Premium
Late Holocene climate change in central Sweden inferred from lacustrine stable isotope data
Author(s) -
Andersson Sofia,
Rosqvist Gunhild,
leng Melanie j.,
Wastegård Stefan,
Blaauw Maarten
Publication year - 2010
Publication title -
journal of quaternary science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.142
H-Index - 94
eISSN - 1099-1417
pISSN - 0267-8179
DOI - 10.1002/jqs.1415
Subject(s) - chara , holocene , precipitation , geology , carbonate , stable isotope ratio , diatom , algae , paleoclimatology , climate change , water cycle , sedimentary rock , physical geography , oceanography , paleontology , ecology , chemistry , geography , physics , organic chemistry , quantum mechanics , biology , meteorology
Abstract Stable isotopes (δ 18 O and δ 13 C) of lacustrine carbonates ( Chara spp. algae and Pisidium spp. molluscs) from a lake sedimentary sequence in central Sweden were analysed to infer changes in lake hydrology and climate during the late Holocene. Results from analysis of lake water isotopes (δ 18 O and δ 2 H) show that Lake Blektjärnen water isotope composition is responsive to the balance between evaporation and input water ( E / I ratio). A high E / I ratio results from a dry and probably warmer climate, decreasing the relative importance of precipitation input. Under such conditions evaporation and atmospheric equilibration probably enrich lake water in 18 O and 13 C, respectively, which is reflected in the isotopic composition of the carbonates in the lake. From the relatively positive Chara δ 18 O values we infer that conditions were dry and warm between 4400 and 4000 cal. a BP, whereas more negative values indicate that conditions were wetter and probably cooler between 4000 and 3000 cal. a BP. A drier climate is inferred from more positive values between 2500 and 1000 cal. a BP. However, a successive depletion after ca. 1750 cal. a BP, also detected in several other δ 18 O records (carbonate and diatom), suggest increasingly wetter conditions in Scandinavia after that time, which is probably related to increased strength of the zonal flow. Copyright © 2010 John Wiley & Sons, Ltd.