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Comparative analysis of pyruvate kinases from the hyperthermophilic archaea Archaeoglobus fulgidus, Aeropyrum pernix, and Pyrobaculum aerophilum and the hyperthermophilic bacterium Thermotoga maritima: unusual regulatory properties in hyperthermophilic archaea.

Pyruvate kinases (PK, EC 2.7.1.40) from three hyperthermophilic archaea (Archaeoglobus fulgidus strain 7324, Aeropyrum pernix, and Pyrobaculum aerophilum) and from the hyperthermophilic bacterium Thermotoga maritima were compared with respect to their thermophilic, kinetic, and regulatory properties. PKs from the archaea are 200-kDa homotetramers composed of 50-kDa subunits. The enzymes required divalent cations, Mg2+ and Mn2+ being most effective, but were independent of K+. Temperature optima for activity were 85 degrees C (A. fulgidus) and above 98 degrees C (A. pernix and P. aerophilum). The PKs were highly thermostable up to 110 degrees C (A. pernix) and showed melting temperatures for thermal unfolding at 93 degrees C (A. fulgidus) or above 98 degrees C (A. pernix and P. aerophilum). All archaeal PKs exhibited sigmoidal saturation kinetics with phosphoenolpyruvate (PEP) and ADP indicating positive homotropic cooperative response with both substrates. Classic heterotropic allosteric regulators of PKs from eukarya and bacteria, e.g. fructose 1,6-bisphosphate or AMP, did not affect PK activity of hyperthermophilic archaea, suggesting the absence of heterotropic allosteric regulation. PK from the bacterium T. maritima is also a homotetramer of 50-kDa subunits. The enzyme was independent of K+ ions, had a temperature optimum of 80 degrees C, was highly thermostable up to 90 degrees C, and had a melting temperature above 98 degrees C. The enzyme showed cooperative response to PEP and ADP. In contrast to its archaeal counterparts, the T. maritima enzyme exhibited the classic allosteric response to the activator AMP and to the inhibitor ATP. Sequences of hyperthermophilic PKs showed significant similarity to characterized PKs from bacteria and eukarya. Phylogenetic analysis of PK sequences of all three domains indicates a distinct archaeal cluster that includes the PK from the hyperthermophilic bacterium T. maritima.

Adenosine Diphosphate↗

Molecular identification of methanogenic archaea from sheep in Queensland, Australia reveal more uncultured novel archaea.

Molecular diversity of rumen methanogens in sheep in Queensland, Australia was investigated using 16S rRNA gene libraries prepared from pooled rumen contents from nine merino sheep. A total of 78 clones were identified revealing 26 different sequences. Of these 26 sequences, eight sequences (15 clones) were 95-100% similar to cultivated methanogens belonging to the orders Methanobacteriales and Methanomicrobiales, and the remaining 18 phylotypes (63 clones) were 72-75% similar to Thermoplasma acidophilum and Thermoplasma volcanium. These unique sequences clustered within a distinct and strongly supported (100% bootstrap support) phylogenetic group, exclusively composed of sequences from uncharacterized archaea from very diverse anaerobic environments. Members of this unique group that were previously considered atypical for the rumen environment were the predominant clones.

Anaerobiosis↗

Association of marine archaea with the digestive tracts of two marine fish species.

Recent studies have shown that archaea which were always thought to live under strict anoxic or extreme environmental conditions are also present in cold, oxygenated seawater, soils, the digestive tract of a holothurian deep-sea-deposit feeder, and a marine sponge. In this study, we show, by using PCR-mediated screening in other marine eukaryotes, that marine archaea are also present in the digestive tracts of flounder and grey mullet, two fish species common in the North Sea, in fecal samples of flounder, and in suspended particulate matter of the North Sea water column. No marine archaea could be detected in the digestive tracts of mussels or the fecal pellets of a copepod species. The archaeal 16S ribosomal DNA clone libraries of feces of flounder and the contents of the digestive tracts of grey mullet and flounder were dominated by group II marine archaea. The marine archaeal clones derived from flounder and grey mullet digestive tracts and feces formed a distinct cluster within the group II marine archaea, with 76.7 to 89. 8% similarity to previously described group II clones. Fingerprinting of the archaeal community of flounder digestive tract contents and feces by terminal restriction fragment length polymorphism of archaeal 16S rRNA genes after restriction with HhaI showed a dominant fragment at 249 bp, which is likely to be derived from group II marine archaea. Clones of marine archaea that were closely related to the fish-associated marine archaea clones were obtained from suspended particulate matter of the water column at two stations in the North Sea. Terminal restriction fragment length polymorphism fingerprinting of the archaeal community present in suspended particulate matter showed the same fragment pattern as was found for the archaeal community of the flounder digestive tract contents and feces. These data demonstrate that marine archaea are present in the digestive tracts and feces of very common marine fish. It is possible that the marine archaea associated with the digestive tracts of marine fish are liberated into the water column through the feces and subsequently contribute to the marine archaeal community of suspended particulate matter.

