{"title":"Poblamiento prehistórico de la península ibérica: dinámica demográfica versus frecuencias del C14","authors":"A. Alday-Ruiz, Adriana Soto Sebastián","doi":"10.21630/MAA.2018.69.04","DOIUrl":null,"url":null,"abstract":"espanolEl trabajo reune y analiza 1.395 dataciones C14 de la prehistoria iberica, del lapso cronologico 13000-5000 BP. A partir de ellas se plantea si las mismas sirven para evaluar correctamente el poblamiento tanto a nivel iberico como entre las regiones en las que se divide el territorio. Para su evaluacion se sigue el procedimiento de suma de probabilidades una vez calibradas cada uno de los resultados. Como variacion a los sistemas tradicionales se incorpora una rutina matematica que evita las duplicaciones de contextos repetidamente datados (con valores solapados). En la lectura de los resultados obtenidos (regional y globalmente) se tienen en cuentan los factores derivados de la curva de calibracion, los sesgos tafonomicos y de investigacion, asi como eventos climaticos. En consecuencia, se observa que la compilacion de fechas puede producir efectos ilusorios, ya advertidos criticamente por Bayliss, de tal manera que debe sopesarse con cuidado su valor como proxy de la demografia prehistorica. Las ausencias en tramos temporales y geograficos remiten a problemas de invisibilidad de registros arqueologico, y las alteraciones en las frecuencias tiene que mucho que ver con los cambios en las estrategias humanas. EnglishIn this work we analyse 1,395 14C dates from the Iberian prehistory, belonging to the 13000-5000 BP chronological span. The only selection criterion considers their accuracy: a standard deviation of less than a century was required. It is the largest compilation published for this geographical area. Each date has been calibrated using OxCal program and IntCal13 calibration curve before the construction of the summed calibrated date probability distributions (SCDPD). We have followed the habitual methodology for the SCDPD, incorporating a mathematical routine into our process that avoids duplications of overlapping data from contexts repeatedly dated. At the same time, for a detailed evaluation, the exercise is also performed individually for different regions: Cantabrian region, Ebro basin, Central plateau, Catalonia, Valencia, Andalusia and Portugal. The aim of this work is to evaluate in which way this kind of compilations can be interpreted as demographic proxy, in this case as the Iberian population dynamics during the final Paleolithic and the first half of the Holocene. In this sense, we think that for interpreting the SCDPD it is firstly necessary to evaluate different factors that could distort the final distribution: factors related to the calibration curve itself, to taphonomic and research biases, or to the methodology employed. We also observe the individualised behaviors between the series of samples of long and short life that, contrary to the assumption, do not show striking dissonances. On the other hand, the participation of some very specific archaeological contexts, such as shell middens, can originate false demographic processes derived from their high archaeological visibility and their easy dating. For this reason, we justify the exclusion of certain archaeological sites, like the multiple megalithic burials for the end of our sequence, in these kind of exercises. They could create an overrepresentation. On the other hand, our interpretation is linked to the detailed knowledge of the archaeological contexts. We think that the understanding of a SCDPD only makes sense in the permanent dialogue between the radiocarbon data and the known archaeological record (and even the absent one). It is necessary to know the cultural (pre)historical development involved; the functionality of the sites; the archaeological research programs… The opposite is to make interpretations without a critical reading of the archaeological record. In this sense, as an example, the sharp drop in the date probability frequency after the start of the Neolithic, which in the logic of these kind of studies would attribute to a loss of population, could be related with changes in the strategies adopted by those societies. In conclusion, we think that the compilation of 14C dates can produce illusory effects, already warned critically by A. Bayliss, that they must be corrected by the archaeologist - the data by themselves do not do archeology-. The SCDPD cannot be taken as a proxy of prehistoric demography. The absence of data in temporary sections and geographic areas could refer to invisibility problems of the archaeological record, and the modifications in the probability frequencies are related with different human decisions about the exploitation of the territories, the number and characters of the deposits generated, or the inherent problems of the dating method and the exploitation of the results. The demographic patterns are hidden under these problems. EuskaraLan honetan, 13000 -5000 BP tarteko iberiar penintsulako 1395 datu erradiokarbonikoak biltzen eta aztertzen ditugu. Datu erradiokarboniko bakoitzak kalibratu ondoren probabilitate gehieketa egiten dugu, ariketa matematiko berria inplementatuz kontextu arkeologiko berean errepikatzen diren datazioak saihesteko. Gure helburua datu erradiokarboak proxy demografiko moduan erabiltzearen balioa aztertzea da, hau da, bildutako datazioek iberiar penintsulako populazioaren eboluzioa isladatzen dute? Lortutako emaitzen interpretazioan faktore ezberdinak hartu ditugu kontuan: kalibrazio kurbaren irregularitateak, sesgo tafonomikoak eta akademikoak, eta klimaren eboluzioa. Lanaren ondoria Bayliss autorearen interpretazioan lerrotzen da: datu erradiokarbonikoen gehieketak ez du zuzenki populazioaren eboluzioa isladatzen. Gehieketaren emaitza faktore ezberdinengatik influentziatua dago, bi faktore nabarmenduz hutsune kronologiko eta geografikoak azaltzeko: arazo tafonomikoak eta ikuspen gutxiko erregistro arkeologikoaren eragina, baita historiaurreko gizarteen estrategia ekonomiko eta sozialena ere.","PeriodicalId":38152,"journal":{"name":"Munibe Antropologia-Arkeologia","volume":"32 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2018-07-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Munibe Antropologia-Arkeologia","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.21630/MAA.2018.69.04","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"Arts and Humanities","Score":null,"Total":0}
