C4 plants (e.g. maize, millet), part of our current diet, are only endemic of reduced areas in South-Europe due to their need of warm climates. Since the first vestiges of agriculture in Europe remains of C4 plants were recorded but their overall proportion in the human diet remains unknown. Therefore, isotopic (δ13C and δ15N) composition of bone collagen from the skeletal remains (human and animals) of a Celtic population, Cenomani Gauls, from Verona (3rd to 1st century BC) in the NE Italy provide a new perspective on this matter. The δ13C collagen values of 90 human skeletal individuals range between −20.2‰ and −9.7‰ (V-PDB) with a mean value of −15.3‰. As present day C4 plants have δ13C values around −11‰, which is equivalent to −9.5‰ for samples of preindustrial age, the less negative δ13C values in these individuals indicate a diet dominated by C4 plants. This palaeodietary study indicates that some European populations predominantly consumed cultivated C4 plants 2100 year B.P. This is supported by the paleobotanical records and ancient Roman sources (e.g. Pliny the Elder), which indicate that millet was a staple food in South-Europe.
The term C4 plants refers to the type of photosynthetic pathway (Hatch-Slack or C4 cycle) used by these plants, which has less isotopic discrimination than the C3 cycle (C3 plants). In the C4 cycle the first stable compound namely oxaloacetic acid is formed by 4 carbon atoms. This group includes warm climate grasses like maize, millets, sorghum and sugar cane, among others1.
Paleobotanical studies have shown the presence of domesticated C4 plants (in particular broomcorn or Panicum Miliaceum L. and foxtail millet or Setaria Italica L. Beauv.) in Central and Eastern Europe as early as 5000-4000 BC for Panicum Miliaceum and Late Bronze Age for Setaria Italica2; while in Asia (China) and in the Caucasian region (Georgia) this is documented as early as ca. 10000 years B.P.3,4,5. Based on the botanical evidence, it seems that millet was first introduced into Central and Eastern Europe from the Steppe regions during the Neolithic period6,7,8. Broomcorn millet seems to have arrived in the Mediterranean zone from the north or the north-east9; in northern Italy, millet appears in early Bronze Age settlements (1700-1500 BC)2. The earliest records of foxtail millet (Setaria Italica L. Beauv.) come from Peigang and Cishan (North China) in the 6th millennium BC3. In Europe the first carbonized seeds of foxtail millet appear in the 2nd millennium BC, from Bronze Age settlements in central Europe10 and France11. It is also reported from the late Bronze age Kastanas site (Macedonia, Greece)12. In the Near East the earliest evidence for foxtail millet cultivation dates back to the Iron Age (c. 600 BC) in Tille Höyük, south-east Turkey7. However, these data only indicate the presence of millet, but do not reveal their role in the human diet.
C4 plants are typical of warm climates and their abundance is highly correlated with climatic factors, such as temperature, precipitation and the degree of aridity. In general, they are not present in environments where night temperatures are lower than 8 °C13,14. Nowadays in Europe C4 biomass is very scarce; however these plants are naturally present in small proportions especially in the SW-Europe (e.g. Spain, Portugal, SW-France and Italy)15. Before the onset of agriculture, herbivores collagen isotopic δ13C values from S-Italy (32.6 to 13.3 ka B.P.) suggest that C4 biomass was practically absent (calculated vegetal biomass is around −25‰ vs V-PDB)16. Even during the warmer periods of the Late Miocene, fossil isotopic data indicate the absence of C4 biomass in central and southern Europe17,18. Man has introduced certain species, such as millet, with a planting strategy in the warm season (i.e. summer), possibly as a response to Holocene arid periods11.
The stable isotope composition (δ13C and δ15N) is a very effective tool to study the trophic web in ecosystems19,20,21,22,23. This methodology is crucial for studying past ecosystems and paleodiets, because direct observation is impossible24,25,26,27. In addition this technique allows quantitative analysis, which even in current ecosystems is difficult to obtain with the classical methods of observation. Isotopic carbon traceability suffers less change in the steps of the food chain than isotopic nitrogen one. Therefore, the footprint of primary producers (e.g. plants) is clearer28.
