Direct isotopic evidence for human millet consumption in the Middle Mumun period: Implication and importance of millets in early agriculture on the Korean Peninsula
Introduction
The origins, cultivation, and consumption of domesticated plants on the Korean Peninsula in prehistory is debated due to the paucity of direct dietary evidence (Ahn, 2005; 2006; 2010; Bale, 2001; Crawford and Lee 2003; 2011; Kim, 2015; Kwak et al., 2017; Kim and Park, 2020). Most previous studies focused on the development of early agriculture on the Korean Peninsula were based on the analyses of plant and animal remains from excavated sites (Lee, 2001, 2003, Lee, 2011; Crawford and Lee, 2003). Based on the archaeobotanical evidence, it is assumed that early agriculture was intensified during the Bronze Age in Korean prehistory or the Mumun period (1500–100 BC) (Ahn, 2010; 2011; Kwak et al., 2017). Although the earliest evidence for cultivated plants is reported from the Middle Chulmun period (3500–2000 BC), it is believed that domesticated crops started to be important from the Early Mumun period (1500–800 BC) (Lee, 2011; Bale, 2001; Lee and Bale, 2016). The Mumun people cultivated various domesticated plants such as rice (Oryza sativa), foxtail millet (Setaria italica), broomcorn millet (Panicum miliaceum), six-rowed barley (Hordeum vulgare), naked bread wheat (Triticum aestivum), soybean (Glycine max), and adzuki bean (Vigna angularis) (Lee, 2003; Ahn, 2010). Despite abundant evidence for the cultivation of multiple crops during the Mumun period, most previous studies were mainly focused on the importance of rice agriculture (Kim, B–C., 2005; 2006; Cho, 2008; Ahn, 2010; Kim, M., 2015). Along with rice, other crops also are believed to be important foods for the Mumun people (Ahn, 2010; Lee, 2011). However, previous archaeobotanical research on domesticated crops has been limited in its ability to directly determine the relative contribution of these crops to the whole diet. In addition, recent studies on organic residues in pottery also have provided evidence of the presence rather than the dietary significance, of different food resources in the Mumun diets (Kwak and Marwick, 2015; Shoda et al., 2017; Kwak et al., 2017). Until now, little research has been conducted on the direct dietary significance of each cultivated crop to the whole Mumun diet. Hence, it is necessary to investigate the relative contribution of each crop (e.g. rice vs. millet) in terms of the Mumun diet in order to better understand the nature and type of agriculture that the Mumun engaged in on the Korean Peninsula.
While archaeobotanical analysis of cultivated cereals provides valuable information about the dietary resources of past populations (Ahn, 2010; Kim, 2015), the presence of plant remains in excavated sites does not imply direct human consumption of these plant remains because they can be encountered as artifacts or as natural deposits in archaeological sites (Kusaka et al., 2010). In order to bridge these disparities between the preservation and direct consumption of plant remains, stable isotope ratio analysis of human bone collagen is applied here. This approach is an established method in bioarchaeology used to reconstruct direct dietary patterns of ancient individuals or population (Lee-Thorp, 2008; Richards, 2020). Isotopic measurements of bone collagen provide direct evidence of the long-term dietary record of an individual related to the average foods consumed over their lifetime (Katzenberg, 2000; Richards, 2020). Specifically, carbon stable isotope ratios (δ13C) distinguish diets based on the consumption of plants that use different photosynthetic pathways (C3 vs. C4 plants) (Wang et al., 2019) and between the consumption of terrestrial and marine foods (Richards and Hedges, 1999; Lee-Thorp, 2008). In Asia, the main C4 domestic plants, broomcorn and foxtail millet, are significantly 13C-enriched, which results in measurable differences in the bone collagen of consumers of these foods (Chen et al., 2016, Lu et al., 2009; Dai et al., 2016; Ma et al., 2016a, 2016b, 2016c; Wang et al., 2016, 2018, 2019).
Bulk nitrogen stable isotope ratio measurements (δ15N) provide information about the trophic level of a consumer in a food chain, with human and animal bone collagen 15N-enriched by ~3–5‰ compared to dietary sources (Minagawa and Wada, 1984; Bocherens and Drucker, 2003; Hedges and Reynard, 2007). Thus, human δ15N values higher than associated faunal δ15N values are interpreted as indicating a diet with significant quantities of these animals, whereas δ15N values close to the associated herbivore values are interpreted as indicating a diet based mainly on plant proteins (Lee-Thorp, 2008).