Animals↗

Pathogenic archaea: do they exist?

Archaea are microorganisms that are distinct from bacteria and eukaryotes. They are prevalent in extreme environments, and yet found in most ecosystems. They are a natural component of the microbiota of most, if not all, humans and other animals. Despite their ubiquity and close association with humans, animals and plants, no pathogenic archaea have been identified. Because no archaeal pathogens have yet been identified, there is a general assumption that archaeal pathogens do not exist. This review examines whether this is a good assumption by investigating the potential for archaea to be or become pathogens. This is achieved by addressing: the diversity of archaea versus known pathogens, opportunities for archaea to demonstrate pathogenicity and be detected as pathogens, reports linking archaea with disease, and immune responses to archaea. In addition, molecular and genomic data are examined for the presence of systems utilised in pathogenesis. The view of this report is that, although archaea can presently be described as non-pathogenic, they have the potential to be (discovered as) pathogens. The present optimistic view that there are no archaeal pathogens is tainted by a severe lack of relevant knowledge, which may have important consequences in the future.

Animals↗

Phylogenetic analysis of Archaea in the deep-sea sediments of west Pacific Warm Pool.

Archaea are known to play important roles in carbon cycling in marine sediments. The main compositions of archaeal community in five deep-sea sediment samples collected from west Pacific Warm Pool area (WP-0, WP-1, WP-2, WP-3, WP-4), and in five sediment layers (1 cm-, 3 cm-, 6 cm-, 10 cm-, 12 cm- layer) of the 12 cm sediment core of WP-0 were checked and compared by denaturing gradient gel electrophoresis and 16 S rRNA gene sequencing. It was revealed that all the deep-sea sediment samples checked contained members of non-thermophilic marine group I crenarchaeota as the predominant archaeal group. To further detect groups of archaea possibly relating with C1 metabolism, PCR amplification was carried out using primers targeting methane-oxidizing archaea. Although no methane-oxidizing archaea was detected, a group of novel archaea (named as WPA) was instead identified from all these five WP samples by clone analysis. They could be placed in the euryarchaeota kingdom, separated into two distinct groups, the main group was peripherally related with methanogens, the other group related with Thermoplasma. The vertical distributions of WPA, archaea and bacteria along the WP-0 sediment column were determined by quantitative-PCR. It was found that bacteria dominated at all depths, the numbers of bacteria were 10-10(4) times more than those of archaea. The proportion of archaea versus bacteria had a depth related increasing tendency, it was lowest at the first layer (0.01%), reached highest at the 12 cm- layer (10%). WPA only constituted a small proportion of the archaeal community (0.05% to 5%) of west Pacific Warm Pool sediment.

Archaea↗

Archaea in coastal marine environments.

Archaea (archaebacteria) are a phenotypically diverse group of microorganisms that share a common evolutionary history. There are four general phenotypic groups of archaea: the methanogens, the extreme halophiles, the sulfate-reducing archaea, and the extreme thermophiles. In the marine environment, archaeal habitats are generally limited to shallow or deep-sea anaerobic sediments (free-living and endosymbiotic methanogens), hot springs or deep-sea hydrothermal vents (methanogens, sulfate reducers, and extreme thermophiles), and highly saline land-locked seas (halophiles). This report provides evidence for the widespread occurrence of unusual archaea in oxygenated coastal surface waters of North America. Quantitative estimates indicated that up to 2% of the total ribosomal RNA extracted from coastal bacterioplankton assemblages was archaeal. Archaeal small-subunit ribosomal RNA-encoding DNAs (rDNAs) were cloned from mixed bacterioplankton populations collected at geographically distant sampling sites. Phylogenetic and nucleotide signature analyses of these cloned rDNAs revealed the presence of two lineages of archaea, each sharing the diagnostic signatures and structural features previously established for the domain Archaea. Both of these lineages were found in bacterioplankton populations collected off the east and west coasts of North America. The abundance and distribution of these archaea in oxic coastal surface waters suggests that these microorganisms represent undescribed physiological types of archaea, which reside and compete with aerobic, mesophilic eubacteria in marine coastal environments.