The importance of carbon isotopes as a racer for the presence of C4 plants in the diet, is that atmospheric CO2 is fixed into organic matter by the enzyme PEP carboxylase (C4 plants) which discriminates much less against 13C than the enzyme RuBisCO (C3 plants)29. In present day C3 plants biomass show typical δ13C values around −26‰ (V-PDB), while C4 plants are around −11‰ (V-PDB)30,31, −24.5‰ and −9.5‰ (V-PDB), respectively in preindustrial age, because δ13C values of CO2 were less negative by 1.5‰ compared to the present values (−8‰ V-PDB). This 15‰ difference between C3 and C4 plants allows an accurate calculation of the percentage of C4 plants in the diet. The δ13Ccollagen values of humans and animals are proportional to the isotopic signal from the base of the food chain (plants), but enriched by 0.8 and 1.3‰ for herbivores and carnivores, respectively32. The δ15N of the collagen is also related with the food chain and can be used to evaluate the trophic system, because in a particular ecosystem there is a significant enrichment in 15N between 3 and 5‰ for each trophic level25,26,27.On the other hand δ15N cannot be used to distinguish between C3 and C4 plants consumption.
There is little knowledge about the nutritional habits of protohistorical populations such as Pre-Roman-Celtic ones. Therefore, we performed an isotopic study to unveil the dietary habits of the Celtic population Cenomani Gauls, from the necropolis of Seminario Vescovile in Verona (Italy) dated between the 3rd to 1st century BC33. This necropolis counts with a minimum of 174 skeletons in a good state of preservation, and the majority of them are non-adults (see Supplementary Information for detailed descriptions of the archaeological context). Surprisingly, we recorded relatively high, i.e. less negatives, δ13Ccollagen values in the human samples, and even in some animals found in the necropolis. In our initial considerations, we suspected the presence of protein in the diet from marine sources, or even anomalous fresh water sources (enriched 13C in DIC-Dissolved Inorganic Carbon, “dead carbon” from marine carbonates), or alternatively an extensive consumption of C4 plants. The first hypothesis seemed from the beginning improbable, taking into account the geographic location of the necropolis, which was far from the sea (about 120 km). Additionally, the less negative δ13C collagen, −10‰ (V-PDB), is higher than what would be expected for a signal from marine primary production22. A second alternative explanation is a freshwater tropic web with an anomalous enriched 13C source of carbon (DIC) from dissolution or thermic decomposition of carbonates. This geochemical scenario is present in some areas of Italy34 in which natural water becomes enriched in CO2. This archaeological site was near to the Adige River that runs through Verona. Therefore, water samples from the Adige river and its tributaries were collected and analysed. In addition, 14C dating was done on some human remains to detect the presence of “dead carbon”.
The main objective of this study is to demonstrate that these less negative δ13C values are related to the consumption of C4 plants and refute the improbable hypothesis of a significant marine or anomalous fresh water dietary intake (enriched in 13C). At the same time, we set out to quantify the proportion of C4 plants in the diet and propose an interpretation about the alimentary habits of Celtic populations of Italy which up to now have been elusive.
Isotopic values of the human and animal sample from Verona
The human δ13C values range from −20.2‰ to −9.7‰ (V-PDB) with a mean value of −15.3‰ (±2.2‰) (V-PDB) while δ15N values are between +6.9‰ and +12.9‰ (AIR), showing a mean value of +9.4‰ (±1.3‰) (AIR) (Fig. 1; Table 1; Supplementary Table S2). The atomic C/N ratio of the samples falls inside the range of 2.9–3.6, which corresponds to typical values of well-preserved samples, as suggested by DeNiro35. Isotopic data from animal bones (Tables 1 and 2) suggests that domesticated herbivores had a diet mainly based on C3 plants, although one of these (VRAR-1 with −17.2‰ V-PDB) showed a less negative δ13C value that could suggest that this animal partly fed on C4 plants. Dogs (n = 2) usually eat men’s leftovers, showing relatively high δ13C values (≈ −13‰ V-PDB). One of them also has a relatively low δ15N value for an omnivore. This implies a diet poor in animal proteins, supporting the hypothesis of an important influence in their diet of human food scabs, rich in (C4) plants.
