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 Google Scholar
Right arrow Citing Articles via Scopus
Google Scholar
Right arrow Articles by Stevenson, J.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
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?

A late-Holocene record of human impact from the southwest coast of New Caledonia

Janelle Stevenson

Department of Archaeology and Natural History, Research School of Pacific and Asian Studies, Australian National University, Canberra ACT 0200, Australia; Janelle.Stevenson{at}anu.edu.au

A late-Holocene vegetation record is presented from the southwest coast of New Caledonia. Lac Saint Louis is a freshwater swamp at 3 m a.s.l. adjacent to the River Coulee delta. Pollen analysis, charcoal analysis, radiocarbon dating and stratigraphic analyses have been used to reconstruct the vegetation and sedimentary history of the swamp. The sediment record commences at 6000 BP and reflects rapid flood-plain development associated with postglacial sea-level rise. This rapid accumulation of sediment ceased around 5500 BP and the site became a freshwater swamp. From 5500 to 3000 BP the pollen record reflects several aspects of this coastal landscape; coastal forest, the swamp surface and the adjacent mangrove zone. At 3000 BP charcoal levels increase significantly in conjunction with abrupt changes in the pollen record. Mangrove pollen declines and pollen indicative of coastal forest is replaced by pollen indicative of coastal savanna. These changes coincide with the commencement of the archaeological record in New Caledonia and mirror similar changes in other late-Holocene records elsewhere on the island, and are interpreted as representing human impact. Yam terraces surrounding Lac Saint Louis may have been built around 2000 BP based on mineral magnetic measurements and charcoal accumulation. The decline in mangrove vegetation adjacent to site may be the result of a late-Holocene fall in sea level. Increased sediment accumulation along the coastal foreshore as a result of forest clearance in the River Coulee's catch-ment, however, is also considered.

Key Words: New Caledonia • palynology • fire • human impact • sea level • tropical Pacific • late Holocene

The Holocene, Vol. 14, No. 6, 888-898 (2004)
DOI: 10.1191/0959-683604hl755rp


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?