Mechanism of Deep-Sea Fish α-Actin Pressure Tolerance Investigated by Molecular Dynamics Simulations

The pressure tolerance of monomeric α-actin proteins from the deep-sea fish Coryphaenoides armatus and C. yaquinae was compared to that of non-deep-sea fish C. acrolepis, carp, and rabbit/human/chicken actins using molecular dynamics simulations at 0.1 and 60 MPa. The amino acid sequences of actins are highly conserved across a variety of species. The actins from C. armatus and C. yaquinae have the specific substitutions Q137K/V54A and Q137K/L67P, respectively, relative to C. acrolepis, and are pressure tolerant to depths of at least 6000 m. At high pressure, we observed significant changes in the salt bridge patterns in deep-sea fish actins, and these changes are expected to stabilize ATP binding and subdomain arrangement. Salt bridges between ATP and K137, formed in deep-sea fish actins, are expected to stabilize ATP binding even at high pressure. At high pressure, deep-sea fish actins also formed a greater total number of salt bridges than non-deep-sea fish actins owing to the formation of inter-helix/strand and inter-subdomain salt bridges. Free energy analysis suggests that deep-sea fish actins are stabilized to a greater degree by the conformational energy decrease associated with pressure effect.     

Low activity and seasonal change in population size structure of grenadiers in the oligotrophic abyssal central North Pacific Ocean

Analysis of video recordings of swimming in abyssal grenadiers Coryphaenoides spp. revealed site differences in tail-beat frequencies. At the highly oligotrophic deep central North Pacific (CNP; 5800 m depth) station fishes had significantly lower tail-beat frequencies (0·73 ± 0·02 Hz, mean ±  s . e .) than fishes of similar size at the shallower 'Station F' (Sta. F; 4400 m depth) beneath the more productive waters of the California Current Upwelling (1·06 ± 0·04 Hz). These behavioural differences may be evidence for the proposed physiological adaptations of Coryphaenoides armatus and Coryphaenoides yaquinae , to different depths and food supply levels. At CNP, smaller fishes (38·9 cm mean L _T) were present in autumn than in summer (59·4 cm L _T) suggesting large-scale migrations across the abyssal ocean floor despite the observed slow swimming speeds.     

Comparative character of the deep-water and inshore cottoid fishes endemic to Lake Baikal

Lake Baikal's 29 endemic species of cottoid fishes form three groups: shallow-water species in depths to 350 m; eurybathic species from 50 to 1300 m; and abyssal species from 400 to 1600 m. These groups differ in their abilities to withstand high hydrostatic pressure. As in marine deep-water fishes, abyssal cottoids in Baikal have few or no cones in the retina, and some have tubular eyes. Their seismosensory systems predominate, based chiefly on free neuromasts. The proportion of species with canal systems decreases with depth. Diversity of the predominantly gammarid foods also decreases from 45 species in shallow water to five species in deep water, and the lateral line system plays the dominant role in food detection at all depths. Two abyssal cottoids have become secondary pelagic, achieving close to neutral buoyancy through high lipid levels and reduced skeletal mineralization. These forms take advantage of the abundant pelagic planktonic amphipod populations. The adaptations of abyssal forms parallel those seen in deep-water marine fishes.     

Pressure-adaptive differences in lactate dehydrogenases of three hagfishes: <Emphasis Type="Italic">Eptatretus burgeri,Paramyxine atami</Emphasis> and <Emphasis Type="Italic">Eptatretus okinoseanus</Emphasis>

The tolerance of abyssal pressures likely depends on adaptive modifications of fish proteins. However, structural modifications of proteins which allow functioning at high pressure remain unclear. We compared the activities of lactate dehydrogenase (LDH), an important enzyme in glycolytic reaction, in three hagfishes inhabiting different depths under increased pressure. LDH in Eptatretus okinoseanus, found at a depth of 1,000 m, was highly active at high pressure of 100 MPa maintaining the activity at 70% of that at 0.1 MPa. In contrast, LDH activity in Paramyxine atami, found at 250–400 m, decreased to 55% at 15 MPa, and that in Eptatretus burgeri, found at 45–60 m, was completely absent at 5 MPa. The result suggests that subunit interaction of the LDH-tetramer is more stable in E. okinoseanus than that in P. atami and E. burgeri under high-pressure conditions. We found six amino acid substitutions between the three LDH primary structures. Accordingly, these amino acid residues are likely to contribute to the stability of the E. okinoseanus LDH under high-pressure conditions.     

