A 5500-year oxygen isotope record of high arctic environmental change from southern Spitsbergen

• Published in: The Holocene
• Main Authors: Arppe, Laura, Kurki, Eija, Wooller, Matthew J, Luoto, Tomi P, Zajączkowski, Marek, Ojala, Antti EK
• Format: Article in Journal/Newspaper
• Language: English
• Published: SAGE Publications 2017
• Subjects: Arctic; Svartvatnet; North Atlantic; Sea ice; Spitsbergen
• Online Access: http://dx.doi.org/10.1177/0959683617715698; https://journals.sagepub.com/doi/pdf/10.1177/0959683617715698; https://journals.sagepub.com/doi/full-xml/10.1177/0959683617715698

The oxygen isotope composition of chironomid head capsules in a sediment core spanning the past 5500 years from Lake Svartvatnet in southern Spitsbergen was used to reconstruct the oxygen isotope composition of lake water (δ 18 O lw ) and local precipitation. The δ 18 O lw values display shifts from the baseline variability consistent with the timing of recognized historical climatic episodes, such as the Roman Warm Period, the Dark Ages Cold Period and the ‘Little Ice Age’. The highest values of the record, ca. 3‰ above modern δ 18 O lw values, occur at ca. 1900–1800 cal. yr BP. Three negative excursions increasing in intensity toward the present, at 3400–3200, 1250–1100, and 350–50 cal. yr BP, are tentatively linked to roughly synchronous episodes of increased glacier activity and general cold spells around the northern North Atlantic. Their manifestation in the Svartvatnet δ 18 O lw record not only testify to the sensitivity and potential of high Arctic lacustrine δ 18 O chir records in tracking terrestrial climate evolution but also highlight nonlinear dynamics within the northern North Atlantic hydroclimatic system. The ‘Little Ice Age’ period at 350–50 cal. yr BP displays a remarkable 8–9‰ drop in δ 18 O lw values, construed to predominantly represent significantly decreased winter temperatures during a period of increased seasonal differences and extended sea ice cover inducing changes in moisture source regions.