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2019, Fund des Monats (Online)
Die vorgeschichtlichen Burgen Sachsen-Anhalts waren zu ihrer Zeit mächtige Festungen, oft dicht bevölkert und sicher politisch bedeutend. Da aber ihre einst mächtigen Wälle ausschließlich aus Holz und Erde errichtet wurden, ihre Gräben in den anstehenden Boden eingetieft waren und ihre Innenbebauung aus verputzten Holzhäusern bestand, sind die Reste dieser Burgwälle heute meist nur noch anhand von leichten Unebenheiten im Gelände zu erkennen. Sie werden daher oft nur vom archäologisch geschulten Auge erkannt und sonst kaum beachtet. Doch sie sind für uns wichtige Zeugnisse der überraschend komplexen Gesellschaften in der fernen Vergangenheit. So waren sie insbesondere in Sachsen-Anhalt fast stadtartige Zentren, die den Reichtum des Landes kontrollierten und verteidigten. Eine der bedeutenden Burgen der Zeit zwischen 1000 und 500 v. Chr. liegt direkt östlich der Altstadt von Kemberg, Landkreis Wittenberg...
2018 •
2024 •
Im Nordharz konnte kürzlich eine DDR-zeitliche Jagdanlage, die dem Schwarzwildfang diente, dokumentiert werden. Dieser Saufang stellt in der östlichen Harzregion eine jagdhistorische Besonderheit dar und ist dort ein bislang singuläres Objekt.
2019 •
Die komplette Publikation "Aufgedeckt" finden Sie unter: http://www.blfd.bayern.de/medien/publikation-aufgedeckt_2019.pdf
Entstehung der Bandkeramik in Nordwestungarn durch religiöse Protestbewegung innerhalb der Starcevokultur (neue Idole, neuen Haus- und Gemeinschaftsformen). Ausbreitung nach Westen durch Konkurrenz der neu gegründeten Klans. Akkulturation der einheimischen Mesolithiker (Silextradition). Mitwirkung der La Hoguette-Kultur bei der Neolithisierung. Schwanfeld als Beispiel eine ältestbandkeramischen Hofplatzstruktur. Idole und Ahnenkult.
2018 •
Zwischen Italien und Skandinavien – Der hallstattzeitliche Bronzegefäßfund aus dem Schinderfilz-Moor bei Uffing a. Staffelsee, Oberbayern
Metzner Nebelsick Nebelsick Zwischen Italien und Skandinavien – Der hallstattzeitliche Bronzegefäßfund aus dem Schinderfilz-Moor bei Uffing a. Staffelsee, Oberbayern Ber Bay Bodendenk 62 2021 397 426Two bronze vessels, a cordoned cist and a cauldron were found in a raised bog called the Schinderfilzmoos near Uffing, Upper Bavaria, in 1865. The best parallels of the type 1 cist belong to the Certosa group focussed on and probably made in Bologna and dated between c. 510 and 380 BC, focusing on the HaD3 period. The cauldron can be assigned to the type Hallstatt was in use at the close of the Hallstatt Period. Comparative finds make it likely that the two bronze vessels, which also have a uniform patina, were originally deposited together in the bog in or shortly after Ha D3. The Schinderfilzmoos near Uffing lies in one of the wealthiest find-scapes of the southern Bavarian Hallstatt period facing the entrance to the crucial Alpine Pass conduit Loisach- Brenner-Eisack-Etsch that connects Bavaria to Italy. Moreover, the bog is embedded in a Landscape characterised by rich Barrows dating between Ha D1-D3, many incorporating sets of bronze vessels. Interestingly, however, this find has an unusual aspect. It is one of the few water/bog hoards that only multi-component vessel-hoard in the western Hallstatt Region. Typically, bronze vessels are mainly deposited in wet contexts in western and northern Europe. There is, however, evidence for metal vessel hoards, mostly incorporating cordoned cists and found in wet sediments or peat in an area stretching from western Hungary over Moravia, western Poland to southern Sweden dating to the late 7th to 5th centuries BC. In summary, the remarkable fact can be established that the community depositing the two bronze vessels in the Schinderfilzmoos followed a sacrificial practice characteristic of eastern Central and Northern Europe. This convergence is no coincidence is suggested by the intensive exchange between eastern and north-eastern Hallstatt groups (the latter also called the Lusatian culture) with the southern German communities, demonstrated in the younger and late Hallstatt period. The reasons why a southern Bavarian community in the late Hallstatt or early Latène period decided to adopt a foreign custom of material sacrifice and to establish a vessel depot in the raised bog near Uffing were certainly complex. One crucial motivation may have been the cultural-geographical border location of the site in the immediate vicinity of the most important Alpine pass for southern Bavaria. Most scholars agree that the intentional sinking of artefacts in water bodies and bogs practised by many prehistoric communities in Europe was linked to the liquid substrate's perceived liminality and inherent ambiguity. Wet and damp contexts were used as a medium to communicate with the other world. This was a complex action associated with the finality of an expression of value and therefore led to the memorisation, denotation and eventual narrative contextualisation of even these most ephemeral of landscape components. This is especially true for moors, which embody an obvious natural boundary situation. Situlae/cists and cauldrons play a key role in procession and symposium based rituals of the late Hallstatt elite. It can be assumed that the laying down of the ribbed cist and cauldron in the Schinderfilzmoos was involved in similarly complex rites.