Molecular adaptation to high pressure in cytochrome P450 1A and aryl hydrocarbon receptor systems of the deep-sea fish Coryphaenoides armatus

Limited knowledge of the molecular evolution of deep-sea fish proteomes so far suggests that a few widespread residue substitutions in cytosolic proteins binding hydrophilic ligands contribute to resistance to the effects of high hydrostatic pressure (HP). Structure-function studies with additional protein systems, including membrane bound proteins, are essential to provide a more general picture of adaptation in these extremophiles. We explored molecular features of HP adaptation in proteins binding hydrophobic ligands, either in lipid bilayers (cytochrome P450 1A - CYP1A) or in the cytosol (the aryl hydrocarbon receptor - AHR), and their partners P450 oxidoreductase (POR) and AHR nuclear translocator (ARNT), respectively. Cloning studies identified the full-length coding sequence of AHR, CYP1A and POR, and a partial sequence of ARNT from Coryphaenoides armatus, an abyssal gadiform fish thriving down to 5000 m depth. Inferred protein sequences were aligned with many non-deep-sea homologs to identify unique amino acid substitutions of possible relevance in HP adaptation. Positionally unique substitutions of various physicochemical properties were found in all four proteins, usually at sites of strong-to-absolute residue conservation. Some were in domains deemed important for protein-protein interaction or ligand binding. In addition, some involved removal or addition of beta-branched residues; local modifications of beta-branched residue patterns could be important to HP adaptation. In silico predictions further suggested that some unique substitutions might substantially modulate the flexibility of the polypeptide segment in which they are found. Repetitive motifs unique to the abyssal fish AHR were predicted to be rich in glycosylation sites, suggesting that post-translational changes could be involved in adaptation as well. Recombinant CYP1A and AHR showed functional properties (spectral characteristics, catalytic activity and ligand binding) that demonstrate proper folding at 1 atm, indicating that they could be used as deep-sea fish protein models to further evaluate protein function under pressure. This article is part of a Special Issue entitled: Cytochrome P450 biodiversity and biotechnology, edited by Erika Plettner, Gianfranco Gilardi, Luet Wong, Vlada Urlacher, Jared Goldstone".     

Molecular phylogenetic relationships of the deep-sea fish genus Coryphaenoides (Gadiformes: Macrouridae) based on mitochondrial DNA

In order to characterize the phylogenetic relationship and deep-sea adaptation process of the deep-sea fish genus Coryphaenoides, the nucleotide sequences of the mitochondrial (mt) 12 S rRNA and COI gene sequences for seven Coryphaenoides species were analyzed. Our molecular phylogenetic tree shows a new arrangement of seven Coryphaenoides species, which form two distinct groups, abyssal and nonabyssal species, and differs from the results of previous taxonomic studies. Using the mutation rate of mitochondrial genes, the divergence time between abyssal and nonabyssal Coryphaenoides was found to be 3.2-7.6 million years ago. Our study suggests that hydraulic pressure plays an important role in the speciation process in the marine environment.     

New Method for Isolating Barophiles from Intestinal Contents of Deep-Sea Fishes Retrieved from the Abyssal Zone

We devised a new method (the dorayaki method) using marine agar under in situ pressures to isolate barophilic bacteria from the intestinal contents of three deep-sea fishes (two Coryphaenoides yaquinae samples and one Ilyophis sp. sample) retrieved from depths of 4,700 to 6,100 m in the Northwest Pacific Ocean. All 10 strains isolated from one sample (C. yaquinae) were obligately barophilic. One of the 10 strains did not grow at atmospheric pressure and 103.4 MPa but did grow well between 20.7 and 82.7 MPa, with optimal growth at 41.4 MPa. This method is useful for isolating psychrophilic and barophilic deep-sea bacteria.     