Isotopic values of DIC of Adige’s river and Radiocarbon data
The DIC δ13C data (Table 3 and Supplementary Figure S1b) of the Adige river ranges between −4.5‰ and −5.0‰ (V-PDB); this, after isotopic fractionation processes of photosynthesis in algae, would result in values ranging from −23.5‰ and −24‰ (V-PDB) and consequently it would imply δ13C values in fish tissues very close to these values (≈ −22.5‰ to −23‰ V-PDB). These data would result in a value for human collagen resulting from an exclusively fish diet (an extreme that would be relatively rare), between −20‰ to −22‰ (V-PDB), which is not compatible with the least negative values found in this work. The rest of δ13C values of DIC of other tributaries, wells, etc. are even more negative so they also cannot justify the higher δ13C values found in collagen of human remains36.
On the other hand, the age obtained from 14C dating of bone collagen from four individuals (those with less negative δ13C values) is consistent with that extrapolated (Table 4) from the preliminary archaeological analysis of the grave goods36. This indicates the absence of “dead” carbon (e.g. dissolution of marine carbonate rocks), which would lead to apparently much older ages. Such dissolved inorganic carbon (DIC) have δ13C values close to +0‰ or positive values, which would also lead to an aquatic trophic chain with less negative values of δ13C, this being the only alternative to the consumption of C4 plants. The absence of “dead” carbon in the humans collagen rules out this hypothesis, and thus consequently supports the presence of C4 plants in the diet of these individuals.
The isotopic results show the important role that C4 plants had in the diet of this Celtic population from Verona (Fig. 1). Generally, δ13C values of −20‰ (V-PDB) or less negatives would indicate some C4 plant contributions. Thus the vast majority of studied individuals (over 90%) seem to include C4 plants in a direct way (or indirectly through the consumption of herbivores that fed on them) in their diet. Additionally, adult females (mean value of 48.8 ± 15.1%) show significantly (Mann-Whitney U test = 198.0; p = 0.008) higher consumption of C4 plants than adult males (mean of 37.4 ± 16.8%) (Fig. 2). We also found a significant statistical difference in δ15N values between sex in the adult group (t = 3.15 p ≤ 0.01): men display higher δ15N values compared to women (Fig. 3). Thus, there is a clear differentiation in the diet according to sex with a higher intake of animal protein (meat and meat products) for men, while the diet of women included more cereals and vegetable proteins. It is important to note, that some adults related with high intakes of animal protein (highest values in δ15N) have less negative values in δ13C (≈−12‰ vs V-PDB, see for example individuals VRSV-12 and VRSV-24 in the Supplementary Table S2), indicating that domestic herbivorous have also consumed large amount of C4 plants, although the few herbivorous studied show a consumption of C3 plants. However, two dogs show δ13C values which are very similar to those of humans (Fig. 1). Especially the younger dog (VRSV-94) presents a typical value of the middle-low animal protein intake of omnivores: δ15N = +7.1‰ (AIR). While the δ13C value of −13.7‰ (V-PDB) is very close to those of the humans with a C4 diet (Table 2). As mentioned before, a possible explanation is that dogs were fed with the impoverished-protein waste from the meals of their owners.
DIC values (Table 3) from local meteoric water show relatively negative δ13C values (from −4.5 to −13.3‰ vs V-PDB; i.e. an aquatic diet should be approximately between −23.5 and −32.3‰ vs V-PDB) and 14C values of the human samples with less negative δ13Ccollagen values does not indicate the presence of “dead carbon”. Consequently, this excludes a freshwater diet to explain the measured less negative isotopic values of this particular Celtic population and thus supports the hypothesis of a large consumption of C4 plants in their diet. Furthermore, δ15N values in humans (+9.4‰ AIR) plot in about a one trophic level above terrestrial herbivorous (+4.7‰ AIR)36, rule out a marine diet, in agreement with the relative large distance from the coast.
Considering that there are not many known cultivated C4 plant species in this time period (3rd-1st BC), the hypothesis of millet consumption seems reasonable based on the archaeological record and ancient written source. In fact, the investigated necropolis is located in an area which is still today characterized by a fertile plane (called Pianura Padana or Po valley): it offers ideal climatic and environmental conditions for the cultivation of C4 plants during the warm seasons (spring-summer). Pliny the Younger (Epistulae, IV, 6,1) praised the Po Valley region and wrote “in regione Transpadana summa abundantia”37. Since the Middle and Late Bronze age (1550-1170 years BC) this plane was characterized by intensive agriculture, pastoralism and the demand of large amounts of wood for building sites. This lead to a heavy deforestation of the whole Po plain and converting it into an artificial steppe devoted to cereal crops38. Furthermore, paleoclimate records of lake sediments and speleothems show trends towards a drier climate, or alternating wet and dry climates, between 2500 and 2000 BP39,40. This might have induced a change in cropping strategies and the consequent introduction of C4 plant cultivation (probably millet).
