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  • PANGAEA  (19)
  • Cham : Springer  (2)
  • Berlin, Heidelberg : Springer Berlin / Heidelberg  (1)
Document type
Keywords
Language
  • 1
    Keywords: Earth sciences ; Sedimentology ; Oceanography ; Coasts ; Geotechnical engineering ; Climate change ; Earth Sciences ; Ostsee ; Polen ; Küstenmorphologie ; Küstensediment ; Meeresspiegelschwankung ; Strandlinie ; Baltikum ; Deutschland ; Ostsee ; Meeresspiegel ; Zunahme ; Litoral ; Ostsee ; Eustatische Meeresspiegelschwankung ; Ostsee ; Polen ; Küstenmorphologie ; Küstensediment ; Meeresspiegelschwankung ; Strandlinie ; Baltikum ; Deutschland ; Ostsee ; Meeresspiegel ; Zunahme ; Litoral ; Ostsee ; Eustatische Meeresspiegelschwankung
    Description / Table of Contents: This book discusses sea-level and coastline changes. These topics are becoming increasingly important for populations living along the edge of the world’s oceans and seas, especially in areas where eustatic sea-level rise is superimposed on isostatic subsidence and storm-induced coastal erosion. This is the case at the southern and eastern Baltic Sea coast: in the south, glacio-isostatic subsidence enhances the effect of climate-induced sea-level rise and strong storm effects are causing a continuous retreat of the coast. On the eastern coast glacio-isostatic uplift compensates for eustatic sea-level rise, but storm-induced waves are responsible for permanent morphodynamic changes to the coastline. There is an increasing need for protection concepts for defense but also for the economic use of the different types of coastal zones. The elaboration of these management concepts can be facilitated through models that generate future projections of coastal developments in the light of modern climate change. This anthology comprises the results of the research project “Coastline Changes of the southern Baltic Sea - Past and future projection (CoPaF)” funded by the Polish Ministry of Science and Higher Education, which was run by a team of Estonian, German, Lithuanian, and Polish geoscientists and coastal engineers from 2010 to 2013 and overlapped with and complemented the work of COST Action SPLASHCOS supported by COST (European Cooperation in Science and Technology). As the southern and eastern Baltic serves as a natural laboratory for the investigation of coastal processes, the project’s findings contribute not only to the solution of regional problems in Baltic coastal research and engineering, but also to worldwide interests in description, modelling and parameterization of coastal processes and morphodynamics
    Type of Medium: Online Resource
    Pages: Online-Ressource (VIII, 388 p. 151 illus., 126 illus. in color, online resource)
    ISBN: 9783319498942
    Series Statement: Coastal Research Library 19
    Language: English
    Location Call Number Limitation Availability
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  • 2
    Keywords: Earth sciences ; Culture Study and teaching ; Coasts ; Archaeology ; Earth Sciences
    Description / Table of Contents: This book focuses on issues of method and interpretation in studies of submerged landscapes, concentrating on illustrations and case studies from around Europe with additional examples from other parts of the world. Such landscapes were once exposed as dry land during the low sea levels that prevailed during the glacial periods that occupied most of the past million years and provided extensive new territories for human exploitation. Their study today involves underwater investigation, using techniques and strategies which are clearly set out in these chapters. The underwater landscape provides a rich source of information about the archaeology of human settlement and long-term changes in environment, climate and sea-level. This book highlights how such information can be revealed and interpreted. The examples presented here and the focus on techniques make this book of worldwide relevance. Chapters describe examples of underwater archaeological investigation as well as collaboration with offshore industries and legal, management and training issues relating to underwater cultural heritage. Such studies point to the significance of this drowned landscape, and readers are invited to consider its human impact in terms of past settlement and population dispersal through palaeolandscape reconstruction and interpretation in relation to broader themes in human prehistory. This volume is based on work from COST Action SPLASHCOS, a four-year multi-disciplinary and multi-national research program supported by COST (European Cooperation in Science and Technology) and has something to benefit all those with an interest in the sea floor of the continental shelf and the archaeological and social impact of sea-level change, including archaeologists, marine scientists, geographers, cultural-heritage managers, commercial and governmental organisations, policy makers and interested members of the public
    Type of Medium: Online Resource
    Pages: Online-Ressource (XIII, 436 p. 218 illus., 168 illus. in color, online resource)
    ISBN: 9783319531601
    Series Statement: Coastal Research Library 20
    Language: English
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  • 3
    Online Resource
    Online Resource
    Berlin, Heidelberg : Springer Berlin / Heidelberg
    Keywords: Environmental protection ; Baltic Sea.. ; Geology ; Baltic Sea ; Electronic books
    Description / Table of Contents: The product of a special symposium held in 2008, this multidisciplinary volume is the first publication to take a holistic view of a range of aspects relating to the Baltic Sea Basin, including its genesis, structure, ongoing processes and utilisation.
