Vegetation History and Archaeobotany https://doi.org/10.1007/s00334-018-0694-7

ORIGINAL ARTICLE

Earliest use of birch bark tar in Northwest : evidence from organic residues in prehistoric pottery at the Changning site

Huiyun Rao1 · Qianqian Wang2 · Xiaoyan Ren2 · Zhaoxia Zhang1 · Wanxia Huang3 · Qingxi Yuan3 · Xiaochenyang Jiang1,4 · Yimin Yang4

Received: 7 May 2017 / Accepted: 30 July 2018 © Springer-Verlag GmbH Germany, part of Springer Nature 2018

Abstract The analysis of organic residues in pottery can provide abundant information on the lives of ancient people, including the natural resources consumed, the techniques applied, the functions of pottery, and so on. In this paper, a variety of meth- ods, including FT-IR (Fourier transform infrared spectroscopy), GC–MS (gas chromatography-mass spectrometry), SEM (scanning electron microscopy) and SR-μCT (synchrotron radiation micro-computed tomography), have been employed to characterize the carbonized residues from an amphora, unearthed from the Changning site, Province, Northwest China. The pottery residues were identified as birch bark tar, so ancient people in China could have used the particular local plant resources, birch bark, to produce tar as early as the Qijia cultural period (c. 4,000–3,500 bp). The birch bark tar could have been used to make composite tools discovered at the Changning site, and the amphora has probably been used for tar production. This, to our knowledge so far, is the earliest evidence for the use of birch bark tar in China. Due to the special geographical location of the -Qinghai Region, and the transition of subsistence strategy during the Qijia cultural period, the production and utilization of birch bark tar could not rule out the possibility of western influence, which needs further evidence.

Keywords Birch bark tar · Pottery function · Carbonized residues ·

Introduction 1999a; Mottram et al. 1999), dairying (Copley et al. 2003; Evershed et al. 2008; Salque et al. 2013), brewing (Correa- Pottery wares, of different types and functions, are amongst Ascencio et al. 2014) and dyeing (James et al. 2009), have the most common artifacts found at archaeological sites been conducted in pottery vessels, and organic matter pre- across China since the Late Glacial (Kuzmin 2006). A served as carbonized surface residues or absorbed residues variety of processes, such as cooking (Dudd and Evershed in porous ceramic matrices. The characterization of organic residues in pottery can provide valuable information about Communicated by J. Kitagawa. the natural resources consumed or used by ancient people, the techniques applied to prepare all these products and also * Yimin Yang the functions of related pottery. [email protected] Pottery residues have been observed and studied since 1 Key Laboratory of Vertebrate Evolution and Human Origins the end of the 19th century, and research in the area has of Chinese Academy of Sciences, Institute of Vertebrate greatly expanded in recent decades due to improvements in Paleontology and Paleoanthropology, Chinese Academy analytical tools, such as chromatographic and mass spec- of Sciences, Beijing 100044, People’s Republic of China trometric techniques (Evershed et al. 1991; Charters and 2 Qinghai Provincial Institute of Cultural Relics Evershed 1997; Regert et al. 2001; Stott et al. 2003; Hansel and Archaeology, 810007, People’s Republic of China and Evershed 2009; Correa-Ascencio and Evershed 2014). 3 Institute of High Energy Physics, Chinese Academy Fourier transformed infrared spectroscopy (FT-IR) and of Sciences, Beijing 100049, People’s Republic of China mass spectrometric methods [direct inlet electron ionization 4 Department of Archaeology and Anthropology, University mass spectrometry (DI-MS), direct temperature-resolved of Chinese Academy of Sciences, Beijing 100049, mass spectrometry (DT-MS), pyrolysis-mass spectrometry People’s Republic of China

