New data on the chronology of the initial Neolithic Gromatukha culture, Western Amur region
Автор: Derevianko A.P., Derevianko E.I., Nesterov S.P., Tabarev A.V., Uchida K., Kunikita D., Morisaki K., Matsuzaki H.
Журнал: Archaeology, Ethnology & Anthropology of Eurasia @journal-aeae-en
Рубрика: Paleoenvironment, the stone age
Статья в выпуске: 4 т.45, 2017 года.
Бесплатный доступ
Короткий адрес: https://sciup.org/145145339
IDR: 145145339 | DOI: 10.17746/1563-0110.2017.45.4.003-012
Текст обзорной статьи New data on the chronology of the initial Neolithic Gromatukha culture, Western Amur region
The Gromatukha culture was distinguished by A.P. Okladnikov in 1961 by the finds from a multilayered site in the mouth of the Gromatukha River, in the Zeya River basin. For the first time, these materials were presented to the scientific community at the Third Far Eastern Conference in Komsomolsk-on-Amur in 1962 (Okladnikov, 1962). In 1963, stone artifacts and ceramics close to Gromatukha were discovered near the village of Sergeyevka, in the upper Amur basin (Okladnikov, 1966). In various years at the turn of the 20th–21st centuries, in the Zeya and Amur basins, archaeologists found artifacts that could have been assigned to the Gromatukha culture. The Gromatukha culture sites studied via excavations in the Western Amur region are rare. In 1963–1965, studies were conducted at the Sergeyevka settlement; in 1965– 1966 and 2004 at the eponymous site of Gromatukha; in 2006 and 2010 at the Chernigovka-on-Zeya settlement; and since 2004 they have been continued at the Kalinovka rock art site in the upper Amur area (Fig. 1) (Okladnikov, Derevianko, 1977: 8–9; Derevianko, Kang Chan Hwa, Ban Mun Be et al., 2004; Nesterov, Zaitsev, Volkov, 2006; Nesterov, 2008; Zabiyako, Kobyzov, 2011). On the basis of materials from excavations at the Gromatukha site, in 1960s, a detailed typology of stone tools and ceramics belonging to the Gromatukha culture has been developed. A.P. Okladnikov and A.P. Derevianko noted that the artifacts from “three cultural layers of the settlement compose a single well-matured complex”, while the percentage ratio of tools and differently

Fig. 1 . Neolithic sites of the Initial Neolithic in the Amur Region. 1 – Gromatukha; 2 – Chernigovka-on-Zeya; 3 – Sergeyevka;
4 – Novopetrovka II; 5 – Kalinovka.
ornamented ceramics represents development of the Gromatukha culture in time (1977: 79–98). Owing to the absence of radiocarbon dates, the Gromatukha culture was preliminarily dated by the analogs and typology of artifacts to the 5th to the early 4th millennia BC, or to the second half of the 5th to the 4th millennia BC (Ibid.: 161, 173). However, as early as the outset of the study of this culture, assumptions were made regarding its older age, which were taken skeptically by many scientists. For instance, in 1965, one of the authors of this article had occasion to discuss the degree dissertation of a historical sciences candidate in the Paleolithic Department of the Leningrad Branch of the Institute of Archeology of the USSR Academy of Sciences. The disputants rejected the dates of the Early Neolithic cultures of the Middle Amur region, proposed by the defender of thesis: the late 7th to early 6th millennia BC for the Novopetrovka culture, and the late 6th to early 5th millennia BC for Gromatukha. The opponents pointed out that no Neolithic cultures with ceramics of such an ancient age are known either in the Near East or in Europe. Because of the absence of absolute dates and because of this criticism, the author of study was forced to reduce the age of these cultures by two thousand years (Derevianko, 1965).
Radiocarbon dates obtained from charcoal and organic admixture in ceramics
The first data on radiocarbon dating based on charcoal and organic plant admixture in the Gromatukha ceramics were obtained in 1996–2002 (Derevianko, Kuzmin, Burr et al., 2004). The studies at the Gromatukha site in 2004 resulted in the discovery of numerous stone and pottery artifacts, along with 22 samples of charcoal, 11 of which were subjected to radiocarbon dating in laboratories in Russia, Japan, and the USA (Nesterov et al., 2006). Five radiocarbon determinations obtained from these samples correspond to the initial stage of the Gromatukha culture (Table 1, No. 1, 2, 4, 6, 23) (Nesterov et al., 2005: 170). One date belonging to the Initial Neolithic is available for the Chernigovka-on-Zeya settlement (Table 1, No. 32) (Kuzmin, Nesterov, 2010).
