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The Chironomidae of Gróthúsvatn, Sandoy, Faroe Islands: climatic and lake phosphorus reconstructions, and the impact of human settlement

Gathorne-Hardy, FJ; Lawson, IT; Church, MJ; Brooks, SJ; Buckland, PC; Edwards, KJ

Authors

FJ Gathorne-Hardy

IT Lawson

SJ Brooks

PC Buckland

KJ Edwards



Abstract

Chironomids were examined as part of a multiproxy palaeolimnological study of Gróthúsvatn, Sandoy, Faroe Islands. A total of 37 taxa was found in the top 1 m of the core. Chironomid-inferred total phosphorus and temperature reconstructions indicate that after landnám (the Norse settlement period) total phosphorus levels rose slightly, then peaked at a temperature minimum (interpreted as the ‘Little Ice Age’). Total phosphorus levels subsequently fell to only slightly above pre-settlement levels at the sediment surface. Little indication of increased erosion in the catchment after landnám was found, and it is likely that the impacts of human settlement on Gróthúsvatn and its catchment were slight. We therefore propose that the temperature decrease caused the increase in the lake’s productivity.

Citation

Gathorne-Hardy, F., Lawson, I., Church, M., Brooks, S., Buckland, P., & Edwards, K. (2007). The Chironomidae of Gróthúsvatn, Sandoy, Faroe Islands: climatic and lake phosphorus reconstructions, and the impact of human settlement. Holocene, 17(8), 1259-1264. https://doi.org/10.1177/0959683607085133

Journal Article Type Article
Publication Date Dec 1, 2007
Deposit Date Jan 28, 2009
Journal Holocene
Print ISSN 0959-6836
Electronic ISSN 1477-0911
Publisher SAGE Publications
Peer Reviewed Peer Reviewed
Volume 17
Issue 8
Pages 1259-1264
DOI https://doi.org/10.1177/0959683607085133
Publisher URL http://hol.sagepub.com/cgi/content/abstract/17/8/1259


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