首页> 外文期刊>Journal of Archaeological Science >Palaeolimnological impacts of early prehistoric farming at Lough Dargan, County Sligo, Ireland
【24h】

Palaeolimnological impacts of early prehistoric farming at Lough Dargan, County Sligo, Ireland

机译:史前早期农业在爱尔兰斯莱戈郡达格港的古生物学影响

获取原文
获取原文并翻译 | 示例
       

摘要

This study provides a unique method of inquiry for archaeological investigation with an aim to assess the intensity and effects of Neolithic and Bronze Age farming practices at Lough Dargan, northwest Ireland, through a multi-proxy analysis of a lake sediment core. Chironomid (non-biting midge fly) subfossils and lake sediment geochemistry (δ~(13)C, δ~(15)N and C:N ratios) were used to assess changes in limnological conditions through time. The limnological data were compared with macroscopic charcoal concentration and pollen data to examine the potential influence that early farmers had on a freshwater lake system within a prehistorically active catchment. Results from the chironomid analysis show that the first substantial period of agricultural activity in the early Neolithic (c. 3730-3190 BC) resulted in a temporary shift to more eutrophic lake conditions. There is evidence of animal husbandry with substantial levels of animal waste reaching the lake, leaving an imprint in the geochemical record of increased δ~(15)N values and decreased δ~(13)C values and C:N ratios during this time. The chironomid community reverted back to its pre-impacted state c. 3190 BC in response to a period of reduced farming (c. 3390-3000 BC) which eventually led to a distinct lull in activity, with possible cessation of farming from 3000 to 2700 BC. A return to eutrophic conditions coincided with the gradual return of agriculture, with more permanently altered lake conditions dominating from 2400 BC, even during a 250-year period of reduced human activity commencing at c. 1440 BC. Increased sedimentation rate, along with increases in δ~(13)C, δ~(15)N and C:N, the presence of chironomid taxa indicative of erosion, more eutrophic lake conditions and high concentrations of macroscopic charcoal all point to more intensive land use practices during the Bronze Age. Palaeolimnological data exhibited an immediate response to intensified farming during this time, and were especially responsive to pastoral farming due either to scale of activity or proximity to the lakeside. The success of this study demonstrates the effectiveness of palaeolimnological analysis in the investigation of prehistoric farming. This approach will help inform Neolithic and Bronze Age land-use practice and human-environment relations in the region, and highlights the potential for chironomid-based archaeological research.
机译:这项研究提供了一种独特的考古调查方法,旨在通过对湖泊沉积物核心的多代理分析来评估爱尔兰西北达格港的新石器时代和青铜时代的耕作方式的强度和影响。 Chironomid(无咬mid蝇)亚化石和湖泊沉积物地球化学(δ〜(13)C,δ〜(15)N和C:N比)用于评估随时间变化的湖泊学条件。将其物理学数据与宏观木炭浓度和花粉数据进行比较,以检验早期农民对史前活跃流域内的淡水湖泊系统的潜在影响。尺虫分析的结果表明,新石器时代早期(约3730-3190 BC)农业活动的第一个实质时期导致了向富营养化湖泊条件的暂时转变。有证据表明,畜牧业有大量的动物废物到达湖泊,在这段时间的δ〜(15)N值增加,δ〜(13)C值和C:N比值​​降低的地球化学记录中留下了印记。手足动物群落恢复到其预先受影响的状态。公元前3190年,以应对耕种减少的时期(约3390-3000 BC),这最终导致了活动的明显停顿,并有可能在公元前3000至2700年停止耕种。富营养条件的恢复与农业的逐步恢复相吻合,甚至从公元前2400年开始的人类活动减少的250年期间,更永久改变的湖泊条件从公元前2400年起占主导地位。公元前1440年。沉积速率的增加,以及δ〜(13)C,δ〜(15)N和C:N的增加,存在表明侵蚀的手足类群,更富营养的湖泊条件和高浓度的宏观木炭都表明集约化青铜时代的土地利用实践。在此期间,古生物学数据显示出对集约化耕作的立即反应,并且由于活动规模或靠近湖边,对牧业特别敏感。这项研究的成功证明了古遗迹学分析在史前农业研究中的有效性。这种方法将有助于为该地区的新石器时代和青铜时代的土地利用实践以及人与环境之间的关系提供信息,并突出了基于手性的考古学研究的潜力。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号