A series of 17 radiocarbon dates for the Gromatukha and Chernigovka-on-Zeya sites obtained in 2010* supplemented the relative chronology of sites, which was based on stratigraphic observations and typological analysis of material, with absolute indicators.
Table 1. Radiocarbon dates of the Gromatukha culture, obtained in 1996–2002
No. |
Site, layer |
Material |
Laboratory code |
14C-date, BP |
Calendar date, BP, ±2σ |
Source |
1 |
Gromatukha, layer 3 |
Charcoal |
MTS-05937 |
12,380 ± 70 |
14,820–14,090 |
(Nesterov et al., 2006) |
2 |
ʺ ʺ |
ʺ |
MTS-05936 |
12,340 ± 70 |
14,740–14,030 |
(Ibid.) |
3 |
ʺ ʺ |
ʺ |
AA-36079 |
12,340 ± 60 |
14,700–14,040 |
(Ibid.) |
4 |
ʺ ʺ |
ʺ |
MTS-05936 |
12,300 ± 70 |
14,560–13,980 |
(Ibid.) |
5 |
ʺ ʺ |
ʺ |
AA-60765 |
12,120 ± 40 |
14,090–13,840 |
(Ibid.) |
6 |
ʺ ʺ |
ʺ |
SOAN-5762 |
11,580 ± 190 |
13,810–13,100 |
(Ibid.) |
7 |
ʺ ʺ |
ʺ |
AA-36447 |
9895 ± 50 |
11,600–11,200 |
(Jull et al., 2001) |
8 |
ʺ ʺ |
Organic admixture (grass) |
AA-20940 |
13,310 ± 110 |
16,260–15,350 |
(Derevianko et al., 2004) |
9 |
ʺ ʺ |
Ditto |
AA-20939 |
13,240 ± 85 |
16,120–15,300 |
(Ibid.) |
10 |
ʺ ʺ |
ʺ |
SNU02-002 |
11,320 ± 150 |
13,360–13,050 |
(Ibid.) |
11 |
ʺ ʺ |
ʺ |
AA-38108 |
10,450 ± 60 |
12,650–12,120 |
(Ibid.) |
12 |
ʺ ʺ |
ʺ |
AA-38102 |
8660 ± 90 |
10,200–9630 |
(Ibid.) |
13 |
ʺ ʺ |
ʺ |
AA-38107 |
7310 ± 45 |
8200–8010 |
(Ibid.) |
14 |
ʺ ʺ |
Charred remains |
MTS-17798 |
12,400 ± 100 |
15,010–14,050 |
This study |
15 |
ʺ ʺ |
ʺ |
Tka-15189 |
12,170 ± 50 |
14,190–13,840 |
Ditto |
16 |
ʺ ʺ |
ʺ |
MTS-17808 |
11,440 ± 80 |
13,450–13,140 |
ʺ |
17 |
ʺ ʺ |
ʺ |
MTS-17799 |
9680 ± 80 |
11,230–10,770 |
ʺ |
18 |
ʺ ʺ |
ʺ |
MTS-17800 |
9620 ± 80 |
11,200–10,730 |
ʺ |
19 |
ʺ ʺ |
ʺ |
MTS-17797 |
9360 ± 80 |
10,780–10,280 |
ʺ |
20 |
ʺ ʺ |
ʺ |
MTS-17802 |
9460 ± 80 |
11,090–10,510 |
ʺ |
21 |
ʺ ʺ |
ʺ |
MTS-17796 |
9150 ± 80 |
10,520–10,190 |
ʺ |
22 |
ʺ ʺ |
ʺ |
MTS-17801 |
9280 ± 90 |
10,680–10,250 |
ʺ |
23 |
ʺ layer 2.2 |
Charcoal |
Beta-205394 |
10,660 ± 40 |
12,820–12,650 |
(Nesterov et al., 2006) |
24 |
ʺ layer 2 |
Charred remains |
MTS-17805 |
12,530 ± 90 |
15,120–14,190 |
This study |
25 |
ʺ ʺ |
ʺ |
MTS-17794 |
10,060 ± 90 |
11,970–11,270 |
Ditto |
26 |
ʺ ʺ |
ʺ |
MTS-17793 |
9960 ± 80 |
11,750–11,730 |
ʺ |
27 |
ʺ layer 2.2 |
ʺ |
MTS-17806 |
9910 ± 70 |
11,680–11,200 |
ʺ |
28 |
ʺ layer 2 |
ʺ |
MTS-17795 |
9900 ± 80 |
11,700–11,190 |
ʺ |
29 |
ʺ ʺ |
ʺ |
MTS-17807 |
9360 ± 70 |
10,760–10,300 |
ʺ |
30 |
ʺ layer 1 |
ʺ |
MTS-17803 |
9670 ± 80 |
11,220–10,770 |
ʺ |
31 |
Novopetrovka II |
Organic admixture (grass) |
AA-38103 |
12,720 ± 130 |
15,430–14,320 |
(Derevianko et al., 2004) |
32 |
