Diatom Si deposition, spring warming duration, and spring mixing duration of sediment core Tiefer-See

Monitoring during three meteorologically different spring seasons in 2012, 2013, and 2014 revealed that temperature increase in spring, which influences spring lake mixing duration, markedly affected nutrient availability and diatom deposition in a sediment trap close to the bottom of deep Tiefer See, NE Germany. Deposition of Stephanodiscus taxa and small Cyclotella taxa was much higher after late ice out and a deep, short lake mixing period in spring 2013, compared to that after gradual warming and lengthy lake mixing periods in spring 2012 and 2014, when only brief or marginal ice cover occurred. Availability of dissolved Si and P was 33 and 20 % higher, respectively, in 2013 compared to 2014. The observed relation between high (low) diatom deposition and short (lengthy) mixing duration in spring was applied to varved sediments deposited between AD 1924 and 2008. Low detrital Si content in trapped material and a sediment core enabled use of µXRF-counts of Si as a proxy for diatom silica. The spring mixing duration for 1951-2008 was derived from FLake-model calculations. The spring warming duration related to lake mixing was approximated from air temperatures for 1924-2008 using the dates when daily mean air temperature exceeded 5 °C (start) and 10 °C (end). Diatom silica deposition showed a significant (p < 0.0001) inverse linear relationship with the modeled spring mixing duration (R2 = 0.36) and the spring warming duration (R2 = 0.28). In both cases, the relationship is strengthened when data from the period of low diatom production (1987-2005) is excluded (R2 = 0.59 and R2 = 0.35). Part of this low diatom production is related to external nutrient supply that favored growth of cyanobacteria at the expense of diatoms. This approach shows that diatom Si deposition was strongly influenced by the availability of light and nutrients, related to the duration of lake mixing and warming in spring, during most of the studied period. The remaining unexplained variability, however, indicates that additional factors influence Si deposition. Further tests in other deep, temperate lakes are necessary to verify if this relation is a common feature and consequently, if diatom Si can be used as a proxy for spring mixing duration in such lakes.

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Kienel, Ulrike, Kirillin, Georgiy, Brademann, Brian, Plessen, Birgit, Lampe, Reinhard, Brauer, Achim (2017). Dataset: Diatom Si deposition, spring warming duration, and spring mixing duration of sediment core Tiefer-See. https://doi.org/10.1594/PANGAEA.871003

DOI retrieved: 2017

Additional Info

Field Value
Imported on November 29, 2024
Last update November 29, 2024
License CC-BY-3.0
Source https://doi.org/10.1594/PANGAEA.871003
Author Kienel, Ulrike
Given Name Ulrike
Family Name Kienel
More Authors
Kirillin, Georgiy
Brademann, Brian
Plessen, Birgit
Lampe, Reinhard
Brauer, Achim
Source Creation 2017
Publication Year 2017
Resource Type text/tab-separated-values - filename: Kienel-etal_2017
Subject Areas
Name: Ecology

Name: LakesRivers

Name: Lithosphere

Related Identifiers
Title: Effects of spring warming and mixing duration on diatom deposition in deep Tiefer See, NE Germany
Identifier: https://doi.org/10.1007/s10933-016-9925-z
Type: DOI
Relation: IsSupplementTo
Year: 2016
Source: Journal of Paleolimnology
Authors: Kienel Ulrike , Kirillin Georgiy , Brademann Brian , Plessen Birgit , Lampe Reinhard , Brauer Achim .