In addition, compound specific stable isotope ratio analysis of individual amino acids (CSIA-AA) is used to overcome limitations associated with bulk carbon and nitrogen isotopic measurements and provide more detailed dietary reconstructions (Hare et al., 1991; Fogel and Tuross, 2003; Smith et al., 2009; Jaouen et al., 2019). In particular, carbon amino acid measurements (δ13CAA) can better distinguish between C3 vs. freshwater consumers as well as C4 vs. marine consumers in environmental settings with diverse dietary resources (Corr et al., 2005; Choy et al., 2010a; Honch et al., 2012; Webb et al., 2015, 2018; Ma et al., 2021). Further, nitrogen amino acid measurements (δ15NAA) can provide more accurate trophic level determinations without direct comparisons of associated faunal specimens (Fuller and Petzke, 2017; Ohkouchi et al., 2017; Jaouen et al., 2019). An in-depth discussion of bulk and CSIA-AA is beyond the scope of this work, and the following reviews should be consulted for additional details (Lee-Thorp, 2008; Reitsema, 2015; McMahon and Newsome, 2019; Richards, 2020).
In Korean archaeology, the application of bulk and CSIA-AA analysis to palaeodiet reconstruction has provided important information about subsistence practices in prehistoric populations (Choy and Richards, 2009, 2010b; Choy et al., 2010a, 2012; Shin and Lee, 2009; Kim, H–S., 2010). In particular, isotopic results revealed that the Chulmun (8000–1500 BC) people were mainly dependent on marine food resources before the introduction of domesticated crops (Choy et al., 2012). However, after the arrival of domesticated crops on the Korean Peninsula, during the Mumun period (1500–100 BC) there are few applications of stable isotope analysis to human bone collagen largely due to the lack of human remains from this time. Most previous studies on dietary patterns during the Mumun period are based on the analysis of charred plant remains (Lee, 2001; Lee, 2003; Crawford and Lee, 2003; Ahn, 2010; Kim, M., 2015). In this study, we were fortunate to obtain access to human (n = 7) and animal bones (n = 4) from three Mumun sites (Hwangsok-ri, Jungdo, Maedun Cave), which are all located in the inland portion of central South Korea (Fig. 1). Bulk and δ13CAA analyses were applied to these specimens to directly reconstruct the dietary patterns of the Mumun people. Direct radiocarbon measurements were also conducted on three of these humans to firmly anchor these isotopic measurements in time. In addition, the contribution of each food source to the entire human diet is investigated and the importance of agriculture crops in terms of human consumption patterns, is examined during the Mumun period in South Korea.
Section snippets
The Korean Bronze Age: Mumun culture
Korean archaeologists refer to the Mumun period (1500–100 BC) as the Bronze Age in Korean prehistory. The beginning of the Mumun period is marked by the first appearance of an undecorated plain pottery style, called “Mumun” pottery (Fig. 2A) (Kim, 2015). On the basis of distinct characteristics of artifacts and features, this period can be subdivided into several periods: Early Mumun (1500-800 B.C.), Middle Mumun (800–400 BC), and Late Mumun (400–100 BC) (Bale, 2001; Bale and Ko, 2006; Lee and
Archaeological context
A total of 7 human and 4 animal bone specimens were available for isotopic analyses from the three Mumun sites described below (see Fig. 1). There are an extremely limited number of human and animal specimens dating to the Mumun period in South Korea due to the poor bone perseveration compared with the previous Chulmun period. This is the reason for the small number of Mumun specimens analyzed and presented in this study.
Jecheon Hwangsok-ri
The Hwangsok-ri site lies on a low alluvial deposit floodplain that was formed by a stream meandering on the South Han River in the middle of North Chungchung Province, South Korea, (37° 1′ E, 128° 8’ N). The site is situated 103 m above sea level and is surrounded by high mountains ranging from 500 to 700 m. This site was investigated by the Korean National Museum (KNM) in 1962 and was later investigated by Chungbuk National University Museum (CNUM) in 1982 and 1983 because of the construction
Chuncheon Jungdo
The Jungdo site lies on a small alluvial island in the middle of the confluence of the North Han River and Soyang River near Chuncheon City in Kangwon Province, South Korea (37° 41′ E, 127° 30’ N). This site was investigated by several institutes supervised by the Cultural Heritage Administration (CHA) from 2013 to 2017 because of the construction of Legoland Korea (Korea Institute of Cultural Heritage , 2017). This island site was occupied from the Mumun (1500–100 BC) to Proto-Three Kingdom
Jeongseon Maedun Cave
The Maedun Cave site is located at the bottom of a limestone cliff in Jeongseon County, Kangwon Province, South Korea (37° 19′ E, 128° 41’ N). This cave site is situated 330 m above sea level and is 29 m long and 7 m high and the entrance of the cave is located at the bottom of a slope next to the Chijang River, a tributary to the South Han River. The Maedun Cave is a karstic limestone cave that was periodically occupied. This site was systematically excavated four times by the Yeonsei
Radiocarbon dating
Three human bones (ER-HW1, ER-KO8, ER-JE9) were selected for radiocarbon dating because the collagen extracts from these individuals met the quality control criteria for well-preserved collagen (%C, % N, and C: N) (DeNiro, 1985; van Klinken, 1999). The collagen was dated at BETA Analytic in Florida, USA.