Chernigovka-on-Zeya, layer 2 |
Charcoal |
AA-78935 |
9885 ± 55 |
11,600–11,200 |
(Kuzmin, 2006) |
33 |
Charred remains |
MTS-17811 |
9080 ± 230 |
11,060–9550 |
This study |
|
34 |
Sergeyevka |
Organic admixture (grass) |
AA-38104 |
7940 ± 45 |
8980–8640 |
(Derevianko et al., 2004) |
Stratigraphic analysis of strata on the area where the Gromatukha site is situated has shown that three Neolithic cultural layers (Fig. 2, 1 ) lie under the layer associated with the Russian settlement that emerged during intense development of the territory in the 20th century.
Layer 1 is composed of tawny light loam. Its thickness varies from 10 to 40 cm. In the eastern part of the area unearthed by excavation in 2004, traces of a ground dwelling belonging to the Osinovoye Ozero culture were recorded (Volkov, Nesterov, 2008). Charcoal from layer 1 produced one date: 3600 ± 45 BP (SOAN-5759), the calendar value of which corresponds to (±2σ) 3730– 4080 BP. This is in good agreement with three determinations based on samples from the dwelling, which could have existed in the interval from 3410 to 3690 BP (3290 ± 40 BP (MTS-05940), 3340 ± 40 BP (MTS-05939), and 3350 ± 40 BP (MTS-05941)) (Kuzmin, Nesterov, 2010: 105). Only one charcoal sample from this dwelling has shown the date of 2600 ± ± 95 BP (SOAN-5760), which corresponds to the time of the Uril culture of the Early Iron Age ((±2σ), 920– 410 BP)), whose separate pottery fragments are found in redeposited form at this site.
Layer 2 is composed of dark humic sandy loam. In the majority of sections made in 2004, it was possible to identify a division of this layer into two horizons. In certain sections, a thin (5–7 mm) sandy interlayer was established between the horizons. The thickness of layer 2 is from 20 to 70 cm, or 40–50 cm on average. The calibrated dates based on two charcoal samples from this layer (6175 ± 125 BP (SOAN-5761), 10660 ± ± 40 BP (Beta-205394)) and on one collagen sample from a roe-deer bone (5140 ± 140 BP (AA-36085)) indicate a calendar calibrated age of the layer in the interval (±2σ) from 5600 to 12,820 BP (Ibid.: 104–105).
Layer 3 is composed of gray sandy loam represented discretely by lenses in all sections. In the places where layer 3 is absent, layer 2 lies directly on crushed-stony/ clay layer 4, containing no archaeological artifacts. For layer 3, 13 radiocarbon dates have been obtained from charcoal and organic remains (grass) in clay texture (Table 1, No. 1–13), according to which the calendar calibrated age of the layer (±2σ) is approximately 8010– 16,260 BP (Derevianko, Kuzmin, Burr et al., 2004; Kuzmin, Nesterov, 2010: 104–105).