Unfortunately, during the archaeological excavation of Verona, archaeologists have not found seeds (or charcoal) and the ceramic grave goods (vessels and others) are still under study and initially seem not to indicate macroscopic remains of organic waste. Some previous archaeobotanical studies of Neolithic, Bronze and Iron Age sites of the NE of Italy, and particularly of the area of Verona, seem to confirm the presence of Panicum Miliaceum and of Setaria italica among the carpological remains41,42. Another comparative paleobotanical study relating to some Iron Age sites located between the Northern and Southern Alps (Eastern Switzerland, Austria and Northern Italy), also describes the presence of millet (Panicum Miliaceum L.) and foxtail millet (Setaria Italica L. Beauv.) remains43. This is also confirmed by the results of the study about carpological remains found at the site of Oppeano (Verona), dated to the second Iron Age (about 6th to 3rd century BC) and located in the same geographical context of the Seminario Vescovile necropolis. The majority of the determined cereal remains correspond to millet (Panicum miliaceum L.) and foxtail millet (Echinochloa crus-galli L. Beauv. and Setaria italica L. Beauv)44. Thus, the Iron Age seems to be characterized by a greater crops specialization that fits with the assumption of the pursuit of a cereal type that best fits different climates (biomass increase with more efficiency in water use). In this case of the sandy Pianura Padana (Verona), the crops of millet were preferred, because it is a plant that adapts very well to poor substrates characterized by water scarcity during summer44.
Finally, other isotopic results from bone collagen analysis of some individuals proceeding from the Bronze Age necropolis of Olmo di Nogara, Verona (1600-1200 cal. BC) and of Arano di Cellore, Verona (2040-1890 cal. BC) support the hypothesis of C4 plants consumption, and in particular of millet in some areas of the Verona province45,46(Fig. 4). In conclusion, to these archaeological data we add the testimonies of some ancient authors such as Pliny the Elder (Naturalis Historiae XVIII, 83-84) and Columella (De Re Rustica, 2, 9, 14–16) who report the use of millet flour for the production of bread and a sort of porridge cooked in water and salt and often accompanied with vegetables and cheese and very rarely with meat. Pliny (XVIII.XXIV) exactly noted: “millet is used to prepare a very white puls (i.e. similar to present-day polenta). Panic, when ground and freed from bran, and millet as well, makes a porridge which, especially with milk, is not to be despised even in time of plenty”. Columella (2.9.19), agreed with Pliny and wrote: “bread is made of millet, and it may be eaten without distaste before it cools”.
The isotopic data obtained in this study reveal that the proportion of C4 plants was substantial (above ≈40%) in the daily diet of this Celtic population. Traces of C4 plant consumption are reported in other studies45,46 from more ancient necropolis of the zone. While Olmo de Nogara (ODN) dated to Middle Bronze Age share very similar isotopic values with Verona (Fig. 4), confirming a preponderant C4 plants based diet, Arano di Cellore (AC), dated to Early Bronze Age, shows a diet based on the consumption of C3 cereal-type plants. Hence, the data from AC and ODN firmly place the shift in C4 crop use in the region at a transition period between the late phases of the Early Bronze Age and the beginning of the Middle Bronze Age46, consequently our data show that successively, in pre-Roman times, the diet of most habitants of the zone was almost exclusively based on C4 plants. This, indirectly indicates that this Celtic population had mastered agriculture techniques to such an extent that they could live off the harvest of their cultivated crops the year round.
A sample of 90 human ribs, consisting of both sexes and different ages (Supplementary Information Table S1), and 7 animal bones, was selected for analysis of bone collagen. The animal bone sample is composed of 5 herbivorous species (2 horses, 1 goat/sheep and 2 cows) and 2 omnivorous species (2 dogs). The extraction of collagen is performed using the protocol described by Bocherens et al.47,48 and following the routine procedures of the Stable Isotope Biogeochemistry Laboratory of the Andalusian Institute of Earth Sciences (CSIC, Granada, Spain). We also determined the current DIC values of the Adige’s river (and of some of its tributaries) and dated with 14C the collagen samples of the less negative human values (a source of “dead” inorganic carbon would show abnormally high ages).