K o n r a d T h e i s s V e r l a g D a r m s t a d t N a c h r i c h t e n a u s N i e d e r s a c h s e n s U r g e s c h i c h t e 8 6 , 2 0 1 7, 1 1 – 3 3 Zusammenfassung In den Spätsommermonaten im Jahr 2016 und 2017 wurden auf dem Fundplatz Hunte 3 Forschungsgrabungen durchgeführt. Hunte 3 (= Damme FStNr. 113) liegt am nördlichen Ende des Dümmer Sees in Niedersachsen. Die Ausgrabungen wurden mit der Unterstützung von Studenten der Universitäten Hamburg, Berlin und Bremen durchgeführt. Die bisherigen Informationen zu Hunte 3 gehen vor allem auf die Aktivität H. Reinerths zurück, der den Feuchtbodenfundplatz im Jahre 1940 mit einem Probeloch untersucht hatte. Die jüngsten Ausgrabungen führten zur Entdeckung eines frühneolithischen Fundhorizontes. Während die Flint-artefakte noch mesolithische Traditionen erkennen lassen, weisen wenige verzierte Keramikfragmente in den Horizont der Swifterbant-Kultur. Hierzu passen auch die 14 C-Daten. Das Spektrum der Tierknochen umfasst so-wohl Haus-als auch Wildtiere. Leider waren kaum botanische Reste oder andere organische Funde erhalten. Zusammen mit der südlich des Dümmers gelegenen Moorfundstelle Hüde 1 und dem westlich des Dümmers im Campemoor entdeckten Bohlenweg Pr 31 deuten die Neufunde an, dass das Dümmerbecken für die Menschen der Swifterbant-Kultur eine gewisse Anziehungskraft hatte. Leider hat die Erhaltung der Feuchtbodenfundstelle unter der vorausgehenden Entwässerung und Jahrzehnte langen Nutzung als Ackerfläche stark gelitten. Tiefe Trockenrisse durchziehen die Seeablagerungen unter der Fundstelle. Über der Fundstelle sind Teile der schützen-den Deckschichten verschwunden. Abstract In the late summer months of 2016 and 2017 two research excavations were carried out on the site Hunte 3. Hunte 3 (= Damme FStNr. 113) is located north of Lake Dümmer in Lower Saxony. The excavations were carried out with the help of students of the Universities of Hamburg, Berlin and Bremen. Previous information about Hunte 3 goes back mainly to the activities of H. Reinerth, who had examined the wetland site in 1940 with a trial hole. The recent excavations have led to the discovery of an early Neolithic occupation layer. While the flint artefacts still seem to reveal Mesolithic traditions, a few decorated ceramic fragments point into the horizon of the Swifterbant culture. The 14 C data also fits this purpose. The spectrum of animal bones includes both domestic and wild animals. Unfortunately, hardly any botanical remains or other organic finds were preserved. Together with the peatland site Hüde 1 at the south of the Dümmer Lake and the trackway Pr 31, discovered at the western Area near the Dümmer Lake in the Campemoor, the new finds indicate, that the Dümmer Area had a certain appeal for the people of the Swifterbant culture. Unfortunately, the conservation of the wetland site under the previous drainage and decades of use as arable land has suffered greatly. Deep dry cracks run through the lake deposits below the site Hunte 3. Former protective soil layers above the excavated occupation layer have disappeared today.
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