Skip to main content
Advertisement
Browse Subject Areas
?

Click through the PLOS taxonomy to find articles in your field.

For more information about PLOS Subject Areas, click here.

  • Loading metrics

Variations of the metabolome in the digestive system of Antarctic krill, Euphausia superba, between summer and autumn

  • Simone Heyen ,

    Roles Conceptualization, Data curation, Formal analysis, Investigation, Methodology, Validation, Visualization, Writing – original draft, Writing – review & editing

    simone.heyen@uol.de

    Affiliation Institute for Chemistry and Biology of the Marine Environment (ICBM), Carl von Ossietzky University of Oldenburg, Oldenburg, Germany

  • Verena Töpker,

    Roles Investigation, Methodology, Writing – review & editing

    Affiliation Institute for Chemistry and Biology of the Marine Environment (ICBM), Carl von Ossietzky University of Oldenburg, Oldenburg, Germany

  • Bernd Kopke,

    Roles Formal analysis, Methodology, Writing – review & editing

    Affiliation Institute for Chemistry and Biology of the Marine Environment (ICBM), Carl von Ossietzky University of Oldenburg, Oldenburg, Germany

  • Nevenka Cakić,

    Roles Investigation, Writing – review & editing

    Affiliation Institute for Chemistry and Biology of the Marine Environment (ICBM), Carl von Ossietzky University of Oldenburg, Oldenburg, Germany

  • Lukas Hüppe,

    Roles Investigation, Writing – review & editing

    Affiliations Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany, Julius-Maximilians-University of Würzburg, Würzburg, Germany

  • Bettina Meyer,

    Roles Conceptualization, Funding acquisition, Investigation, Supervision, Writing – review & editing

    Affiliations Institute for Chemistry and Biology of the Marine Environment (ICBM), Carl von Ossietzky University of Oldenburg, Oldenburg, Germany, Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany, Helmholtz Institute for Marine Functional Biodiversity (HIFMB), Carl von Ossietzky University of Oldenburg, Oldenburg, Germany

  • Heinz Wilkes

    Roles Conceptualization, Funding acquisition, Investigation, Resources, Supervision, Writing – review & editing

    Affiliation Institute for Chemistry and Biology of the Marine Environment (ICBM), Carl von Ossietzky University of Oldenburg, Oldenburg, Germany

Abstract

Rapid climate change threatens the relatively pristine environment of the Southern Ocean. The effects on biogeochemical cycles and their subsequent consequences for the organisms in this area are of significant interest. Antarctic krill, Euphausia superba, is the dominant species in the Antarctic ecosystem and a vital component of the Southern Ocean food web. Its metabolism is influenced by the feeding regime, which is governed by environmental conditions. However, little is yet known about the metabolome of Antarctic krill. Here, we investigated metabolite classes that can serve as tracers for documenting variations in the metabolic and biochemical status of krill. To this end, we utilised targeted metabolomics to analyse coenzyme A thioesters, amino acids, B vitamins, and respiratory quinones in the digestive system of Antarctic krill, sampled during two campaigns in the Antarctic summer and autumn. A significant proportion of the detected coenzyme A thioesters were associated with the β-oxidation of fatty acids and, consequently, with lipid metabolism. Propionyl-CoA was particularly abundant in samples from the digestive gland, while malonyl- and succinyl-CoA were more prevalent in stomach and hindgut samples. 3-Hydroxy-3-methylglutaryl-CoA, an intermediate in the metabolism of branched amino acids and the biosynthesis of isoprenoids, occurred almost exclusively in the summer samples. Analyzing the free amino acids, very high levels of the non-proteinogenic amino acid sarcosine were found, which possibly serves as an osmolyte for the Antarctic krill and/or plays a role in its digestive process. Among the B vitamins, there were seasonal fluctuations, particularly in B1 and B5. The respiratory quinones exhibited more homogeneous patterns, with UQ10:10 as the dominant representative. These seasonal and organ-dependent variations in the composition of the different metabolite classes can serve as a reference point in future studies to better assess the influence of changing conditions in Antarctic waters.

Introduction

Antarctic krill (Euphausia superba, hereafter referred to as krill) is a small, shrimp-like crustacean that plays a crucial role in the ecosystem of the Southern Ocean, serving as an essential part of the diet for many marine animals and occupying an important role in the biogeochemical cycles of Antarctic waters [1]. Krill is a highly abundant species in the Southern Ocean, with an enormous biomass of approximately 379 million tonnes [2]. Its nutritional value, derived from characteristics such as a high content of essential omega-3 fatty acids, makes it appealing for medical applications and highlights its importance as a subject of study [3,4].

Krill are filter feeders, consuming food particles that are filtered through the feeding basket formed by their thoracopods [5]. After being initially crushed in the mouthparts, food items are further ground in the gastric mill of the stomach, filtered, and passed into the digestive gland [6,7]. Enzymes break down the filtered chyme in the digestive gland before the remains are compacted into fecal pellets and excreted through the hindgut. The initial breakdown of complex materials in the stomach, such as chitinous food, is indicated by elevated endochitinase activity, with subsequent degradation to amino sugars occurring in the digestive gland [8]. It has also been shown that the activity of digestive enzymes is generally higher in the stomach than in the digestive gland [810].

Due to changes in food availability, the efficiency of food absorption can vary greatly between seasons. This is reflected in changes in egestion rates, densities, and C:N ratios in fecal pellets [11]. Conversely, the composition of metabolic products in the digestive system will likely also depend on the food ingested by krill across seasons. These seasonal variations have already been documented in the compositions of lipids and fatty acids, suggesting that seasonal patterns may also occur in other metabolite classes [1215].

Metabolites play vital roles in biological processes, including energy production, growth, reproduction, and responses to environmental stimuli. Consequently, the metabolome of krill can reflect the diverse biochemical processes occurring within these organisms. It can vary based on several factors, such as diet, environmental conditions, and life stage.

As ongoing climate change affects the habitat and food availability of krill, understanding their metabolome is of great value in studying their biology and ecological roles [16,17]. While considerable research has been conducted on krill’s lipid and fatty acid composition, limited data exist on other classes of metabolites [13,15,18,19]. The first untargeted metabolomic study was conducted by Zhang et al., which focused on contaminants found in krill tissues [20]. Thus, there remains significant potential to expand knowledge of the krill’s metabolome, which prompted us to analyse key metabolite classes that may exhibit seasonal patterns due to changes in food supply. These included coenzyme A thioesters (acyl-CoAs), amino acids, B vitamins, and respiratory quinones.

Acyl-CoAs are essential intermediates involved in numerous metabolic pathways within cells. They function as carriers of acyl groups in metabolic reactions, playing a vital role in energy metabolism, lipid metabolism, and the synthesis and degradation of various cellular constituents. Amino acids are crucial for protein synthesis and play a role in metabolism, immune response, and other physiological processes. They serve as precursors for synthesising various bioactive compounds and are involved in signalling pathways and enzymatic reactions. The organism cannot synthesize essential amino acids, which must be obtained from the diet, while non-essential amino acids can be synthesized within the body. B vitamins are necessary for energy metabolism, the nervous system’s function, and DNA synthesis, among other functions. Respiratory quinones shuttle electrons between different respiratory chain complexes and thus play a role in ATP synthesis. While there are no comprehensive studies on the composition of acyl-CoAs, B vitamins, and respiratory quinones in krill, studies on the amino acid content and composition have mainly focused on their nutritional value [2123].

