Late Holocene Palaeoenvironment of TSE Dura, a Later Stone Age (Lsa) Rock Shelter, North-Central Nigeria

IF 0.6 Q4 GEOSCIENCES, MULTIDISCIPLINARY
E. Orijemie
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引用次数: 6

Abstract

Abstract Palynological and archaeobotanical analyses were conducted on excavated sediments from Tse Dura, a Later Stone Age rock shelter in north-central Nigeria with the aim of reconstructing the environment conditions at the site within the last millennium. From 933 ± 29 BP to 802 ± 29 BP, the environment alternated between Guinea savanna with dry conditions, and secondary and riverine forests with humid conditions. During these periods of environmental fluctuations, the LSA populations engaged in the management of economic plants the most significant of which included Dioscorea spp. Pennisetum glaucum and Elaeis guineensis, and exploited wild plants such as Pavetta crassipes, Sarcocephalus latifolius and Lophira cf. lanceolata for dietary and ethnomedicinal purposes. Around 310 ± 30 BP cal, the environment became very wet after which it was succeeded by a drier period. It was during this period that Sorghum bicolor became prominent, and the environment attained its current status dominated by Guinea savanna elements and secondary forests.
尼日利亚中北部晚石器时代(Lsa)岩石避难所TSE Dura晚全新世古环境
摘要对尼日利亚中北部石器时代晚期岩石避难所Tse Dura的挖掘沉积物进行了考古学和古植物学分析,目的是重建该遗址上千年的环境条件。从933±29 BP到802±29 BP,环境在几内亚稀树草原干旱条件和次生林和河岸林潮湿条件之间交替。在这些环境波动的时期,LSA种群参与了经济植物的管理,其中最重要的包括薯蓣属植物。蓝盾叶狼尾草和盾叶狼蛛,并利用野生植物,如凤眼莲、宽叶Sarcoccephalus和Lophira cf.lanceolata,用于饮食和民族药用目的。在310±30 BP cal左右,环境变得非常潮湿,之后又经历了一段干燥期。正是在这一时期,双色高粱变得突出,环境达到了以几内亚稀树草原元素和次生林为主的现状。
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来源期刊
Studia Quaternaria
Studia Quaternaria GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.40
自引率
0.00%
发文量
0
期刊介绍: Studia Quaternaria is designed to publish scientific works concerning the Quaternary, on local, regional and global scale. Studia Quaternaria is interested in all fields of research dealing with stratigraphy and reconstruction of the past environments, including palaeogeography, palaeoecology, palaeoclimatology, palaeohydrology etc. The journal is also open to studies of natural environmental processes, and to recognition of mechanisms involved in the dynamics of our environment. The clue is that the Quaternary is still ongoing and vivid, and understanding of its past and present development support each other.
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