Collagen extraction
The humans and animals from the three Mumun sites were prepared for collagen extraction using the protocol outlined in Richards and Hedges (1999) with the addition of an ultrafiltration step (
Radiocarbon dating
The radiocarbon dates for the three Mumun humans are listed in Table 1. The dates were calibrated by the CALIB REV8.2 program (Stuiver et al., 2020). The Mumun humans date from approximately 770 to 410 cal BC (2σ) with the median probability dates occurring at 625 cal BC for ER-HW1, 535 cal BC for ER-KO8, and 635 cal BC for ER-JE9. Thus, the three humans from each of these sites belong approximately to the Middle Mumun period (800–400 BC) in Korean prehistory.
Bulk isotopic results
The bulk isotopic results for the
Evidence for millet consumption in the mumun period
The bulk isotopic data show that all 6 individuals from the three Mumun sites have high δ13C and low δ15N values, suggesting that C4 plants were consumed. Given the absence of wild C4 plants on the Korean Peninsula, the isotopic results indicate that these Mumun inhabitants in the inland central region of South Korea cultivated millets (foxtail and broomcorn millets) as a major component of their diet. In addition, the CSIA-AA results, in particular the δ13CPhe and δ13CVal values also indicate
Conclusions
Here bulk and δ13CAA isotopic analysis of bone collagen provided direct evidence for the diet of humans and animals from three Middle Mumun sites in central inland South Korea. The isotopic data found that the Mumun humans consumed diets mainly from C4 plants such as broomcorn and foxtail millet. This work represents direct evidence for human millet consumption in the Middle Mumun period. This isotopic evidence is in contrast with the current emphasis on the importance of rice farming during
Declaration of competing interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
Acknowledgements
We are extremely grateful to Soyoung Lee, curator at the Chungbuk National University Museum, Byungmo Kim, director at the Korea Institute of Heritage, and Professor Taesup Cho at Yeonsei University for access to skeletal materials. We would like to thank Marcello Mannino and Anastasia Brozou in Aarhus University for help with sample preparation and collagen extraction. We are also grateful to Tim Howe and Norma Haubenstock for analytical help at the Alaska Stable Isotope Facility at the
References (78)
- et al.
Stable isotope evidence of human diet at the Nukdo shell midden site, South Korea
J. Archaeol. Sci.
(2009) - et al.
Investigation of amino acid δ13C signatures in bone collagen to reconstruct human palaeodiets using liquid chromatography-isotope ratio mass spectrometry
Geochem. Cosmochim. Acta
(2010) - et al.
Stable isotopic analysis of human and faunal remains from the Incipient Chulmun (Neolithic) shell midden site of Ando Island, Korea
J. Archaeol. Sci.
(2012) - et al.
The carbon isotope ratio of alanine in red blood cells is a new candidate biomarker of sugar-sweetened beverage intake
J. Nutr.
(2013) - et al.
A novel marine dietary indicator utilizing compound-specific bone collagen amino acid d13C values of ancient humans
J. Archaeol. Sci.
(2005) - et al.
Extending the limits of palaeodietary studies of humans with compound specific carbon isotope analysis of amino acids
J. Archaeol. Sci.
(2003) - et al.
Hydrolysis and amino acid composition analysis of proteins
J. Chromatogr. A
(1998) - et al.
Nitrogen isotopes and the trophic level of humans in archaeology
J. Archaeol. Sci.
(2007) - et al.
Carbon and nitrogen stable isotope analysis on the diet of Jomon populations from two coastal regions of Japan
J. Archaeol. Sci.
(2010) - et al.
Aminoisoscapes and palaeodiet reconstruction: new perspectives on millet-based diets in China using amino acid δ13C values
J. Archaeol. Sci.
(2021)
Amino acid isotope analysis: a new frontier in studies of animal migration and foraging ecology
Stepwise enrichment of δ15N along food chains: further evidence and the relation between δ15N and animal age
Geochem. Cosmochim. Acta
Advances in the application of amino acid nitrogen isotopic analysis in ecological and biogeochemical studies
Org. Geochem.
