Holocene climate in the subarctic fjord Malangen, northern Norway: a multi‐proxy study

• Published in: Boreas
• Main Authors: HALD, MORTEN, HUSUM, KATRINE, VORREN, TORE O., GRØSFJELD, KARI, JENSEN, HENNING B., SHARAPOVA, ALLA
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2003
• Subjects: Malangen; Norway; North Atlantic; Northern Norway; Subarctic
• Online Access: http://dx.doi.org/10.1111/j.1502-3885.2003.tb01234.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.2003.tb01234.x; https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.2003.tb01234.x

A Holocene sedimentary record from the deep‐silled Malangen fjord in northern Norway reveals regional changes in sedimentary environment and climate. Down‐core analysis of two sediment cores includes multi‐core sensor logging, grain size, x‐radiography, foraminifera, oxygen isotopes, dinoflagellates, pollen, trace elements and radiocarbon datings. The cores are located just proximal to the submarine Younger Dryas moraine complex, and reveal the deglaciation after Younger Dryas and the postglacial evolution. Five sedimentary units have been identified. The oldest units, V and IV, bracket the Younger Dryas glacial readvance in the fjord between 12700 cal. years BP and 11 800 cal. years BP. This is followed by deposition of glaciomarine sediments (units IV and III) starting around 12100 cal. years BP. Glaciomarine sedimentation ceased in the fjord c. 10300 cal. years BP and was replaced by open marine sedimentation (units II and I). A rapid stepwise warming occurred during the Preboreal. Onset of surface water warming lagged bottom water warming by several hundred years. The δ 18 O record indicates a significant, gradual bottom water cooling (c. 4°C) between 8000 and 2000 cal. years BP, a trend also supported by the other proxy data. Other records in the region, as well as GCM simulations, also support this long‐term climatic evolution. Superimposed on this cooling were brief warmings around 6000 cal. years BP and 2000 cal. years BP. The long‐term change may be driven by orbitally forced reduction in insolation, whereas the short‐term changes may be linked to for example solar forcing, meltwater and NAO changes all causing regional changes in the North Atlantic heat transport.