    Type of Medium: Online Resource
    Pages: 1 online resource (444 pages)
    Edition: 1st ed.
    ISBN: 9783642172205
    Series Statement: Central and Eastern European Development Studies (CEEDES) Ser.
    DDC: 551.461334
    Language: English
    Note: Description based on publisher supplied metadata and other sources
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  • 4
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    PANGAEA
    In:  Supplement to: Lampe, Reinhard; Endtmann, Elisabeth; Janke, Wolfgang; Meyer, Hinrich; Lübke, Harald; Harff, Jan; Lemke, Wolfram (2005): A new relative sea-level curve for the Wismar Bay, N-German Baltic coast. Meyniana, 57, 5-35, https://doi.org/10.2312/meyniana.2005.57.5
    Publication Date: 2023-01-13
    Description: The Baltic coast of Mecklenburg-Vorpommern is located in the transition Zone between the region of Fennoscandian Uplift and the Central European Depression. In relation to the eustatic sea-level rise, the northeast coast shows a slower inundation, while for the southwestern area a faster transgression is indicated, which can be attributed to crustal movements. To determine the spatial and temporal differences since the onset of the Littorina Transgression, three relative sea-level curves have been established along a transect parallel to the gradient of upliftlsubsidence. The Wismar Bay area is one endpoint of the transect demonstrating today 10 Abb., 2 Tab. a relative sea-level rise of 1.4 mm/a. To determine the relative sea-level curve for the Wismar Bay, two sites were investigated on Rustwerder Spit (Poel) and Redentin. They provided reliable depth-age data, while the stratigraphy was additionally supported by lithological/geochemical, pollen, diatom and macrofossil data. Additional evidence was provided by archaeological submarine surveys and excavations. Comparing the new relative sea-level curve with a curve from the Vorpommern coast, it can be shown that for the period from 4000 cal BC until present, the differences between the two curves are caused by a constant neotectonic movement, while for the older periods an increasing isostatic component must be taken into account.
    Keywords: Age; Age, 14C AMS; Age, comment; Age, dated; Age, dated standard deviation; Age, error; Comment; Facies name/code; Sample code/label; Site; wismarbay; Wismar Bay, Baltic Sea, Germany; δ13C
    Type: Dataset
    Format: text/tab-separated-values, 1012 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Perner, Kerstin; Moros, Matthias; Lloyd, Jerry M; Kuijpers, Antoon; Telford, Richard J; Harff, Jan (2011): Centennial scale benthic foraminiferal record of late Holocene oceanographic variability in Disko Bugt, West Greenland. Quaternary Science Reviews, 30(19-20), 2815-2826, https://doi.org/10.1016/j.quascirev.2011.06.018
    Publication Date: 2024-02-02
    Description: A new centennial scale benthic foraminiferal record of late Holocene climate variability and oceanographic changes off West Greenland (Disko Bugt) highlights substantial subsurface water mass changes (e.g. temperature and salinity) of the West Greenland Current (WGC) over the past 3.6 ka BP. Benthic foraminifera reveal a long-term late Holocene cooling trend, which may be attributed to increased advection of cold, low-salinity water masses derived from the East Greenland Current (EGC). Cooling becomes most pronounced from c. 1.7 ka BP onwards. At this point the calcareous Atlantic benthic foraminiferal fauna decrease significantly and is replaced by an agglutinated Arctic fauna. Superimposed on this cooling trend, centennial scale variability in the WGC reveals