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(Py-MS) etc.] have been employed as preliminary analyses microscopic observations (scanning electron microscopy, of organic residues and could provide the general chemi- SEM, and synchrotron radiation micro-computed tomog- cal information of residues to guide further investigations raphy, SR-μCT), and analytical techniques (FT-IR and (Oudemans and Boon 1991; McGovern et al. 1996; Regert GC–MS). and Rolando 2002; Oudemans et al. 2007; Kaal et al. 2014). Because of their hydrophobicity and thermal resistance, lipids are more likely to be preserved in pottery, and gas Site description chromatography-mass spectrometry (GC–MS) is the most commonly used technique for lipid analysis (Evershed Within the valley of the Huangshui River, the Changn- et al. 1990, 2002; Evershed 2008; Heron et al. 2016). With ing site is situated on the second terrace of the Beichuan the identification of specific biomarkers, a wide range of River, which is approximately 100 km east of Qinghai lipid commodities have been revealed, including animal Lake, Northwest China (Fig. 1). The valley of the Huang- fats (Evershed et al. 2002; Poulain et al. 2016), plant oils shui River has a semi-arid plateau continental climate (Romanus et al. 2007; Dunne et al. 2016), beeswax (Ever- and diverse ecological landscapes, which include desert shed et al. 1997; Heron et al. 2015), epicuticular leaf waxes steppe, steppe, meadow steppe and forest, alpine meadow, (Charters and Evershed 1997; Dunne et al. 2016), birch glaciers, and so on (Wang 2015). Combining fauna with bark tar (Lucquin et al. 2007; Mitkidou et al. 2008), pine pollen data, it can be inferred that the environmental con- resin (Colombini et al. 2005; Jerkovic et al. 2011) and so ditions of the Changning site were similar to today’s tem- on. Recently, gas chromatography-combustion-isotope ratio perate steppe-forest landscape (Li 2012). mass spectrometry (GC-C-IRMS) has also been applied to In 2006, a total area of 3,000 m2 was unearthed, includ- calculate isotope ratios of individual fatty acids in organic ing 15 houses, 150 pits and cellars, and 6 tombs. Vari- residues, and has enabled the differentiation of ruminant ous artifacts were found, such as pottery wares, stone adipose, ruminant dairy fats, non-ruminant adipose, fresh- tools, jade articles, bronze vessels, bone implements and water and marine resources (Evershed et al. 2008; Craig so on. Storage and cooking vessels were the main pot- et al. 2011; Heron et al. 2015; Nieuwenhuyse et al. 2015; tery collections (QPICRA 2006). Besides artifacts, ani- Oras et al. 2017). Immunological methods and proteomic mal bones (sheep, cattle, pig, horse, dog etc.) and plant approaches have been conducted to identify the proteina- remains (Setaria italica—foxtail millet, Panicum mili- ceous residues (Craig and Collins 2000; Wiktorowicz et al. aceum—broomcorn millet, Triticeae tribe etc.) were also 2017). discovered, indicating that both agriculture and animal The Changning site (dated to approximately husbandry have played important roles in the Changning 4,000–3,500 bp; QPICRA 2006) is a large settlement of people’s lives (Li 2012; Li et al. 2013; Wang 2015). As a the Qijia culture in Qinghai Province, Northwest China large settlement of the Qijia culture, the Changning site (QPICRA 2006; Li 2012). A two-handled amphora was developed over a transition period between agriculture and unearthed in a pit at this site, with black charred residues pastoralism, and also within an intermediate period from inside. In this paper, an interdisciplinary methodology has the Neolithic era to the , which is an important been developed to analyse the residues in this amphora, time span for the formation of Chinese civilization (QPI- in order to identify their nature and origins and to reveal CRA 2006; Li 2012). the functions of related pottery. This method comprises

Fig. 1 Location of the Changn- ing site, Datong County, Qing- hai Province, Northwest China