Stratigraphic studies at the Chernigovka-on-Zeya site have determined that the top layer of the terrace is a weakly sodded arable field exposed to severe water and wind erosion (Fig. 2, 2 ). In fact, this is the upper horizon of archaeological layer 1. As a result of its destruction, some artifacts proved to be redeposited. Apart from the Gromatukha finds, rare potsherds belonging to the Uril culture of the Early Iron Age and the Early Middle Ages (Mohe) were encountered here. The part of layer 1 (red sandy loam) undisturbed by tillage wedges out towards the south in the meridional sections, while its underlying layer 2 (black sandy loam) and, occasionally, sterile layer 3 near the southern wall of the excavation area, lie immediately under the arable field. The thickness of the layers increases towards the north by 30–40 cm for
Layer of the Russian settlement

Fig. 2 . Stratigraphy of Gromatukha ( 1 ) and Chernigovka-on-Zeya ( 2 ) sites.
layer 1, and by 40–50 cm for layer 2. At the same time, it reduces eastwards. A blade-based arrowhead, discovered in the arable land layer, is similar to the arrowheads from Novopetrovka III (Western Amur region), where for layer 1 a radiocarbon calibrated date of (±2σ) 8610–9240 BP (8040 ± 90 BP (MTS-05943)) is available (Nesterov et al., 2005: 170). The radiocarbon date obtained from the charcoal sample found in layer 2 (9885 ± 55 BP (AA-78935)) has shown an interval of 11,200–11,600 BP (Kuzmin, Nesterov, 2010: 104).
Radiocarbon dates from charred remains on pottery
In 2015, for the first time for the Gromatukha culture, our Japanese colleagues conducted radiocarbon (AMS) dating of charred remains (deposited during cooking) on ceramicware fragments from the Gromatukha (20 samples) and Chernigovka-on-Zeya sites (1)*. Potsherds for analysis were taken from collections of the Gromatukha (excavations by A.P. Okladnikov, A.P. Derevianko, E.I. Derevianko in 1966 (14 samples), and S.P. Nesterov in 2004 (6)) and Chernigovka-on-Zeya sites (excavations by Nesterov in 2006 (1 sample)) (Table 2; Fig. 3, 4). Samples of charred remains on pottery were dated in the University of Tokyo, Japan (laboratory codes MTS and Tka).
Radiocarbon dating of charred remains on Neolithic pottery from the Western Amur region resulted in 21 dates, 17 of which were attributed to the Gromatukha culture. For the Gromatukha site, nine dates were established based on samples from layer 3, six dates from layer 2, and one date from layer 1. One date (9070 ± 240 BP) (MTS-17811)) was derived from charred remains on pottery from layer 2 of the Chernigovka-on-Zeya site**.
Discussion of results
The dates of the Gromatukha sites were derived from charcoal, organic remains (grass) in clay texture, and charred remains on vessels.
Dating of charred remains on pottery is performed using the standard procedure; however, its interpretation should take into account some special features. The matter is that the cooking of food is often accompanied by absorption of carbon dissolved in water, which can have a greater (up to several hundreds of years) radiocarbon age than plant or animal food cooked in a ceramic vessel. In such a case, the date determined from the charred remains will be more ancient than that established from contemporaneous charcoal from a hearth or a layer (Fischer, Heinemeier, 2003; Kuzmin, Nesterov, 2010: 103, 106).
As for radiocarbon dating of an organic admixture (usually, chopped grass) in clay texture of ceramics, it is based on carbon (approx. 1.0–0.1 %) released as a result of heating the milled ceramics (preliminarily cleared from carbonates and humic acids) under oxygen atmosphere at a temperature of 400 ºC. However, even at 400 ºC, there remains a probability of the organic admixture’s being polluted with more ancient carbon from clay. Radiocarbon dates from organic material in pottery, as compared with 14С-dates from charcoal and charred remains at the same sites, give a greater chronological range, but show the similarity of age for all other types of carbon-containing materials. This makes the dates obtained from organic remains in clay texture sufficiently reliable as well (Kuzmin, Nesterov, 2010: 106).
The largest number of charcoal and pottery samples for radiocarbon analysis was obtained from layer 3 at the Gromatukha site. Comparison of dates from charcoal and organic admixture has revealed a somewhat older age (approximately by 1 thousand years) of pottery samples with grass in clay texture (see Table 1). In general, the dates of artifacts from Gromatukha layer 3 are in the range of (hereinafter ± 2σ) 14,820–11,200 calendar years ago for charcoal, and 16,260–8010 BP for organic admixture. A charcoal sample from interlayer 2.2 of layer 2, taken at the boundary with layer 3, has also demonstrated a considerably ancient age of 12,820–12,650 BP. The dates of finds from layer 2 of the Chernigovka-on-Zeya are comparable with the dates of samples from layer 3 of the Gromatukha site. Dates corresponding to the period of the Gromatukha culture have also been derived from ceramics containing grass in clay texture at the Novopetrovka II and Sergeyevka sites. Pottery from Novopetrovka II represents the period up to 15,430 BP, while the Sergeyevka sample (8980–8640 BP), obviously represents the final stage of Gromatukha development in the Western Amur region, contemporaneous with the Novopetrovka culture.