Animals↗

DNA-binding proteins and evolution of transcription regulation in the archaea.

Likely DNA-binding domains in archaeal proteins were analyzed using sequence profile methods and available structural information. It is shown that all archaea encode a large number of proteins containing the helix-turn-helix (HTH) DNA-binding domains whose sequences are much more similar to bacterial HTH domains than to eukaryotic ones, such as the PAIRED, POU and homeodomains. The predominant class of HTH domains in archaea is the winged-HTH domain. The number and diversity of HTH domains in archaea is comparable to that seen in bacteria. The HTH domain in archaea combines with a variety of other domains that include replication system components, such as MCM proteins, translation system components, such as the alpha-subunit of phenyl-alanyl-tRNA synthetase, and several metabolic enzymes. The majority of the archaeal HTH-containing proteins are predicted to be gene/operon-specific transcriptional regulators. This apparent bacterial-type mode of transcription regulation is in sharp contrast to the eukaryote-like layout of the core transcription machinery in the archaea. In addition to the predicted bacterial-type transcriptional regulators, the HTH domain is conserved in archaeal and eukaryotic core transcription factors, such as TFIIB, TFIIE-alpha and MBF1. MBF1 is the only highly conserved, classical HTH domain that is vertically inherited in all archaea and eukaryotes. In contrast, while eukaryotic TFIIB and TFIIE-alpha possess forms of the HTH domain that are divergent in sequence, their archaeal counterparts contain typical HTH domains. It is shown that, besides the HTH domain, archaea encode unexpectedly large numbers of two other predicted DNA-binding domains, namely the Arc/MetJ domain and the Zn-ribbon. The core transcription regulators in archaea and eukaryotes (TFIIB/TFB, TFIIE-alpha and MBF1) and in bacteria (the sigma factors) share no similarity beyond the presence of distinct HTH domains. Thus HTH domains might have been independently recruited for a role in transcription regulation in the bacterial and archaeal/eukaryotic lineages. During subsequent evolution, the similarity between archaeal and bacterial gene/operon transcriptional regulators might have been established and maintained through multiple horizontal gene transfer events.

Archaea↗

Identification and quantification of archaea involved in primary endodontic infections.

Members of the domain Archaea, one of the three domains of life, are a highly diverse group of prokaryotes, distinct from bacteria and eukaryotes. Despite their abundance and ubiquity on earth, including their close association with humans, animals, and plants, so far no pathogenic archaea have been described. As some archaea live in close proximity to anaerobic bacteria, for instance, in the human gut system and in periodontal pockets, the aim of our study was to assess whether archaea might possibly be involved in human endodontic infections, which are commonly polymicrobial. We analyzed 20 necrotic uniradicular teeth with radiographic evidence of apical periodontitis and with no previous endodontic treatment. Using real-time quantitative PCR based on the functional gene mcrA (encoding the methyl coenzyme M reductase, specific to methanogenic archaea) and on archaeal 16S rRNA genes, we found five cases to be positive. Direct sequencing of PCR products from both genes showed that the archaeal community was dominated by a Methanobrevibacter oralis-like phylotype. The size of the archaeal population at the diseased sites ranged from 1.3 x 10(5) to 6.8 x 10(5) 16S rRNA gene target molecule numbers and accounted for up to 2.5% of the total prokaryotic community (i.e., bacteria plus archaea). Our findings show that archaea can be intimately connected with infectious diseases and thus support the hypothesis that members of the domain Archaea may have a role as human pathogens.

Archaea↗

Archaea produce peptidoglycan hydrolases that kill bacteria.

