The impact of human activities in the Gutaiului Mountains, Romania

The examination of pollen and charcoal from the Gutâiului Mountains in northwestern Romania and the archaeological evidence from surroundings provides some information on how past human activities have changed the vegetation in this region. The first evidence of potential human influence upon the wo...

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Main Authors: Angelica Feurdean, Ciprian Astalos
Format: Article
Language:English
Published: Cluj University Press 2005-04-01
Series:Studia Universitatis Babes-Bolyai: Geologia
Online Access:http://scholarcommons.usf.edu/geologia/vol50/iss1/art7/
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spelling doaj-41aa1c7d60224b07b0651e0c21028d692020-11-24T22:26:10ZengCluj University PressStudia Universitatis Babes-Bolyai: Geologia1221-08031937-86022005-04-015016372The impact of human activities in the Gutaiului Mountains, RomaniaAngelica Feurdean0Ciprian Astalos1Western University “Vasile Goldiş”; Quaternary Research Group, Department of Geology, “Babeş-Bolyai” UniversitySatu Mare County MuseumThe examination of pollen and charcoal from the Gutâiului Mountains in northwestern Romania and the archaeological evidence from surroundings provides some information on how past human activities have changed the vegetation in this region. The first evidence of potential human influence upon the woodlands is manifested by fire clearance recorded at approximately 7900 cal. yr BP coinciding with the Early Neolithic. The charcoal peaks at ca. 5750, 3300, 2700, 1500, 1000 cal. yr BP, and during the last 300 years are associated with episodes of decline of main woodland constituents (Ulmus, Tilia, Fraxinus, and Corylus), and the expansion of fire-precursors (Betula, Alnus, and Corylus), and of herb species that indicate an anthropogenic disturbance. The small openings created within the woodlands were probably used as grazing areas. The first signs of agriculture appear at ca. 1500 cal. yr BP. Only during the last 300 years does pollen of the cereals e.g. Secale, Hordeum-group, Poaceae >40 μm, suggest the spread of arable field in the lowlands (Oaş Depression), but not in the proximity of the study basins. http://scholarcommons.usf.edu/geologia/vol50/iss1/art7/
collection DOAJ
language English
format Article
sources DOAJ
author Angelica Feurdean
Ciprian Astalos
spellingShingle Angelica Feurdean
Ciprian Astalos
The impact of human activities in the Gutaiului Mountains, Romania
Studia Universitatis Babes-Bolyai: Geologia
author_facet Angelica Feurdean
Ciprian Astalos
author_sort Angelica Feurdean
title The impact of human activities in the Gutaiului Mountains, Romania
title_short The impact of human activities in the Gutaiului Mountains, Romania
title_full The impact of human activities in the Gutaiului Mountains, Romania
title_fullStr The impact of human activities in the Gutaiului Mountains, Romania
title_full_unstemmed The impact of human activities in the Gutaiului Mountains, Romania
title_sort impact of human activities in the gutaiului mountains, romania
publisher Cluj University Press
series Studia Universitatis Babes-Bolyai: Geologia
issn 1221-0803
1937-8602
publishDate 2005-04-01
description The examination of pollen and charcoal from the Gutâiului Mountains in northwestern Romania and the archaeological evidence from surroundings provides some information on how past human activities have changed the vegetation in this region. The first evidence of potential human influence upon the woodlands is manifested by fire clearance recorded at approximately 7900 cal. yr BP coinciding with the Early Neolithic. The charcoal peaks at ca. 5750, 3300, 2700, 1500, 1000 cal. yr BP, and during the last 300 years are associated with episodes of decline of main woodland constituents (Ulmus, Tilia, Fraxinus, and Corylus), and the expansion of fire-precursors (Betula, Alnus, and Corylus), and of herb species that indicate an anthropogenic disturbance. The small openings created within the woodlands were probably used as grazing areas. The first signs of agriculture appear at ca. 1500 cal. yr BP. Only during the last 300 years does pollen of the cereals e.g. Secale, Hordeum-group, Poaceae >40 μm, suggest the spread of arable field in the lowlands (Oaş Depression), but not in the proximity of the study basins.
url http://scholarcommons.usf.edu/geologia/vol50/iss1/art7/
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