2016
DOI: 10.1007/s00334-016-0560-4
|View full text |Cite
|
Sign up to set email alerts
|

The isotopic footprint of irrigation in the western Mediterranean basin during the Bronze Age: the settlement of Terlinques, southeast Iberian Peninsula

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

1
6
0
1

Year Published

2017
2017
2020
2020

Publication Types

Select...
8

Relationship

2
6

Authors

Journals

citations
Cited by 31 publications
(8 citation statements)
references
References 57 publications
1
6
0
1
Order By: Relevance
“…The difference between the average Δ 13 C values of wheat and barley (about 1‰) is in the same range as observed in modern crops [54], and suggests that both kinds of crops were grown under overall similar conditions. The obtained data are in agreement with those from pioneering comprehensive work by Araus et al [24,53], that does not point to any deliberate irrigation, an interpretation which stands in contrast to that offered by Mora-González et al [81]. According to basic research by Wallace et al and Styring et al [51,77,80,82], the carbon isotope values of the cereal grains from La Bastida and Gatas correspond to a wide range of poor to moderate water conditions, whereas deliberate irrigation should have resulted in higher and more uniform Δ 13 C values (Fig 7).…”
Section: Growing Conditions Of Cerealssupporting
confidence: 91%
See 1 more Smart Citation
“…The difference between the average Δ 13 C values of wheat and barley (about 1‰) is in the same range as observed in modern crops [54], and suggests that both kinds of crops were grown under overall similar conditions. The obtained data are in agreement with those from pioneering comprehensive work by Araus et al [24,53], that does not point to any deliberate irrigation, an interpretation which stands in contrast to that offered by Mora-González et al [81]. According to basic research by Wallace et al and Styring et al [51,77,80,82], the carbon isotope values of the cereal grains from La Bastida and Gatas correspond to a wide range of poor to moderate water conditions, whereas deliberate irrigation should have resulted in higher and more uniform Δ 13 C values (Fig 7).…”
Section: Growing Conditions Of Cerealssupporting
confidence: 91%
“…The overall dryness of the landscape in the growing period is reflected by the Δ 13 C values of the charred cereal grains, which are at the lower end of the data spectrum of C 3 winter cereals [79]. The Δ 13 C values of the barley grains from La Bastida and Gatas (Fig 7) overlap with data from modern fields in Morocco that represent low precipitation rates [80] as well as with those from the Bronze Age site of Terlinques about 100 km NE of La Bastida and 200 km NE of Gatas [81].…”
Section: Growing Conditions Of Cerealsmentioning
confidence: 79%
“…Mean isotopic values for four food groups (cereals, terrestrial protein, freshwater fish and marine fish) were used in modelling human diets in the Valencina population. The average isotopic values for cereals (δ 13 C = −22.81 ± 0.1‰; δ 15 N = 7.82 ± 0.15‰) include archaeobotanical barley and wheat from Bronze Age Terlinques, in southeast Spain (δ 13 C: Mora-González et al 2016 ; δ 15 N: Mora-González pers. comm).…”
Section: A Sensitivity Analysis: the Possibility Of Dietary Offsetsmentioning
confidence: 99%
“…Los valores δ 13 C calculados para la producción primaria terrestre (-22,5 a -20,5 ‰ vs V-PDB) están en el rango de las gramíneas (cereales) del sur de la península ibérica (Mora 2017), siendo menos negativos que los cereales (entre -23 y -26) del noroeste (Mora et al 2018) con un clima muy húmedo y, por tanto, menor WUE y más discriminación isotópica que en los ambientes áridos (Farquhar y Richards 1984). Por otra parte, considerando áreas áridas del este de la península donde los cereales irrigados estaban comprendidos entre -23 y -25 ‰, en el mismo rango que los pinos con mayor capacidad radicular y menos eficiencia en el aprovechamiento del agua (WUE), se ha calculado que las gramíneas en la Edad del Bronce pudieron ser sobre un 3 ‰ menos negativas (debido a una mayor WUE), estando comprendidas entre -20 y -22 (Mora et al 2016). Ello estaría en el rango que se deduce a partir de los valores de los humanos de Los Millares.…”
Section: Discussionunclassified