a marked cold phase at c. 2.5 ka BP, which may correspond to the 2.7 ka BP cooling-event recorded in marine and terrestrial archives elsewhere in the North Atlantic region. A warm phase recognized at c. 1.8 ka BP is likely to correspond to the 'Roman Warm Period' and represents the warmest bottom water conditions. During the time period of the 'Medieval Climate Anomaly' we observe only a slight warming of the WGC. A progressively more dominant cold water contribution from the EGC on the WGC is documented by the prominent rise in abundance of agglutinated Arctic water species from 0.9 ka BP onwards. This cooling event culminates at c. 0.3 ka BP and represents the coldest episode of the 'Little Ice Age'. Gradually increased influence of cold, low-salinity water masses derived from the EGC may be linked to enhanced advection of Polar and Arctic water by the EGC. These changes are possibly associated with a reported shift in the large-scale North Atlantic Oscillation atmospheric circulation pattern towards a more frequent negative North Atlantic Oscillation mode during the late Holocene.
    Keywords: Age; AGE; Baffin Bay; Benthic foraminifera; Dendrochronological crossdating; East Greenland Current; Event label; GC; Gravity corer; GREENClim; Irminger; Islandiella norcrossi; Late Holocene; Maria S. Merian; MSM05/3; MSM05/3_343310-2-2; MSM05/3_343310-5-1; MUC; MultiCorer; NAO; Nonionellina labradorica; Percentage; Ratio; West Greenland Current
    Type: Dataset
    Format: text/tab-separated-values, 1938 data points
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  • 6
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-01-12
    Keywords: Calculated; Course; CT; DATE/TIME; HE244; HE244-track; Heincke; LATITUDE; LONGITUDE; Speed; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 3334 data points
    Location Call Number Limitation Availability
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  • 7
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    PANGAEA
    In:  Leibniz Institute for Baltic Sea Research, Warnemünde
    Publication Date: 2024-06-26
    Keywords: Baltic Sea System Study; BASYS; DEPTH, sediment/rock; Gotland Basin, Baltic Sea; Gravity corer (Kiel type); Greyscale value; Gulf of Riga; IOW211660-4; KOT99/97/02.1; Multi-Sensor Core Logger/colorscan/scion image; Petr Kottsov; SL
    Type: Dataset
    Format: text/tab-separated-values, 85493 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-06-26
    Description: Die Datenpublikation besteht aus den Korngrößenverteilungen von Oberflächensedimenten aus der südlichen Ostsee und umfaßt 7 Korngrößendatensätze gegliedert nach unterschiedlichen Klassen entsprechend der Methoden von Kolb und Koehn mit insgesamt 111025 Korngrößenwerten. Seit Beginn der fünfziger Jahre werden in Warnemünde systematisch Untersuchungen der Sedimente der westlichen Ostsee durchgeführt. Dabei werden die im Institut für Meereskunde der damaligen Akademie der Wissenschaften der DDR und davor im Seehydrographischen Dienst begonnenen Arbeiten am Institut für Ostseeforschung seit seiner Gründung 1992 fortgeführt. Aus Geheimhaltungsgründen standen die Daten vor 1989 für die wissenschaftliche Interpretation nur eingeschränkt zur Verfügung. Um auch diese 'Altdaten' der freien Forschung zugänglich zu machen, wurde 1994-1996 vom BMFT ein Forschungsprojekt gefördert (03F0079A), das die Erschließung und Publikation dieser teilweise kodierten Daten für die Ostseeforschung zum Ziel hatte. Im Laufe des Projektes wurde ein Bearbeitungsschema für die Daten entwickelt, welches generell für das Management von geomarinen Daten am IOW genutzt werden soll.
