The stable carbon isotopic composition of Daphnia ephippia in small, temperate lakes reflects in‐lake methane availability

Abstract

AbstractDaphnia can ingest methane‐oxidizing bacteria and incorporate methanogenic carbon into their biomass, leading to low stable carbon isotope ratios (expressed as δ13C values) of their tissue. Therefore, δ13C analysis of Daphnia resting eggs (ephippia) in lake sediment records can potentially be used to reconstruct past in‐lake availability of methane (CH4). However, detailed multilake studies demonstrating that δ13C values of recently deposited Daphnia ephippia (δ13Cephippia) are systematically related to in‐lake CH4 concentrations ([CH4]aq) are still missing. We measured δ13Cephippia from surface sediments of 15 small lakes in Europe, and compared these values with late‐summer [CH4]aq. δ13Cephippia ranged from −51.6‰ to −25.9‰, and was strongly correlated with [CH4]aq in the surface water and above the sediment (r −0.73 and −0.77, respectively), whereas a negative rather than the expected positive correlation was found with δ13C values of carbon dioxide (CO2) (r −0.54), and no correlation was observed with [CO2]aq. At eight sites, offsets between δ13 and δ13Cephippia exceeded offsets between δ13 and δ13Calgae reported in literature. δ13Cephippia was positively correlated with δ13C values of sedimentary organic matter (r 0.54), but up to 20.7‰ lower in all except one of the lakes (average −6.1‰). We conclude that incorporation of methanogenic carbon prior to ephippia formation must have been widespread by Daphnia in our study lakes, especially those with high [CH4]aq. Our results suggest a systematic relationship between δ13Cephippia values and [CH4]aq in small temperate lakes, and that δ13Cephippia analysis on sediment records may provide insights into past changes in in‐lake [CH4]aq.