Forschungsliteratur: Archäologie

Auf dieser Seite finden Sie eine Sammlung von Links zu wissenschaftlichen Veröffentlichungen, die für dieses Projekt relevant sind oder die dazu beitragen können, ein tieferes exemplarisches Verständnis über die Prozesse und Umstände zu erlangen, welche möglicherweise in einem Zusammenhang mit der hier vorgestellten Neuinterpretation der Germania Magna stehen. Dabei handelt es sich um Veröffentlichungen unterschiedlicher Forschungsbereiche.

Die Sammlung umfasst:

• Primärliteratur: Wissenschaftliche Veröffentlichungen, die die Ergebnisse neuer Forschung präsentieren.
• Sekundärliteratur: Wissenschaftliche Veröffentlichungen, die die Primärliteratur zusammenfassen, analysieren oder interpretieren.
• Vergleichende Literatur: Veröffentlichungen, die Ihnen exemplarisch ähnliche Prozesse und Umstände in anderen Kontexten aufzeigen.
• Weitere Ressourcen: Links zu Websites, Datenbanken und anderen Ressourcen, die für die Neuinterpretation relevant sein können.

Die folgenden Publikationen sollen dabei helfen, bestimmte Fragestellungen exemplarisch zu beantworten, welche in einem möglichen Zusammenhang mit den notwendigen Prozessen und Vorgängen stehen, die für eine umfangreiche Landschaftstransformation erforderlich sind. Hierzu zählen beispielsweise Überlegungen über tektonische Bruchereignisse und Rift-Systeme, mit entsprechender Auswirkung auf maritime Rutschungsereignisse und die Entstehung neuer Sedimentationsbecken.

What caused terrestrial dust loading and climate downturns between A.D. 533 and 540?

19. August 20247. August 2024 von Sven Mildner

DOI https://doi.org/10.1130/2014.2505(23) Abstract Sn-rich particles, Ni-rich particles, and cosmic spherules are found together at four discrete stratigraphic levels within the 362–360 m depth interval of the Greenland Ice Sheet Project 2 (GISP2) ice core (72.6°N, 38.5°W, elevation: 3203 m). Using a previously derived calendar-year time scale, these particles span a time of increased dust loading of Earth’s atmosphere between A.D. 533 and 540. The Sn-rich and Ni-rich particles contain an average of 10–11 wt% C. Their high C contents coupled with local enrichments in the volatile elements I, Zn, Cu, and Xe suggest a cometary source for the dust. The late spring timing of extraterrestrial input best matches the Eta Aquarid meteor shower associated with comet 1P/Halley. An increased flux of cometary dust might explain a modest climate downturn in A.D. 533. Both cometary dust and volcanic sulfate probably contributed to the profound global dimming during A.D. 536 and 537 … WeiterlesenWhat caused terrestrial dust loading and climate downturns between A.D. 533 and 540?

Continental-scale temperature variability during the past two millennia

19. August 202410. April 2024 von Sven Mildner

DOI https://doi.org/10.1038/ngeo1797 Abstract Past global climate changes had strong regional expression. To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to two millennia. The most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multi-decadal to centennial scales, temperature variability shows distinctly different regional patterns, with more similarity within each hemisphere than between them. There were no globally synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period or Little Ice Age, but all reconstructions show generally cold conditions between AD 1580 and 1880, punctuated in some regions by warm decades during the eighteenth century. The transition to these colder conditions occurred earlier in the Arctic, Europe and Asia than in North America or the Southern Hemisphere regions. Recent warming reversed the long-term cooling; during the period AD 1971–2000, … WeiterlesenContinental-scale temperature variability during the past two millennia