Materials and methods

Krill samples

Krill were sampled during two expeditions (03.05.-17.06.2021 and 02.01.-26.03.2022) aboard the commercial krill fishing vessel (FV) Antarctic Endurance of the company Aker BioMarine. This beam trawler is equipped with a continuous fishing system that uses a vacuum system to pump krill from the cod end of two nets on board. The first collection took place on the 13th, 15th and 31st of May (autumn) of 2021 in the Bransfield Strait, while the second occurred on the 19th of January and 8th of March (summer) of 2022 at the South Orkney Islands. Upon capture, the stomach, digestive gland, and hindgut of krill individuals were immediately dissected on board under a stereomicroscope, frozen, and stored at −80°C for later analysis. Individual krill specimens were utilized for the assessment of amino acids. At the same time, body parts collected and pooled from three animals were used for the analysis of acyl-CoAs, B vitamins, and respiratory quinones. Five to twelve replicates were used for each sampling time point and organ.

Extraction

Bead beating.

To avoid autolytic processes and thus alterations of the metabolite composition, sample transportation and extraction was performed under dark conditions using minimal artificial light as well as storage on dry ice when samples were not actively treated [24]. Bead-beating was used for the extraction of all samples. The respective internal standards as listed in Table 1 were added prior to the individual extraction procedures.

thumbnail
Table 1. Internal standards used for individual metabolite classes.

https://doi.org/10.1371/journal.pone.0327747.t001

For samples intended for analysis of respiratory quinones, a mixture of methanol (MeOH) and hexane (2:1) was used, while all other samples were extracted with MeOH. Tissue samples were transferred into cryotubes filled with 0.5 g of 0.1-mm glass beads and 0.7 g of 0.7-mm zirconia beads. Bead-beating was performed with 1 mL of solvent in three cycles of 30 seconds with intervening cooling phases on dry ice of 90 seconds. After centrifugation and removal of the solvent, two additional rounds of extraction were done by re-adding 0.5 mL solvent, vortexing, and centrifuging the sample again. The entire procedure was repeated twice, resulting in a total extract volume of 6 mL. Depending on the targeted metabolite class, the subsequent extraction process was adjusted accordingly.

Coenzyme A thioesters and B vitamins.

For acyl-CoAs and B vitamins, bead-beater MeOH extracts were evaporated to dryness under a nitrogen stream, resuspended in ultrapure water, and filtered using centrifuge filters. The filtrates were stored at −80°C.

Amino acids.

Hydrolysis of protein-bound and derivatization of protein-bound as well as free amino acids was conducted according to Vane et al. and Walsh et al. [26,27]. For this procedure, bead-beater MeOH extracts were evaporated to dryness and resuspended in 1 mL MeOH. 100 µL each for the hydrolysis as well as the direct derivatization were placed in conical vials with a capacity of 500 µL and evaporated. In case of the hydrolysis of protein-bound amino acids, the samples were resuspended in 200 µL of 6 M hydrochloric acid (HCl). To prevent oxidation, 40 µL of ascorbic acid were added before flushing the vials with nitrogen and placing them in the oven at 110°C for 20 h. After cooling, the samples were evaporated to dryness. The following derivatization procedure for these samples as well as for those not hydrolysed was similar. The samples were resuspended in 200 µL of 0.1 M HCl before 70 µL of MeOH, 60 µL of pyridine and 30 µL of methyl chloroformate were added. Subsequently, 200 µL of chloroform were added to each sample, the sample was mixed and the lower layer containing methoxycarbonyl (MOC) esters was dried over sodium sulphate after waiting for phase separation.

Respiratory quinones.

Respiratory quinones were extracted based on the method described by Tindall [28]. Bead-beater extracts were stirred for 30 minutes at room temperature in the dark. Ice-cold hexane was added to change the ratio of MeOH and hexane to 1:1 (v:v) and the sample was vortexed. After incubating on ice for 15 minutes, the samples were centrifuged, and the hexane phase was transferred to a glass vial. 2 mL of hexane and 2 mL of aqueous 0.3% sodium chloride were added to the samples and mixed. Succeeding another round of centrifugation, the hexane phases were pooled and evaporated under a stream of nitrogen. The samples were resuspended in hexane:MeOH (1:10 v:v), filtered, and stored at −80°C until measurement.

Instrumental analyses

Gas chromatography-mass spectrometry.

Gas chromatographic-mass spectrometric analysis of the derivatized amino acids was executed based on the method described in Heyen et al. on a Trace GC Ultra gas chromatograph coupled to a TriPlus autosampler and an ISQ QD mass spectrometer (all from Thermo Scientific, Dreieich, Germany) with an optimized temperature gradient [29]. The temperature program started at a temperature of 60°C, which was held for 1 min and then increased first at a rate of 3 K/min to 250°C and then at a rate of 10 K/min to 320°C, which was held for further 15 min.

Liquid chromatography – mass spectrometry.

B vitamins were measured on an Ultimate 3000 HPLC coupled to a TSQ Quantum UltraAM mass spectrometer (both Thermo Fisher Scientific, Dreieich, Germany). Separation was achieved on a Kinetex Evo C18 column (150 x 2 mm, 2.6 µm, Phenomenex, Torrance, CA, USA). Settings for the chromatography and the mass spectrometric method operated in selected reaction monitoring mode were adopted from Bruns et al. [30].

Acyl-CoAs and respiratory quinones were analysed using a Vanquish Flex UHPLC connected to an Orbitrap Fusion mass spectrometer (both Thermo Fisher Scientific, Dreieich, Germany). Acyl-CoAs were measured and identified as described in Cakić et al. on a Gemini C18 column (150 × 2.0 mm, 3 μm pore size, Phenomenex, Torrance, CA, USA) [25]. Reference standards were either purchased from a supplier or synthesized as described in Cakić et al. [25].

For the separation of respiratory quinones, the same column was used as for the B vitamins, with a chromatographic method based on Zhu et al. [31]. The eluents consisted of MeOH:H2O (85:15 v:v) (eluent A) and isopropanol (eluent B), both with a 10 mM ammonium acetate puffer at pH 8.1. Gradient started at 100% A for 2.5 min, which was increased to 15% B by 2.64 min. After increasing to 85% B in 22.49 min and to 100% B in 1.38 min, which was held for 6.25 min, the gradient went back to 100% A in 2.25 min, where it was held for 7.6 min. The total runtime was 42.6 min at a flow rate of 0.3 mL/min. For mass spectrometric analysis, initial measurements were conducted to assess the qualitative composition of respiratory quinones in krill samples based on characteristic fragmentation patterns as described by Elling et al. [32]. Samples with up to 15 pooled organs were used to assemble a targeted method in order to enhance the sensitivity of the measurements. These targeted MS2 measurements were run in parallel to full scan experiments for all samples. Instrument settings for both modes are summarized in S1 and S2 Tables in the supporting information.

