparition of inner layers; 3) for all species there is a similar trend towards increasing delta18O values with increasing water depths and increasing dissolution. This effect may be as high as 0.6 ‰ per thousand meters for Globorotalia tumida; 4) below the lysocline, around 3500 m, it appears that 13C/12C ratios slightly increase towards equilibrium values for thick shelled species: G. tumida, P. obliquiloculata and S. dehiscens. 14C dates and isotope stratigraphy of two box-cores show that all samples are recent in age, and exclude upward mixing of glacial deposits as an important factor.
    Keywords: BC; Box corer; DEPTH, sediment/rock; Elevation of event; ERDC; ERDC-079BX; ERDC-088BX; ERDC-092BX; ERDC-120BX; ERDC-123BX; ERDC-125BX; ERDC-128BX; ERDC-129BX; ERDC-131BX; ERDC-136BX; ERDC-141BX; Event label; Globigerinoides quadrilobatus, δ13C; Globigerinoides quadrilobatus, δ18O; Globigerinoides ruber, δ13C; Globigerinoides ruber, δ18O; Globigerinoides sacculifer, δ13C; Globigerinoides sacculifer, δ18O; Globorotalia tumida, δ13C; Globorotalia tumida, δ18O; Isotope ratio mass spectrometry; Latitude of event; Longitude of event; Pulleniatina obliquiloculata, δ13C; Pulleniatina obliquiloculata, δ18O; Sphaeroidinella dehiscens, δ13C; Sphaeroidinella dehiscens, δ18O; Thomas Washington
    Type: dataset
    Format: text/tab-separated-values, 92 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Anderson, Patricia A; Charles, Christopher D; Berger, Wolfgang H (2001): Walvis Paradox confirmed for the Early Quaternary at the Southern End of the Namibia upwelling system, ODP Site 10851. In: Wefer, G; Berger, WH; Richter, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 175, 1-31, https://doi.org/10.2973/odp.proc.sr.175.201.2001
    Publication Date: 2024-07-22
    Description: The Walvis Paradox states that opal accumulation fluctuates in counterphase to general productivity on Walvis Ridge, off northern Namibia. Sediments of early Quaternary age from Site 1085 (Cores 175-1085A-7H to 10H, off South Africa) were studied to check the phase relationships of general productivity and opal deposition in the region off the Oranje River, near the southern end of the Namibia upwelling system. The proxies used are delta18O of Cibicidoides wuellerstorfi, delta13C of C. wuellerstorfi, benthic foraminifers per gram (BF/g), Uvigerina spp. per gram (U/g), estimated diatom abundance (EDA) and sulfide and oxide aggregates (SOA) in the coarse fraction. EDA and BF/g are taken to indicate diatom and organic matter productivity, respectively. Oxygen isotopes were used to determine phase within the glacial-interglacial cycles. The phase relationships between the different proxies emerge when applying internal stacking methods. For Core 175-1085A-7H, five prescribed 41-k.y. cycles were combined into an average 41-k.y. cycle for the different indices. Productivity indices (BF/g and U/g) tend to follow delta18O in the accustomed manner (with glacial periods showing maximum productivity), but not EDA, whose maximum appears closer to interglacials, offset toward cooling. Thus, phase relationships are similar to those on Walvis Ridge, extending the Walvis Paradox to the southern end of the Namibia upwelling system for the early Quaternary. A tentative reconstruction of the phase of intensity of mixing is given, based on the two productivity indicators EDA and BF/g. Mixing is strongest during the glacial maximum.
    Keywords: 175-1085A; AGE; Age, minimum/young; Aggregates; Benguela Current, South Atlantic Ocean; Calculated, see reference(s); Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; Comment; Counting 〉250 µm fraction; Counting 150-250 µm fraction; DEPTH, sediment/rock; Depth, sediment revised; Depth, top/min; Diatom abundance; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Foraminifera, benthic; Joides Resolution; Leg175; Mass spectrometer Finnigan MAT 252; Ocean Drilling Program; ODP; Sample code/label; Sample ID; Size fraction 〉 0.063 mm, sand; Size fraction 〉 0.250 mm; Smear slide analysis; Uvigerina peregrina, δ13C; Uvigerina peregrina, δ18O; Uvigerina spp.; δ13C, carbonate; δ18O, carbonate
    Type: dataset
    Format: text/tab-separated-values, 3184 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Berger, Wolfgang H (2003): Climate future in a warming world: lessons from the ice ages. IEEE, Proccedings of the International Conference OCEANS 2003, MTS/IEEE Holland Enterprises, Escondido CA, 1, 404-408, https://doi.org/10.1109/OCEANS.2003.178603
    Publication Date: 2024-07-23
    Description: Global warming is real and has been with us for at least two decades. Questions arise regarding the response of the ocean to greenhouse forcing, including expectations for changes in ocean circulation, in uptake of excess carbon dioxide, and in upwelling activity. The large climate variations of the ice ages, within the last million years, offer the opportunity to study responses of the ocean to climate change. A histogram of sealevel positions for the last 700,000 years (based on a new d/sup 18/O stratigraphy here compiled) shows that the present is near the margin of the range of fluctuations, with only 6 percent of positions indicating a warmer climate. Thus, the future will be largely outside of experience with regard to fluctuations of the recent geologic past. The same is true for greenhouse forcing. Our inability to explain sudden climate change in the past, including the rapid rise of carbon dioxide during deglaciation, and differences in ocean productivity between glacial and interglacial conditions, demonstrates a lack of understanding that makes predictions suspect. This is the lesson from ice age studies.
    Keywords: AGE; Calculated; δ18O, adjusted/corrected
    Type: dataset
    Format: text/tab-separated-values, 420 data points
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