Stable isotope evidence for similarities in the types of marine foods used by Late Mesolithic humans at sites along the Atlantic coast of Europe
J. Archaeol. Sci.
A three-phase liquid chromatographic method for δ13C analysis of amino acids from biological protein hydrolysates using liquid chromatography-isotope ratio mass spectrometry
Anal. Biochem.
Bone collagen quality indicators for palaeodietary and radiocarbon measurements
J. Archaeol. Sci.
Compound-specific amino acid isotopic proxies for detecting freshwater resource consumption
J. Archaeol. Sci.
Review of the neolithic agriculture in southern Korea
Journal of the Korean Neolithic study (Hankuk Shinsukki Yeongu)
Beginning of agriculture and sedentary settlement in East Asia
Journal of the Korean Neolithic study (Hankuk Shinsukki Yeongu)
Crop assemblage of Korean bronze age
Journal of the Honam Archaeological Society
The emergence of rice agriculture in Korea: archeobotanical perspectives
Archaeological and Anthropological Sciences
Dietary reconstruction by stable isotopic analysis: the Konam-r shell midden in Korea
Journal of the Korean Ancient Historical Society
Archaeology of early agriculture in Korea: an update on recent developments
Bulletin of the Indo-pacific Prehistory Association
An examination of surplus and storage in prehistoric complex societies using two settlements of the Korean peninsula
World Archaeol.
Craft production and social change in Mumun pottery Period Korea
Asian Perspect.
Trophic level isotopic enrichment of carbo and nitrogen in bone collagen: case studies from recent and ancient terrestrial ecosystems
Int. J. Osteoarchaeol.
Improved collagen extraction by modified Longin method
Radiocarbon
Isotopic reconstruction of the late Longshan period (ca. 4200-3900 BP) dietary complexity before the onset of state-level societies at the wadian site in the ying river valley, central plains, China
Int. J. Osteoarchaeol.
The Archaeology of Early Rice Cultivation in Korean Peninsula
Isotopic evidence for diet in the middle Chulmun period: a case study from the Tongsamdong shell midden, Korea
Archaeological and Anthropological Sciences
Excavation Report of Chewon Hwangsok-Ri District B, Archaeological Investigation of Cultural Properties in Chungju Dam Area
Development of N-acetyl methyl ester derivatives for the determination of δ13C values of amino acids using gas chromatography-combustion- isotope ratio mass spectrometry
Anal. Chem.
Agricultural origins in the Korean peninsula
Antiquity
Agricultural origins in North China pushed back to the Pleistocene-Holocene boundary
Proc. Natl. Acad. Sci. Unit. States Am.
An isotopic perspective on animal husbandry at the Xinzhai site during the initial stage of the Xia Dynasty (2,070 – 1,600 BC)
International Journal of Osteoarcaheology
Postmortem preservation and alteration of in vivo bone collagen isotope ratios in relation to palaeodietary reconstruction
Nature
The dietary protein paradox and threonine 15N-depletion: pyridoxal-5’-phosphate enzyme activity as a mechanism for the δ15N trophic level effect
Rapid Commun. Mass Spectrom.
The isotopic composition of carbon and nitrogen in individual amino acids isolated from modern and fossil proteins
J. Archaeol. Sci.
First molecular and isotopic evidence of millet processing in prehistoric pottery vessels
Sci. Rep.
Cited by (6)
Aquatic resource consumption at the Odense leprosarium: Advancing the limits of palaeodiet reconstruction with amino acid δ<sup>13</sup>C measurements
2022, Journal of Archaeological ScienceCitation Excerpt :δ13CAA measurements have become a particularly important tool in the fields of ecology and biochemistry (e.g. Johnson et al., 1998; Scott et al., 2006; McCullagh et al., 2008; Arthur et al., 2014; Thorp and Bowes, 2017; Liew et al., 2019; Matos and Jackson, 2020). They have also proven valuable for palaeodietary reconstructions (e.g. Hare et al., 1991; Choy et al., 2010; Colonese et al., 2014; Cooper et al., 2016; Mora et al., 2017; Choy et al., 2021; Soncin et al., 2021). In contrast to the isotopic analysis of bulk tissues, which reflects the sum of different dietary inputs of an element in the analysed sample (i.e. C3, C4, freshwater, marine), δ13CAA measurements offer the advantage of differentiating between dietary resources that overlap isotopically (e.g. C3 vs. freshwater or C4 vs. marine).
Multi-proxy analysis of starchy plant consumption: a case study of pottery food crusts from a Late Iron Age settlement at Pada, northeast Estonia
2024, Vegetation History and ArchaeobotanyThe importance of wild resources as a reflection of the resilience and changing nature of early agricultural systems in East Asia and Europe
2022, Frontiers in Ecology and Evolution