Effects of Crowding and Cosolutes on Biomolecular Function at Extreme Environmental Conditions.

The extent of the effect of cellular crowding and cosolutes on the functioning of proteins and cells is manifold and includes the stabilization of the biomolecular systems, the excluded volume effect, and the modulation of molecular dynamics. Simultaneously, it is becoming increasingly clear how important it is to take the environment into account if we are to shed light on biological function under various external conditions. Many biosystems thrive under extreme conditions, including the deep sea and subseafloor crust, and can take advantage of some of the effects of crowding. These relationships have been studied in recent years using various biophysical techniques, including neutron and X-ray scattering, calorimetry, FTIR, UV-vis and fluorescence spectroscopies. Combining knowledge of the structure and conformational dynamics of biomolecules under extreme conditions, such as temperature, high hydrostatic pressure, and high salinity, we highlight the importance of considering all results in the context of the environment. Here we discuss crowding and cosolute effects on proteins, nucleic acids, membranes, and live cells and explain how it is possible to experimentally separate crowding-induced effects from other influences. Such findings will contribute to a better understanding of the homeoviscous adaptation of organisms and the limits of life in general.

Acidification-based mineral weathering mechanism involves a glucose/methanol/choline oxidoreductase in Caballeronia mineralivorans PML1(12).

While mineral weathering (MWe) plays a key role in plant growth promotion and soil fertility, the molecular mechanisms and the genes used by bacteria to weather minerals remain poorly characterized. Acidification-based dissolution is considered the primary mechanism used by bacteria. This mechanism is historically associated with the conversion of glucose to protons and gluconic acid through the action of particular glucose dehydrogenases (GDH) dependent on the pyrroquinoline quinone (PQQ) cofactor. Recently, bacteria lacking the GDH-PQQ system have been shown to perform the same enzymatic conversion with a glucose/methanol/choline (GMC) FAD-dependent oxidoreductase. Determining whether this particular enzyme is specific or widespread is especially important in terms of ecology and evolution. Genome analysis of the effective MWe strain Caballeronia mineralivorans PML1(12) revealed the presence of both systems (i.e., GDH-PQQ and several GMC oxidoreductases). The combination of mutagenesis, functional assays, and geochemical analyses demonstrated the key role of one of these GMC oxidoreductases in the mineral weathering ability of strain PML1(12) and the importance of the carbon source metabolized. Mass spectrometry confirmed the conversion of glucose to gluconic acid. Phylogenetic analyses highlighted a good relatedness of this new GMC oxidoreductase with GMC oxidoreductases presenting a GDH activity in Burkholderia cepacia and Collimonas pratensis and conferring its mineral weathering ability to the last one. Together, our analyses expand the number of bacteria capable of weathering minerals using GMC oxidoreductases, showing that such enzymes are not restricted to Collimonas. IMPORTANCE: This work deciphers the molecular and genetic bases used by strain PML1(12) of Caballeronia mineralivorans to weather minerals. Through bioinformatics analyses, we identified a total of four GMC-FAD oxidoreductases in the genome of strain PML1(12) and a putative PQQ-dependent glucose dehydrogenase. Through a combination of physiological and geochemical analyses, we revealed that one of them (i.e., GMC3) was the enzyme responsible for the acidification-based mineral weathering mechanism used by strain PML1(12). To date, a single representative of this enzyme family has been identified in the effective mineral-weathering bacterial strain Collimonas pratensis PMB3(1). Phylogenetic analyses revealed that this new system appeared conserved in the Collimonas genus. The new findings presented in this work demonstrate that GMC oxidoreductases can have an active role in other effective MWe bacteria outside of collimonads and that Caballeronia are capable of weathering minerals using this type of enzyme. Our findings offer relevant information for different fields of research, such as environmental genomics, microbiology, chemistry, evolutionary biology, and soil sciences.

The non-ribosomal peptide synthetase-independent siderophore (NIS) rhizobactin produced by Caballeronia mineralivorans PML1(12) confers the ability to weather minerals.