The social life of archaea is poorly understood. In particular, even though competition and conflict are common themes in microbial communities, there is scant evidence documenting antagonistic interactions between archaea and their abundant prokaryotic brethren: bacteria. Do archaea specifically target bacteria for destruction? If so, what molecular weaponry do they use? Here, we present an approach to infer antagonistic interactions between archaea and bacteria from genome sequence. We show that a large and diverse set of archaea encode peptidoglycan hydrolases, enzymes that recognize and cleave a structure-peptidoglycan-that is a ubiquitous component of bacterial cell walls but absent from archaea. We predict the bacterial targets of archaeal peptidoglycan hydrolases using a structural homology approach and demonstrate that the predicted target bacteria tend to inhabit a similar niche to the archaeal producer, indicative of ecologically relevant interactions. Using a heterologous expression system, we demonstrate that two peptidoglycan hydrolases from the halophilic archaeaon Halogranum salarium B-1 kill the halophilic bacterium Halalkalibacterium halodurans, a predicted target, and do so in a manner consistent with peptidoglycan hydrolase activity. Our results suggest that, even though the tools and rules of engagement remain largely unknown, archaeal-bacterial conflicts are likely common, and we present a roadmap for the discovery of additional antagonistic interactions between these two domains of life. Our work has implications for understanding mixed microbial communities that include archaea and suggests that archaea might represent a large untapped reservoir of novel antibacterials.

N-Acetylmuramoyl-L-alanine Amidase↗

Genetic technologies for Archaea.

Members of the third domain of life, the Archaea, possess structural, physiological, biochemical and genetic features distinct from Bacteria and Eukarya and, therefore, have drawn considerable scientific interest. Physiological, biochemical and molecular analyses have revealed many novel biological processes in these important prokaryotes. However, assessment of the function of genes in vivo through genetic analysis has lagged behind because suitable systems for the creation of mutants in most Archaea were established only in the past decade. Among the Archaea, sufficiently sophisticated genetic systems now exist for some thermophilic sulfur-metabolizing Archaea, halophilic Archaea and methanogenic Archaea. Recently, there have been developments in genetic analysis of thermophilic and methanogenic Archaea and in the use of genetics to study the physiology, metabolism and regulatory mechanisms that direct gene expression in response to changes of environmental conditions in these important microorganisms.

Archaea↗

Molecular phylogeny of Archaea from soil.

Cultivation methods have contributed to our present knowledge about the presence and diversity of microbes in naturally occurring communities. However, it is well established that only a small fraction of prokaryotes have been cultivated by standard methods and, therefore, the prokaryotes that are cultivated may not reflect the composition and diversity within those communities. Of the two prokaryotic phylogenetic domains, Bacteria and Archaea, members of the former have been shown to be ubiquitous in nature, with ample evidence of vast assemblages of uncultured organisms. There is also now increasingly compelling evidence that the Archaea, which were once thought to occupy a limited number of environments, are also globally widespread. Here we report the use of molecular phylogenetic techniques, which are independent of microbial cultivation, to conduct an assessment of Archaea in a soil microbial community. Small subunit ribosomal RNA genes of Archaea were amplified from soil and cloned. Phylogenetic and nucleotide signature analyses of these cloned small subunit ribosomal RNA gene sequences revealed a cluster of Archaea from a soil microbial community that diverge deeply from the crenarchaeotal line of descent and has the closest affiliation to the lineage of planktonic Archaea. The identification and phylogenetic classification of this archaeal lineage from soil contributes to our understanding of the ecological significance of Archaea as a component of microbial communities in non-extreme environments.

Archaea↗

Phenotypic characterization of Rice Cluster III archaea without prior isolation by applying quantitative polymerase chain reaction to an enrichment culture.