Data analysis

Peaks were integrated using the Xcalibur Quan Browser or TraceFinder (for acyl-CoAs), version 4.1.31.4 (Thermo Scientific, Dreieich, Germany). For acyl-CoAs and respiratory quinones, the internal standard was used to obtain semi-quantitative data, as no authentic standards were available, so that response and linearity differences within the targeted compound class were not taken into account. For the B vitamins and amino acids, a corresponding authentic standard was used for the calibration for each analyte. Amino acids were calibrated using 15 standards with concentrations between 0.01 and 30 µg/mL with and without hydrolysis. Since the tyrosine standard precipitated during determination of calibration curves due to poor solubility, the inclusion of this amino acid would have led to an overestimation of the content and it was therefore excluded. Methionine and cysteine were destroyed during hydrolysis and are excluded from the evaluation of the composition of the protein-bound fraction. Asparagine and any glutamine present were transformed to their corresponding acids during hydrolysis. Concentrations of ornithine, tryptophan, and lysine were below the quantification limit and excluded from further analysis.

For B vitamins, individual calibration ranges were selected based on the expected concentrations in the samples. These ranges as well as the number of levels are listed in S3 Table. Calibrations for both B vitamins and amino acids were generated in quadruplicate, with outliers eliminated applying the Grubbs test at a significance threshold of 0.05. For each area ratio of a B vitamin or amino acid to the internal standard in a sample, five calibration levels were selected to calculate the concentration. Process blanks were subtracted from all samples. B3 was detected in some samples, but due to high matrix loading, especially in the summer samples, peaks were difficult to integrate correctly. To avoid over- or underestimation of the content, B3 was removed from the evaluation.

Since it was not possible to weigh the samples without causing significant changes in the composition emerging from autolytic processes and considering that the weights of body parts are likely to vary by month, sex, and krill size, the evaluations were conducted solely based on the percentage distributions of the analytes in each sample. Although the samples were segregated based on sex, no discernible patterns were observed, so this variable was not considered in the subsequent analysis.

Statistical analyses were performed using the non-parametric Kruskal-Wallis and Dunn’s tests. Calculations and principal component analyses (PCA) for every class of metabolite were performed in R version 4.2.2, with the package ggbiplot used for visualisation [33,34]. PCA was used to identify trends and patterns in the data sets in addition to bar graphs, as the distribution of the data in the PCA plots is driven by metabolites with dominant influences on the sample. The percetanges given on each axis represent the proportion of variance explainable by the component. Results of the statistical tests as well as PCA plots can be found in the supporting information.

Results and discussion

Coenzyme A thioesters

To our knowledge, acyl-CoAs have not been studied in krill or other crustacean species. Therefore, this is the first time such a dataset can be presented. We detected 97 acyl-CoAs, ranging from acetyl-CoA to the CoA ester of a C12 acid that contains an additional oxygen atom. Thirty-one of these acyl-CoAs were identified by comparison with reference standards that were either commercially available or synthesised in-house. The remaining acyl-CoAs were characterised according to their sum formulas derived from high-resolution mass spectrometry. A list of all peaks, their respective sum formulas, and acyl-rests is provided in S4 Table. Their relative distribution is displayed in S1 Fig The distribution of 21 acyl-CoAs, which had a relative abundance of more than 1% among all 97 detected acyl-CoAs in at least one organ, is shown in Fig 1.

thumbnail
Fig 1. Relative distribution of coenzyme A thioesters with an abundance above 1% between organs and seasons.

a. Including acetyl-CoA and b. excluding acetyl-CoA. Acyl-CoAs without confirmation of the structure by comparison with a reference standard are numbered as U1- to U6-CoA, with their sum formulas in parentheses.

https://doi.org/10.1371/journal.pone.0327747.g001

In all samples, acetyl-CoA constituted over 40% of the total acyl-CoA content (Fig 1a). Given that acetyl-CoA is a vital intermediate in numerous metabolic pathways, essential for both energy conservation and the biosynthesis of cellular constituents, this was to be expected. However, the proportion of acetyl-CoA increases from the digestive gland via the stomach to the hind gut. To better illustrate the compositional variability of the other acyl-CoAs, Fig 1b presents their distribution, excluding acetyl-CoA.

The most diverse pattern was observed in samples taken from the digestive glands, as reflected in the principal component analysis presented in S2 Fig of the supporting information. Variations in these samples were caused by entirely different CoAs, therefore plotting at opposite directions in the PCA plot, whereas trends in all other organs could be explained by a similar set of CoAs. As digestive glands had the highest biomass, acyl-CoAs below the detection limit in stomach and hindgut samples could still be detected here. Interestingly, the second most abundant acyl-CoA in the digestive glands was propionyl-CoA. In contrast, succinyl-CoA was the second most abundant acyl-CoA in the stomachs and hindguts during both seasons, often followed by malonyl-CoA. While the latter two, like acetyl-CoA, are involved in numerous metabolic pathways, propionyl-CoA hints at the biosynthesis or degradation of odd-chain fatty acids or branched-chain amino acids [35,36]. Possible explanations for this phenomenon may include the activity of different metabolic pathways, variation of the microbiome across the three sections of the digestive system, or the prevalence of the krill-derived signal in the digestive gland due to the greater quantity of krill tissue compared to bacteria or food particles.

The composition of acyl-CoAs also varied between summer and autumn. For instance, 3-hydroxy-3-methylglutaryl-CoA was nearly absent in autumn samples, whereas it was found in significant amounts in all three organs in the summer samples. In contrast, U6-CoA, possibly nonenoyl-CoA, was relatively abundant in the digestive gland samples collected in autumn. Statistical analysis using the Kruskal-Wallis and Dunn’s tests indicated that pentanoyl-CoA was significantly more prevalent in autumn samples, while isopentanoyl-CoA was dominant in summer (data presented in S5 Table of the supporting information).

3-Hydroxy-3-methylglutaryl-CoA plays a role in various metabolic processes. It serves as an intermediate in the metabolism of the branched amino acids leucine, isoleucine and valine. Additionally, it is a crucial intermediate in isoprenoid biosynthesis, where it is converted to mevalonic acid by 3-hydroxy-3-methylglutaryl coenzyme A reductase. Crustaceans require this metabolic pathway, among others, to produce the juvenile hormone methyl farnesoate, which is involved in their reproductive processes [37]. Our data indicate that the metabolic pathways involving 3-hydroxy-3-methylglutaryl-CoA do not exhibit equal levels of activity throughout the year.

An important metabolic pathway to which a considerable portion of the acyl-CoAs could be assigned is the β-oxidation of saturated fatty acids; 29 detected acyl-CoAs, 16 verified by comparison with a reference standard, fall into this group (Fig 2).

thumbnail
Fig 2. β-Oxidation of saturated even and odd chain fatty acids and detection of potentially related acyl-CoAs.

