Modern limnology and varve-formation processes in Lake Zabinskie, northeastern Poland: comprehensive process studies as a key to understand the sediment record

Reconstruction of paleoclimatic and paleoenvironmental conditions from sediment records require a thorough knowledge of the physical, chemical and biological factors that influence sediment-formation processes and signal preservation in lake sediments. Lake Zabinskie, a eutrophic hardwater lake located in northeastern Poland (Masurian Lake District), provides a unique environment for the investigation of processes that lead to varve formation. During a two-year observation period we investigated limnological and hydrochemical conditions within the water column, recent sediment fluxes and laminations preserved in the sediments of this lake to understand the relationship between the lake water properties and the sediment formation processes. We demonstrate that dimictic to meromictic mixing patterns may occur in Lake Zabinskie, depending on the meteorological conditions. Regardless of the water mixing pattern, the lake was stratified during much of the year which led to significant differences between surface and near-bottom water environments. The hypolimnion was characterized by higher conductivity and anoxic conditions with only short periods of available oxygen, which created conditions ideal for the formation and preservation of biogenic varves in Lake Zabinskie. The material collected from the sediment trap revealed notable changes in sediment fluxes with characteristic spring maxima and, optionally, a second late fall maxima. Considerable variability was also observed for the fluxes of total organic carbon, biogenic silica and calcite. Microscopic investigation of the topmost sediments revealed a complex structure of the varves showing a distinct spring calcite lamina followed by several fine calcite laminae interbedded with diatom-rich laminae and, finally, by an organic-rich lamina with minerogenic admixtures deposited during winter. This seasonal variability was also reflected in the chemical composition inferred from high-resolution XRF measurements which allowed for the recognition of individual seasons within one varve. A characteristic annual succession of elemental composition followed a distinct pattern: spring was marked with a silica peak followed by a major calcium peak; during summer and fall minor calcium peaks occurred as well as maxima in iron and sulphur; winter was characterized by a peak in potassium. This study shows the potential that the sediment record from Lake Zabinskie has as high-resolution paleoenvironmental archive.