Elucidating the details of the formation, stability, interactions, and reactivity of biomolecular systems under extreme environmental conditions, including high salt concentrations in brines and high osmotic and high hydrostatic pressures, is of fundamental biological, astrobiological, and biotechnological importance. Bacteria and archaea are able to survive in the deep ocean or subsurface of Earth, where pressures of up to 1 kbar are reached. The deep subsurface of Mars may host high concentrations of ions in brines, such as perchlorates, but we know little about how these conditions and the resulting osmotic stress conditions would affect the habitability of such environments for cellular life. We discuss the combined effects of osmotic (salts, organic cosolvents) and hydrostatic pressures on the structure, stability, and reactivity of biomolecular systems, including membranes, proteins, and nucleic acids. To this end, a variety of biophysical techniques have been applied, including calorimetry, UV/vis, FTIR and fluorescence spectroscopy, and neutron and X-ray scattering, in conjunction with high pressure techniques. Knowledge of these effects is essential to our understanding of life exposed to such harsh conditions, and of the physical limits of life in general. Finally, we discuss strategies that not only help us understand the adaptive mechanisms of organisms that thrive in such harsh geological settings but could also have important ramifications in biotechnological and pharmaceutical applications.

Disease-associated progression of protein dysfunction is typically determined by an interplay of transition pathways leading to liquid−liquid phase separation (LLPS) and amyloid fibrils. As LLPS introduces another layer of complexity into fibrillization of metastable proteins, a need for tunable model systems to study these intertwined processes has emerged. Here, we demonstrate the LLPS/fibrillization properties of a family of chimeric peptides, ACC 1−13 K n , in which the highly amyloidogenic fragment of insulin (ACC 1−13 ) is merged with oligolysine segments of various lengths (K n , n = 8, 16, 24, 32, 40). LLPS and fibrillization of ACC 1−13 K n are triggered by ATP through Coulombic interactions with K n fragments. ACC 1−13 K 8 and ACC 1−13 K 16 form fibrils after a short lag phase without any evidence of LLPS. However, in the case of the three longest peptides, ATP triggers instantaneous LLPS followed by the disappearance of droplets occurring in-phase with the formation of amyloid fibrils. The kinetics of the phase transition and the stability of mature co-aggregates are highly sensitive to ionic strength, indicating that electrostatic interactions play a pivotal role in selecting the LLPS-fibrillization transition pathway. Densely packed ionic interactions that characterize ACC 1−13 K n −ATP fibrils render them highly sensitive to hydrostatic pressure due to solvent electrostriction, as demonstrated by infrared spectroscopy. Using atomic force microscopy imaging of rapidly frozen samples, we demonstrate that early fibrils form within single liquid droplets, starting at the droplet/bulk interface through the formation of single bent fibers. A hypothetical molecular scenario underlying the emergence of the LLPS-to-fibrils pathway in the ACC 1−13 K n −ATP system has been put forward.

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Deep subsurface environments can harbour high concentrations of dissolved ions, yet we know little about how this shapes the conditions for life. We know even less about how the combined effects of high pressure influence the way in which ions constrain the possibilities for life. One such ion is perchlorate, which is found in extreme environments on Earth and pervasively on Mars. We investigated the interactions of high pressure and high perchlorate concentrations on enzymatic activity. We demonstrate that high pressures increase α-chymotrypsin enzyme activity even in the presence of high perchlorate concentrations. Perchlorate salts were shown to shift the folded α-chymotrypsin phase space to lower temperatures and pressures. The results presented here may suggest that high pressures increase the habitability of environments under perchlorate stress. Therefore, deep subsurface environments that combine these stressors, potentially including the subsurface of Mars, may be more habitable than previously thought.

High pressure is an important feature of certain natural environments, such as the deep sea where pressures up to about 1000 bar are encountered. Further, pressure effects on biosystems are of increasing interest for biotechnological applications, such as baroenzymology. We studied the effect of two different natural osmolyte mixtures, with major components being glycine and trimethylamine-N-oxide (TMAO), on the activity of α-chymotrypsin, using high-pressure stopped-flow methodology in combination with fast UV/Vis detection. We show that pressure is not only able to drastically enhance the catalytic activity and efficiency of the enzyme, but also that glycine has a significant and diverse effect on the enzymatic activity and volumetric properties of the reaction compared to TMAO. The results might not only help to understand the modulation of enzymatic reactions by natural osmolytes, but also elucidate ways to optimize enzymatic processes in biotechnological applications.