Acetyl-CoA formed during β-oxidation of a fatty acid is channelled through the tricarboxylic acid (TCA) cycle. The remaining acyl-CoA, shortened by two carbon atoms, is processed by repeated β-oxidation. In the case of even-chain fatty acids, the final product is acetyl-CoA, which directly enters the TCA cycle. For odd-chain fatty acids, propionyl-CoA remains, which is converted to succinyl-CoA via (S)- and (R)-methylmalonyl-CoA, the latter two being inseparable with our analytical method, before it also enters the TCA cycle. The presence of bolded acyl-CoAs and acetyl-, succinyl- and methylmalonyl-CoA was confirmed by comparison with reference standards. The other acyl-CoAs listed in this figure were assigned through determination of the corresponding sum formulas by high-resolution mass spectrometry. In the case of isomeric acyl-CoAs with molecular formulas for which reference standards were unavailable, the retention sequence was used as an additional criterion. It was considered that acyl-CoA thioesters of unbranched alkanoic acids within a group of isomers have the highest retention times [25]. 3-Hydroxydecanoyl-CoA is shown in brackets, as it eluted earlier than heptanoyl-CoA and therefore did not correspond to the assumed retention time for this compound. The bar graphs depict the percentage of the different types of degradation products for even- and odd-chain fatty acids in summer (light blue) and autumn (dark blue) samples, with percentages indicated above the bars.

https://doi.org/10.1371/journal.pone.0327747.g002

Since lipids can comprise over 40% of the dry mass of krill, the presence of fatty acid degradation products in the form of acyl-CoAs is not surprising, although this has not been studied in krill [38]. Metabolites associated with the degradation of up to dodecanoic acid were identified. Overall, as expected, the relative proportions of acyl-CoAs associated with the β-oxidation of even-chain fatty acids were higher than those related to the β-oxidation of odd-chain fatty acid. An exception to this trend was the abundance of odd-chain fatty acyl-CoAs in autumn samples, mainly due to pentanoyl-CoA. In the majority of the stomach and hindgut samples from autumn, this acyl-CoA was the most abundant and the only acyl-CoA associated with β-oxidation. The composition of intact phospholipids from the same organs and during the same seasons also reflected a higher abundance of odd-chain fatty acids in autumn [15,39]. Therefore, acyl-CoAs may also serve as a valuable tracer for active metabolic pathways at the time of sampling.

Amino acids

During the amino acid analysis, 15 proteinogenic and two non-proteinogenic amino acids (β-alanine and sarcosine) were detected and quantified. Fig 3 shows the composition of the quantifiable free and protein-bound amino acids.

thumbnail
Fig 3. Relative distribution of amino acids between organs and seasons.

The different diagrams show a. all free amino acids, b. only free proteinogenic amino acids and c. protein-bound amino acids.

https://doi.org/10.1371/journal.pone.0327747.g003

Interestingly, sarcosine had the highest relative amounts of all free amino acids at 47–78%. As sarcosine is not a proteinogenic amino acid, it does not occur in the protein-bound fraction. Sarcosine has previously been detected in krill [20] and, among other amino acids, in high proportions in muscle-free krill meal for fish aquaculture [40]. Sarcosine contents between 4 and 15% of the free amino acids were found in whole animals of three species of North Atlantic krill (Meganyctiphanes norvegica, Thysanoessa inermis, T. raschii) [41]. In another study, sarcosine was detected in the muscles of M. norvegica and T. inermis, but not in those of E. superba [42].

Sarcosine has also been identified in various other crustaceans. Significant amounts were found in trichloroacetic acid extracts from hepatopancreas and blood of the rock lobster (Jasus lalandii) [43]. The authors also mentioned that they had found sarcosine in the freshwater crab Potamon (Potamonantes) perlatus/sydneyi. Sarcosine was also found in considerable proportions (13–53% of the free amino acids) in the hepatopancreas of the snow crab (Chionoecetes opilio) [44]. During the analysis of 16 shrimp species (frozen animals) of different geographical origin, sarcosine was only detected in the two species analysed from the family Pandilidae (Plesionika edwardsi, Pandalus montagui) in amounts between 61 and 89 mg per 100 g sample [45]. Furthermore, sarcosine was detected in unspecified amounts in the metasomal muscle of freshwater amphipods from Lake Baikal [46] and in freshwater shrimps of the species Macrobrachium rosenbergii [47], whereby the sarcosine content of the latter was considerably higher in moulting animals than in the non-moulting control (C-stage).

Overall, the available findings seem to provide evidence that the occurrence of sarcosine in crustaceans is associated with their digestive tract and that sarcosine plays a role in the digestive process of these animals. However, the origin of sarcosine is unclear. One possibility is that it is produced by microorganisms in the crustacean’s digestive system. A recently published genome and transcriptome study has shown that the biosynthesis of sarcosine is absent in the genome of both prokaryotic and eukaryotic marine microorganisms, with the exception of Alphaproteobacteria, 55% of which had a synthesis pathway [48]. The authors concluded that the source of sarcosine in the ocean is relatively unknown. In contrast to biosynthesis, sarcosine degradation was far more common in both the prokaryotic and eukaryotic groups [48].

This suggests that, alternatively, the krill itself could produce the sarcosine detected in its digestive system. In fact, digestive juices of Cancer pagarus, a marine crustacean, contain emulsifiers identified as fatty acylsarcosyltaurines; these compounds along with a fatty acid and taurine contain sarcosine as a building block [49]. After injection of 1-14C acetate into C. pagarus, radioactive labeling was detected in the sarcosine contained in the emulsifiers. This finding proves that it was produced biosynthetically using acetate and is therefore of endogenous origin [50].

The high sarcosine level could furthermore be related to krill’s lipid metabolism, which is also reflected in the occurrence of acyl-CoAs involved in β-oxidation (see above). One of the most abundant lipids found in krill are phosphatidylcholines [15,51]. Its choline moiety may be converted to sarcosine through dimethylglycine as an intermediate, which is also detectable in our samples [48,52]. Consequently, high concentrations of choline in the form of phosphatidylcholine could elucidate why the metabolism is directed towards sarcosine production.

In addition to its involvement in digestive processes, sarcosine could also play a role as an osmolyte. In general, osmolytes are substances that fulfill cell-protective functions in organisms living under water stress, which may be related to salinity, temperature and pressure, among others, by increasing the osmotic pressure in the cytoplasm [5355]. Three groups of low molecular weight organic osmolytes are known, namely polyols, amino acids (including sarcosine) and urea in combination with methylamines. Osmolytes occur in a wide variety of marine organisms [42,48,56,57]. A characteristic property of osmolytes is that they do not affect the structure of proteins, even at high concentrations, so that their functionality is not impaired, and that they can contribute to the stabilisation of proteins without being directly bound to them [58]. An elevated level of sarcosine may serve as an important protective factor by promoting the stabilisation of cold-adapted enzymes [59].

In a study examining human dietary supplementation with Antarctic krill oil, increased plasma levels of sarcosine were also found [52]. The authors attributed this to the fact that supplementation with choline directs human metabolism toward sarcosine production, possibly similar to its formation in the krill’s digestive system.

As the high sarcosine may mask the distribution patterns of the other amino acids, Fig 3b illustrates the composition while excluding the non-proteinogenic amino acids. Notably, the protein-bound amino acids were fairly evenly distributed across seasons and organs, with no significant differences, although this is not surprising given that the composition of protein amino acids is rather uniform even across different taxa [60]. At the same time, differences are observable in the free fraction, which is also reflected in the principal component analysis (S3 Fig of the supporting information). The most considerable differences were observed between the stomach samples of the two seasons, with significant variations found for alanine, arginine, glutamic acid, proline and valine (cf. S5 Table). The food entering the stomach, the first part of the digestive system, is not yet fully processed. Dietary-driven differences may be best seen in this organ, which is expected to reflect the freshest food signal.