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Materials and methods

Fragments of a two-handled amphora with a red coarse clay body were unearthed from pit H34 at the Changning site. The wall thickness was approximately 1 cm. Figure 2 shows the inner and outer surfaces of two shards S1 and S2 of this amphora. Black residues with a variable thickness were observed on the inner surfaces of these shards (Fig. 2b, d), while black soot traces were detected near the rim on the outer surfaces of the shards (Fig. 2a, c). At the bottom of the amphora, some brown or black charred lumps were found. Fig. 3 The archaeological samples analysed; a the inner surface of The black residues adhering to the inner surface of shard S3 shard S3, where surface residues were sampled (sample label ISR). were scraped with a sterilized blade and collected for further The outer surface residues were also sampled as the control sample (labeled as OSR). Scale bar 4 cm. b The charred lumps (sample label analyses (labelled as ISR) (Fig. 3a), while the outer surface CL), which were sampled from the bottom of the amphora. Scale residues were collected in the same manner as the control bar 1 cm sample (labelled as OSR). Charred lumps were also sampled (labelled as CL) (Fig. 3b). Fresh modern birch bark (Betula platyphylla, plant No. UCAS 20140102, labelled as MB1) Rao et al. (2017).The pottery residue samples and modern was collected as a reference sample from the campus of Uni- birch bark reference sample were further analysed with a versity of Chinese Academy of Sciences. To obtain the mod- 7890A gas chromatograph and a 5975C mass detector in ern charred reference sample (labelled as MB2), the birch 70 eV electron impact mode (GC–MS). The procedure was bark was heated in a muffle furnace at 250 °C for 4 days. modified from procedures used by Regert et al. (2003b), Charred lumps (CL) and inner surface residues (ISR) Mitkidou et al. (2008) and Rao et al. (2017). In brief, CL, were analysed with a Nicolet 6700 (Thermo Scientific) ISR, OSR and MB1 were extracted using chloroform/meth- FT-IR spectrometer. The detailed procedure is described in anol (2:1 v/v), derivatised by BSTFA (bis(trimethylsilyl) trifluoroacetamide with 1% trimethylchlorosilane) and re- dissolved with CH­ 2Cl2 for the GC–MS analysis. The oven temperature program was as follows: initial temperature 50 °C for 2 min; increased to 150 °C (2 min) at 10 °C/min; then increased to 290 °C at 4 °C/min; 290 °C was main- tained for 20 min. An analytical blank was also prepared and run along with the samples under the same experimental conditions for contamination control. An archaeological CL and modern charred birch bark (MB2) were scanned by SEM. The sample was fixed on the object mount by a conducting glue (graphite-based) and coated with gold. ZEISS EVO 25 scanning electron micros- copy was used with an electron beam of 10 keV. A CL was scanned by SR-μCT in a 4W1A beamline in the Beijing Synchrotron Radiation Facility (BSRF), Beijing, China. The X-ray source energy used was 12 keV and the CCD detec- tor (photonic science VHR16 M) had a space resolution of 7.4 μm.

Results and discussion

The identification of birch bark tar

The FT-IR spectra of the pottery residue samples were domi- Fig. 2 The outer and inner surfaces of the amphora shards; a and b nated by absorption bands of organic matter, especially the show the outer and inner surfaces of shard S1, respectively; c and d show the outer and inner surfaces of shard S2, respectively. Scale CL discovered at the bottom of the amphora (Fig. 4). Com- bar 10 cm pared with the published data (Bellamy 1980; Schrader

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Fig. 4 FT-IR spectrum of CL. The specific peaks attributed to organic matter, probably birch bark tar

