Environmental Controls on Crenarchaeol Distributions in Hydrothermal Springs

TL;DR

This study finds that the unique archaeal lipid crenarchaeol is most abundant at neutral pH and moderate temperatures in hydrothermal springs.

Contribution

The study identifies optimal environmental conditions for crenarchaeol production and links pH as the strongest predictor of archaeal lipid composition.

Findings

Crenarchaeol relative abundance peaks at pH 7.4 and 46°C.

pH is the strongest predictor of iGDGT composition and cyclopentyl ring numbers.

The cyclohexyl ring in crenarchaeol may optimize membranes for neutral pH and moderate temperatures.

Abstract

Thermophilic archaea synthesise cellular membranes composed primarily of isoprenoid glycerol dibiphytanyl glycerol tetraethers (iGDGTs). Cells can adjust the packing of their lipids by increasing cyclopentyl ring production, thereby decreasing membrane permeability and fluidity to maintain cellular function at high temperature, acidic pH, or nutrient limitation. Archaea of the class Nitrososphaeria synthesise crenarchaeol, an iGDGT with four cyclopentyl rings and a cyclohexyl ring, the function of which is unknown. Structural modelling suggests the cyclohexyl ring may increase membrane fluidity, potentially optimising membranes for mesophilic conditions. To investigate the role of crenarchaeol in archaeal membranes in natural settings, we quantify iGDGT compositions of forty‐one thermal springs in Yellowstone National Park (YNP), USA, and contextualise these within a global compilation of thermal spring iGDGTs spanning pH values of 1.1–10.1 and temperatures of 16°C–95°C. Spring pH is the strongest predictor of both crenarchaeol relative abundance and the number of cyclopentyl rings per iGDGT. Crenarchaeol relative abundance exhibits a nonlinear relationship with pH and temperature, with highest relative abundances at pH 7.4 and 46°C, decreasing above and below these values. These observations indicate that the cyclohexyl ring of crenarchaeol optimises archaeal cellular membranes for circumneutral and moderate temperature environmental conditions.

The optimal pH and temperature for crenarchaeol (a unique archaeal lipid) production in hydrothermal springs are 7.4°C and 46°C, respectively, which has important implications for archaeal evolution. Our study also indicates that pH is the most important environmental variable for archaeal lipid membrane compositions.

Figures