Stone Age Pottery Chronology in the Northeast European Forest Zone: New AMS and EA-IRMS Results on Foodcrusts

Radiocarbon ◽  
2016 ◽  
Vol 58 (2) ◽  
pp. 267-289 ◽  
Author(s):  
Henny Piezonka ◽  
John Meadows ◽  
Sönke Hartz ◽  
Elena Kostyleva ◽  
Nadezhda Nedomolkina ◽  
...  

AbstractPottery produced by mobile hunter-gatherer-fisher groups in the northeast European forest zone is among the earliest in Europe. Absolute chronologies, however, are still subject to debate due to a general lack of reliable contextual information. Direct radiocarbon dating of carbonized surface residues (“foodcrusts”) on pots can help to address this problem, as it dates the use of the pottery. If a pot was used to cook fish or other aquatic species, however, carbon in the crust may have been depleted in 14C compared to carbon in terrestrial foods and thus appear older than it really is (i.e. showing a “freshwater reservoir effect,” or FRE). A connected problem, therefore, is the importance of aquatic resources in the subsistence economy, and whether pots were used to process aquatic food. To build better chronologies from foodcrust dates, we need to determine which 14C results are more or less likely to be subject to FRE, i.e. to distinguish crusts derived mainly from aquatic ingredients from those composed mainly of terrestrial foods. Integrating laboratory analyses with relative chronologies based on typology and stratigraphy can help to assess the extent of FRE in foodcrust dates. This article reports new 14C and stable isotope measurements on foodcrusts from six Stone Age sites in central and northern European Russia, and one in southeastern Estonia. Most of these 14C results are not obviously influenced by FRE, but the isotopic data suggest an increasing use of aquatic products over the course of the 6th and 5th millennia cal BC.

10.4312/dp.8 ◽  
2018 ◽  
Vol 44 ◽  
pp. 122
Author(s):  
Henny Piezonka ◽  
Nadezhda Nedomolkina ◽  
Marina Ivanishcheva ◽  
Natalya Kosorukova ◽  
Marianna Kulkova ◽  
...  

The onset of the Neolithic period in the Russian North is defined by the emergence of pottery vessels in the archaeological record. The ceramics produced by mobile hunter-gatherer-fisher groups in the north-eastern European forest zone are among the earliest in Europe, starting around 6000 cal BC. After the initial mosaic of local styles in the Early Neolithic, including sparsely decorated wares and early Comb Ware, the Middle Neolithic period, starting in the 5th millennium cal BC, saw the development and spread of larger, more homogenous typological entities between the Urals and the Baltic, the Comb-Pit and Pit-Comb wares. Absolute chronologies, however, are still subject to debate, due to a general lack of reliable contextual information. Direct 14C dating of carbonised surface residues (‘food crusts’) on pots can help to address this problem, as it dates the use of the pottery; but if aquatic foods were processed in the vessels, the respective radiocarbon ages can appear to be too old due to the freshwater reservoir effect. In this pa­per, we discuss the radiocarbon chronologies of four important stratified archaeological complexes in the region between Lake Onega and the Sukhona basin, Berezovaya Slobodka, Veksa, Karavaikha, and Tudo­zero. A growing series of dates, including AMS dates, sheds new light on the onset and further periodisation of the Early and Middle Neolithic in this important area between Eastern Fennoscandia, Central Rus­sia and the Far North-East of Europe, although problems concerning the absolute chronology of the initial Neolithic remain.


2018 ◽  
Vol 44 ◽  
pp. 122-151 ◽  
Author(s):  
Henny Piezonka ◽  
Nadezhda Nedomolkina ◽  
Marina Ivanishcheva ◽  
Natalya Kosorukova ◽  
Marianna Kulkova ◽  
...  

The onset of the Neolithic period in the Russian North is defined by the emergence of pottery vessels in the archaeological record. The ceramics produced by mobile hunter-gatherer-fisher groups in the north-eastern European forest zone are among the earliest in Europe, starting around 6000 cal BC. After the initial mosaic of local styles in the Early Neolithic, including sparsely decorated wares and early Comb Ware, the Middle Neolithic period, starting in the 5th millennium cal BC, saw the development and spread of larger, more homogenous typological entities between the Urals and the Baltic, the Comb-Pit and Pit-Comb wares. Absolute chronologies, however, are still subject to debate, due to a general lack of reliable contextual information. Direct 14C dating of carbonised surface residues (‘food crusts’) on pots can help to address this problem, as it dates the use of the pottery; but if aquatic foods were processed in the vessels, the respective radiocarbon ages can appear to be too old due to the freshwater reservoir effect. In this pa­per, we discuss the radiocarbon chronologies of four important stratified archaeological complexes in the region between Lake Onega and the Sukhona basin, Berezovaya Slobodka, Veksa, Karavaikha, and Tudo­zero. A growing series of dates, including AMS dates, sheds new light on the onset and further periodisation of the Early and Middle Neolithic in this important area between Eastern Fennoscandia, Central Rus­sia and the Far North-East of Europe, although problems concerning the absolute chronology of the initial Neolithic remain.


