Mid-Late Holocene Vegetational History and Land-Use Dynamics in County Monaghan, Northeastern Ireland—The Palynological Record of Lough Muckno

Q1 Arts and Humanities
C. Chique, Karen Molloy, A. Potito
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引用次数: 12

Abstract

Abstract We conducted high-resolution palynological analysis on a sediment core obtained from Lough Muckno, County Monaghan, Ireland. The results presented represent the first paleoecological account of Mid-Late Holocene vegetational change and land-use dynamics in the study region. Human activity and agriculture is first recorded during the Early Neolithic (ca. 3870–3500 B.C.). After a period of undiscernible human activity of ∼900 years, farming resumes during the Early Bronze Age (ca. 2600 B.C.). Henceforth, human presence on the landscape is constant with fluctuating levels of intensity. During the Bronze Age, anthropogenic activity is most pronounced during ca. 2000–1750 B.C. and ca. 1500–1300 B.C. followed by a phase of reduced intensity in the Late Bronze Age (ca. 1000–650 B.C.). Farming activity increases during the Iron Age and is disrupted with the onset of a period of rapid woodland regeneration from ca. 200 B.C. to A.D. 200. During the prehistorical period agriculture has a strong focus on pastoral grazing with a limited arable component. An upsurge in agricultural activity is recorded in the historical period from ca. A.D. 400 in which a mixed agricultural economy placing more emphasis on cereal-crop cultivation is adopted. Arable farming attains its maximum levels ca. A.D. 990–1140. Evidence of farming disruptions in the pollen record may reflect of a period of local “conflict” during the Viking Age/Medieval period (ca. A.D. 800–1190). We explore the characterizing features of the pollen assemblage of this large lake system and its use in reconstructing past cultural landscape change.
爱尔兰东北部莫纳汉郡全新世中晚期植被历史与土地利用动态——穆克诺湖孢粉记录
我们对爱尔兰莫纳汉郡穆克诺湖的沉积物岩心进行了高分辨率孢粉学分析。研究结果是研究区中晚全新世植被变化和土地利用动态的第一个古生态学解释。人类活动和农业最早记录于新石器时代早期(约公元前3870-3500年)。经过大约900年难以辨认的人类活动后,农业在青铜时代早期(约公元前2600年)恢复。从此以后,人类在景观上的存在是恒定的,强度是波动的。在青铜时代,人类活动在公元前2000年至1750年和公元前1500年至1300年最为明显,随后在青铜时代晚期(公元前1000年至650年)出现了强度降低的阶段。在铁器时代,农业活动有所增加,但在公元前200年至公元200年,随着林地快速更新时期的开始,农业活动中断了。在史前时期,农业以放牧为主,耕地成分有限。据记载,从公元400年开始的历史时期,农业活动激增,采用了更加强调谷物和作物种植的混合农业经济。可耕种农业大约在公元990-1140年达到最高水平。花粉记录中农业中断的证据可能反映了维京时代/中世纪时期(约公元800-1190年)当地的“冲突”时期。我们探讨了这一大型湖泊系统花粉组合的特征及其在重建过去文化景观变化中的应用。
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来源期刊
Journal of the North Atlantic
Journal of the North Atlantic Arts and Humanities-History
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