2008; Cîntă-Pînzaru et al. 2012; Silverstein et al. 2014), the absorption peaks could be assigned to specific functional Fig. 5 Partial gas chromatogram of a MB1 (modern birch bark); b CL (charred lumps) and c ISR (inner surface residues); showing a series groups and chemical components, which are summarized in of triterpenoid biomarkers derived from birch bark. d is a partial Table 1. These peaks have also been found in ancient birch enlarged detail of a. 1, lupa-2, 20(29)-diene; 2, lupa-2,20(29)-dien- bark or birch bark tar published elsewhere and implied that 28-ol; 3, allobetul-2-ene; 4, lupenone; 5, lupeol; 6, betulone; 7, betu- the CL could have derived from birch bark (Bosquet et al. lin; 8, betulinic acid. The hydroxyl triterpenoids were all identified as their TMS derivatives 2001; Regert and Vacher 2001; Regert et al. 2003a; Regert 2007; Trąbska et al. 2011; Pietrzak and Langer 2012; Rao et al. 2017). The specific band at 886 cm−1 also indicated considered as specific constituents in fresh birch bark (Cui that the CL was rather birch bark tar than pine resin (Pietrzak and Zheng 1994), while the other three (lupa-2,20(29)-diene, and Langer 2012), which would be further confirmed by lupa-2,20(29)-dien-28-ol and allobetul-2-ene) were regarded GC–MS analysis. as indicators of thermal treatment and degradation (Reu- A series of triterpenoid biomarkers were detected by nanen et al. 1993; Aveling and Heron 1998; Regert 2004). GC–MS in MB1, CL and ISR (Fig. 5). These biomarkers None of these biomarkers were detected in the analytical were identified based on mass spectra as well as retention blank and the control sample (OSR).The results showed that time, which were searched against the NIST 08 Mass Spec- the discovered pottery residues were products of birch bark tral Library and also compared with modern birch bark ref- with a thermal treatment, which confirmed the preliminary erence and published data (Table 2) (Charters et al. 1993; result of FT-IR. Reunanen et al. 1993; Colombini and Modugno 2009; Rao With increasing duration and intensity of pyrolytic treat- et al. 2017). Of all the eight biomarkers, five components ment, the proportions of different biomarkers change (Koller (betulin, betulin acid, lupeol, betulone and lupenone) were et al. 2001). Regert et al. (2003b) have calculated a variable named “MD/BioM”, defined as the ratio between the main original biomarkers (lupeol and betulin) and the degradation Table 1 The observed IR bands (cm­ −1) of charred lumps (CL) and markers (lupa-2,20(29)-diene, lupa-2,20(29)-dien-28-ol and their assignments allobetul-2-ene). In their publication (Regert et al. 2003b), IR bands (cm­ −1) Assignments three different distribution patterns were classified, i.e. bio- markers predominant (MD/BioM < 0.5), similar amounts of 3,421 ν (O–H) biomarkers and degradation markers (0.5< MD/BioM< 1.5) 2,922; 2,851 νas (C–H), νs (C–H) and degradation markers predominant (MD/BioM > 1.5). 1,705 ν (C=O) After quantifying the relative percentages of the identified 1,597 ν (C=C) triterpenoids, the MD/BioM values of our ancient CL and 1,456; 1,375 δ ­(CH3) + δ(CH2) ISR were calculated as 3.76 and 2.08 respectively, indicating 1,173 ν (C–C) the predominance of degradation products. Thus it implied 886 ω (C–H) that birch bark has been heated to some extent (over 400 °C ν, stretching; δ, bending; ω, out-of-plane bending; as, asymmetrical; or for a long time) to make this product in the amphora s, symmetrical (Dudd and Evershed 1999b; Koller et al. 2001).

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Table 2 The biomarker Biomarkers CL ISR MB1 Ancient birch Modern birch Ancient composition of archaeological ­barka bark ­tarb birch bark samples and birch bark (tar) ­tarc references Lupa-2, 20(29)-diene X X X X Lupa-2,20(29)-dien-28-ol X X X X X Allobetul-2-ene X X X Lupenone X X X X X Lupeol X X X X X X Betulone X X X X Betulin X X X X X X Allobetulinol X Betulinic acid X X

CL charred lumps, ISR inner surface residues, MB1 modern birch bark reference a Rao et al. (2017) b Mitkidou et al. (2008) c Regert et al. (2003b)