Table 2. New radiocarbon dates for the Gromatukha and Chernigovka-on-Zeya sites
Sample No. |
Year of excavations, No. of pottery fragment according to the list, archaeological culture |
Location of charred remains on a vessel |
с ГО _ГО 3 .У ел ч= ГО о 6 г |
Laboratory code |
14C-date, BP |
Calendar date, BP, ±2σ |
"с го "с О о^ с О о го О |
"с го 8^ 5Z О) о iz |
с го О) £z F о S о §Е ГО О |
1 |
2 |
3 |
4 |
5 |
6 |
7 |
8 |
9 |
10 |
Gromatukha |
|||||||||
Gro-1 |
1966, layer 3, Gromatukha culture |
On the inside of the body |
3, 1 |
Tka-15189 |
12,170 ± 50 |
13,843–14,185 (100 %) |
39.3 |
4.9 |
9.3 |
2015Gro-1 |
1966, layer 2, No. 12598, culture not identified |
On the inside of the rim |
3, 2 |
MTS-17792 |
5680 ± 60 |
6318–6375 (10 %) 6387–6574 (80 %) 6577–6634 (10 %) |
48.0 |
3.7 |
15.3 |
2015Gro-2 |
1966, layer 2, No. 8256, Gromatukha culture |
Ditto |
3, 3 |
MTS-17793 |
9960 ± 80 |
11,228–11,728 (99 %) 11,731–11,751 (1 %) |
44.3 |
4.5 |
11.5 |
2015Gro-3 |
1966, layer 2, Gromatukha culture |
" |
3, 4 |
MTS-17794 |
10,060 ± 90 |
11,272–11,844 (89 %) 11,858–11,973 (11 %) |
54.7 |
5.8 |
10.9 |
2015Gro-4 |
1966, layer 2, No. 3457, Gromatukha culture |
On the inside of the body |
3, 7 |
MTS-17795 |
9900 ± 80 |
11,187–11,629 (98 %) 11,672–11,699 (2 %) |
30.1 |
4.0 |
8.8 |
2015Gro-5 |
Layer 3, Gromatukha culture |
On the inside of the rim |
3, 6 |
MTS-17796 |
9150 ± 80 |
10,189–10,519 (100 %) |
8.7 |
0.9 |
10.7 |
2015Gro-6 |
Layer 3, No. 2494, Gromatukha culture |
On the inside of the body |
3, 5 |
MTS-17797 |
9360 ± 80 |
10,275–10,775 (100 %) |
4.3 |
0.4 |
12.1 |
2015Gro-7 |
1966, layer 3, No. 9285, the Gromatukha culture |
Ditto |
3, 9 |
MTS-17798 |
12,400 ± 100 |
14,048–15,009 (100 %) |
42.2 |
6.4 |
7.7 |
2015Gro-8 |
1966, layer 3, Gromatukha culture |
" |
3, 10 |
MTS-17799 |
9680 ± 80 |
10,773–11,229 (100 %) |
52.5 |
5.4 |
11.4 |
2015Gro-9 |
1966, layer 3, No. 895, Gromatukha culture |
" |
3, 8 |
MTS-17800 |
9620 ± 80 |
10,733–11,197 (100 %) |
54.8 |
5.7 |
11.3 |
2015Gro-10 |
1966, layer 3, No. 2657, Gromatukha culture |
On the inside of the rim |
3, 11 |
MTS-17801 |
9280 ± 90 |
10,247–10,679 (100 %) |
– |
– |
– |
2015Gro-11 |
1966, layer 3, No. 8921, Gromatukha culture |
On the inside of the body |
3, 12 |
MTS-17802 |
9460 ± 80 |
10,508–10,898 (77 %) 10,917–11,088 (23 %) |
8.6 |
1.1 |
9.0 |
2015Gro-12 |