A so far uncultured member of the Euryarchaeota was enriched from an anoxic riparian soil and phenotypically characterized using quantitative polymerase chain reaction (qPCR; "real-time PCR"). The microorganism is related to the Thermoplasmatales and belongs to Rice Cluster III (RC-III). Enrichment cultures utilized yeast extract (YE) by transiently accumulating acetate as major fermentation product, which was subsequently converted to methane. The abundance of RC-III archaea within the enrichment cultures was quantified by analysis of the terminal restriction fragment length polymorphism (T-RFLP) and by qPCR. We developed qPCR assays targeting the 16S rRNA genes (16S rDNA) specific for RC-III as well as for the Archaea in general. The enrichment cultures consisted of a mixed methanogenic community of Bacteria and Archaea, the latter consisting of up to 60% of members of RC-III. The other archaea belonged to Methanosarcinaceae, Methanomicrobiaceae and Methanobacteriaceae. The enriched RC-III archaea were represented by two sequences (LL25A, LL37A) that were highly similar to each other and to those detected in the soil inoculum (>98% similarity). However, the 16S rDNA copy numbers of RC-III archaea were about 1000-fold lower than those of Bacteria. Nevertheless, we were able to estimate growth parameters and physiological properties of one of the enriched RC-III archaea (LL25A) by measuring the increase of 16S rDNA copy numbers specific for this group under different growth conditions. The enriched RC-III archaeon grew optimally at temperatures between 20 and 30 degrees C and neutral pH using YE, meat extract, peptone or tryptone under anoxic conditions. Doubling time was approximately 3 days. No proliferation was detected on carbohydrates, amino acids, fatty acids, glycerol, alcohols, aromatic compounds, purine and pyrimidine bases or pyruvate. Various exogenous electron acceptors (e.g. ferric iron, S(0)) did not support growth on YE. Proliferation of the enriched RC-III archaeon was hardly affected by the antibiotics ampicillin, kanamycin and streptomycin. These findings suggest that the enriched archaeon is a mesophilic anaerobe, which can grow heterotrophically on peptides. Further enrichment on peptone and kanamycin eventually allowed the microscopic detection of coccoid cells stained by fluorescence in situ hybridization (FISH).

Acetates↗

Comparison of simple sequence repeats in 19 Archaea.

All organisms that have been studied until now have been found to have differential distribution of simple sequence repeats (SSRs), with more SSRs in intergenic than in coding sequences. SSR distribution was investigated in Archaea genomes where complete chromosome sequences of 19 Archaea were analyzed with the program SPUTNIK to find di- to penta-nucleotide repeats. The number of repeats was determined for the complete chromosome sequences and for the coding and non-coding sequences. Different from what has been found for other groups of organisms, there is an abundance of SSRs in coding regions of the genome of some Archaea. Dinucleotide repeats were rare and CG repeats were found in only two Archaea. In general, trinucleotide repeats are the most abundant SSR motifs; however, pentanucleotide repeats are abundant in some Archaea. Some of the tetranucleotide and pentanucleotide repeat motifs are organism specific. In general, repeats are short and CG-rich repeats are present in Archaea having a CG-rich genome. Among the 19 Archaea, SSR density was not correlated with genome size or with optimum growth temperature. Pentanucleotide density had an inverse correlation with the CG content of the genome.

Archaea↗

Mechanisms of thermal adaptation revealed from the genomes of the Antarctic Archaea Methanogenium frigidum and Methanococcoides burtonii.

We generated draft genome sequences for two cold-adapted Archaea, Methanogenium frigidum and Methanococcoides burtonii, to identify genotypic characteristics that distinguish them from Archaea with a higher optimal growth temperature (OGT). Comparative genomics revealed trends in amino acid and tRNA composition, and structural features of proteins. Proteins from the cold-adapted Archaea are characterized by a higher content of noncharged polar amino acids, particularly Gln and Thr and a lower content of hydrophobic amino acids, particularly Leu. Sequence data from nine methanogen genomes (OGT 15 degrees -98 degrees C) were used to generate 1111 modeled protein structures. Analysis of the models from the cold-adapted Archaea showed a strong tendency in the solvent-accessible area for more Gln, Thr, and hydrophobic residues and fewer charged residues. A cold shock domain (CSD) protein (CspA homolog) was identified in M. frigidum, two hypothetical proteins with CSD-folds in M. burtonii, and a unique winged helix DNA-binding domain protein in M. burtonii. This suggests that these types of nucleic acid binding proteins have a critical role in cold-adapted Archaea. Structural analysis of tRNA sequences from the Archaea indicated that GC content is the major factor influencing tRNA stability in hyperthermophiles, but not in the psychrophiles, mesophiles or moderate thermophiles. Below an OGT of 60 degrees C, the GC content in tRNA was largely unchanged, indicating that any requirement for flexibility of tRNA in psychrophiles is mediated by other means. This is the first time that comparisons have been performed with genome data from Archaea spanning the growth temperature extremes from psychrophiles to hyperthermophiles.

Adaptation, Physiological↗

Phylogenomic Analyses Reveal that Panguiarchaeum Is a Clade of Genome-Reduced Asgard Archaea Within the Njordarchaeia.