Some amino acids, such as alanine, glutamic acid, glycine, and proline, were more abundant in the free form. In contrast, others, such as arginine, leucine, isoleucine, and threonine had a higher proportion in the protein-bound fraction when the stomach samples from autumn were excluded. These distributions and shifts are comparable with previously published data from whole krill [22,23,61], where greater variances in the content of free amino acids in whole krill between late summer and autumn were noted. Meanwhile, the distributions of the hydrolysed fractions were quite similar [22]. However, these differences were not as pronounced as those observed in the stomach samples. Therefore, while a seasonal trend might also be detected in whole krill samples, the most reliable indicators of recent food intake are found in the stomach.

The possibility that the high levels of propionyl-CoA in the digestive gland are an indication of increased metabolism of branched amino acids (see above) is not confirmed by the levels of isoleucine and valine found. Propionyl-CoA is therefore possibly an indicator of increased β-oxidation of odd-numbered fatty acids.

B vitamins

Eight of the eleven B vitamins measured by our method were above the detection limit in the samples analysed. Of the cobalamins, which include cyano-, hydroxy-, methyl-, and adenosylcobalamin (AB12), only the latter was detected.

As illustrated in Fig 4, the composition of B vitamins varied across seasons and within organs. The observed trends, when comparing the relative amounts in the organs, remained largely consistent. However, the proportion of AB12 decreased from the digestive gland via the stomach to the hind gut. The two vitamins that had the greatest effect on the variation in seasonal patterns were B1 and B5. Summer samples consistently exhibited higher levels of B5, while B1 was more abundant in the autumn samples. Of these two vitamins, a statistical difference was only confirmed for B1, which had the highest impact on stomach samples taken in autumn (S5 Table and S4 Fig of the supporting information). Vitamin B1 is the coenzyme of numerous enzymes involved in acetyl-CoA synthesis, the tricarboxylic acid cycle, the pentose phosphate pathway, and in isoprenoid biosynthesis, among others [62]. Genes of twenty-one B1-requiring enzymes have been documented to be encoded in genomes of marine prokaryotes and eukaryotes, five of which (pyruvate dehydrogenase, acetolactate synthase, 1-deoxy-D-xylulose-5-phosphate synthase, transketolase, and α-ketoglutarate dehydrogenase) were present in all taxonomic groups examined (alphaproteobacteria, gammaproteobacteria, cyanobacteria, bacteroidetes, eukaryotes) [63]. It is reasonable that these enzymes also occur in the krill gut’s microbiome, implying the requirement for B1. Vitamin B5 constitutes an integral part of the coenzyme A molecule and, therefore, is essential for many metabolic pathways, such as fatty acid biosynthesis or energy production via the citric acid cycle [64]. Similar to other metabolic classes, the variations observed in vitamin B content may suggest either endogenous processes or reflect signals from recent food intake.

thumbnail
Fig 4. Relative distribution of B vitamins between organs and seasons.

B1, thiamine; B2, riboflavin; B5, pantothenic acid; B6, pyridoxine; B7, biotin; B9, folic acid; AB12, adenosylcobalamine.

https://doi.org/10.1371/journal.pone.0327747.g004

In a previous study, Kim et al. measured the monthly changes of B1, B5, and B6 in whole krill to determine their nutritional composition [22]. Contrary to our results, they documented high levels of B6 and only minor concentrations of B5. Additionally, they reported a decrease in B1 and B6 from summer to autumn, whereas our data suggest the opposite. These differences could be due to the fact that they measured the concentration in whole krill and not in isolated organs.

Respiratory quinones

To our knowledge, the composition of respiratory quinones in krill, similar to acyl-CoAs, has not been previously investigated. As initial data for this class of biomolecules, we identified fourteen different respiratory quinones from three subclasses, namely eight ubiquinones (UQ), five menaquinones (MK) and one plastoquinone (PQ) (Fig 5). The most abundant respiratory quinone was UQ10:10, a 1,4-benzoquinone with 10 unsaturated isoprenyl subunits in the side chain, also referred to as coenzyme Q10. Like the essential omega-3 fatty acids obtained from krill, coenzyme Q10 plays an important role in human consumption as a dietary supplement [65,66]. Even though there are reports that UQ9 is the predominant respiratory quinone in Antarctic fish to achieve cold adaptation due to its lower crystallization temperature compared to UQ10, UQ10 is usually the predominant ubiquinone in other fishes and marine invertebrates [6769].

thumbnail
Fig 5. Relative distribution of respiratory quinones between organs and seasons.

Types of ubiquinones are coloured in shades of blue, menaquinones in green and the plastoquinone in orange.

https://doi.org/10.1371/journal.pone.0327747.g005

Despite the generally similar distributions of respiratory quinones as reflected in the principal component analysis (S5 Fig of the supporting information), some seasonal variations can be observed. UQ10:10 and UQ10:9 predominated in the autumn samples, a pattern also noted in the summer samples, albeit with a higher proportion of other UQs, MKs, and PQ. Any variations in the composition of respiratory quinones may be related to dietary composition or adaptations of the digestive system due to changes in food intake, considering that there are several potential origins for the detected respiratory quinones [70].

As the name suggests, ubiquitous ubiquinones are found in almost all living organisms. They have also been detected in various bacterial isolates from the Antarctic marine environment [7173]. UQ8:8 has been classified as the major respiratory quinone in a bacterium isolated from Antarctic krill [74]. Additionally, UQ9:9 was found in bacteria isolated from an Antarctic green alga, suggesting a potential dietary uptake of this respiratory quinone [75]. Menaquinones are mainly microbial respiratory quinones [70]. Several MKs, such as MK7:7 and MK8:8, have been described in Antarctic coastal marine environments [76,77]. Some bacteria can produce respiratory quinones with different degrees of unsaturation, providing a potential source of these kind of respiratory quinones, such as MK8:7 [78]. Plastoquinone 9 plays a significant role in photosynthesis, suggesting possibly phytoplankton uptake [79]. However, we detected only minimal amounts of PQ9:8, which contained one isoprenyl unit that was not unsaturated.

Implications for krill environmental adaptation

Throughout the year, krill experience pronounced seasonal changes in their habitat, with low sea ice cover and almost constant daylight promoting extensive primary production, providing abundant food for krill during summer. In contrast, food becomes scarce due to shorter days and increased sea ice cover in winter. In this challenging habitat, krill maintain a substantial biomass which can sustain the entire Southern Ocean ecosystem. The ability of krill to thrive in such a challenging environment is attributed to their capacity to adapt to the extreme environmental conditions, including low temperatures and strong seasonal fluctuations [80].

Krill adapt to these seasonal fluctuations by regulating several physiological functions. During winter, krill enter a state of “energy-saving mode,” characterised by a halt in development and reproduction [81,82], an accumulation of lipids [38,83], and a reduction in overall metabolism [83,84], enabling them to survive the harsh winter conditions. In contrast, in spring, krill transition back to an “active mode,” with increased feeding activity, heightened metabolism, and active reproduction and development.