Birch bark could have been heated to produce birch bark material with similar density, except for some pores (Fig. 7). tar, which was usually used as an adhesive in Europe (Char- Because of their size and number, these pores did not belong ters et al. 1993; Roebroeks and Villa 2011), or charred birch to birch bark structure and would have been formed dur- bark, which was a type of important Chinese traditional ing the production and utilization of birch bark tar. Thus it medicine (Li 1991). In order to differentiate both birch bark could be inferred that the CL were birch bark tar (rather than products and obtain more information about the process charred birch bark), which could be obtained by high-tem- technology, an archaeological CL and modern charred birch perature treatment (definitely higher than the experimental bark reference sample (MB2) were chosen for SEM observa- carbonization temperature of 250 °C) or repeated/lengthy tion (Fig. 6). Although MB2 has been heated at 250 °C for heating treatment. 4 days, the primary plant structure was clearly visible, with Birch bark tar was usually used as an adhesive in ancient numerous cork layers which were composed of two differ- Europe and could be traced back to the Middle Palaeolithic ent cell types (Fig. 6b). The different cellular structures of (at least 200,000 years ago) (Roebroeks and Villa 2011). these two cell types were attributed to their different chemi- Birch bark tar was used for hafting composite tools (Roe- cal constituents, as the thicker walled cells were more heav- broeks and Villa 2011), repairing pottery (Charters et al. ily suberized (Orsini et al. 2015). As for the archaeological 1993), coating or waterproofing pottery (Regert et al. CL, only the compact homogeneous structure was observed 2003b), decorating pottery (Trąbska et al. 2011; Jakucs (Fig. 6a), indicating a complete tar distillation that trans- and Sándorné Kovács 2012) etc. In China, although plant formed the bark into an amorphous matrix (Pawlik 2004). adhesives, including lacquer, plant oils, starch, gum, resin, The CT image of the cross section of a CL also revealed bark tar (from Ilex integra) and various others, have been that the main part of the lump was homogeneous organic recorded in the literature or identified on archaeological

Fig. 6 The SEM images of a CL (charred lumps) and b MB2 (modern charred birch bark). There were two different cell types, one with narrower radial dimension and thicker cell walls. Scale bar = 0.2 mm

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The ‘double-pot’ method is conducted with one pot placed on top of another; the pot on top (retort) is pierced with holes in the bottom, filled with birch bark, covered with a lid and sealed with clay. These pots are put in a pit, where a fire is lit on top to transform the bark to tar dripping into the pot underneath (receptacle) (Evans and Heron 1993; Jauch 1994; Hennius et al. 2005; Fuchs and Wahl 2013). While the use of birch bark tar is well reported in various archaeologi- cal contexts (Grünberg 2002; Lucquin et al. 2007; Mitki- dou et al. 2008; Roebroeks and Villa 2011), the discovered remains in association with its production are quite rare, especially during the prehistoric period. To our knowledge, the earliest retort was unearthed at an Early Bronze Age site in Eastern Hungary (Jakucs and Sándorné Kovács 2012). It is necessary to find the retort on top to deduce the amphora as a receptacle more confidently. Unfortunately, no Fig. 7 The cross section image of a CL obtained by SR-μCT. Scale pottery with pierced holes in the bottom has been reported bar = 0.5 mm. The image indicated homogeneous organic material with some pores at the Changning site up to now. But at other Qijia cultural sites in the adjacent Gansu Province, this type of pottery was discovered and named as ‘Zeng’, which is a part of artifacts (Chen 2003; Wei et al. 2011; Rao et al. 2015), birch the composite cooking utensil ‘Yan’ (Xie 2002). ‘Yan’ is a bark tar has never been mentioned. This is the first time that kind of steamer with ‘Zeng’ on top of another pottery ves- birch bark tar has been identified in China, which improves sel ‘Li’; water is added to the ‘Li’ and boiled down to give our understanding of Chinese adhesives. Composite tools rise to steam, which heats up the food in the ‘Zeng’ through made of bones and microblades were also discovered at the the holes in its bottom (Zhang 2002). Actually Yan-shaped Changning site (QPICRA 2006; Wang 2015), and birch bark pottery has been discovered at more than 70 sites all over tar might have played a role in manufacturing these tools, China since the Middle Neolithic period, and their functions but this needs further confirmation. are sometimes doubtful (Shi 1993; Fu 2014). With organic residues analysis, we may provide significant information The function of the amphora on the pottery function, and also have a chance of finding a retort for birch bark tar production. Understanding pottery function is usually very difficult as there is no one-to-one correlation between use and the The possible origin of birch bark tar morphology or physical properties of a vessel (Rice 1987). Combining the morphological observations with the organic Betula (birch), with between 50 and 60 species of broad- residue results, we intend to make a better interpretation leaved deciduous trees or shrubs, is the largest genus in the of the function of this amphora. Birch bark tar has been family of Betulaceae (Li and Skvortsov 2013). Betulaceae identified in this amphora, which could be related to pot- first appeared in the Late Cretaceous and began to flourish in tery utilization (adhesive production or storage), produc- the Tertiary (Chen 1994). After originating in central China, tion (coating or decoration) or repair (Regert 2007). Based Betulaceae spread westwards to Europe and were distributed on the distribution and morphology of the pottery residues mainly in the temperate zone of the Northern Hemisphere and charred lumps, the function of this amphora is probably (Chen 1994). In China, 32 species (14 endemic) of birch associated with the production or storage of birch bark tar are mostly found in the northeast, northwest and southwest (Regert 2007). Amphorae are usually used for storage, but mountain areas (Li and Skvortsov 2013). Five species of the coarse property of this amphora makes it also suitable Betula, deciduous trees or shrubs, naturally grow in Qing- for heating (Skibo 2013). The soot traces, detected on the hai Province (Northwest China), among which one species outer surface near the rim of the amphora (Figs. 2a, c), also (B. albosinensis) prevails around Datong County where the imply that this amphora could have been heated, probably archaeological site is located (NWIPB and ECFQ 1997). from the upper part near the rim. All these characteristics of Ancient textual research has indicated the presence of broad- the amphora are, to some degree, consistent with those of the leaved deciduous forest (including birch) around the vicinity receptacles that are used for the collection of birch bark tar of the Changning site during the 18th century (Wen and He in the ‘double-pot’ method, a typical method of birch bark 1979). Fauna and pollen data have also revealed a temper- tar production. ate steppe-forest landscape for the Changning site, which

