Abstract
Glycerol dialkyl glycerol tetraethers (GDGTs) are microbial membrane-spanning lipids that are produced in a variety of environments. To better understand the potentially confounding effect of soil chemistry on the temperature relationship of branched GDGTs (brGDGTs), isoprenoid GDGTs (isoGDGTs) and GDGT-based proxies MBT’5ME and TEX86, soils from 6 elevation transects (mean annual air temperature 0 – 26 ℃, n = 74) were analyzed. Corroborating earlier work, the MBT’5ME index correlates well with mean annual air temperature in the low pH (pH < 7), non-arid soils under study (r = 0.87, p < 0.001). However, a clear over-estimation of reconstructed temperature in the lowest pH (<3.5) soils is observed, explained by the correlation between brGDGT Ia and free acidity. TEX86 also shows a significant correlation with mean annual air temperature (r = 0.45, p < 0.001), driven by temperature dependent concentration changes of isoGDGTs 3 and cren’. However, an overarching correlation with P/E values dominates concentration changes of all supposed Thaumarchaeotal isoGDGTs lipids (GDGT1-3, cren and cren’), implying a potential impact of soil moisture on TEX86 values. In addition to identifying the impact of these confounding factors on the temperature proxy, GDGT ratios that can be used to constrain changes in soil chemistry, specifically exchangeable Ca2+, sum of basic cations, exchangeable Fe3+ and sum of soil metals are proposed (0.53 < r2 < 0.68), while existing ratios for soil moisture availability are tested for the first time in a dataset of non-arid soils. While the impact of soil chemistry on GDGTs may complicate the interpretation of their temperature proxies, our proposed GDGT ratios can potentially be used to constrain a subset of soil chemistry changes through time.
Original language | English |
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Article number | 104706 |
Pages (from-to) | 1-15 |
Number of pages | 15 |
Journal | Organic Geochemistry |
Volume | 187 |
DOIs | |
Publication status | Published - Jan 2024 |
Bibliographical note
Publisher Copyright:© 2023 The Authors
Funding
We acknowledge the insightful comments of two anonymous reviewers and the editorial team that have improved the manuscript. The authors of this manuscript acknowledge the following funding agencies; SNSF PRIMA Fellowship (PR00P2_179783) to CDJ, Swedish National Science Foundation (VR) grant 2017-04430 to RS, Bolin Center for Climate Research funded field work on Sumatra to PH. Soils from Austria, Bolivia, China and Tanzania are collected through the regional Technical Cooperation Project INT5153, from the International Atomic Energy Agency (IAEA). A NWO-Vidi grant (192.074) was awarded to FP. In addition, we are grateful for assistance in processing samples for analysis on EA-irms (ETH Zurich) by Madalina Jäggi.
Funders | Funder number |
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Swedish National Science Foundation | |
Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung | PR00P2_179783 |
Nederlandse Organisatie voor Wetenschappelijk Onderzoek | 192.074 |
Vetenskapsrådet | 2017-04430, INT5153 |
International Atomic Energy Agency |