In this study, we identified several metabolite classes that exhibited pronounced seasonal changes between summer and autumn samples (Fig 6). Among the acyl-CoAs, 3-hydroxy-3-methylglutaryl-CoA, a potential marker for reproductive processes [37], was detected in significant quantities throughout the entire digestive system in summer, while it was absent in autumn samples, aligning with the period of active reproduction in krill during that time of year. Vitamin B5, which is involved in fatty acid metabolism and energy production pathways [64], displayed heightened levels during krill’s active phase in summer, when overall metabolism is elevated.

thumbnail
Fig 6. Summary of characteristic metabolites with significant differences between seasons for each organ.

Metabolites marked with a yellow sun had a significantly higher abundance in summer samples, whereas metabolites with an orange sun where significantly more abundant in autumn samples.

https://doi.org/10.1371/journal.pone.0327747.g006

In addition to its adaptation to seasonal fluctuations, krill is highly adapted to the cold waters of the Southern Ocean, where temperatures can drop to −2°C.

Interestingly, the amino acid sarcosine is found in high proportions (up to 78%) among all free amino acids, but shows no clear seasonal differences. It is conceivable that sarcosine is involved in the digestive processes in krill, but it could also play an important role in cold adaptation mechanisms [e.g., 85], which in turn reflects the adaptation of krill to the polar habitat. Seasonal fluctuations in water temperatures within the Southern Ocean are typically minimal, and krill must be prepared to encounter extremely low temperatures throughout the year. This may explain the absence of seasonal differences in sarcosine levels. In summary, our data reinforce the fundamental importance of krill’s adaptation to its extreme environment.

Conclusion

In this study, classes of metabolic products that have rarely been investigated in krill or comparable species were analysed for the first time. These initial measurements provide a valuable basis for future evaluations and interpretations. The dataset presented in this study documents the enormous potential of important classes of metabolites that can be used as tracers to detect shifts in the composition of Antarctic krill due to changing environmental conditions or variations in its food supply. Further long-term datasets will additionally support and extend these new insights, allowing the development of useful new tools to detect small changes in the metabolome. Since Euphausia superba plays a central role in biogeochemical cycles and is also relevant for human consumption, early detection of changes in diet and, thus, in the environment can be crucial.

Supporting information

S1 Table. Full-scan orbitrap settings.

Settings used for full-scan high-resolution mass spectrometry on the Orbitrap instrument for the detection of respiratory quinones.

https://doi.org/10.1371/journal.pone.0327747.s001

(PDF)

S2 Table. Targeted orbitrap settings.

Settings for targeted mass spectrometry for the detection of respiratory quinones.

https://doi.org/10.1371/journal.pone.0327747.s002

(PDF)

S4 Table. Detected coenzyme A thioesters.

List of all peaks detected during coenzyme A measurements, including their exact masses, sum formulas and, where applicable, their identification.

https://doi.org/10.1371/journal.pone.0327747.s004

(PDF)

S5 Table. Results of the Kruskal-Wallis and Dunn’s tests where significances were observed.

https://doi.org/10.1371/journal.pone.0327747.s005

(PDF)

S1 Fig. Relative distribution of all coenzyme A thioesters between organs and seasons. a.

Including acetyl-CoA and b. excluding acetyl-CoA.

https://doi.org/10.1371/journal.pone.0327747.s006

(PDF)

S2 Fig. Principal component analysis of the percentage distribution of coenzyme A thioesters numbered according to S4 Table.

Colours indicate the sampling months while shades and symbols represent the organ sampled from krill as indicated in the legend. Due to crowding on the right side, not all numbers are displayed.

https://doi.org/10.1371/journal.pone.0327747.s007

(PDF)

S3 Fig. Principal component analysis of the percentage distribution of free and protein-bound amino acids.

Colours indicate the sampling months while shades and symbols represent the organ sampled from krill as indicated in the legend.

https://doi.org/10.1371/journal.pone.0327747.s008

(PDF)

S4 Fig. Principal component analysis of the percentage distribution of B vitamins.

Colours indicate the sampling months while shades and symbols represent the organ sampled from krill as indicated in the legend.

https://doi.org/10.1371/journal.pone.0327747.s009

(PDF)

S5 Fig. Principal component analysis of the percentage distribution of respiratory quinones.

Colours indicate the sampling months while shades and symbols represent the organ sampled from krill as indicated in the legend.

https://doi.org/10.1371/journal.pone.0327747.s010

(PDF)

Acknowledgments

We thank Pia Ebert and Mathias Wolterink for the extraction, derivatisation and measurement of amino acid samples as well as Regina Grundmann for the purification of acyl-CoAs. We also like to thank Dominik Bahlburg for his support in sample handling for this project on board in 2021 and Sara Driscoll in 2022. Furthermore, our thank goes to the fishing company Aker BioMarine for allowing us to conduct our research on one of their krill fishing vessels and the captains, officers and crew of the FV Antarctic Endurance, who supported us in successfully conducting our research in the different seasons.

