8 research outputs found

    Isotope record of the first lower molars of domestic cattle from the early medieval Pohansko-Southern bailey and Kostice-”Zadní hrúd” localities (Czech Republic)

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    In this essay, we focused on the evaluation of isotope analyses (δ13Ccoll and δ15Ncoll) of the first lower molars (m1) of domestic cattle (Bostaurus) from two early medieval Pohansko-Southern bailey (Pohansko-JP) and Kostice-”Zadní hrúd” (Kostice-ZH) sites. The aim of the study is the evidence of the breast-feeding effect of calves and subsequent weaning on the dentine average isotope  composition. Results from both sites are compared with the data obtained from recent experimental cattle breeding. Possible differences in the cattle breeding between both studied localities are evaluated. The first lower molars of the domestic cattle (n = 15) were selected for analyses from both sites supplemented by a sample of the compact bone of the shinbone of an adult individual from the Pohansko-JP site. The determination of the ontogenetic age of the analyzed individuals is based on the dentition development stage. For the purpose of isotope analyzes (δ13Ccoll and δ15Ncoll), dentine collagen was extracted from all tooth crowns. The δ13Ccoll dentine values of the m1 of cattle from the Pohansko-JP ranged from -17.75‰ to -21.8‰ (n = 11) with mean value of -19.81 ± 1.03‰. δ15Ncoll values for dentine of all m1 samples from Pohansko-JP range from 6.2‰ to 11.87‰ with mean value of 8.29 ± 1.71‰ (n = 11). The highest δ15Ncoll values were observed primarily in samples of juvenile individuals, with the exception of one adult specimen (10.90 ‰). δ13Ccoll values in m1 of adult individuals from the Kostice-ZH site range from -19.30‰ to -20.91‰ (n = 4). The mean value -19.83 ± 1.01‰ is lower if compared to results from recent experimental breedings. The volume of 15N isotope is significantly lower contrary to those in Pohansko-JP and aforementioned experimental study. It can be assumed that the diet of the cattle in both studied sites was primarily based on C3 plants; however, we cannot exclude a small admixture of C4 plants (millet) in the diet of some observed individuals. The cattle from the Pohansko-JP could be driven to graze from the open meadows up to the ecotones in the vicinity of the forest which is partly supported by the palaeobotanic record. In Kostice-ZH site, the grazing in open meadows was most prevalent. The volume of 15N from the Pohansko-JP site shows that in most cases, calves were not prematurely weaned. In samples from Kostice-ZH, the 15N content in adult individuals was significantly lower contrary to values from Pohansko-JP. A present stage of the knowledge indicates that the cattle (i. e., including mother cows) was probably fed plants characterized by low δ15N values; however, a premature weaning to increase the milk production cannot be excluded.In this essay, we focused on the evaluation of isotope analyses (δ13Ccoll and δ15Ncoll) of the first lower molars (m1) of domestic cattle (Bostaurus) from two early medieval Pohansko-Southern bailey (Pohansko-JP) and Kostice-”Zadní hrúd” (Kostice-ZH) sites. The aim of the study is the evidence of the breast-feeding effect of calves and subsequent weaning on the dentine average isotope  composition. Results from both sites are compared with the data obtained from recent experimental cattle breeding. Possible differences in the cattle breeding between both studied localities are evaluated. The first lower molars of the domestic cattle (n = 15) were selected for analyses from both sites supplemented by a sample of the compact bone of the shinbone of an adult individual from the Pohansko-JP site. The determination of the ontogenetic age of the analyzed individuals is based on the dentition development stage. For the purpose of isotope analyzes (δ13Ccoll and δ15Ncoll), dentine collagen was extracted from all tooth crowns. The δ13Ccoll dentine values of the m1 of cattle from the Pohansko-JP ranged from -17.75‰ to -21.8‰ (n = 11) with mean value of -19.81 ± 1.03‰. δ15Ncoll values for dentine of all m1 samples from Pohansko-JP range from 6.2‰ to 11.87‰ with mean value of 8.29 ± 1.71‰ (n = 11). The highest δ15Ncoll values were observed primarily in samples of juvenile individuals, with the exception of one adult specimen (10.90 ‰). δ13Ccoll values in m1 of adult individuals from the Kostice-ZH site range from -19.30‰ to -20.91‰ (n = 4). The mean value -19.83 ± 1.01‰ is lower if compared to results from recent experimental breedings. The volume of 15N isotope is significantly lower contrary to those in Pohansko-JP and aforementioned experimental study. It can be assumed that the diet of the cattle in both studied sites was primarily based on C3 plants; however, we cannot exclude a small admixture of C4 plants (millet) in the diet of some observed individuals. The cattle from the Pohansko-JP could be driven to graze from the open meadows up to the ecotones in the vicinity of the forest which is partly supported by the palaeobotanic record. In Kostice-ZH site, the grazing in open meadows was most prevalent. The volume of 15N from the Pohansko-JP site shows that in most cases, calves were not prematurely weaned. In samples from Kostice-ZH, the 15N content in adult individuals was significantly lower contrary to values from Pohansko-JP. A present stage of the knowledge indicates that the cattle (i. e., including mother cows) was probably fed plants characterized by low δ15N values; however, a premature weaning to increase the milk production cannot be excluded

    Data from: The evolution of dual meat and milk cattle husbandry in Linearbandkeramik societies

