2021
DOI: 10.1016/j.orggeochem.2021.104222
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Identifying plant wax inputs in lake sediments using machine learning

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Cited by 22 publications
(38 citation statements)
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“…Specifically, this study provides evidence that submerged aquatic plants are the primary sources of mid‐chain waxes to QPT lake sediments, and thus can be used in paleoclimate studies to reconstruct changes in lake water δ 2 H over time (Gorbey et al., 2021). While we were unable to quantify the proportion of terrestrial and aquatic plant contribution to long‐chain waxes in QPT lake sediments, future studies may be able to achieve this using a machine learning or multi‐source mixing model approach (Peaple et al., 2021; Yang & Bowen, 2022).…”
Section: Discussionmentioning
confidence: 93%
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“…Specifically, this study provides evidence that submerged aquatic plants are the primary sources of mid‐chain waxes to QPT lake sediments, and thus can be used in paleoclimate studies to reconstruct changes in lake water δ 2 H over time (Gorbey et al., 2021). While we were unable to quantify the proportion of terrestrial and aquatic plant contribution to long‐chain waxes in QPT lake sediments, future studies may be able to achieve this using a machine learning or multi‐source mixing model approach (Peaple et al., 2021; Yang & Bowen, 2022).…”
Section: Discussionmentioning
confidence: 93%
“…n ‐alkanes are less prone to degradation than n ‐alkanoic acids in sediments (Cranwell, 1981), and their distributions are additional tools for assessing the source of plant waxes to lake sediments (Ficken et al., 2000; Gao et al., 2011; Peaple et al., 2021). Due to their resistance to degradation in high‐latitude environments like the QPT catchment, however, terrestrial plant n ‐alkanes may be prone to prolonged storage in soils prior to erosion and deposition in the lake sediment (Drenzek et al., 2007; Kusch et al., 2021).…”
Section: Discussionmentioning
confidence: 99%
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“…This allows δ 13 C to be used to constrain the uncertainty associated with n-alkane chain length distributions, which have previously been used in isolation to reconstruct vegetation (Gao et al, 2011;Jansen et al, 2010;Peaple et al, 2021). The model also addresses a common assumption in the interpretation of lipid δ 13 C data via linear mixing relationships, in which n-alkane production for a selected chain is assumed to be the same among all sources (Bush and Mcinerney, 2013;Garcin et al, 2014).…”
Section: Model Achievementsmentioning
confidence: 99%
“…The large uncertainties associated with characteristic n-alkane chain length distributions have limited their application in quantitative vegetation reconstruction (Bush and McInerney, 2013). Several models have been developed to reconstruct vegetation composition from n-alkyl lipid chain length distribution (Jansen et al, 2010;Gao et al, 2011;Peaple et al, 2021), but they all require a wide spectrum of chains to be analyzed, which may not be feasible depending on the type of sediment analyzed.…”
Section: Introductionmentioning
confidence: 99%