A submerged Stone Age hunting architecture from the Western Baltic Sea

19. August 202425. März 2024 von Sven Mildner

DOI https://doi.org/10.1073/pnas.2312008121 Abstract The Baltic Sea basins, some of which only submerged in the mid-Holocene, preserve Stone Age structures that did not survive on land. Yet, the discovery of these features is challenging and requires cross-disciplinary approaches between archeology and marine geosciences. Here, we combine shipborne and autonomousunderwater vehicle hydroacoustic data with up to a centimeter range resolution, sedimentological samples, and optical images to explore a Stone Age megastructure located in 21 m water depth in the Bay of Mecklenburg, Germany. The structure is made of 1,673 individual stones which are usually less than 1 m in height, placed side by side over a distance of 971 m in a way that argues against a natural origin by glacial transport or ice push ridges. Running adjacent to the sunken shoreline of a paleolake (or bog), whose youngest phase was dated to 9,143 ±36 ka B.P., the stonewall was likely used … WeiterlesenA submerged Stone Age hunting architecture from the Western Baltic Sea

Abrupt Holocene ice loss due to thinning and ungrounding in the Weddell Sea Embayment

19. August 202422. März 2024 von Sven Mildner

DOI https://doi.org/10.1038/s41561-024-01375-8 Abstract The extent of grounded ice and buttressing by the Ronne Ice Shelf, which provides resistance to the outflow of ice streams, moderate West Antarctic Ice Sheet stability. During the Last Glacial Maximum, the ice sheet advanced and was grounded near the Weddell Sea continental shelf break. The timing of subsequent ice sheet retreat and the relative roles of ice shelf buttressing and grounding line changes remain unresolved. Here we use an ice core record from grounded ice at Skytrain Ice Rise to constrain the timing and speed of early Holocene ice sheet retreat. Measured δ18O and total air content suggest that the surface elevation of Skytrain Ice Rise decreased by about 450 m between 8.2 and 8.0 kyr before 1950 CE (±0.13 kyr). We attribute this elevation change to dynamic thinning due to flow changes induced by the ungrounding of ice in the area. Ice core sodium concentrations suggest that the ice front … WeiterlesenAbrupt Holocene ice loss due to thinning and ungrounding in the Weddell Sea Embayment

One Thousand Centuries of Climatic Record from Camp Century on the Greenland Ice Sheet

19. August 202420. März 2024 von Sven Mildner

DOI http://dx.doi.org/10.1126/science.166.3903.377 Abstract A correlation of time with depth has been evaluated for the Camp Century, Greenland, 1390 meter deep ice core. Oxygen isotopes in approximately 1600 samples throughout the core have been analyzed. Long-term variations in the isotopic composition of the ice reflect the climatic changes during the past nearly 100,000 years. Climatic oscillations with periods of 120, 940, and 13,000 years are observed. W. Dansgaard et al. ,One Thousand Centuries of Climatic Record from Camp Century on the Greenland Ice Sheet. Science166, 377-381 (1969). DOI: 10.1126/science.166.3903.377

The catastrophic final flooding of Doggerland by the Storegga Slide tsunami

19. August 202420. März 2024 von Sven Mildner

DOI https://doi.org/10.4312/dp.35.1 Abstract Around 8200 calBP, large parts of the now submerged North Sea continental shelf (‘Doggerland’) were catastrophically flooded by the Storegga Slide tsunami, one of the largest tsunamis known for the Holocene, which was generated on the Norwegian coastal margin by a submarine landslide. In the present paper, we derive a precise calendric date for the Storegga Slide tsunami, use this date for reconstruction of contemporary coastlines in the North Sea in relation to rapidly rising sea-levels, and discuss the potential effects of the tsunami on the contemporaneous Mesolithic population. One main result of this study is an unexpectedly high tsunami impact assigned to the western regions of Jutland. Weninger, B., Schulting, R., Bradtmöller, M., Clare, L., Collard, M., Edinborough, K., Hilpert, J., Jöris, O., Niekus, M., Rohling, E. J., & Wagner, B. (2008). The catastrophic final flooding of Doggerland by the Storegga Slide tsunami. Documenta Praehistorica, 35, 1-24. https://doi.org/10.4312/dp.35.1

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