The δ13C mean values of present day C3 and C4 plants are respectively −26‰ and −11‰ (V-PDB)49,50, but before the industrial revolution the isotopic composition of atmospheric CO2 was 1.5‰ less negative51. Hence, to make a more precise estimate we considered that these two carbon sources would respectively correspond to values of −24.5‰ and −9.5‰ (V-PDB) (see Supplementary Information for detailed descriptions about the different methodologies applied).
How to cite this article: Laffranchi, Z. et al. Stable C & N isotopes in 2100 Year-B.P. human bone collagen indicate rare dietary dominance of C4 plants in NE-Italy. Sci. Rep. 6, 38817; doi: 10.1038/srep38817 (2016).
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Van der Merwe, N. J. Carbon isotopes, photosynthesis and archaeology: different pathways of photosynthesis cause characteristic changes in carbon isotope ratios that make possible the study of prehistoric human diets. Am. Sci. 70, 596–606 (1982).
Zohary, D. & Hopf, M. Domestication of plants in the Old world. (Clarendon Press, Oxford, 1993).
An, Z. Prehistoric agriculture in China. in Foraging and farming: the evolution of plant exploitation (eds Harris, D. R. & Hillman, G. C. ) 643–649 (Unwin & Hyman, London, New Jersey, 1989).
Lisitsina, G. N. The Caucasus- A centre of ancient farming in Eurasia. in Plants and ancient man (eds Van Zeist, W. & Casparie, W. A. ) 293–305 (Balkema, Rotterdam, 1984).
Cheng-Bang, A. et al. Variability of the stable carbon isotope ratio in modern and archaeological millets: evidence from Northern China. J. Archaeol. Sci. 53, 316–322 (2015).
Hjelmqvi, H. Spelt and Millet from Bronze Age of Southern Sweden and some observations on its later history in Sweden. Bot. Notiser. 122, 260–283 (1969).
Nesbitt, M. & Summers, G. D. Some recent discoveries of millets (Panicum miliaceum and Setaria italica) at excavations in Turkey and Iran. Anatolian Stud. 38, 85–97 (1988).
Murphy, E. M. et al. Iron Age pastoral nomadism and agriculture in the eastern Eurasian steppe: implications from dental palaeopathology and stable carbon and nitrogen isotopes. J. Archaeol. Sci. 40, 2547–2560 (2013).
Van Zeist, W. Aperçu sur la diffusion des végétaux cultivés dans la région Méditerranéene. in Colloque sur la mise en place, l’évolution et la caractérisation de la flore et la végétation circumméditerranéenne (Fundation L. Emberger), 129–145 (Naturalia Monspelensia, Montpellier, 1980).
Netolitzky, F. Die Hirse aud alten Funden. Sitzungsber. K. Akad. Wiss. Wien. 73, 1–35 (1914).
Goude, G., Rey, L., Toulemonde, F., Cervel, M. & Rottier, S. Dietary changes and millet consumption in northern France at the end of Prehistory: evidence from archaeobotanical and stable isotope data. Environ. Archaeol. 21, doi: 10.1080/14614103.2016.1215799 (2016).
Kroll, H. J. Die Pflanzenfunde. in Kastanas. Ausgrabungen in einem Siedlungshügel der Bronze- und Eisenzeit Makedoniens 1975-1979. Prähistorische Archäologie in Südosteuropa Vol. 2 (Spiess, Berlin, 1983).
Teeri, J. A. & Stowe, L. G. Climatic patterns and the distribution of C4 grasses in North America. Oecol. 23, 1–12 (1976).
Ehleringer, J. R., Cerling, T. E. & Helliker, B. R. C4 photosynthesis, atmospheric CO2, and climate. Oecol. 112, 285–299 (1997).
Pyankov, V. I., Ziegler, H., Akhani, H., Deigele, C. & Luttge, U. European plants with C 4 phosynthesis: geographical and taxonomic distribution and relations to climate parameters. Bot. J. Linn. Soc. 163, 283–304 (2010).