2004, layer 1, No. 347, Gromatukha culture |
On the inside of the rim |
4, 3 |
MTS-17803 |
9670 ± 80 |
10,766–11,223 (100 %) |
27.0 |
3.1 |
10.2 |
2015Gro-13 |
2004, Osinovoye Ozero culture dwelling, No. 1001 |
Ditto |
4, 6 |
MTS-17804 |
3460 ± 50 |
3587–3602 (2 %) 3610–3852 (98 %) |
37.9 |
4.5 |
9.8 |
2015Gro-14 |
1966, layer 2, Gromatukha culture |
On the inside of the body |
4, 1 |
MTS-17805 |
12,530 ± 90 |
14,191–15,117 (100 %) |
16.5 |
2.5 |
7.6 |
Table 2 (end)
1 |
2 |
3 |
4 |
5 |
6 |
7 |
8 |
9 |
10 |
2015Gro-15 |
2004, layer 2.2, No. 7935, Gromatukha culture |
On the outside of the rim |
4, 2 |
MTS-17806 |
9910 ± 70 |
11,202–11,619 (99.9 %) 11,680–11,681 (0.1 %) |
38.9 |
1.8 |
25.6 |
2015Gro-16 |
2004, layer 2.2, No. 8030, Gromatukha culture |
Ditto |
4, 7 |
MTS-17807 |
9360 ± 70 |
10,299–10,325 (1 %) 10,341–10,353 (1 %) 10,373–10,756 (98 %) |
14.6 |
1.5 |
11.4 |
2015Gro-17 |
1966, layer 3, No. 9397, Gromatukha culture |
" |
4, 4 |
MTS-17808 |
11,440 ± 80 |
13,136–13,450 (100 %) |
– |
– |
– |
2015Gro-18 |
2004, layer 1, No. 1003, Osinovoye Ozero culture |
On the inside of the rim |
4, 8 |
MTS-17809 |
3380 ± 45 |
3479–3721 (99 %) 3800–3811 (1 %) |
– |
– |
– |
2015Gro-19 |
2004, layer 1, No. 301–302, culture not identified |
On the inside of the body |
4, 9 |
MTS-17810 |
5430 ± 50 |
6020–6052 (3 %) 6061–6079 (1 %) 6111–6154 (7 %) 6174–6313 (89 %) |
23.4 |
3.4 |
8.0 |
Chernigovka-on-Zeya |
|||||||||
Cher-P1 |
2006, layer 2, No. 1714, Gromatukha culture |
Ditto |
4, 5 |
MTS-17811 |
9080 ± 230 |
9545–10,785 (99.5 %) 10,979–10,988 (0.1 %) 11,036–11,059 (0.4 %) |
– |
– |
– |
Note. Gro-1 and 2015Gro-1…-19 are indices of pottery samples from the Gromatukha site for 14C-analysis, Cher-P1 is from the Chernigovka-on-Zeya site.
Radiocarbon dates were calibrated using the Сalib radiocarbon calibration program (Calib 611) (Stuiver, Reimer, 1993).

Fig. 3 . Pottery-fragments with charred remains on the surface, from the Gromatukha site.

Fig. 4 . Pottery-fragments with charred remains on the surface, from the Gromatukha site ( 1–4 , 6–9 ) and Chernigovka-on-Zeya site ( 5 ).

Fig. 5. Ranges of radiocarbon dates for the Gromatukha culture of Western Amur region. Gro – Gromatukha, Cher-P1, Cher – Chernigovka-on-Zeya, NP-II – Novopetrovka-II, Serg – Sergeyevka.
1 – by organic admixture; 2 – by charred remains; 3 – by charcoal.