    Keywords: Baltic Sea; Bottom grab (Peterson); BP; different cruises; DIVER; IOW10; IOW100; IOW1000; IOW10000; IOW100000; IOW100010; IOW100020; IOW100030; IOW100040; IOW100050; IOW100060; IOW100070; IOW100080; IOW100090; IOW10010; IOW100100; IOW100110; IOW100120; IOW100130; IOW100150; IOW100160; IOW100170; IOW100180; IOW100190; IOW10020; IOW100200; IOW100210; IOW100220; IOW100230; IOW100240; IOW100250; IOW100260; IOW100270; IOW100280; IOW100290; IOW10030; IOW100300; IOW100310; IOW100320; IOW100330; IOW100340; IOW100350; IOW100360; IOW100370; IOW100380; IOW100390; IOW10040; IOW100400; IOW100410; IOW100420; IOW100430; IOW100440; IOW100450; IOW100460; IOW100470; IOW100480; IOW100490; IOW10050; IOW100500; IOW100510; IOW100520; IOW100530; IOW100540; IOW100550; IOW100560; IOW100570; IOW100580; IOW100590; IOW10060; IOW100600; IOW100610; IOW100620; IOW100630; IOW100640; IOW100650; IOW100660; IOW100670; IOW100680; IOW100690; IOW10070; IOW100700; IOW100710; IOW100720; IOW100730; IOW100740; IOW100750; IOW100760; IOW100770; IOW100780; IOW100790; IOW10080; IOW100800; IOW100810; IOW100820; IOW100830; IOW100840; IOW100850; IOW100860; IOW100870; IOW100880; IOW100890; IOW10090; IOW100900; IOW100910; IOW100920; IOW100930; IOW100940; IOW100950; IOW100960; IOW100970; IOW100980; IOW100990; IOW1010; IOW10100; IOW101000; IOW101010; IOW101020; IOW101030; IOW101040; IOW101050; IOW101060; IOW101070; IOW101080; IOW101090; IOW10110; IOW101100; IOW101110; IOW101120; IOW101130; IOW101140; IOW101150; IOW101160; IOW101170; IOW101180; IOW10120; IOW101210; IOW101220; IOW101230; IOW101240; IOW101250; IOW101260; IOW101270; IOW10130; IOW10140; IOW10150; IOW101570; IOW101580; IOW10160; IOW10170; IOW10180; IOW10190; IOW1020; IOW10200; IOW10210; IOW10220; IOW10230; IOW102980; IOW102990; IOW1030; IOW10300; IOW103000; IOW103010; IOW103020; IOW103030; IOW103040; IOW103050; IOW103060; IOW103070; IOW103080; IOW103090; IOW10310; IOW103100; IOW103110; IOW103120; IOW103130; IOW103140; IOW103150; IOW103160; IOW103170; IOW103180; IOW103190; IOW10320; IOW103200; IOW103210; IOW103220; IOW103230; IOW103240; IOW103250; IOW103260; IOW103270; IOW103280; IOW103290; IOW10330; IOW103300; IOW103310; IOW103320; IOW103330; IOW103340; IOW103350; IOW103360; IOW103370; IOW103380; IOW103390; IOW10340; IOW103400; IOW103410; IOW103420; IOW103430; IOW103440; IOW103450; IOW103460; IOW103470; IOW103480; IOW103490; IOW10350; IOW103500; IOW103510; IOW103520; IOW103530; IOW103540; IOW103550; IOW103560; IOW103570; IOW103580; IOW103590; IOW10360; IOW103600; IOW103610; IOW103620; IOW103630; IOW103640; IOW103650; IOW103660; IOW103670; IOW103680; IOW103690; IOW10370; IOW103700; IOW103710; IOW103720; IOW103730; IOW103740; IOW103750; IOW103760; IOW103770; IOW103780; IOW103790; IOW10380; IOW103800; IOW103810; IOW103820; IOW103830; IOW103840; IOW103850; IOW103860; IOW103870; IOW103880; IOW103890; IOW10390; IOW103900; IOW103910; IOW103920; IOW103930; IOW103940; IOW103950; IOW103960; IOW103970; IOW103980; IOW103990; IOW1040; IOW10400; IOW104000; IOW104010; IOW104020; IOW104030; IOW104040; IOW104050