Dual roles of Gln137 of actin revealed by recombinant human cardiac muscle alpha-actin mutants

The actin filament is quite dynamic in the cell. To determine the relationship between the structure and the dynamic properties of the actin filament, experiments using actin mutants are indispensable. We focused on Gln(137) to understand the relationships between two activities: the conformational changes relevant to the G- to F-actin transition and the activation of actin ATPase upon actin polymerization. To elucidate the function of Gln(137) in these activities, we characterized Gln(137) mutants of human cardiac muscle alpha-actin. Although all of the single mutants, Q137E, Q137K, Q137P, and Q137A, as well as the wild type were expressed by a baculovirus-based system, only Q137A and the wild type were purified to high homogeneity. The CD spectrum of Q137A was similar to that of the wild type, and Q137A showed the typical morphology of negatively stained Q137A F-actin images. However, Q137A had an extremely low critical concentration for polymerization. Furthermore, we found that Q137A polymerized 4-fold faster, cleaved the gamma-phosphate group of bound ATP 4-fold slower, and depolymerized 5-fold slower, as compared with the wild-type rates. These results suggest that Gln(137) plays dual roles in actin polymerization, in both the conformational transition of the actin molecule and the mechanism of ATP hydrolysis.     

Pressure effects on actin self-assembly: interspecific differences in the equilibrium and kinetics of the G to F transformation

Purified skeletal muscle actins from species whose ambient pressures range from 1 to greater than 500 atm were examined for the sensitivity to hydrostatic pressure of the globular (G) to filamentous (F) self-assembly reaction. Both the equilibrium position and the kinetics of self-assembly were affected by pressure. Increased pressure shifted the self-assembly equilibrium toward the monomer (G) state and reduced the rate of F-actin assembly. For most of the actins studied, the perturbation by pressure of F-actin formation decreased with increasing measurement of pressure, indicating that F-actin has a higher compressibility than G-actin. The increase in system volume and compressibility concomitant with the assembly of F-actin can be interpreted as reflections of the major role played by hydrophobic effects in stabilizing F-actin and of the existence of "hard" binding sites, in the terminology of Torgerson et al. [Torgerson, P. M., Drickamer, H. G., & Weber, G. (1979) Biochemistry 18, 3079-3083], in the actin subunits. For actin from the deepest occurring species studied, the teleost fish Coryphaenoides armatus, which occurs to depths of approximately 5000 m (equivalent to 501 atm of pressure), there was no difference in compressibility between G-actin and F-actin; that is, the effect of increasing pressure on self-assembly was linear over the entire pressure range examined, 600 atm. The self-assembly reaction of the actin from C. armatus also differed from that of the other actins examined in that the G to F equilibrium was relatively insensitive to increased pressure; i.e., the volume change (delta V) of assembly was small.(ABSTRACT TRUNCATED AT 250 WORDS)     

Pressure inactivation of tetrameric lactate dehydrogenase homologues of confamilial deep-living fishes

Summary The susceptibility to inactivation by hydrostatic pressure of the tetrameric (Fig. 1) muscletype (M₄) lactate dehydrogenase homologues (LDH, EC 1.1.1.27;l-lactate: NAD⁺ oxidoreductase) from six confamilial macrourid fishes was compared at 4 °C. These marine teleost fishes occur over depths of 260 to 4815 m. The pressures necessary to half-inactivate the LDH homologues are related to the pressures which the enzymes are exposed to in vivo (Table 1); higher hydrostatic pressures are required to inactivate the LDH homologues of the deeper-occurring macrourids. The resistance of the LDH homologues to inactivation by pressure is affected by protein concentration (Fig. 3). After an hour of incubation at pressure, the percent remaining activity approaches an asymptotic value (Fig. 2). The inactivation of the macrourid LDH homologues by pressure was not fully reversible. Assuming that inactivation by pressure was due to dissociation of the native tetramer to monomers, apparent equilibrium constants (K _eq) were calculated. Volume changes (V) were calculated over the range of pressures for which plots inK _eq versus pressure were linear (Fig. 4). The V of dissociation values of the macrourid homologues range from –219 to –439 ml mol^–1 (Table 1). Although the hydrostatic pressures required to inactivate the LDH homologues of the macrourid fishes are greater than those which the enzymes are exposed to in vivo, the pressure-stability of these enzymes may reflect the resistance of these enzymes to pressure-enhanced proteolysis in vivo.     