To mobilize nutrients entrapped into minerals and rocks, heterotrophic bacteria living in nutrient-poor environments have developed different mechanisms based mainly on acidolysis and chelation. However, the genetic bases of these mechanisms remain unidentified. To fill this gap, we considered the model strain Caballeronia mineralivorans PML1(12) known to be effective at weathering. Based on its transcriptomics and proteomics responses in Fe-depleted conditions, we pointed a cluster of genes differentially expressed and putatively involved in the production of siderophores. In this study, we report the characterization of this gene region coding for the production of a non-ribosomal peptide synthetase-independent siderophore (NIS). Targeted mutagenesis associated with functional assays and liquid chromatography coupled to high-resolution tandem mass spectrometry demonstrated the production of a single siderophore, identified as rhizobactin. This siderophore represents the first NIS containing malic acid in its structure. The evidence for the implication of rhizobactin in mineral weathering was demonstrated during a hematite dissolution assay. This study provides the first demonstration of the synthesis of a NIS in the genus Caballeronia and its involvement in mineral weathering. Our conclusions reinforce the idea that strain PML1(12) is particularly well adapted to nutrient-poor environments. IMPORTANCE This work deciphers the molecular and genetic bases used by strain PML1(12) of Caballeronia mineralivorans to mobilize iron and weather minerals. Through the combination of bioinformatics, chemical, and phylogenetic analyses, we characterized the siderophore produced by strain PML1(12) and the related genes. This siderophore was identified as rhizobactin and classified as a non-ribosomal peptide synthetase-independent siderophore (NIS). Contrary to the previously identified NIS synthetases that form siderophores containing citric acid, α-ketoglutarate, or succinic acid, our analyses revealed that rhizobactin contains malic acid in its structure, representing, therefore, the first identified NIS with such an acid and probably a new NIS category. Last, this work demonstrates for the first time the effectiveness at weathering minerals of a siderophore of the NIS family. Our findings offer relevant information for different fields of research, such as environmental genomics, microbiology, chemistry, and soil sciences.

Phytoplanktonic species in the haloalkaline Lake Dziani Dzaha select their archaeal microbiome.

Microorganisms are key contributors of aquatic biogeochemical cycles but their microscale ecology remains largely unexplored, especially interactions occurring between phytoplankton and microorganisms in the phycosphere, that is the region immediately surrounding phytoplankton cells. The current study aimed to provide evidence of the phycosphere taking advantage of a unique hypersaline, hyperalkaline ecosystem, Lake Dziani Dzaha (Mayotte), where two phytoplanktonic species permanently co-dominate: a cyanobacterium, Arthrospira fusiformis, and a green microalga, Picocystis salinarum. To assay phycospheric microbial diversity from in situ sampling, we set up a flow cytometry cell-sorting methodology for both phytoplanktonic populations, coupled with metabarcoding and comparative microbiome diversity. We focused on archaeal communities as they represent a non-negligible part of the phycospheric diversity, however their role is poorly understood. This work is the first which successfully explores in situ archaeal diversity distribution showing contrasted phycospheric compositions, with P. salinarum phycosphere notably enriched in Woesearchaeales OTUs while A. fusiformis phycosphere was enriched in methanogenic lineages affiliated OTUs such as Methanomicrobiales or Methanofastidiosales. Most archaeal OTUs, including Woesearchaeales considered in literature as symbionts, were either ubiquitous or specific of the free-living microbiome (i.e. present in the 3-0.2 µm fraction). Seminally, several archaeal OTUs were enriched from the free-living microbiome to the phytoplankton phycospheres, suggesting (i) either the inhibition or decrease of other OTUs, or (ii) the selection of specific OTUs resulting from the physical influence of phytoplanktonic species on surrounding Archaea.

Bradyrhizobium commune sp. nov., isolated from nodules of a wide range of native legumes across the Australian continent.

Bradyrhizobia are particularly abundant in Australia, where they nodulate native legumes growing in the acidic and seasonally dry soils that predominate in these environments. They are essential to Australian ecosystems by helping legumes to compensate for nutrient deficiencies and the low fertility of Australian soils. During a survey of Australian native rhizobial communities in 1994-1995, several Bradyrhizobium genospecies were identified, among which genospecies B appeared to be present in various edaphic and climatic conditions and associate with a large range of leguminous hosts across the whole continent. We took advantage of the recent sequencing of the genome of strain BDV5040T, representative of Bradyrhizobium genospecies B, to re-evaluate the taxonomic status of this lineage. We further characterized strain BDV5040T based on morpho-physiological traits and determined its phylogenetic relationships with the type strains of all currently described Bradyrhizobium species using both small subunit (SSU) rRNA gene and complete genome sequences. The digital DNA-DNA hybridization relatedness with any type strain was less than 35 % and both SSU rRNA gene and genome phylogenies confirmed the initial observation that this strain does not belong to any formerly described species within the genus Bradyrhizobium. All data thus support the description of the novel species Bradyrhizobium commune sp. nov. for which the type strain is BDV5040T (=CFBP 9110T=LMG 32898T), isolated from a nodule of Bossiaea ensata in Ben Boyd National Park in New South Wales, Australia.