1 3 Vegetation History and Archaeobotany was favourable for the growth of Betula (Li 2012). What is to improve our understanding of the process technology and more, direct evidence of Betula pollen has also been found origin of birch bark tar in Northwest China. in the Qijia cultural layers of the Changning palaeosol sec- tion (Dong et al. 2012) and adjacent cores of sediment from Acknowledgements The authors would like to thank Matthew Collins, Alexandre Lucquin and Shannon Croft from University of York for Qinghai Lake (Liu et al. 2002). giving professional comments on the identification of birch bark tar. Plentiful Betula resources could be found around the This study was supported by the Strategic Priority Research Program of Changning site, even North China (Chen 1994; Li and Chinese Academy of Sciences (XDB26000000), the National Natural Skvortsov 2013), and they have been well exploited by Science Foundation of China (Grant Nos. 41702186 and 41472145), National Young Top-Notch Talent Support Program in China and ancient people. For example, at the contemporary Liuwan Youth Innovation Promotion Association of CAS. cemetery, which is approximately 100 km southeast of the Changning site and belongs to the same Huangshui region, Betula wood and a birch bark quiver have been discovered in tombs (Wen 2006; Liu 2010). Birch bark has also been long References exploited in North China with abundant historical records and plenty of birch bark artifacts discovered at archaeolog- Aveling E, Heron C (1998) Identification of birch bark tar at the Meso- ical sites, known for “birch bark culture” (Yu 2006; Yin lithic site of Star Carr. Ancient Biomol 2:69–80 2009). Thus, the birch bark tar identified at the Changning Bellamy LJ (1980) The infra-red spectra of complex molecules, 2 edn, Betula vol 2. Chapman and Hall, London and New York site could have been produced using local resources. Bosquet D, Regert M, Dubois N, Jadin I (2001) Identification de brai Although this is the first birch bark tar found in China, it de bouleau sur quatre vases du site rubané de Fexhe-le-Haut- was frequently produced and used in ancient Europe since Clocher « Podrîl’Cortri». 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