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    Cattle dominate archaeozoological assemblages from the north-central Europe between the sixth and fifth millennium BC and are frequently considered as exclusively used for their meat. Dairy products may have played a greater role than previously believed. Selective pressure on the lactase persistence mutation has been modelled to have begun between 6000 and 4000 years ago in central Europe. The discovery of milk lipids in late sixth millennium ceramic sieves in Poland may reflect an isolated regional peculiarity for cheese making or may signify more generalized milk exploitation in north-central Europe during the Early Neolithic. To investigate these issues, we analysed the mortality profiles based on age-at-death analysis of cattle tooth eruption, wear and replacement from 19 archaeological sites of the Linearbandkeramik (LBK) culture (sixth to fifth millennium BC). The results indicate that cattle husbandry was similar across time and space in the LBK culture with a degree of specialization for meat exploitation in some areas. Statistical comparison with reference age-at-death profiles indicate that mixed husbandry (milk and meat) was practised, with mature animals being kept. The analysis provides a unique insight into LBK cattle husbandry and how it evolved in later cultures in central and western Europe. It also opens a new perspective on how and why the Neolithic way of life developed through continental Europe and how dairy products became a part of the human diet

    ESM1: Mortality data based on dental eruption, replacement and wear stages.

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    Mortality data and site information for Apc-Berekalja (APC), Füzseabony-Gubakút (FUZ), Polgár-Piócási-dűlő (PPIO), Polgár-Ferenci-hát (PFER), Polgár-Csőszhalom-dűlő (PCSO), Tĕšetice-Kyjovice (TES), Hostivice-Sadová (HOS), Chotěbudice phase IIa (CHO1), Chotěbudice phase IIb (CHO2), Chotěbudice phase IIc-IIIa (CHO3), Chotěbudice phase IIIa-IIIb (CHO4), Černý Vůl (CER), Ludwinowo phase IIb (LUD1), Ludwinowo III (LUD2), Mold (MOLD), Eilsleben (EIL), Stephansposching (STE), Dillingen-Steinheim (WIK), Rosheim (ROS), Bischoffsheim (BIS1, 2, 3, 4), Herxheim-settlement (HEXs), Herxheim-ditch (HEXd), Etigny (ETI) and Balloy (BAL). Mortality data for the four production models (post-lactation and intensive milk, and meat) based on the archaeological sites: Bercy, Popină-Borduşani, Grimes Graves and La Montagne

    ESM: Mortality profiles from sites

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    Supplementary figures: Mortality profiles from Apc-Berekalja, Füzseabony-Gubakút, Polgár-Piócási-dűlő, Polgár-Ferenci-hát, Polgár-Csőszhalom-dűlő (Hungary), Hostivice-Sadová, Chotěbudice, Černý Vůl, Tĕšetice-Kyjovice( Czech republic), Ludwinowo (Poland), Mold, Elisleben, Stephansposching, Dillingen-Steinheim, Herxheim (Germany), Rosheim, Balloy and Bischoffsheim (France)

    Mortality data based on dental eruption, replacement and wear stages.; R_code; Legge age classes for R code; Supplementary figures: Age-at-death profiles from studied sites from The evolution of dual meat and milk cattle husbandry in Linearbandkeramik societies

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    Mortality data based on dental eruption, replacement and wear for Apc-Berekalja (APC), Füzseabony-Gubakút (FUZ), Polgár-Piócási-dűlő (PPIO), Polgár-Ferenci-hát (PFER), Polgár-Csőszhalom-dűlő (PCSO), Tĕšetice-Kyjovice (TES), Hostivice-Sadová (HOS), Chotěbudice phase IIa (CHO1), Chotěbudice phase IIb (CHO2), Chotěbudice phase IIc-IIIa (CHO3), Chotěbudice phase IIIa-IIIb (CHO4), Černý Vůl (CER), Ludwinowo phase IIb (LUD1), Ludwinowo III (LUD2), Mold (MOLD), Eilsleben (EIL), Stephansposching (STE), Dillingen-Steinheim (WIK), Rosheim (ROS), Bischoffsheim (BIS1, 2, 3, 4), Herxheim-settlement (HEXs), Herxheim-ditch (HEXd), Etigny (ETI) and Balloy (BAL). Mortality data for the four husbandry models based on the cattle remains from Bercy, Popina-Bordusani, Grimes Graves and La Montagne.;R code for the gernating the mortality profiles and Dirichlet simulations for the correspondence analysis.;Legge (1992) age classes for the R code.;Mortality profiles for Apc-Berekalja (APC), Füzseabony-Gubakút (FUZ), Polgár-Piócási-dűlő (PPIO), Polgár-Ferenci-hát (PFER), Polgár-Csőszhalom-dűlő (PCSO), Tĕšetice-Kyjovice (TES), Hostivice-Sadová (HOS), Chotěbudice phase IIa (CHO1), Chotěbudice phase IIb (CHO2), Chotěbudice phase IIc-IIIa (CHO3), Chotěbudice phase IIIa-IIIb (CHO4), Černý Vůl (CER), Ludwinowo phase IIb (LUD1), Ludwinowo III (LUD2), Mold (MOLD), Eilsleben (EIL), Stephansposching (STE), Dillingen-Steinheim (WIK), Rosheim (ROS), Bischoffsheim (BIS1, 2, 3, 4), Herxheim-settlement (HEXs), Herxheim-ditch (HEXd), Etigny (ETI) and Balloy (BAL)
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