引用次数: 2
Abstract
espanolEl trabajo reune y analiza 1.395 dataciones C14 de la prehistoria iberica, del lapso cronologico 13000-5000 BP. A partir de ellas se plantea si las mismas sirven para evaluar correctamente el poblamiento tanto a nivel iberico como entre las regiones en las que se divide el territorio. Para su evaluacion se sigue el procedimiento de suma de probabilidades una vez calibradas cada uno de los resultados. Como variacion a los sistemas tradicionales se incorpora una rutina matematica que evita las duplicaciones de contextos repetidamente datados (con valores solapados). En la lectura de los resultados obtenidos (regional y globalmente) se tienen en cuentan los factores derivados de la curva de calibracion, los sesgos tafonomicos y de investigacion, asi como eventos climaticos. En consecuencia, se observa que la compilacion de fechas puede producir efectos ilusorios, ya advertidos criticamente por Bayliss, de tal manera que debe sopesarse con cuidado su valor como proxy de la demografia prehistorica. Las ausencias en tramos temporales y geograficos remiten a problemas de invisibilidad de registros arqueologico, y las alteraciones en las frecuencias tiene que mucho que ver con los cambios en las estrategias humanas. EnglishIn this work we analyse 1,395 14C dates from the Iberian prehistory, belonging to the 13000-5000 BP chronological span. The only selection criterion considers their accuracy: a standard deviation of less than a century was required. It is the largest compilation published for this geographical area. Each date has been calibrated using OxCal program and IntCal13 calibration curve before the construction of the summed calibrated date probability distributions (SCDPD). We have followed the habitual methodology for the SCDPD, incorporating a mathematical routine into our process that avoids duplications of overlapping data from contexts repeatedly dated. At the same time, for a detailed evaluation, the exercise is also performed individually for different regions: Cantabrian region, Ebro basin, Central plateau, Catalonia, Valencia, Andalusia and Portugal. The aim of this work is to evaluate in which way this kind of compilations can be interpreted as demographic proxy, in this case as the Iberian population dynamics during the final Paleolithic and the first half of the Holocene. In this sense, we think that for interpreting the SCDPD it is firstly necessary to evaluate different factors that could distort the final distribution: factors related to the calibration curve itself, to taphonomic and research biases, or to the methodology employed. We also observe the individualised behaviors between the series of samples of long and short life that, contrary to the assumption, do not show striking dissonances. On the other hand, the participation of some very specific archaeological contexts, such as shell middens, can originate false demographic processes derived from their high archaeological visibility and their easy dating. For this reason, we justify the exclusion of certain archaeological sites, like the multiple megalithic burials for the end of our sequence, in these kind of exercises. They could create an overrepresentation. On the other hand, our interpretation is linked to the detailed knowledge of the archaeological contexts. We think that the understanding of a SCDPD only makes sense in the permanent dialogue between the radiocarbon data and the known archaeological record (and even the absent one). It is necessary to know the cultural (pre)historical development involved; the functionality of the sites; the archaeological research programs… The opposite is to make interpretations without a critical reading of the archaeological record. In this sense, as an example, the sharp drop in the date probability frequency after the start of the Neolithic, which in the logic of these kind of studies would attribute to a loss of population, could be related with changes in the strategies adopted by those societies. In conclusion, we think that the compilation of 14C dates can produce illusory effects, already warned critically by A. Bayliss, that they must be corrected by the archaeologist - the data by themselves do not do archeology-. The SCDPD cannot be taken as a proxy of prehistoric demography. The absence of data in temporary sections and geographic areas could refer to invisibility problems of the archaeological record, and the modifications in the probability frequencies are related with different human decisions about the exploitation of the territories, the number and characters of the deposits generated, or the inherent problems of the dating method and the exploitation of the results. The demographic patterns are hidden under these problems. EuskaraLan honetan, 13000 -5000 BP tarteko iberiar penintsulako 1395 datu erradiokarbonikoak biltzen eta aztertzen ditugu. Datu erradiokarboniko bakoitzak kalibratu ondoren probabilitate gehieketa egiten dugu, ariketa matematiko berria inplementatuz kontextu arkeologiko berean errepikatzen diren datazioak saihesteko. Gure helburua datu erradiokarboak proxy demografiko moduan erabiltzearen balioa aztertzea da, hau da, bildutako datazioek iberiar penintsulako populazioaren eboluzioa isladatzen dute? Lortutako emaitzen interpretazioan faktore ezberdinak hartu ditugu kontuan: kalibrazio kurbaren irregularitateak, sesgo tafonomikoak eta akademikoak, eta klimaren eboluzioa. Lanaren ondoria Bayliss autorearen interpretazioan lerrotzen da: datu erradiokarbonikoen gehieketak ez du zuzenki populazioaren eboluzioa isladatzen. Gehieketaren emaitza faktore ezberdinengatik influentziatua dago, bi faktore nabarmenduz hutsune kronologiko eta geografikoak azaltzeko: arazo tafonomikoak eta ikuspen gutxiko erregistro arkeologikoaren eragina, baita historiaurreko gizarteen estrategia ekonomiko eta sozialena ere.