2021 ◽  
Vol 48 ◽  
pp. 2-21
Author(s):  
Irina Khrustaleva ◽  
Aivar Kriiska

High-quality documentation that was made during fieldwork at archaeological sites can provide new information for old excavations, even decades later. The revision of the archival data of the Stone Age settlement site Lommi III, located in the border zone of Russia and Estonia and excavated by Richard Indreko in 1940, allowed us to identify the remains of a Comb Ware culture (4th millennium cal BC) pit-house based on the concentration of artefacts marked in the field drawings. The rectangular shape and size of the concentration (c. 7.1x4.4m, depth 0.7–0.75m) corresponds to the architectural form common in the European forest zone and has numerous analogies at the settlement sites of that time in Finland, Karelia (Russia) and Estonia. The composition and diversity of the finds and their distribution indicate the (semi-)sedentary way of life of inhabitants of the pit-house. The radiocarbon age obtained from the organic crust on pottery fragments collected in the pit-house corresponds to the first half of 4th millennium cal BC.


Radiocarbon ◽  
2003 ◽  
Vol 45 (3) ◽  
pp. 449-466 ◽  
Author(s):  
Anders Fischer ◽  
Jan Heinemeier

Radiocarbon dates of food residue on pottery from northern European inland areas seem to be influenced significantly by the freshwater reservoir effect (“hardwater” effect) stemming from fish and mollusks cooked in the pots. Bones of freshwater fish from Stone Age åmose, Denmark, are demonstrated to be 100 to 500 14C yr older than their archaeological context. Likewise, food residues on cooking pots, seemingly used for the preparation of freshwater fish, are shown to have 14C age excesses of up to 300 yr. It is probable that age excesses of similar or even larger magnitude are involved in food residue dates from other periods and regions. Since this effect cannot, so far, be quantified and corrected for, 14C dating of food residue, which may potentially include material from freshwater ecosystems, should be treated with reserve.


2019 ◽  
Vol 12 (9-10) ◽  
pp. 38-48
Author(s):  
V. I. Batuev ◽  
I. L. Kalyuzhny

The development of the European North of Russia, where flat and high-hummocky bog complexes are spread, requires information on the processes of formation of their hydrological regime and freezing of this territory. For the first time, based on observational data, for the period from 1993 to 2013, characteristics of the hydrological regime and freezing of hummocky bogs in Northern European Russia are presented, the case study of the Lovozerskoye bog. The observations were carried out in accordance with the unified methods, approved for the specialized network of Roshydromet bog stations. The regularities of the formation of the hydrological regime of hummocky bogs have been revealed: bog water level drops dramatically from the beginning of freezing to the end of March, rises during snow melt period, slightly drops in summer and rises in autumn. The main feature of hummocky bogs is permafrost, which determines their specific structure. It has been discovered that gravitation snowmelt and liquid precipitation waters relatively quickly run down the hummocks over the frozen layer into hollows between them. Levels of bog waters on the hummocks are absent for a longer period of time. In spring, the amplitude of water level rise in swamplands is on average 60–80 cm. Air temperature and insulation properties of snow are the main factors that influence the bog freezing. Hummocks freeze out as deep as 63–65 cm, which corresponds to the depth of their seasonal thawing in the warm period of the year, and adjoin the permafrost. The greatest depth of freezing of the swamplands is 82 – 87 cm, with an average of 68 cm. The frozen layer at swamplands thaws out from both its upper and bottom sides. The melting of the frozen layer at hummocks occurs only from the bog surface with an average intensity of 0,51 cm/day.


Author(s):  
Svtelana B. Selyanina ◽  
◽  
Marina V. Trufanova ◽  
Svtelana A. Zabelina ◽  
Mikhail V. Bogdanov ◽  
...  

2007 ◽  
Vol 415 (1) ◽  
pp. 711-713 ◽  
Author(s):  
E. N. Borisenko ◽  
V. I. Velichkin ◽  
T. A. Vorob’eva ◽  
A. V. Evseev ◽  
A. Yu. Miroshnikov

2021 ◽  
Vol 18 (1) ◽  
pp. 1-12
Author(s):  
K.I. Sunday ◽  
F.B. Ada

The possibilities of pathogens transmitting zoonotic diseases to fish or aquatic environments are dependent on seasons, patients’ contact with fish or fish related environment, nutritional habits and the immune system level of the exposed individual. Consumption of aquatic food is on the increase, and thus explains the answers to the increase in zoonotic contraction cases found in man. Zoonotic infections can be classified into infections caused by: a) direct interaction with infected animals b) consumption of raw or undercooked aquatic products. Pathogens may be natives of the said aquatic environment or may occur as a result of environmental pollution such as the use of fertilizer, human waste or any of the anthropogenic substances. Zoonotic infections can be passed to man through fish via any of the following hosts: Helminths, Bacteria, Protozoa and Arthropods.Nevertheless, once the chemistry and control of zoonoses is understood, putting up measure to adequately address them when necessary will not be challenging. More so, educating the public on the need for prevention, proper cooking of aquatic products, and also a constant reminder of potential dangers are necessary to reinforce proper sea food handling practices. Keywords: Zoonoses, Fish, Effect and Control


Boreas ◽  
1999 ◽  
Vol 28 (1) ◽  
pp. 23-45 ◽  
Author(s):  
VALERY I. ASTAKHOV ◽  
JOHN INGE SVENDSEN ◽  
ALEXEI MATIOUCHKOV ◽  
JAN MANGERUD ◽  
OLGA MASLENIKOVA ◽  
...  

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