39 Lakes as Sentinels of Environmental Change

Tuesday, 19 May 2020
1:30 PM - 5:30 PM
Lake Superior Ballroom MN


HYDROGEN ISOTOPES OF DIATOM-DERIVED C20 HIGHLY BRANCHED ISOPRENOIDS FROM LAKE SEDIMENTS TRACK LAKE WATER HYDROGEN ISOTOPES

Paper number: 39-7
Program: Theme Sessions
Time: 3:10 PM – 3:30 PM


Authors


Abstract

The hydrogen isotopic composition of lake water (δ2Hlw) contains hydrologic information, which can yield records of past evaporation and precipitation changes when studied from lake sediment archives. Unfortunately, few proxies exist that record only δ2Hlw and instead represent a mix of aquatic and terrestrial material. Diatoms are single-celled microalgae that produce highly branched isoprenoids (HBIs) in marine and lacustrine settings. We present a pilot dataset that indicates that the hydrogen isotopic composition of HBIs (δ2HHBI) is a novel way to track δ2Hlw. A total of 42 sediment samples from 10 lakes in the Adirondacks in NY were analyzed for δ2HHBI and compared to δ2Hlw to determine that the average fractionation (εHBI/lw) between HBIs and lake water is -127+16‰. There is a large consistency between εHBI/lw in samples taken at deeper (>4m) lake water depths whereas samples collected from shallow depths have a larger εHBI/lw suggesting that other factors may influence HBI fractionation. Further work needs to be done to determine what factors such as salinity, seasonality, pH and diatom community compositions, might also influence fractionation. We are optimistic that the δ2H of HBIs can be used to reconstruct lake water δ2H through time to in order to better assess how lake systems have changed in the past.

Geological Society of America Abstracts with Programs. Vol. 52, No. 5

doi: 10.1130/abs/2020NC-348192

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