Disturbance Phases in the Mid-Holocene Vegetation at North Gill, North York Moors: Form and Process
The results of a multi-profile analysis of disturbance phases using Fine Resolution Pollen Analysis (FRPA) are presented. The locale is the North Gill, a peat section 400 m long at an altitude of 370 m, and the time the mid-Holocene in a region known to have been occupied by later Mesolithic and ear...
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Veröffentlicht in: | Journal of archaeological science 1996-03, Vol.23 (2), p.183-191 |
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description | The results of a multi-profile analysis of disturbance phases using Fine Resolution Pollen Analysis (FRPA) are presented. The locale is the North Gill, a peat section 400 m long at an altitude of 370 m, and the time the mid-Holocene in a region known to have been occupied by later Mesolithic and early Neolithic cultures during the time of peat accumulation. Some of the fine detail of the FRPA is given and interpretations advanced which throw more light upon the probable manipulation of vegetation by human groups during the 5th millenium
bp. It is concluded that the emphasis on hazel (
Corylus avellana) as an object of vegetation management may need to be supplemented by that of the encouragement of a grassy ground flora in what was a mostly wooded environment. |
doi_str_mv | 10.1006/jasc.1996.0016 |
format | Article |
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bp. It is concluded that the emphasis on hazel (
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bp. It is concluded that the emphasis on hazel (
Corylus avellana) as an object of vegetation management may need to be supplemented by that of the encouragement of a grassy ground flora in what was a mostly wooded environment.</description><subject>ANTHROPOGENIC</subject><subject>ENGLAND</subject><subject>Epipalaeolithic and mesolithic</subject><subject>Europe</subject><subject>FIRE</subject><subject>MESOLITHIC</subject><subject>North West Europe</subject><subject>Palaeolithic and mesolithic</subject><subject>POLLEN ANALYSIS</subject><subject>Prehistory and protohistory</subject><subject>UPLANDS</subject><subject>WOODLANDS</subject><issn>0305-4403</issn><issn>1095-9238</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1996</creationdate><recordtype>article</recordtype><sourceid>K30</sourceid><recordid>eNp1kMFPwyAUh4nRxDm9eibRo61ASwvejLrNZNMdFhNPhFJwzK5MYCb-97Js8ebpkcf3ey_vA-ASoxwjVN2uZFA55rzKEcLVERhgxGnGScGOwQAViGZliYpTcBbCKhGYUjIA6tGGuPWN7JWG86UMOkDbw7jUcGbbbOI6p3Sv4Zv-0FFG63ooI3xxPi7h2HbdzeH97vwnnDnnwx0cOb-Gsm_h3KdwCOfgxMgu6ItDHYLF6GnxMMmmr-Pnh_tpJouqillbkYZo2mCKjGkbopSiSFFepw9WViUznBqOpJE1r2uODGO4rBTnuJE1ZcUQXO3Hbrz72uoQxcptfZ82inRriRjhpExUvqeUdyF4bcTG27X0PwIjsfModh7FzqPYeUyB68PY1Jed8UmVDX-pgjBKKE0Y22M6XfhttRdBWZ2sttZrFUXr7H8bfgHZJIUA</recordid><startdate>19960301</startdate><enddate>19960301</enddate><creator>Simmons, I.G.</creator><creator>Innes, J.B.</creator><general>Elsevier Ltd</general><general>Elsevier Science</general><general>Academic Press</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>FUVTR</scope><scope>IZSXY</scope><scope>K30</scope><scope>PAAUG</scope><scope>PAWHS</scope><scope>PAWZZ</scope><scope>PAXOH</scope><scope>PBHAV</scope><scope>PBQSW</scope><scope>PBYQZ</scope><scope>PCIWU</scope><scope>PCMID</scope><scope>PCZJX</scope><scope>PDGRG</scope><scope>PDWWI</scope><scope>PETMR</scope><scope>PFVGT</scope><scope>PGXDX</scope><scope>PIHIL</scope><scope>PISVA</scope><scope>PJCTQ</scope><scope>PJTMS</scope><scope>PLCHJ</scope><scope>PMHAD</scope><scope>PNQDJ</scope><scope>POUND</scope><scope>PPLAD</scope><scope>PQAPC</scope><scope>PQCAN</scope><scope>PQCMW</scope><scope>PQEME</scope><scope>PQHKH</scope><scope>PQMID</scope><scope>PQNCT</scope><scope>PQNET</scope><scope>PQSCT</scope><scope>PQSET</scope><scope>PSVJG</scope><scope>PVMQY</scope><scope>PZGFC</scope></search><sort><creationdate>19960301</creationdate><title>Disturbance Phases in the Mid-Holocene Vegetation at North Gill, North York Moors: Form and Process</title><author>Simmons, I.G. ; 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The locale is the North Gill, a peat section 400 m long at an altitude of 370 m, and the time the mid-Holocene in a region known to have been occupied by later Mesolithic and early Neolithic cultures during the time of peat accumulation. Some of the fine detail of the FRPA is given and interpretations advanced which throw more light upon the probable manipulation of vegetation by human groups during the 5th millenium
bp. It is concluded that the emphasis on hazel (
Corylus avellana) as an object of vegetation management may need to be supplemented by that of the encouragement of a grassy ground flora in what was a mostly wooded environment.</abstract><cop>Amsterdam</cop><pub>Elsevier Ltd</pub><doi>10.1006/jasc.1996.0016</doi><tpages>9</tpages></addata></record> |
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subjects | ANTHROPOGENIC ENGLAND Epipalaeolithic and mesolithic Europe FIRE MESOLITHIC North West Europe Palaeolithic and mesolithic POLLEN ANALYSIS Prehistory and protohistory UPLANDS WOODLANDS |
title | Disturbance Phases in the Mid-Holocene Vegetation at North Gill, North York Moors: Form and Process |
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