АА-38104-Serg, organic admixture MTS-17811-Cher-P1, layer 2, charred remains
АА-78935-Cher, layer 2, charcoal
АА-38103-Np-ll, organic admixture
MTS-17803-Gro, layer 1, charred remains
MTS-17807-Gro, layer 2"
MTS-17795-Gro ""
MTS-17806-Gro, layer 2.2"
MTS-17793-Gro, layer 2"
MTS-17794-Gro ""
MTS-17805-Gro ""
Beta-205394-Gro, layer 2.2, charcoal
MTS-17801-Gro, layer 3, charred remains
MTS-17796-Gro ""
MTS-17802-Gro ""
MTS-17797-Gro ""
MTS-17800-Gro ""
MTS-17799-Gro ""
MTS-17808-Gro ""
Tka-15189-Gro ""
MTS-17798-Gro ""
АА-38107-Gro, layer 3, organic admixture
АА-38102-Gro ""
АА-38108-Gro ""
SNU02-002-Gro ""
АА-20939-Gro ""
АА-20940-Gro ""
АА-36447-Gro, layer 3, charcoal
SOAN-5762-Gro ""
АА-60765-Gro ""
MTS-05938-Gro ""
АА-36079-Gro ""
MTS-05936-Gro ""
MTS-05937-Gro ""
The Gromatukha culture dates derived from charred remains on pottery from layer 3 of the Gromatukha site pertain to its initial period, which falls between the calendar calibrated dates (±2σ) from 15,010 (MTS-17798) to 10,250 BP (MTS-17801). Determinations from charred remains on pottery from layer 2 of the same site also correspond to the Initial Neolithic, from 15,120 (MTS-17805) to 10,300 BP (MTS-17807). Another early date (11,220–10,770 BP (MTS-17803)) was determined from charred remains on the Gromatukha pottery (Fig. 4, 3 ) that were discovered in layer 1. The date for Chernigovka-on-Zeya obtained from charred remains on pottery from layer 2 (Fig. 4, 5 ) (11,060–9550 BP) (MTS-17811) is close to this. The latter dates have a greater standard deviation (or a standard error) of ±230 as compared to that for other radiocarbon dates (from ±70 to 90 years (see Table 1)).
Several explanations for a resemblance between the dates for layers 3 and 2 of the Gromatukha site can be proposed. The first is a discrete distribution of layer 3 over a terrace, whereby layer 2 (interlayer 2.2) in some places is located directly on crushed-stony/clay layer 4. The second is the presence of Gromatukha lithic industry and ceramics in layer 2, similar to artifacts from layer 3; i.e. continuous deposition of material. And the third is the displacement of early material from layer 3 during digging by the Gromatukha people themselves, and by later inhabitants that left deposits in layers 2 and 1. Trampling and subsidence of subjects into the underlying layers cannot be ruled out. For instance, during excavations in 2004, a fragment of Osinovoye Ozero pottery-rim with appliquéd segmented fillets was found lying 7 cm below layer 1. A piece of ocher and an adjacent cluster of Osinovoye Ozero pottery can be assigned to the boundary between layers 1 and 2. Chalcedonic flakes were found near the cluster. All these objects could have been trampled in by inhabitants of the Osinovoye Ozero dwelling.
The presence of a more ancient pottery sample (Fig. 4, 3 ) in layer 1 of the Gromatukha site is explained by its redeposition as a result of the activities of inhabitants of the site at the mouth of the Gromatukha River, which could have taken place at any stage after the Gromatukha culture, from the Late Neolithic to the period of the site’s occupation in the first half of the 20th century.
Conclusions
According to the data from radiocarbon analysis of charcoal and organics from pottery, the chronological framework of the Gromatukha culture is 16,260– 8010 BP, i.e. this culture existed for about 8250 years. Actually, this time-range corresponds to the dates derived from organic admixture in ceramics; the charcoal-based dates fall within the said chronological limits. However, if we rely on the dates established from charcoal only (14,820–11,200 BP), this period is reduced to 3620 years (see Table 1) (Kuzmin, Nesterov, 2010).
New radiocarbon dates determined from charred remains on the Gromatukha pottery give a chronological range of 15,010–9550 BP (for Gromatukha layers 3 and 2, and Chernigovka-on-Zeya layer 2); in other words, the duration of existence of ceramics within the Gromatukha culture of the Initial Neolithic in the Western Amur region was 5460 years. This is 2790 years less than the period of existence of the tradition of manufacture of the said ceramicware, established by organic remains in clay texture, and 1840 years more than the Gromatukha culture period determined from charcoal found in the cultural layers of the sites (Fig. 5). Comparative studies of the lithic industry and ceramics of the Gromatukha sites will demonstrate to what extent such existence periods of the Gromatukha culture, determined from charcoal, organic remains in pottery, and charred remains on pottery, are realistic, and which of them represents actual events.
Acknowledgement
This study was supported by the Russian Science Foundation (Project No. 14-50-00036).