Iacumin, P., Bocherens, H. & Huertas, A. A stable isotope study of fossil mammal remains from the Paglicci cave, Southern Italy. N and C as palaeoenvironmental indicators. Earth. Planet Sci. Lett. 148, 349–357(1997).
Domingo, L. et al. Late neogene and early quaternary paleoenvironmental and paleoclimatic conditions in southwestern Europe: isotopic analyses on mammalian taxa. PLoS ONE 8(5), e63739 (2013).
Tütken, T., Kaiser, T. M., Vennemann, T. & Merceron, G. Opportunistic feeding strategy for the earliest old world hypsodont equids: evidence from stable isotope and dental wear proxies. PLoS ONE 8(9), e74463 (2013).
Anderson, W. B. & Polis, G. A. Nutrient fluxes from water to land: seabirds affect plant nutrient status on Gulf of California islands. Oecol. 118, 324–332 (1999).
Balter, V., Simon, L., Fouillet, H. & Lecuyer, C. Box-modeling of N-15/N-14 in mammals. Oecol 147, 212–222 (2006).
Cabana, G. & Rasmussen, J. B. Modelling food chain structure and contaminant bioaccumulation using stable nitrogen isotopes. Nature 372, 255–257 (1994).
Chisholm, B. S., Nelson, D. E. & Schwarcz, H. P. Stable-carbon isotope ratios as a measure of marine versus terrestrial protein in ancient diets. Science 216, 1131–1132 (1982).
Vander Zanden, M. J., Casselman, J. M. & Rasmussen, J. B. Stable isotope evidence for the food web consequences of species invasions in lakes. Nature 401, 464–467 (1999).
Bocherens, H., Drucker, D. G. & Madelaine, S. Evidence for a 15N positive excursion in terrestrial foodwebs at the Middle to Upper Palaeolithic transition in south-western France: implications for early modern human palaeodiet and palaeoenvironment. J. Hum. Evol. 69, 31–43 (2014).
Ambrose, S. H. & DeNiro, M. J. Bone nitrogen isotope composition and climate. Nature 325, 201–201 (1987).
DeNiro, M. J. Postmortem preservation and alteration of in vivo bone-collagen isotope ratios in relation to paleodietary reconstruction. Nature 317, 806–809 (1985).
Hedges, R. E. M. & Reynard, L. M. Nitrogen isotopes and the trophic level of humans in archaeology. J. Archaeol. Sci. 34, 1240–1251 (2007).
Post, D. M. Using stable isotopes to estimate trophic position: Models, methods, and assumptions. Ecology 83, 703–718 (2002).
Bender, M. M. Variations in C-13/C-12 ratios of plants in relation to pathway of photosynthetic carbon dioxide fixation. Phytochemistry 10, 1239–1244 (1971).
Cerling, T. E. The stable isotopic composition of modern soil carbonate and its relationship to climate. Earth Planet. Sci. Lett. 71, 229–240 (1984).
Peterson, B. J. & Fry, B. Stable isotopes in ecosystem studies. Annu Rev Ecol System 18, 293–320 (1987).
Bocherens, H. & Drucker, D. Trophic level isotopic enrichment of carbon and nitrogen in bone collagen: case studies from recent and ancient terrestrialecosystems. Int. J. Osteoarchaeol. 13, 46–53 (2003).
Laffranchi, Z., Martín Flórez, J. S., Jiménez Brobeil, S. A. & Castellani, V. 2015. Foot polydactyly and bipartite medial cuneiform: a case of co-occurrence in a Celtic skeleton from Verona (Italy). Homo. 66, 216–228 (2015).
Di Benedetto, F. et al. Biotic and inorganic control on travertine deposition at Bullicame 3 spring (Viterbo, Italy): A multidisciplinary approach. Geochim Cosmochim Ac 75, 4441–4455 (2011).
DeNiro, M. J. Postmortem preservation and alteration of in vivo bone collagen isotope ratios in relation to palaeodietary reconstruction. Nature 317, 806–809 (1985).
Laffranchi, Z. Antropología de la población Pre-Romana de Verona (Italia). PhD Thesis. (Universidad de Granada, Granada, 2015).