Biochemical and mutational studies of an endonuclease V from the hyperthermophilic crenarchaeon Sulfolobus islandicus REY15A.

Endonuclease V (EndoV), which is widespread in bacteria, eukarya and Archaea, can cleave hypoxanthine (Hx)-containing DNA or RNA strand, and play an essential role in Hx repair. However, our understanding on archaeal EndoV's function remains incomplete. The model archaeon Sulfolobus islandicus REY15A encodes a putative EndoV protein (Sis-EndoV). Herein, we probed the biochemical characteristics of Sis-EndoV and dissected the roles of its seven conserved residues. Our biochemical data demonstrate that Sis-EndoV displays maximum cleavage efficiency at above 60 °C and at pH 7.0-9.0, and the enzyme activity is dependent on a divalent metal ion, among which Mg2+ is optimal. Importantly, we first measured the activation energy for cleaving Hx-containing ssDNA by Sis-EndoV to be 9.6 ± 0.8 kcal/mol by kinetic analyses, suggesting that chemical catalysis might be a rate-limiting step for catalysis. Mutational analyses show that residue D38 in Sis-EndoV is essential for catalysis, but has no role in DNA binding. Furthermore, we first revealed that residues Y41 and D189 in Sis-EndoV are involved in both DNA cleavage and DNA binding, but residues F77, H103, K156 and F161 are only responsible for DNA binding.

Membrane adaptation in the hyperthermophilic archaeon Pyrococcus furiosus relies upon a novel strategy involving glycerol monoalkyl glycerol tetraether lipids.

Microbes preserve membrane functionality under fluctuating environmental conditions by modulating their membrane lipid composition. Although several studies have documented membrane adaptations in Archaea, the influence of most biotic and abiotic factors on archaeal lipid compositions remains underexplored. Here, we studied the influence of temperature, pH, salinity, the presence/absence of elemental sulfur, the carbon source and the genetic background on the lipid core composition of the hyperthermophilic neutrophilic marine archaeon Pyrococcus furiosus. Every growth parameter tested affected the lipid core composition to some extent, the carbon source and the genetic background having the greatest influence. Surprisingly, P. furiosus appeared to only marginally rely on the two major responses implemented by Archaea, i.e. the regulation of the ratio of diether to tetraether lipids and that of the number of cyclopentane rings in tetraethers. Instead, this species increased the ratio of glycerol monoalkyl glycerol tetraethers (GMGT, aka. H-shaped tetraethers) to glycerol dialkyl glycerol tetraethers in response to decreasing temperature and pH and increasing salinity, thus providing for the first time evidence of adaptive functions for GMGT. Besides P. furiosus, numerous other species synthesize significant proportions of GMGT, which suggests that this unprecedented adaptive strategy might be common in Archaea.

The mineral weathering ability of Collimonas pratensis PMB3(1) involves a Malleobactin-mediated iron acquisition system.

Mineral weathering by microorganisms is considered to occur through a succession of mechanisms based on acidification and chelation. While the role of acidification is established, the role of siderophores is difficult to disentangle from the effect of the acidification. We took advantage of the ability of strain Collimonas pratensis PMB3(1) to weather minerals but not to acidify depending on the carbon source to address the role of siderophores in mineral weathering. We identified a single non-ribosomal peptide synthetase (NRPS) responsible for siderophore biosynthesis in the PMB3(1) genome. By combining iron-chelating assays, targeted mutagenesis and chemical analyses (HPLC and LC-ESI-HRMS), we identified the siderophore produced as malleobactin X and how its production depends on the concentration of available iron. Comparison with the genome sequences of other collimonads evidenced that malleobactin production seems to be a relatively conserved functional trait, though some collimonads harboured other siderophore synthesis systems. We also revealed by comparing the wild-type strain and its mutant impaired in the production of malleobactin that the ability to produce this siderophore is essential to allow the dissolution of hematite under non-acidifying conditions. This study represents the first characterization of the siderophore produced by collimonads and its role in mineral weathering.