Explaining bathymetric diversity patterns in marine benthic invertebrates and demersal fishes: physiological contributions to adaptation of life at depth

Bathymetric biodiversity patterns of marine benthic invertebrates and demersal fishes have been identified in the extant fauna of the deep continental margins. Depth zonation is widespread and evident through a transition between shelf and slope fauna from the shelf break to 1000 m, and a transition between slope and abyssal fauna from 2000 to 3000 m; these transitions are characterised by high species turnover. A unimodal pattern of diversity with depth peaks between 1000 and 3000 m, despite the relatively low area represented by these depths. Zonation is thought to result from the colonisation of the deep sea by shallow‐water organisms following multiple mass extinction events throughout the Phanerozoic. The effects of low temperature and high pressure act across hierarchical levels of biological organisation and appear sufficient to limit the distributions of such shallow‐water species. Hydrostatic pressures of bathyal depths have consistently been identified experimentally as the maximum tolerated by shallow‐water and upper bathyal benthic invertebrates at in situ temperatures, and adaptation appears required for passage to deeper water in both benthic invertebrates and demersal fishes. Together, this suggests that a hyperbaric and thermal physiological bottleneck at bathyal depths contributes to bathymetric zonation. The peak of the unimodal diversity–depth pattern typically occurs at these depths even though the area represented by these depths is relatively low. Although it is recognised that, over long evolutionary time scales, shallow‐water diversity patterns are driven by speciation, little consideration has been given to the potential implications for species distribution patterns with depth. Molecular and morphological evidence indicates that cool bathyal waters are the primary site of adaptive radiation in the deep sea, and we hypothesise that bathymetric variation in speciation rates could drive the unimodal diversity–depth pattern over time. Thermal effects on metabolic‐rate‐dependent mutation and on generation times have been proposed to drive differences in speciation rates, which result in modern latitudinal biodiversity patterns over time. Clearly, this thermal mechanism alone cannot explain bathymetric patterns since temperature generally decreases with depth. We hypothesise that demonstrated physiological effects of high hydrostatic pressure and low temperature at bathyal depths, acting on shallow‐water taxa invading the deep sea, may invoke a stress–evolution mechanism by increasing mutagenic activity in germ cells, by inactivating canalisation during embryonic or larval development, by releasing hidden variation or mutagenic activity, or by activating or releasing transposable elements in larvae or adults. In this scenario, increased variation at a physiological bottleneck at bathyal depths results in elevated speciation rate. Adaptation that increases tolerance to high hydrostatic pressure and low temperature allows colonisation of abyssal depths and reduces the stress–evolution response, consequently returning speciation of deeper taxa to the background rate. Over time this mechanism could contribute to the unimodal diversity–depth pattern.     

Motility of myosin V regulated by the dissociation of single calmodulin

Myosin V is a calmodulin-binding motor protein. The dissociation of single calmodulin molecules from individual myosin V molecules at 1 microM Ca(2+) correlates with a reduction in sliding velocity in an in vitro motility assay. The dissociation of two calmodulin molecules at 5 microM Ca(2+) correlates with a detachment of actin filaments from myosin V. To mimic the regulation of myosin V motility by Ca(2+) in a cell, caged Ca(2+) coupled with a UV flash system was used to produce Ca(2+) transients. During the Ca(2+) transient, myosin V goes through the functional cycle of reduced sliding velocity, actin detachment and reattachment followed by the recovery of the sliding velocity. These results indicate that myosin V motility is regulated by Ca(2+) through a reduction in actin-binding affinity resulting from the dissociation of single calmodulin molecules.     

A seasonal analysis of the nutritional condition of deep-sea macrourid fishes in the north-east Pacific

Of three common macrourids Coryphaenoides armatus and Coryphaenoides yaquinae were collected from 1995 to 1998 at an abyssal station, c . 220 km west of Point Conception, California in the north-east Pacific (4100 m depth). Coryphaenoides acrolepis was collected from 1997 to 1998 in the San Diego Trough (1200 m depth). Energy storage in all three species was primarily in the liver, which was up to 56% lipid (wet mass) and up to 96% triglyceride. No seasonal variation in nutritional condition was found for C. armatus or C. yaquinae . There was, however, a significant increase in muscle water content and liver lipid content and a significant decline in muscle lactate dehydrogenase activity for C. armatus between 1996 and 1998. Potential mechanisms for these interannual shifts are proposed. No seasonal variation in parameters was found for C. acrolepis but a small seasonal periodicity in feeding activity may have existed. The seasonal deposition of phytodetritus in the deep sea is of little or no consequence to these fishes.     

