AI Article Synopsis

  • Branched glycerol dialkyl glycerol tetraethers (brGDGTs) are bacterial lipids found in peatland soils, and their distribution is linked to climate changes and temperature, but current models for temperature prediction using brGDGTs have high uncertainty.
  • In a boreal peatland study over four years of warming, it was found that total brGDGT concentrations increased, with changes in their distribution in surface layers while deeper layers remained unaffected, suggesting limited microbial activity there.
  • The study identified depth-specific responses of brGDGTs to temperature changes and emphasized that soil temperature and water table depth are key factors influencing brGDGT distribution, indicating a need for a deeper understanding in paleoenvironment

Article Abstract

Branched glycerol dialkyl glycerol tetraethers (brGDGTs) are bacterial membrane lipids whose distribution in peatland soils serves as an important proxy for past climate changes due to strong linear correlations with temperature in modern environments. However, commonly used brGDGT-based temperature models are characterized by high uncertainty (ca. 4 °C) and these calibrations can show implausible correlations when applied at an ecosystem level. This lack of accuracy is often attributed to our limited understanding of the exact mechanisms behind the relationship between brGDGTs and temperature and the potential effect of temperature-independent factors on brGDGT distribution. Here, we examine the abundance and distribution of brGDGTs in a boreal peatland after four years of in-situ warming (+0, +2.25, +4.5, +6.75 and +9 °C). We observed that with warming, concentrations of total brGDGTs increased. Furthermore, we determined a shift in brGDGT distribution in the surface aerobic layers of the acrotelm (0-30 cm depth), whereas no detectable change was observed at deeper anaerobic depths (>40 cm), possibly due to limited microbial activity. The response of brGDGTs to warming was also reflected by a strong increase in the methylation index of 5-methyl brGDGTs (MBT'), classically used as a temperature proxy. Further, the relationship between the MBT' index and soil temperature differed between 0-10, 10-20 and 20-30 cm depth, highlighting depth-specific response of brGDGTs to warming, which should be considered in paleoenvironmental and paleoecological studies. As the bacterial community composition was generally unaltered, the rapid changes in brGDGT distribution argue for a physiological adaptation of the microorganisms producing these lipids. Finally, soil temperature and water table depth were better predictors of brGDGT concentration and distribution, highlighting the potential for these drivers to impact brGDGT-based proxies. To summarize, our results provide insights on the response of brGDGT source microorganisms to soil warming and underscore brGDGTs as viable temperature proxies for better understanding of climatic perturbation in peatlands.

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http://dx.doi.org/10.1016/j.scitotenv.2024.171666DOI Listing

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Article Synopsis
  • Branched glycerol dialkyl glycerol tetraethers (brGDGTs) are bacterial lipids found in peatland soils, and their distribution is linked to climate changes and temperature, but current models for temperature prediction using brGDGTs have high uncertainty.
  • In a boreal peatland study over four years of warming, it was found that total brGDGT concentrations increased, with changes in their distribution in surface layers while deeper layers remained unaffected, suggesting limited microbial activity there.
  • The study identified depth-specific responses of brGDGTs to temperature changes and emphasized that soil temperature and water table depth are key factors influencing brGDGT distribution, indicating a need for a deeper understanding in paleoenvironment
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Christian-Albrechts-University, Institute of Geosciences, Ludewig-Meyn-Straße 10, 24118 Kiel, Germany; Western Australian Organic and Isotope Geochemistry Centre, The Institute for Geoscience Research, School of Earth and Planetary Sciences, Curtin University, Perth, WA 6102, Australia. Electronic address:

Branched glycerol dialkyl glycerol tetraethers (brGDGTs) are common in lake sediments, where they are frequently employed to infer mean annual air temperatures (MAAT) or air temperatures of months above freezing (MAF) using the MBT' lipid paleothermometer. The reliable reconstruction of such temperatures, however, requires robust calibration functions. Here, we investigated brGDGT distributions in surface sediments from 41 freshwater lakes located along an altitudinal gradient across the Alps (Central Europe) and spanning a MAAT range from 1.

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Department of Geological Sciences and Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, CO 80309, USA.

Bacterial brGDGT lipids are a prevalent tool in studies of terrestrial paleoclimate. Their distributions correlate empirically with environmental temperature and pH, and their ubiquity in terrestrial, freshwater, and marine environments gives them wide applicability. Whether correlations with temperature and pH emerge due to a physiological response of source organisms and/or a shift in bacterial community composition remains an open question with important implications for proxy development and application.

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Distributions of soil branched glycerol dialkyl glycerol tetraethers from different climate regions of China.

Sci Rep

February 2019

Guangdong Provincial Key Laboratory of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou, China.

Distributions of branched glycerol dialkyl glycerol tetraethers (brGDGTs) from soil bacteria have been recently used for reconstructions of past soil pH and air temperature history. Here, we report the brGDGTs distribution patterns from different climate regions of China, using 42 novel brGDGT data from sub-tropical Chinese soils, compiled alongside previously-published data encompassing different environmental conditions across China. These patterns show high abundance of Ia fraction in soils from humid areas, and high abundance of IIa' and IIIa' fractions corresponds to semi-humid or semi-arid conditions, implying a possible relationship with precipitation.

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