; IOW104060; IOW104070; IOW104080; IOW104090; IOW10410; IOW104100; IOW104110; IOW104120; IOW104130; IOW104140; IOW104150; IOW104160; IOW104170; IOW104180; IOW104190; IOW10420; IOW104200; IOW104210; IOW104220; IOW104230; IOW104240; IOW104250; IOW104260; IOW104270; IOW104280; IOW104290; IOW10430; IOW104300; IOW104310; IOW104320; IOW104330; IOW104340; IOW104350; IOW104360; IOW104370; IOW104380; IOW104390; IOW10440; IOW104400; IOW104410; IOW104420; IOW104430; IOW104440; IOW104450; IOW104460; IOW104470; IOW104480; IOW104490; IOW10450; IOW104500; IOW104510; IOW104520; IOW104530; IOW104540; IOW104550; IOW104560; IOW104570; IOW104580; IOW104590; IOW10460; IOW104600; IOW104610; IOW104620; IOW104630; IOW104640; IOW104650; IOW104660; IOW104670; IOW104680; IOW104690; IOW10470; IOW104700; IOW104710; IOW104720; IOW104730; IOW104740; IOW104750; IOW104760; IOW104770; IOW104780; IOW104790; IOW10480; IOW104800; IOW104810; IOW104820; IOW104830; IOW104840; IOW104850; IOW104860; IOW104870; IOW104880; IOW104890; IOW10490; IOW104900; IOW104910; IOW104920; IOW104930; IOW104940; IOW104950; IOW104960; IOW104970; IOW104980; IOW104990; IOW1050; IOW10500; IOW105000; IOW105010; IOW105020; IOW105030; IOW105040; IOW105050; IOW105060; IOW105070; IOW105080; IOW105090; IOW10510; IOW105100; IOW105110; IOW105120; IOW105130; IOW105140; IOW105150; IOW105160; IOW105170; IOW105180; IOW105190; IOW10520; IOW105200; IOW105210; IOW105220; IOW105230; IOW105240; IOW105250; IOW105260; IOW105270; IOW105280; IOW105290; IOW10530; IOW105300; IOW105310; IOW105320; IOW105340; IOW105350; IOW105360; IOW105370; IOW105380; IOW105390; IOW10540; IOW105400; IOW105410; IOW105420; IOW105430; IOW105440; IOW105450; IOW105460; IOW105470; IOW105480; IOW105490; IOW10550; IOW105500; IOW105510; IOW105520; IOW105530; IOW105540; IOW105550; IOW105560; IOW105570; IOW105580; IOW105590; IOW10560; IOW105600; IOW105610; IOW105620; IOW105630; IOW105640; IOW105650; IOW105660; IOW105670; IOW105680; IOW105690; IOW10570; IOW105700; IOW105710; IOW105720; IOW105730; IOW105740; IOW105750; IOW105760; IOW105770; IOW105780; IOW10580; IOW105800; IOW105810; IOW105820; IOW105830; IOW105840; IOW105850; IOW105860; IOW105870; IOW105880; IOW105890; IOW10590; IOW105900; IOW105910; IOW105920; IOW105930; IOW105940; IOW105950; IOW105960; IOW105970; IOW105980; IOW105990; IOW1060; IOW10600; IOW106000; IOW106010; IOW106020; IOW106030; IOW106040; IOW106050; IOW106060; IOW106070; IOW106080; IOW106090; IOW10610; IOW106100; IOW106110; IOW106120; IOW106130; IOW106140; IOW106150; IOW106160; IOW106170; IOW106180; IOW106190; IOW10620; IOW106200; IOW106210; IOW106220; IOW106230; IOW106240; IOW106250; IOW106260; IOW106270; IOW106280; IOW106290; IOW10630; IOW106300; IOW106310; IOW106320; IOW106330; IOW106340; IOW106350; IOW106360; IOW106370; IOW106380; IOW106390; IOW10640; IOW106400; IOW106410; IOW106420; IOW106430; IOW106440; IOW106450; IOW106460; IOW106470; IOW106480; IOW106490; IOW10650; IOW106500; IOW106540; IOW106550; IOW106560; IOW106570; IOW106580; IOW106590; IOW10660; IOW106600; IOW106610; IOW106620; IOW106640; IOW106