Deep-sea scavenging demersal fish fauna of the Nazaré Canyon system, Iberian coast, north-east Atlantic Ocean

A baited imaging lander was deployed six times in the Nazaré Canyon at depths from 909 to 4361 m during August 2005 to investigate the demersal scavenging fishes. Species observed and lander-derived abundance estimates were similar to previous data from the Porcupine Seabight and abyssal plain, north-east Atlantic Ocean.     

Dissociation of F-actin induced by hydrostatic pressure.

F-actin purified from rabbit skeletal muscle undergoes reversible dissociation when subjected to hydrostatic pressures up to 240 MPa. Dissociation and reversibility were detected by the following procedures: fluorescence spectral changes observed under pressure, when either intrinsic tryptophan or pyrenyl emission of N-(1-pyrenyl)iodoacetamide-labeled actin were monitored; electron microscopy of samples fixed under pressure; size-exclusion HPLC of pressurized actin. The effect of pressure upon F-actin that had been polymerized in the presence of either Mg2+, Ca2+ or K+ was studied. The standard volume changes for the association of actin subunits, calculated from pressure/dissociation curves were 74 +/- 14 ml/mol for Mg-F-actin, 79 +/- 12 ml/mol for Ca-F-actin and 328 +/- 63 ml/mol for K-F-actin, indicating that actin subunits are packed differently in the polymer depending on which cation is present. All pressure/dissociation data could be fitted by a model for dissociation of a dimer, which suggests that in the F-actin filament there is a predominant intersubunit interaction interface, most likely the head-to-tail intrastrand interaction between two subunits which repeats itself along the polymer. A tenfold change in total protein concentration from 20 micrograms to 200 micrograms/ml Mg-F-actin did not cause a change in the pressure required for half-maximal dissociation. This indicates a heterogeneity of free energy of association among actin monomers in the Mg-F-actin polymer, suggesting that, in addition to the predominant intersubunit interaction, the disordered interactions in the filament significantly contribute to the heterogeneity of microenvironments in the interface between the subunits.     

Motor function and regulation of myosin X.

Myosin X is a member of the diverse myosin superfamily that is ubiquitously expressed in various mammalian tissues. Although its association with actin in cells has been shown, little is known about its biochemical and mechanoenzymatic function at the molecular level. We expressed bovine myosin X containing the entire head, neck, and coiled-coil domain and purified bovine myosin X in Sf9 cells. The Mg(2+)-ATPase activity of myosin X was significantly activated by actin with low K(ATP). The actin-activated ATPase activity was reduced at Ca(2+) concentrations above pCa 5 in which 1 mol of calmodulin light chain dissociates from the heavy chain. Myosin X translocates F-actin filaments with the velocity of 0.3 microm/s with the direction toward the barbed end. The actin translocating activity was inhibited at concentrations of Ca(2+) at pCa 6 in which no calmodulin dissociation takes place, suggesting that the calmodulin dissociation is not required for the inhibition of the motility. Unlike class V myosin, which shows a high affinity for F-actin in the presence of ATP, the K(actin) of the myosin X ATPase was much higher than that of myosin V. Consistently nearly all actin dissociated from myosin X in the presence of ATP. ADP did not significantly inhibit the actin-activated ATPase activity of myosin X, suggesting that the ADP release step is not rate-limiting. These results suggest that myosin X is a nonprocessive motor. Consistently myosin X failed to support the actin translocation at low density in an in vitro motility assay where myosin V, a processive motor, supports the actin filament movement.     

