Advanced Search

Journal Navigation

Journal Home

Subscriptions

Archive

Contact Us

Table of Contents

Click here to sign up for SAGE Journal Email Alerts today!

Sign In to gain access to subscriptions and/or personal tools.
The Holocene
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Add to Saved Citations
Right arrow Download to citation manager
Right arrowRequest Permissions
Right arrow Request Reprints
Right arrow Add to My Marked Citations
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Right arrow Citing Articles via Scopus
Google Scholar
Right arrow Articles by Meadows, J.
Right arrow Search for Related Content
Social Bookmarking
 Add to CiteULike   Add to Complore   Add to Connotea   Add to Del.icio.us   Add to Digg   Add to Reddit   Add to Technorati   Add to Twitter  
What's this?

The Younger Dryas episode and the radiocarbon chronologies of the Lake Huleh and Ghab Valley pollen diagrams, Israel and Syria

John Meadows

Institute of Archaeology, University College London, 31-34 Gordon Square London WC]H OP Y UK) University College London, 31-34 Gordon Square

Pollen diagrams from the former Lake Huleh in Israel and the Ghab Valley in Syria are the most important records of vegetation change in the Levant during the Lateglacial and early Holocene. Environmentally deterministic explanations of the development of agriculture in this region therefore rely on the accuracy of the diagrams radiocarbon chronologies. Radiocarbon results at both sites are subject to large reservoir effects, however: the 14C content of modern water from the Huleh basin implies that the Huleh radiocarbon results require corrections of up to 5500 14C years. A revised chronology of the latest Huleh pollen diagram is proposed. This is consistent with the regional vegetation sequence recorded in eastern Mediterranean marine sediments. The regional sequence also provides the most plausible chronology for the Ghab pollen diagrams.

Key Words: Ghab • Huleh • radiocarbon • reservoir effects • vegetation history • Younger Dryas • early Holocene • Levant • Israel • Syria

The Holocene, Vol. 15, No. 4, 631-636 (2005)
DOI: 10.1191/0959683605hl838fa


Add to CiteULike CiteULike   Add to Complore Complore   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us   Add to Digg Digg   Add to Reddit Reddit   Add to Technorati Technorati   Add to Twitter Twitter    What's this?


This article has been cited by other articles:


Home page
The HoloceneHome page
G. Willcox, R. Buxo, and L. Herveux
Late Pleistocene and early Holocene climate and the beginnings of cultivation in northern Syria
The Holocene, February 1, 2009; 19(1): 151 - 158.
[Abstract] [PDF]


Home page
The HoloceneHome page
L. Hajar, C. Khater, and R. Cheddadi
Vegetation changes during the late Pleistocene and Holocene in Lebanon: a pollen record from the Bekaa Valley
The Holocene, November 1, 2008; 18(7): 1089 - 1099.
[Abstract] [PDF]