Abstract

An integrated analysis of molluscs, ostracods and pollen is presented from early Holocene lake marl at Llangorse Lake, Powys, South Wales. The mollusc and ostracod records reflect a littoral environment with increasing eutrophic conditions and a progressive shallowing of lake waters, although the record does not begin until around 9600 BP, probably due to the isolated location. The pollen profile provides evidence of both local and regional vegetational changes over the first two millennia of the present interglacial. Following climatic amelioration at the beginning of the Holocene, there was rapid colonization by trees and shrubs, with juniper widespread by 9800 BP, birch woodland by 9500 BP, and pine by 9300 BP. Late in the ninth millennium BP, hazel became established, to be followed during the course of the eighth millennium by elm and oak. There are indications in both the pollen and molluscan/ ostracod sequences of a relatively dry climatic regime during the early Holocene, while the pollen record suggests a short-lived climatic cooling in the middle of the tenth millennium BP.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.