The Asgard archaea are a diverse archaeal phylum important for our understanding of cellular evolution because they include the lineage that gave rise to eukaryotes. Recent phylogenomic work has focused on characterizing the diversity of Asgard archaea in an effort to identify the closest extant relatives of eukaryotes. However, resolving archaeal phylogeny is challenging, and the positions of 2 recently described lineages-Njordarchaeales and Panguiarchaeales-are uncertain, in ways that directly bear on hypotheses of early evolution. In initial phylogenetic analyses, these lineages branched either with Asgards or with the distantly related Korarchaeota, and it has been suggested that their genomes may be affected by metagenomic contamination. Resolving this debate is important because these clades include genome-reduced lineages that may help inform our understanding of the evolution of symbiosis within Asgard archaea. Here, we performed phylogenetic analyses revealing that the Njordarchaeales and Panguiarchaeales constitute the new class Njordarchaeia within Asgard archaea. We found no evidence of metagenomic contamination affecting phylogenetic analyses. Njordarchaeia exhibit hallmarks of adaptations to (hyper-)thermophilic lifestyles, including biased sequence compositions that can induce phylogenetic artifacts unless adequately modeled. Panguiarchaeum is metabolically distinct from its relatives, with reduced metabolic potential and various auxotrophies. Phylogenetic reconciliation recovers a complex common ancestor of Asgard archaea that encoded the Wood-Ljungdahl pathway. The subsequent loss of this pathway during the reductive evolution of Panguiarchaeum may have been associated with the switch to a symbiotic lifestyle, potentially based on H2-syntrophy. Thus, Panguiarchaeum may contain the first obligate symbionts within Asgard archaea besides the lineage leading to eukaryotes.

Phylogeny↗

A unique ATG triplet downstream of gene start in archaea: implications for translation initiation and evolution.

Searching for unique features of archaeal genome may shed light on the mechanism of gene regulation in primitive life forms. Statistical analysis of ATG frequency on the complete genome sequences of 16 archaea, 20 bacteria and 2 eukaryotes revealed that most of the archaeal genomes have a remarkably high ATG frequency at the position of nine nucleotide (nt) downstream of the translation initiation site (the first nucleotide of the translation initiation codon is designated as 0). To understand the role of this unique ATG in archaea, we further analyzed the ATG-initiated genes and non-ATG-initiated genes separately, and the results indicated that only the non-ATG-initiated genes contribute to the high ATG frequency at position +9. This led us to speculate that the in-frame ATG at +9 may serve as a remedial initiation site for archaea in case of initiation failure at the regular site. In addition, it seems that this phenomenon does not result from the harsh environment that archaea are usually viable according to the fact that no considerably high ATG frequency at +9 was observed in all the four thermophilic bacteria that also live in harsh environment. We proposed that the high ATG frequency at position +9 might reflect the decreased efficiency of the translation initiation machinery in archaea. Since archaea evolve very slowly, this unique characteristic of high ATG frequency at position +9 may present the primitive state of the Universal Ancestor.

Archaea↗

Marine planktonic archaea take up amino acids.

Archaea are traditionally thought of as "extremophiles," but recent studies have shown that marine planktonic Archaea make up a surprisingly large percentage of ocean midwater microbial communities, up to 60% of the total prokaryotes. However, the basic physiology and contribution of Archaea to community microbial activity remain unknown. We have studied Archaea from 200-m depths of the northwest Mediterranean Sea and the Pacific Ocean near California, measuring the archaeal activity under simulated natural conditions (8 to 17 degrees C, dark and aerobic [corrected]) by means of a method called substrate tracking autoradiography fluorescence in situ hybridization (STARFISH) that simultaneously detects specific cell types by 16S rRNA probe binding and activity by microautoradiography. In the 200-m-deep Mediterranean and Pacific samples, cells binding the archaeal probes made up about 43 and 14% of the total countable cells, respectively. Our results showed that the Archaea are active in the uptake of dissolved amino acids from natural concentrations (nanomolar) with about 60% of the individuals in the archaeal communities showing measurable uptake. Bacteria showed a similar proportion of active cells. We concluded that a portion of these Archaea is heterotrophic and also appears to coexist successfully with Bacteria in the same water.

Amino Acids↗