650; IOW106660; IOW106670; IOW106680; IOW106690; IOW10670; IOW106700; IOW106710; IOW106720; IOW106730; IOW106740; IOW106750; IOW106760; IOW106770; IOW106780; IOW106790; IOW10680; IOW106800; IOW106810; IOW106820; IOW106830; IOW106840; IOW106850; IOW106860; IOW106870; IOW106880; IOW106890; IOW10690; IOW106900; IOW106910; IOW106920; IOW106930; IOW106940; IOW106950; IOW106960; IOW106970; IOW106980; IOW106990; IOW1070; IOW10700; IOW107000; IOW107010; IOW107020; IOW107030; IOW107040; IOW107050; IOW107060; IOW107070; IOW107080; IOW107090; IOW10710; IOW107100; IOW107110; IOW107120; IOW107130; IOW107140; IOW107150; IOW107160; IOW107170; IOW107180; IOW107190; IOW10720; IOW107200; IOW107210; IOW107220; IOW107230; IOW107240; IOW107250; IOW107260; IOW107270; IOW107280; IOW107290; IOW10730; IOW107300; IOW107310; IOW107320; IOW107330; IOW107340; IOW107350; IOW107360; IOW107370; IOW107380; IOW107390; IOW10740; IOW107400; IOW107410; IOW107420; IOW107440; IOW10750; IOW107530; IOW107540; IOW107550; IOW107560; IOW107570; IOW107580; IOW107590; IOW10760; IOW107600; IOW107610; IOW107620; IOW107630; IOW107640; IOW107650; IOW107660; IOW107670; IOW107680; IOW107690; IOW10770; IOW107700; IOW107710; IOW107720; IOW107730; IOW107740; IOW107750; IOW107760; IOW107770; IOW107780; IOW107790; IOW10780; IOW107810; IOW107830; IOW107850; IOW107870; IOW107880; IOW107890; IOW10790; IOW107900; IOW107910; IOW107920; IOW107930; IOW107940; IOW107950; IOW107960; IOW107970; IOW107980; IOW107990; IOW1080; IOW10800; IOW108000; IOW108010; IOW108020; IOW108030; IOW108040; IOW10810; IOW108150; IOW108160; IOW108170; IOW108180; IOW108190; IOW10820; IOW108200; IOW108210; IOW108220; IOW108230; IOW108240; IOW108250; IOW108260; IOW108270; IOW108280; IOW108290; IOW10830; IOW108300; IOW108310; IOW108320; IOW108330; IOW108340; IOW108350; IOW108370; IOW108390; IOW10840; IOW108410; IOW108430;
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 9
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    PANGAEA
    In:  Leibniz Institute for Baltic Sea Research, Warnemünde
    Publication Date: 2024-06-26
    Keywords: Baltic Sea System Study; BASYS; Bornholm Basin, Baltic Sea; DEPTH, sediment/rock; Gravity corer (Kiel type); Greyscale value; IOW211630-8; KOT99/97/02.1; Multi-Sensor Core Logger/colorscan/scion image; Petr Kottsov; SL
    Type: Dataset
    Format: text/tab-separated-values, 105252 data points
    Location Call Number Limitation Availability
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  • 10
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    PANGAEA
    In:  Leibniz Institute for Baltic Sea Research, Warnemünde
    Publication Date: 2024-06-26
    Keywords: Baltic Sea System Study; BASYS; Bornholm Basin, Baltic Sea; DEPTH, sediment/rock; Gravity corer (Kiel type); Greyscale value; IOW211610-3; KOT99/97/02.1; Multi-Sensor Core Logger/colorscan/scion image; Petr Kottsov; SL
    Type: Dataset
    Format: text/tab-separated-values, 65063 data points
    Location Call Number Limitation Availability
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