Hydroclimate variability of High Arctic Svalbard during the Holocene inferred from hydrogen isotopes of leaf waxes. (1st March 2018)

• Record Type: Journal Article
• Authors: Balascio, Nicholas L.; D'Andrea, William J.; Gjerde, Marthe; Bakke, Jostein
• Is Part Of: Quaternary science reviews. Volume 183(2018)
• Page Start: 177
• Page End: 187
• Publication Date: 2018-03-01
• Subjects: Lake sediment -- Hydrogen isotope -- n-Alkane -- Paleoclimate -- Holocene -- Svalbard; Geology, Stratigraphic -- Quaternary -- Periodicals; Stratigraphie -- Quaternaire -- Périodiques; 551.79
• DOI: 10.1016/j.quascirev.2016.11.036
• Languages: English
• ISSNs: 0277-3791

Abstract

Abstract: The response of the Arctic hydrologic cycle to global warming includes changes in precipitation patterns and moisture availability associated with variable sea ice extent and modes of atmospheric circulation. Reconstructions of past hydroclimate changes help constrain the natural range of these systems, identify the manners in which they respond to different forcing mechanisms, and reveal their connections to other components of the climate system, all of which lead to a better understanding of present and future changes. Here we examine hydroclimate changes during the Holocene in the High Arctic archipelago of Svalbard by reconstructing the isotopic composition of precipitation. We measured the hydrogen isotopic composition (δD values) of leaf wax compounds ( n -alkanes; C25 -C31 ) in a sediment core from Lake Hakluytvatnet on the island of Amsterdamøya, northwest Spitsbergen. We interpret δD values of mid-chain (C25 ) and long-chain (C29, C31 ) length n -alkanes to represent changes in the isotopic composition of lake water and precipitation over the last 12.9 ka. After deglaciation of the catchment, water supply became restricted and the lake experienced significant evaporative isotopic enrichment indicating warmer conditions from 12.8 to 7.5 ka. The isotope values suggest an increase in the delivery of moisture from warmer sub-polar air masses between 12.8 and 9.5 ka, followed by generally warm, but unstable conditions between 9.5 and 7.5 ka, possibly indicating a response to meltwater forcing. Sedimentary evidence indicates a hiatus in deposition c. 7.5–5.0 ka, likely as a result of desiccation of the lake. At c. 5.0 ka lacustrine sedimentation resumed and over the last 5 ka there was a progressive increase in the influence of polar air masses and colder conditions, which culminated in an abrupt shift to colder conditions at c. 1.8 ka. This late Holocene cooling ended c. 0.18 ka, when isotopic data indicate warmer conditions and greater influence of moisture derived from lower latitudes. Highlights: A 12, 900-year lake sediment record of hydroclimate variations from Svalbard is presented. Hydroclimate changes are inferred from the hydrogen isotopic composition of leaf wax compounds ( n- alkanes). Results show distinct paleoclimate intervals that reflect changes in the influence of sub-polar and polar air masses.