High temperature molecular motions within a model protomembrane architecture.

Modern phospholipid membranes are known to be in a functional, physiological state, corresponding to the liquid crystalline phase, only under very precise external conditions. The phase is characterised by specific lipid motions, which seem mandatory to permit sufficient flexibility and stability for the membrane. It can be assumed that similar principles hold for proto-membranes at the origin of life although they were likely composed of simpler, single chain fatty acids and alcohols. In the present study we investigated molecular motions of four types of model membranes to shed light on the variations of dynamics and structure from low to high temperature as protocells might have existed close to hot vents. We find a clear hierarchy among the flexibilities of the samples, where some structural parameters seem to depend on the lipid type used while others do not.

Unravelling the Adaptation Mechanisms to High Pressure in Proteins.

Life is thought to have appeared in the depth of the sea under high hydrostatic pressure. Nowadays, it is known that the deep biosphere hosts a myriad of life forms thriving under high-pressure conditions. However, the evolutionary mechanisms leading to their adaptation are still not known. Here, we show the molecular bases of these mechanisms through a joint structural and dynamical study of two orthologous proteins. We observed that pressure adaptation involves the decoupling of protein-water dynamics and the elimination of cavities in the protein core. This is achieved by rearranging the charged residues on the protein surface and using bulkier hydrophobic residues in the core. These findings will be the starting point in the search for a complete genomic model explaining high-pressure adaptation.

Straightforward Synthesis of Chiral Terpenoid Building Blocks by Ru-Catalyzed Enantioselective Hydrogenation.

Starting from commercially available (R)- and (S)-ß-citronellol, two strategies were designed to synthesize all four stereoisomers of 2,6-dimethyloctane monoterpene chirons in four or five steps in 32-47% overall yield. The desired fragments were obtained by a key Ru-catalyzed asymmetric olefin hydrogenation step under moderate temperature (50 °C), pressure (4 bar), and low catalyst loadings (0.5 mol %) under optimized conditions. Screening of commercially available catalysts highlighted the key role of DM-SEGPHOS as an economically advantageous alternative to commonly used H8-BINAP for equal performances. These results open new possibilities for versatile and scalable syntheses of these useful building blocks.

Identification of a novel bifunctional uracil DNA glycosylase from Thermococcus barophilus Ch5.

Genomes of hyperthermophiles are facing a severe challenge due to increased deamination rates of cytosine induced by high temperature, which could be counteracted by base excision repair mediated by uracil DNA glycosylase (UDG) or other repair pathways. Our previous work has shown that the two UDGs (Tba UDG247 and Tba UDG194) encoded by the genome of the hyperthermophilic euryarchaeon Thermococcus barophilus Ch5 can remove uracil from DNA at high temperature. Herein, we provide evidence that Tba UDG247 is a novel bifunctional glycosylase which can excise uracil from DNA and further cleave the phosphodiester bo nd of the generated apurinic/apyrimidinic (AP) site, which has never been described to date. In addition to cleaving uracil-containing DNA, Tba UDG247 can also cleave AP-containing ssDNA although at lower efficiency, thereby suggesting that the enzyme might be involved in repair of AP site in DNA. Kinetic analyses showed that Tba UDG247 displays a faster rate for uracil excision than for AP cleavage, thus suggesting that cleaving AP site by the enzyme is a rate-limiting step for its bifunctionality. Phylogenetic analysis showed that Tba UDG247 is clustered on a separate branch distant from all the reported UDGs. Overall, we designated Tba UDG247 as the prototype of a novel family of bifunctional UDGs. KEY POINTS: We first reported a novel DNA glycosylase with bifunctionality. Tba UDG247 possesses an AP lyase activity.

Non-Polar Lipids as Regulators of Membrane Properties in Archaeal Lipid Bilayer Mimics.

The modification of archaeal lipid bilayer properties by the insertion of apolar molecules in the lipid bilayer midplane has been proposed to support cell membrane adaptation to extreme environmental conditions of temperature and hydrostatic pressure. In this work, we characterize the insertion effects of the apolar polyisoprenoid squalane on the permeability and fluidity of archaeal model membrane bilayers, composed of lipid analogues. We have monitored large molecule and proton permeability and Laurdan generalized polarization from lipid vesicles as a function of temperature and hydrostatic pressure. Even at low concentration, squalane (1 mol%) is able to enhance solute permeation by increasing membrane fluidity, but at the same time, to decrease proton permeability of the lipid bilayer. The squalane physicochemical impact on membrane properties are congruent with a possible role of apolar intercalants on the adaptation of Archaea to extreme conditions. In addition, such intercalant might be used to cheaply create or modify chemically resistant liposomes (archeaosomes) for drug delivery.