Murphy, C. Finding millet in the Roman world. Archaeol. Anthropol. Sci. 8, 65–78 (2016).
Cremaschi, M., Mercuri, A. M., Torri, P., Florenzano, A. & Pizzi, C. Climate change versus land management in the Po Plain (Northern Italy) during the Bronze Age: New insights from the VP/VG sequence of the Terramara Santa Rosa di Poviglio. Quat. Sci. Rev. 136, 153–172 (2016).
McDermott, F. et al. Holocene climate variability in Europe: Evidence from delta O-18, textural and extension-rate variations in three speleothems. Quat. Sci. Rev. 18, 1021–1038 (1999).
Magny, M. et al. North-south palaeohydrological contrasts in the central Mediterranean during the Holocene: tentative synthesis and working hypotheses. Clim Past. 9, 2043–2071 (2013).
Pisoni, L. Aspetti e problemi dell’occupazione del territorio, dell’organizzazione sociale e dell’economia agro-pastorale nell’età del ferro atesina: un’introduzione allo studio dei sistemi alimentari. Preistoria Alpina 44, 225–243 (2009).
Rottoli, M. Crop diversity between Central Europe and the Mediterranean: aspects of northern Italian agriculture in Plants and people: choices and diversity through time (eds. Chevalier, A. et al.) 75–81 (Oxbox book, Oxford, 2014).
Schmidl, A., Jacomet, S. & Oeggl, K. Distribution patterns of cultivated plants in the Eastern Alps (Central Europe) during Iron Age. J. Archaeol. Sci. 34, 243–254 (2007).
Carra, M. L. Per una storia della cerealicoltura in Italia settentrionale dal Neolitico all’età del Ferro: strategie adattive e condizionamenti ambientali. PhD Thesis. (Alma Mater Studiorum, Bologna, 2012).
Tafuri, M. A., Craig, O. E. & Canci, A. Stable isotope evidence of consumption of millet and others plants in Bronze Age Italy. Am. J. Phys. Anthropol. 139, 146–153 (2009).
Varalli, A. et al. Dietary continuity vs. discontinuity in Bronze Age Italy. The isotopic evidence from Arano di Cellore (Illasi, Verona, Italy). J. Archaeol. Sci: Rep. 7, 104–113 (2016).
Bocherens, H. et al. Isotopic biogeochemistry (13C, 15N) of fossil vertebrate collagen: application to the study of a past food web including Neanderthal man. J. Hum. Evol. 20, 481–492 (1991).
Bocherens, H. et al. Paleobiological implications of the isotopic signatures (13C, 15N) of fossil mammal collagen in Scladina cave (Sclayn, Belgium). Quat. Res. 48, 370–380 (1997).
Bender, M. M. Mass spectrometry studies of carbon-13 variations in corn and other grasses. Radiocarbon 10, 468–472 (1968).
O’Leary, M. H. Carbon isotopes in photosynthesis. BioScience 38, 328–336 (1988).
Friedli, H., Lötscher, H., Oeschger, H., Siegenthaler, U. & Stauffer, B. Ice core record of the 13C/12C ratio of atmospheric CO2 of the past two centuries. Nature 324, 2 (1986).
The authors would like to thank Dr. Giuliana Cavalieri Manasse of the Soprintendenza Archeologica of Verona to provide the opportunity to study this skeletal collection and the archaeologists Simon Thompson and Marzia Bersani for the use of their archaeological data. The isotopic analysis were funded by the Projects RNM-8011(Junta de Andalucía, Spain), HAR 2016-75788 (Ministerio de Economía y Competitividad, Spain) and the research group RNM-309 (Junta de Andalucía, Spain). We also wish to express our gratitude to Laura Bignotto (independent researcher) for her assistence with the water sampling of Verona area and Alexander E.S. Van Driessche (ISTerre, Grenoble, France) for proof reading the English version of the manuscript. The comments and suggestions from the Editor Jens Ormö and two anonymous reviewers greatly improved the paper.
The authors declare no competing financial interests.
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Laffranchi, Z., Huertas, A., Jiménez Brobeil, S. et al. Stable C & N isotopes in 2100 Year-B.P. human bone collagen indicate rare dietary dominance of C4 plants in NE-Italy. Sci Rep 6, 38817 (2016). https://doi.org/10.1038/srep38817
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