References

  1. 1. Cavan EL, Belcher A, Atkinson A, Hill SL, Kawaguchi S, McCormack S, et al. The importance of Antarctic krill in biogeochemical cycles. Nat Commun. 2019;10(1):4742. pmid:31628346
  2. 2. Atkinson A, Siegel V, Pakhomov EA, Jessopp MJ, Loeb V. A re-appraisal of the total biomass and annual production of Antarctic krill. Deep Sea Res I Oceanogr Res Pap. 2009;56(5):727–40.
  3. 3. Burri L, Johnsen L. Krill products: an overview of animal studies. Nutrients. 2015;7(5):3300–21. pmid:25961320
  4. 4. Swanson D, Block R, Mousa SA. Omega-3 fatty acids EPA and DHA: health benefits throughout life. Adv Nutr. 2012;3(1):1–7. pmid:22332096
  5. 5. Hamner WM. Biomechanics of filter feeding in the antarctic krill Euphausia superba: review of past work and new observations. J Crustac Biol. 1988;8(2):149–63.
  6. 6. Suh H-L, Nemoto T. Morphology of the gastric mill in ten species of euphausiids. Mar Biol. 1988;97(1):79–85.
  7. 7. Ikeda T, Nash GV, Thomas PG. An observation of discarded stomach with exoskeleton moult from Antarctic krill Euphausia superba Dana. Polar Biol. 1984;3(4):241–4.
  8. 8. Buchholz F, Saborowski R. A field study on the physiology of digestion in the Antarctic krill, Euphausia superba, with special regard to chitinolytic enzymes. J Plankton Res. 1996;18(6):895–906.
  9. 9. Saborowski R, Buchholz F. A laboratory study on digestive processes in the Antarctic krill, Euphausia superba , with special regard to chitinolytic enzymes. Polar Biol. 1999;21(5):295–304.
  10. 10. Ullrich B, Storch V, Marschall H. Microscopic anatomy, functional morphology, and ultrastructure of the stomach of Euphausia superba Dana (Crustacea, Euphausiacea). Polar Biol. 1991;11(3).
  11. 11. Atkinson A, Schmidt K, Fielding S, Kawaguchi S, Geissler PA. Variable food absorption by Antarctic krill: Relationships between diet, egestion rate and the composition and sinking rates of their fecal pellets. Deep Sea Res II Top Stud Oceanogr. 2012;59–60:147–58.
  12. 12. Hellessey N, Ericson JA, Nichols PD, Kawaguchi S, Nicol S, Hoem N, et al. Seasonal and interannual variation in the lipid content and composition of Euphausia superba Dana, 1850 (Euphausiacea) samples derived from the Scotia Sea fishery. J Crustac Biol. 2018.
  13. 13. Ericson JA, Hellessey N, Nichols PD, Kawaguchi S, Nicol S, Hoem N, et al. Seasonal and interannual variations in the fatty acid composition of adult Euphausia superba Dana, 1850 (Euphausiacea) samples derived from the Scotia Sea krill fishery. J Crustac Biol. 2018.
  14. 14. Ericson JA, Hellessey N, Nichols PD, Nicol S, Kawaguchi S, Hoem N, et al. New insights into the seasonal diet of Antarctic krill using triacylglycerol and phospholipid fatty acids, and sterol composition. Polar Biol. 2019;42(11):1985–96.
  15. 15. Heyen S, Schneider V, Hüppe L, Meyer B, Wilkes H. Variations of intact phospholipid compositions in the digestive system of Antarctic krill, Euphausia superba, between summer and autumn. PLoS One. 2023;18(12):e0295677. pmid:38157351
  16. 16. Flores H, Atkinson A, Kawaguchi S, Krafft B, Milinevsky G, Nicol S, et al. Impact of climate change on Antarctic krill. Mar Ecol Prog Ser. 2012;458:1–19.
  17. 17. Deppeler SL, Davidson AT. Southern ocean phytoplankton in a changing climate. Front Mar Sci. 2017;4.
  18. 18. Winther B, Hoem N, Berge K, Reubsaet L. Elucidation of phosphatidylcholine composition in krill oil extracted from Euphausia superba. Lipids. 2011;46(1):25–36. pmid:20848234
  19. 19. Hellessey N, Ericson JA, Nichols PD, Kawaguchi S, Nicol S, Hoem N, et al. Regional diet in Antarctic krill (Euphausia superba) as determined by lipid, fatty acid, and sterol composition. Polar Biol. 2022;45(6):1077–92.
  20. 20. Zhang F, Zhao M, Ma C, Wang L, Feng C, Li L, et al. A metabolomic study of Antarctic krill (Euphausia superba) raises a warning about Antarctic pollution. Crustac. 2018;91(8):961–99.
  21. 21. Chen Y-C, Tou JC, Jaczynski J. Amino acid and mineral composition of protein and other components and their recovery yields from whole Antarctic krill (Euphausia superba) using isoelectric solubilization/precipitation. J Food Sci. 2009;74(2):H31-9. pmid:19323748
  22. 22. Kim M-A, Jung H-R, Lee Y-B, Chun B-S, Kim S-B. Monthly variations in the nutritional composition of Antarctic krill Euphausia superba. Fish Aquat Sci. 2014; 17:409–19.
  23. 23. Li WJ, Chen SS, Qiu WQ. Comparative analysis of amino acid composition in antarctic krill and white shrimp. AMR. 2014;941–944:1114–9.
  24. 24. Ellingsen TE, Mohr V. Biochemistry of the autolytic processes in Antarctic krill post mortem. Autoproteolysis. Biochem J. 1987;246(2):295–305. pmid:3689312
  25. 25. Cakić N, Kopke B, Rabus R, Wilkes H. Suspect screening and targeted analysis of acyl coenzyme A thioesters in bacterial cultures using a high-resolution tribrid mass spectrometer. Anal Bioanal Chem. 2021;413(14):3599–610. pmid:33881564
  26. 26. Walsh RG, He S, Yarnes CT. Compound-specific δ13C and δ15N analysis of amino acids: a rapid, chloroformate-based method for ecological studies. Rapid Commun Mass Spectrom. 2014;28(1):96–108. pmid:24285394
  27. 27. Vane K, Larsen T, Scholz-Böttcher BM, Kopke B, Ekau W. Ontogenetic resource utilization and migration reconstruction with δ13C values of essential amino acids in the Cynoscion acoupa otolith. Ecol Evol. 2018;8(19):9859–69. pmid:30386581
  28. 28. Tindall BJ. A comparative study of the lipid composition of Halobacterium saccharovorum from various sources. Syst Appl Microbiol. 1990;13(2):128–30.
  29. 29. Heyen S, Scholz-Böttcher BM, Rabus R, Wilkes H. Method development and validation for the quantification of organic acids in microbial samples using anionic exchange solid-phase extraction and gas chromatography-mass spectrometry. Anal Bioanal Chem. 2020;412(27):7491–503. pmid:32970177
  30. 30. Bruns S, Wienhausen G, Scholz-Böttcher B, Wilkes H. Simultaneous quantification of all B vitamins and selected biosynthetic precursors in seawater and bacteria by means of different mass spectrometric approaches. Anal Bioanal Chem. 2022;414(27):7839–54. pmid:36195729
  31. 31. Zhu C, Lipp JS, Wörmer L, Becker KW, Schröder J, Hinrichs K-U. Comprehensive glycerol ether lipid fingerprints through a novel reversed phase liquid chromatography–mass spectrometry protocol. Org Geochem. 2013;65:53–62.
  32. 32. Elling FJ, Becker KW, Könneke M, Schröder JM, Kellermann MY, Thomm M, et al. Respiratory quinones in Archaea: phylogenetic distribution and application as biomarkers in the marine environment. Environ Microbiol. 2016;18(2):692–707. pmid:26472620
  33. 33. Vu VQ. ggbiplot: A ggplot2 based biplot. R package version 0.55, http://github.com/vqv/ggbiplot. 2011.