High-Temperature Behavior of Early Life Membrane Models.

Origin of life scenarios generally assume an onset of cell formation in terrestrial hot springs or in the deep oceans close to hot vents, where energy was available for non-enzymatic reactions. Membranes of the protocells had therefore to withstand extreme conditions different from what is found on the Earth surface today. We present here an exhaustive study of temperature stability up to 80 °C of vesicles formed by a mixture of short-chain fatty acids and alcohols, which are plausible candidates for membranes permitting the compartmentalization of protocells. We confirm that the presence of alcohol has a strong structuring and stabilizing impact on the lamellar structures. Moreover and most importantly, at a high temperature (> 60 °C), we observe a conformational transition in the vesicles, which results from vesicular fusion. Because all the most likely environments for the origin of life involve high temperatures, our results imply the need to take into account such a transition and its effect when studying the behavior of a protomembrane model.

Structural Characterization of an Archaeal Lipid Bilayer as a Function of Hydration and Temperature.

Archaea, the most extremophilic domain of life, contain ether and branched lipids which provide extraordinary bilayer properties. We determined the structural characteristics of diether archaeal-like phospholipids as functions of hydration and temperature by neutron diffraction. Hydration and temperature are both crucial parameters for the self-assembly and physicochemical properties of lipid bilayers. In this study, we detected non-lamellar phases of archaeal-like lipids at low hydration levels, and lamellar phases at levels of 90% relative humidity or more exclusively. Moreover, at 90% relative humidity, a phase transition between two lamellar phases was discernible. At full hydration, lamellar phases were present up to 70ᵒC and no phase transition was observed within the temperature range studied (from 25 °C to 70 °C). In addition, we determined the neutron scattering length density and the bilayer's structural parameters from different hydration and temperature conditions. At the highest levels of hydration, the system exhibited rearrangements on its corresponding hydrophobic region. Furthermore, the water uptake of the lipids examined was remarkably high. We discuss the effect of ether linkages and branched lipids on the exceptional characteristics of archaeal phospholipids.

The first study on the impact of osmolytes in whole cells of high temperature-adapted microorganisms.

The hyperthermophilic piezophile, Thermococcus barophilus displays a strong stress response characterized by the accumulation of the organic osmolyte, mannosylglycerate during growth under sub-optimal pressure conditions (0.1 MPa). Taking advantage of this known effect, the impact of osmolytes in piezophiles in an otherwise identical cellular context was investigated, by comparing T. barophilus cells grown under low or optimal pressures (40 MPa). Using neutron scattering techniques, we studied the molecular dynamics of live cells of T. barophilus at different pressures and temperatures. We show that in the presence of osmolytes, cells present a higher diffusion coefficient of hydration water and an increase of bulk water motions at a high temperature. In the absence of osmolytes, the T. barophilus cellular dynamics is more responsive to high temperature and high hydrostatic pressure. These results therefore give clear evidence for a protecting effect of osmolytes on proteins.

Biochemical characterization and mutational studies of the 8-oxoguanine DNA glycosylase from the hyperthermophilic and radioresistant archaeon Thermococcus gammatolerans.

8-oxoguanine (GO) is a major lesion found in DNA that arises from guanine oxidation. The hyperthermophilic and radioresistant euryarchaeon Thermococcus gammatolerans encodes an archaeal GO DNA glycosylase (Tg-AGOG). Here, we characterized biochemically Tg-AGOG and probed its GO removal mechanism by mutational studies. Tg-AGOG can remove GO from DNA at high temperature through a ß-elimination reaction. The enzyme displays an optimal temperature, ca.85-95 °C, and an optimal pH, ca.7.0-8.5. In addition, Tg-AGOG activity is independent on a divalent metal ion. However, both Co2+ and Cu2+ inhibit its activity. The enzyme activity is also inhibited by NaCl. Furthermore, Tg-AGOG specifically cleaves GO-containing dsDNA in the order: GO:C, GO:T, GO:A, and GO:G. Moreover, the temperature dependence of cleavage rates of the enzyme was determined, and from this, the activation energy for GO removal from DNA was first estimated to be 16.9 ± 0.9 kcal/mol. In comparison with the wild-type Tg-AGOG, the R197A mutant has a reduced cleavage activity for GO-containing DNA, whereas both the P193A and F167A mutants exhibit similar cleavage activities for GO-containing DNA. While the mutations of P193 and F167 to Ala lead to increased binding, the mutation of R197 to Ala had no significant effect on binding. These observations suggest that residue R197 is involved in catalysis, and residues P193 and F167 are flexible for conformational change.

