Mobilität und soziale Dynamik in Südbayern und im Nordtiroler Inntal in der Urnenfelderzeit (13.-9. Jh. v. Chr.)

TP 4如临时报告所述，对TP 4进行了新的调整，以便将第一阶段讨论的科学专题扩展到Salzach-Inn-Donube地区。与Inn山谷上游Schwaz-Brixlegg矿区集水区的老Urnfield文化时期的情况类似，聚落建造似乎发生在Salzach山谷，从较年轻的时期开始，一直持续到Urnfield文化晚期(时期HaB1-HyB3，或公元前10世纪至9世纪)。虽然沉降过程仍然没有得到充分的调查，但墓地的新基础是独立的证据。墓地陈设显示出与下巴伐利亚多瑙河地区的密切相似之处。这提出了这样一种假设，即位于密特伯格地区附近的矿区应对这些联系负责。对选定墓葬清单的同位素分析将揭示这些交换接触是否发生在金属贸易过程中，包括迁移现象，或者是在没有移民长期存在的情况下，通过不同的迁移过程采用一种新的陶瓷风格。TP 5在公元前5世纪，弗里岑-桑泽诺文化(FSK)，其特征是几个参数(财产所有权、房屋建筑、铁技术、宗教观念)通过因-埃萨克-埃施通道在泰勒尔和特伦蒂诺南北发展为统一的文化。作为原因，讨论了人口群体的迁徙事件和文化适应现象。迁移假说将通过对人类火化和一些可追溯到FSK及其直接前体形成时间的未火化骨骼的稳定同位素分析来验证。材料可从相关地区获得(北部泰勒尔：昆德尔，沃格尔；南部泰勒尔：莫里津，布里克森，普法滕，拉奇)。潜在的原产地将由稳定的锶和铅同位素组成的同位素指纹来确定。由于这些重元素的同位素比值在热稳定性上是稳定的，火化后的材料适合分析。已火化和未火化的猎物和家养动物遗骸已从坟墓和定居点中挖掘出来，并将进行分析，以支持对当地同位素特征的评估，并将与FSK成员的人类遗骸的同位素比率进行比较。

TP 4As explained in the interim report, TP 4 was newly adjusted to permit an extension of the scientific topic addressed in the course of phase I to the Salzach-Inn-Danube area. In analogy to the situation during the older Urnfield Culture in the catchment area of the ore district Schwaz-Brixlegg in the upper Inn valley, settlement formations seemingly occur in the Salzach valley, starting in the the younger and lasting until the late Urnfield Culture (periods HaB1-HyB3, or 10th to 9th century BC). While the settlement processes are still insufficiently investigated, new foundations of necropoles are evidenced independently. Grave furnishings reveal close parallels to the lower Bavarian Danube area. This poses the assumption that ore districts located in the vicinity of the Mitterberg region were responsible for these connections. Isotopic analyses of selected burial inventories shall reveal whether these exchange contacts had happened in the course of metal trade including migration phenomena, or in terms of an adoption of a new ceramic style through diverse migration processes without any long-lasting presence of immigrants at a site.TP 5In the 5th century BC, the Fritzens-Sanzeno-Culture (FSK), characterized by several parameters (property ownerships, house constructions, iron technology, religious notions) developed as a uniform culture in north and south Tyrole and the Trentino by way of the Inn-Eisack-Etsch passage. As a reason, both migratory events of population groups and acculturation phenomena are discussed. The migration hypothesis shall be tested by stable isotope analysis of human cremations and some uncremated skeletons dating to the formation time of the FSK and its immediate precursors. Material is available from the regions in question (north Tyrole: Kundl, Wörgl; south Tyrole: Moritzing, Brixen, Pfatten, Latsch). Potential regions of origin will be defined by the isotopic fingerprint consisting of stable strontium and lead isotopes. Since isotopic ratios of these heavy elements are thermally stable, cremated material is suitable for analysis. Cremated and uncremated remains of game and domesticates have been excavated both from the graves and the settlements, and will be analyzed as well to support the evaluation of local isotopic signatures, which will be compared with the isotopic ratios of human remains of members of the FSK.