这项工作收集和分析了1395个伊比利亚史前C14年代,时间跨度为13000-5000 BP。本研究的目的是评估伊比利亚半岛和领土划分地区之间的人口分布情况。对每个结果进行校准后,遵循概率和程序进行评估。作为传统系统的变体,它包含了一个数学例程,以避免重复日期上下文的重复(值重叠)。在阅读获得的结果(区域和全球)时,考虑了由校准曲线、tafonomicos和研究偏差以及气候事件产生的因素。因此,我们观察到,日期的汇编可能会产生错觉效应,贝利斯已经批判地警告过这一点,因此,必须仔细考虑它们作为史前人口统计的代表的价值。时间和地理区域的缺失意味着考古记录的不可见性问题,而频率的变化与人类策略的变化有很大关系。EnglishIn this work we analyse 1,395烷为from the Iberian prehistory BP,非to the 13000-5000》paramaribo span。The only selection雅典认为及其准确性:a standard deviation抑制胆was a century required。= =地理= =根据美国人口普查局的数据,该县的总面积为,其中土地和(1.)水。在构建总校准日期概率分布(SCDPD)之前,使用OxCal程序和IntCal13校准曲线对每个日期进行了校准。我们对SCDPD采用了通常的方法,在我们的处理过程中加入了一个数学例程,以避免重复从重复日期的上下文重叠数据。同时,为了进行详细评估,还对不同地区分别进行了练习:坎塔布里亚地区、埃布罗盆地、中央高原、加泰罗尼亚、巴伦西亚、安达卢西亚和葡萄牙。这项工作的目的是评估如何将这类汇编解释为一种人口代理,在这种情况下是作为旧石器时代晚期和全新世前半期的伊比利亚人口动态。在这方面,我们认为,在解释《消除对妇女一切形式歧视公约》时,首先必须评估可能扭曲最终分布的不同因素:与校准曲线本身有关的因素,与测绘和研究偏差有关的因素,或与所采用的方法有关的因素。我们还观察到长寿命和短寿命的一系列样本之间的个性化行为,与假设相反,没有表现出明显的不和谐。另一方面,一些非常具体的考古环境的参与,如贝壳中部,可以产生虚假的人口统计过程,因为它们的高考古能见度和它们的容易交集。因此,我们认为排除某些考古遗址是合理的,例如,在我们的序列结束时,在这些类型的练习中。他们可能会造成过度代表。= =地理= =根据美国人口普查,该镇的土地面积为。我们认为,只有在放射性碳数据与已知的考古记录(甚至是缺失的考古记录)之间不断进行的对话中,才有意义了解《濒危野生动植物种国际贸易公约》。必须了解所涉及的文化(前)历史发展;网站的功能;= =地理= =根据美国人口普查,这个县的面积为。在这方面,例如,在新石器时代开始后,日期概率频率的急剧下降,在这些研究的逻辑中,这归因于人口的损失,可能与这些社会所采取的战略的变化有关。最后,我们认为14C数据的汇编可能会产生一种伪效果,已经被A. Bayliss批评地警告过,它们必须被考古学家修正——数据本身并不构成考古学。= =地理= =根据美国人口普查局的数据,该县总面积为,其中土地和(1.1%)水。The absence of data in临时文件和地理领域可refer to invisibility problems of archaeological记录,and The modifications in The probability frequencies related with都设有人权决定about The剥削of The领土,The number and characters of The开辟generated, or The inherent problems of The dating method and The剥削of The results。人口模式隐藏在这些问题之下。euuskaralan honetan, 13000 -5000 BP tarteko iberiar penintsulako 1395 datu erradiokarbonikoak biltzen eta aztertzen ditugu。