Biochemical characterization of a thermostable DNA ligase from the hyperthermophilic euryarchaeon Thermococcus barophilus Ch5.

DNA ligases are essential enzymes for DNA replication, repair, and recombination processes by catalyzing a nick-joining reaction in double-stranded DNA. The genome of the hyperthermophilic euryarchaeon Thermococcus barophilus Ch5 encodes a putative ATP-dependent DNA ligase (Tba ligase). Herein, we characterized the biochemical properties of the recombinant Tba ligase. The enzyme displays an optimal nick-joining activity at 65-70 °C and retains its DNA ligation activity even after heated at 100 °C for 2 h, suggesting the enzyme is a thermostable DNA ligase. The enzyme joins DNA over a wide pH spectrum ranging from 5.0-10.0, and its optimal pH is 6.0-9.0. Tba ligase activity is dependent on a divalent metal ion: Mn2+, Mg2+, or Ca2+ is an optimal ion for the enzyme activity. The enzyme activity is inhibited by NaCl with high concentrations. Tba ligase is ATP-dependent and can also use UTP as a weak cofactor; however, the enzyme with high concentrations could function without an additional nucleotide cofactor. Mass spectrometric result shows that the residue K250 of Tba ligase is AMPylated, suggesting that the enzyme is bound to AMP. The substitution of K250 of Tba ligase with Ala abolishes the enzyme activity. In addition, the mismatches at the first position 3' to the nick suppress Tba ligase activity more than those at the first position 5' to the nick. The enzyme also discriminates more effectively mismatches at 3' to the nick than those at 5' to the nick in a ligation cycling reaction, suggesting that the enzyme might have potential application in single nucleotide polymorphism.

In Search for the Membrane Regulators of Archaea.

Membrane regulators such as sterols and hopanoids play a major role in the physiological and physicochemical adaptation of the different plasmic membranes in Eukarya and Bacteria. They are key to the functionalization and the spatialization of the membrane, and therefore indispensable for the cell cycle. No archaeon has been found to be able to synthesize sterols or hopanoids to date. They also lack homologs of the genes responsible for the synthesis of these membrane regulators. Due to their divergent membrane lipid composition, the question whether archaea require membrane regulators, and if so, what is their nature, remains open. In this review, we review evidence for the existence of membrane regulators in Archaea, and propose tentative location and biological functions. It is likely that no membrane regulator is shared by all archaea, but that they may use different polyterpenes, such as carotenoids, polyprenols, quinones and apolar polyisoprenoids, in response to specific stressors or physiological needs.

The Effect of Crowding on Protein Stability, Rigidity, and High Pressure Sensitivity in Whole Cells.

In live cells, high concentrations up to 300-400 mg/mL, as in Eschericia coli (Ellis, R. J. Curr. Opin. Struct. Biol. 2001, 11, 114) are achieved which have effects on their proper functioning. However, in many experiments only individual parts of the cells as proteins or membranes are studied in order to get insight into these specific components and to avoid the high complexity of whole cells, neglecting by the way the influence of crowding. In the present study, we investigated cells of the order of Thermococcales, which are known to live under extreme conditions, in their intact form and after cell lysis to extract the effect of crowding on the molecular dynamics of the proteome and of water molecules. We found that some parameters characterizing the dynamics within the cells seem to be intrinsic to the cell type, as flexibility typical for the proteome, others are more specific to the cellular environment, as bulk water's residence time and some fractions of particles participating to the different motions, which make the lysed cells' dynamics similar to the one of another Thermococcale adapted to live under high hydrostatic pressure. In contrast to studies on the impact of crowding on pure proteins we show here that the release of crowding constraints on proteins leads to an increase in the rigidity and a decrease in the high pressure sensitivity. In a way similar to high pressure adaptation in piezophiles, the hydration water layer is decreased for the lysed cells, demonstrating a first link between protein adaptation and the impact of crowding or osmolytes on proteins.