Exploring the Stability Limits of Actin and Its Suprastructures

Actin is the main component of the microfilament system in eukaryotic cells and can be found in distinct morphological states. Global (G)-actin is able to assemble into highly organized, supramolecular cellular structures known as filamentous (F)-actin and bundled (B)-actin. To evaluate the structure and stability of G-, F-, and B-actin over a wide range of temperatures and pressures, we used Fourier transform infrared spectroscopy in combination with differential scanning and pressure perturbation calorimetry, small-angle x-ray scattering, laser confocal scanning microscopy, and transmission electron microscopy. Our analysis was designed to provide new (to our knowledge) insights into the stabilizing forces of actin self-assembly and to reveal the stability of the actin polymorphs, including in conditions encountered in extreme environments. In addition, we sought to explain the limited pressure stability of actin self-assembly observed in vivo. G-actin is not only the least temperature-stable but also the least pressure-stable actin species. Under abyssal conditions, where temperatures as low as 1–4°C and pressures up to 1 kbar are reached, G-actin is hardly stable. However, the supramolecular assemblies of actin are stable enough to withstand the extreme conditions usually encountered on Earth. Beyond ∼3–4 kbar, filamentous structures disassemble, and beyond ∼4 kbar, complete dissociation of F-actin structures is observed. Between ∼1 and 2 kbar, some disordering of actin assemblies commences, in agreement with in vivo observations. The limited pressure stability of the monomeric building block seems to be responsible for the suppression of actin assembly in the kbar pressure range.     

Interrelationships of the subgenera of Coryphaenoides (Teleostei: Gadiformes: Macrouridae): synthesis of allozyme,peptide mapping,and DNA sequence data

DNA sequences of the 12s rRNA mitochondrial gene from 12 species key to the question of the monophyly of the deep-sea fish genus Coryphaenoides (Macrouridae) were analyzed phylogenetically using maximum parsimony and maximum likelihood. The results were compared with those of three previous studies in which allozyme, peptide mapping, and DNA sequence data were similarly analyzed. The allozyme and DNA sequence data suggested that the largest subgenus (Coryphaenoides), which contained most of the species inhabiting continental slopes between approximately 600 and 2000m depth, is monophyletic. Two of the three subgenera containing the species inhabiting abyssal ocean basins below approximately 2000m together formed a sister group to subgenus Coryphaenoides. The macrourids of the abyssal basins and those of the continental slopes thus appear to have experienced separate radiations from a common ancestor.     

Trimethylamine oxide, betaine and other osmolytes in deep-sea animals: depth trends and effects on enzymes under hydrostatic pressure.

Most shallow teleosts have low organic osmolyte contents, e.g. 70 mmol/kg or less of trimethylamine oxide (TMAO). Our previous work showed that TMAO contents increase with depth in muscles of several Pacific families of teleost fishes, to about 180 mmol/kg wet wt at 2.9 km depth in grenadiers. We now report that abyssal grenadiers (Coryphaenoides armatus, Macrouridae) from the Atlantic at 4.8 km depth contain 261 mmol/kg wet wt in muscle tissue. This precisely fits a linear trend extrapolated from the earlier data. We also found that anemones show a trend of increasing contents of methylamines (TMAO, betaine) and scyllo-inositol with increasing depth. Previously we found that TMAO counteracts the inhibitory effects of hydrostatic pressure on a variety of proteins. We now report that TMAO and, to a lesser extent, betaine, are generally better stabilizers than other common osmolytes (myo-inositol, taurine and glycine), in terms of counteracting the effects of pressure on NADH Km of grenadier lactate dehydrogenase and ADP Km of anemone and rabbit pyruvate kinase.     

Population Sizes and Growth Pressure Responses of Intestinal Microfloras of Deep-Sea Fish Retrieved from the Abyssal Zone

The intestinal floras of seven deep-sea fish retrieved at depths of from 3,200 to 5,900 m were examined for population sizes and growth responses to pressure. Large populations of culturable bacteria, ranging from 1.1 x 10(sup6) to 3.6 x 10(sup8) cells per ml of contents, were detected when samples were incubated at conditions characteristic of those of the deep sea. Culturable cell counts at in situ pressures were greater than those at atmospheric pressure in all samples. Most of the strains isolated by the spread-plating method at atmospheric pressure later proved barophilic. Barophilic bacteria were the predominant inhabitants of the abyssal fish intestines.