Abstract

Here, we present new sedimentary data of the amber bearing layer from the Holocene coastal plain on the SW Saaremaa Island where amber is not known in sedimentary successions but is common in Stone Age and Bronze Age archaeological sites. A layer of buried organic matter (BOM), sandwiched between sandy coastal deposits and containing pieces of natural amber, was discovered during fieldwork and analysed in detail. Results show that the BOM layer is buried under approximately 90‐cm‐thick sandy coastal deposits and consists of the remains of different coastal plants. Palaeogeographical reconstructions and sediment compositions indicate that the layer was deposited in the coastal zone and buried quickly by sandy marine sediments. According to AMS radiocarbon dating of knotgrass seeds (Polygonum lapathifolium), deposition of the BOM layer took place in the Late Bronze Age; about 2.7–2.5 cal. ka BP. Infrared spectra and isotopic composition of the analysed amber from the BOM layer indicate Baltic amber, also known as succinite. The stable isotope ratio indicates the origin of the amber to be south of Estonia. Therefore, it is proposed that the amber was probably transported to Saaremaa within organic matter (along the main SW–NE orientated current flows) from the SE coast of the Baltic Sea where secondary Baltic amber deposits are known to exist widely. Amber items are common in Late Bronze Age settlement sites and burials in Saaremaa and are considered to originate from present‐day Latvia, Lithuania, Kaliningrad district (Russia) and Poland. The current study shows that during the Late Bronze Age natural amber accumulated in the coastal zone of Saaremaa Island and that the islanders could collect it. Therefore, the possibility exists that some Bronze Age archaeological amber objects could be made of local material as opposed to being a result of trade with southern neighbours, as formerly thought.

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.