  34. 34. R Core Team. R: A language and environment for statistical computing. Vienna, Austria: R Foundation for Statistical Computing. URL https://www.R-project.org/. 2022.
  35. 35. Zhang L-S, Liang S, Zong M-H, Yang J-G, Lou W-Y. Microbial synthesis of functional odd-chain fatty acids: a review. World J Microbiol Biotechnol. 2020;36(3):35. pmid:32088779
  36. 36. Manoli I, Venditti CP. Disorders of branched chain amino acid metabolism. Transl Sci Rare Dis. 2016;1(2):91–110. pmid:29152456
  37. 37. Homola E, Chang ES. Methyl farnesoate: crustacean juvenile hormone in search of functions. Comp Biochem Physiol B Biochem Mol Biol. 1997;117(3):347–56.
  38. 38. Hagen W, Kattner G, Terbrüggen A, Van Vleet ES. Lipid metabolism of the Antarctic krill Euphausia superba and its ecological implications. Mar Biol. 2001;139(1):95–104.
  39. 39. Heyen S, Schneider V, Hüppe L, Meyer B, Wilkes H. Intact phospholipid and fatty acid compositions in the digestive system of Antarctic krill, Euphausia superba, sampled in January, March and May. PANGAEA. 2023.
  40. 40. Shimizu C, Ibrahim A, Tokoro T, Shirakawa Y. Feeding stimulation in sea bream, Pagrus major, fed diets supplemented with Antarctic krill meals. Aquaculture. 1990;89(1):43–53.
  41. 41. Saether O, Mohr V. Chemical composition of North Atlantic krill. Comp Biochem Physiol. 1987;88(1):157–64.
  42. 42. Carr WES, Netherton Iii JC, Gleeson RA, Derby CD. Stimulants of feeding behavior in fish: analyses of tissues of diverse marine organisms. Biol Bull. 1996;190(2):149–60. pmid:29244587
  43. 43. Novellie L, Schwartz HM. Occurrence and distribution of sarcosine in the rock lobster. Nature. 1954;173(4401):450–450.
  44. 44. Miyagawa M, Nakamato S, Yamane K, Shinpo A, Uezo S, Yahikozawa M, et al. Studies on organic constituents of the snow crab (Chionoecetes opilio)—II Free amino acids in extracts. Nippon Suisan Gakkai Shi. 1979;45:115–20.
  45. 45. Takada K, Aoki T, Kunisaki N. Proximate composition, free amino acid, fatty acid, mineral and cholesterol contents in imported frozen shrimps. Nippon Suisan Gakkai shi. 1988;54(12):2173–9.
  46. 46. Zerbst-Boroffka I, Kamaltynow RM, Harjes S, Kinne-Saffran E, Gross J. TMAO and other organic osmolytes in the muscles of amphipods (Crustacea) from shallow and deep water of Lake Baikal. Comp Biochem Physiol A Mol Integr Physiol. 2005;142(1):58–64. pmid:16139539
  47. 47. Juneta-Nor AS, Noordin NM, Azra MN, Ma H-Y, Husin NM, Ikhwanuddin M. Amino acid compounds released by the giant freshwater prawn Macrobrachium rosenbergii during ecdysis: a factor attracting cannibalistic behaviour?. J Zhejiang Univ Sci B. 2020;21(10):823–34. pmid:33043647
  48. 48. McParland EL, Alexander H, Johnson WM. The osmolyte ties that bind: genomic insights into synthesis and breakdown of organic osmolytes in marine microbes. Front Mar Sci. 2021;8:1847.
  49. 49. Van Den Oord A, Danielsson H, Ryhage R. On the structure of the emulsifiers in gastric juice from the crab, Cancer pagurus L. J Biol Chem. 1965;240(5):2242–7.
  50. 50. van den Oord A. The biosynthesis of the emulsifiers of the crab Cancer pagurus L. Comp Biochem Physiol. 1966;17(3):715–8. pmid:5943908
  51. 51. Clarke A. The biochemical composition of krill, Euphausia superba Dana, from South Georgia. J Exp Mar Biol Ecol. 1980;43(3):221–36.
  52. 52. Bjørndal B, Bruheim I, Lysne V, Ramsvik MS, Ueland PM, Nordrehaug JE, et al. Plasma choline, homocysteine and vitamin status in healthy adults supplemented with krill oil: a pilot study. Scand J Clin Lab Invest. 2018;78(7–8):527–32. pmid:30261756
  53. 53. Yancey PH, Clark ME, Hand SC, Bowlus RD, Somero GN. Living with water stress: evolution of osmolyte systems. Science. 1982;217(4566):1214–22. pmid:7112124
  54. 54. Yancey PH. Organic osmolytes as compatible, metabolic and counteracting cytoprotectants in high osmolarity and other stresses. J Exp Biol. 2005;208(Pt 15):2819–30. pmid:16043587
  55. 55. Burg MB, Ferraris JD. Intracellular organic osmolytes: function and regulation. J Biol Chem. 2008;283(12):7309–13. pmid:18256030
  56. 56. Kirst GO. Salinity tolerance of eukaryotic marine algae. Annu Rev Plant Physiol Plant Mol Biol. 1990;41(1):21–53.
  57. 57. Yancey PH, Siebenaller JF. Co-evolution of proteins and solutions: protein adaptation versus cytoprotective micromolecules and their roles in marine organisms. J Exp Biol. 2015;218(Pt 12):1880–96. pmid:26085665
  58. 58. Arakawa T, Timasheff SN. The stabilization of proteins by osmolytes. Biophys J. 1985;47(3):411–4. pmid:3978211
  59. 59. Siddiqui KS, Shemsi AM, Guerriero G, Najnin T, Taha EH, Ertan H. Biotechnological improvements of cold-adapted enzymes: commercialization via an integrated approach. In: Margesin R, editor. Psychrophiles: From biodiversity to biotechnology. Cham: Springer International Publishing. 2017. p. 477–512.
  60. 60. Bianchi TS, Canuel EA. Chemical biomarkers in aquatic ecosystems. Princeton: Princeton University Press. 2011. pp. 100–101.
  61. 61. Storebakken T. Krill as a potential feed source for salmonids. Aquaculture. 1988;70(3):193–205.
  62. 62. Rapala-Kozik M. Vitamin B1 (thiamine): a cofactor for enzymes involved in the main metabolic pathways and an environmental stress protectant. Biosynthesis of Vitamins in Plants Part A - Vitamins A, B1, B2, B3, B5. Elsevier; 2011. pp. 37–91.
  63. 63. Sañudo-Wilhelmy SA, Gómez-Consarnau L, Suffridge C, Webb EA. The role of B vitamins in marine biogeochemistry. Ann Rev Mar Sci. 2014;6:339–67. pmid:24050603
  64. 64. Webb ME, Smith AG. Pantothenate biosynthesis in higher plants. Biosynthesis of Vitamins in Plants Part A - Vitamins A, B1, B2, B3, B5. Elsevier; 2011. pp. 203–55.
  65. 65. Arenas-Jal M, Suñé-Negre JM, García-Montoya E. Coenzyme Q10 supplementation: efficacy, safety, and formulation challenges. Compr Rev Food Sci Food Saf. 2020;19(2):574–94. pmid:33325173
  66. 66. Testai L, Martelli A, Flori L, Cicero AFG, Colletti A. Coenzyme Q10: clinical applications beyond cardiovascular diseases. Nutrients. 2021;13(5):1697. pmid:34067632
  67. 67. Farbu T, Lambertsen G. Ubiquinone analyses in fish tissues and in some marine invertebrates. Comp Biochem Physiol B. 1979;63(3):395–7. pmid:318418
  68. 68. Giardina B, Gozzo ML, Zappacosta B, Colacicco L, Callà C, Mordente A, et al. Coenzyme Q homologs and trace elements content of Antarctic fishes Chionodraco hamatus and Pagothenia bernacchii compared with the mediterranean fish Mugil cephalus. Comp Biochem Physiol. 1997;118(4):977–80.
  69. 69. Colella A, Patamia M, Galtieri A, Giardina B. Cold adaptation and oxidative metabolism of Antarctic fish. Ital J Zool. 2000;67(sup1):33–6.
  70. 70. Nowicka B, Kruk J. Occurrence, biosynthesis and function of isoprenoid quinones. Biochim Biophys Acta. 2010;1797(9):1587–605. pmid:20599680
  71. 71. Baek K, Choi A, Kang I, Im M, Cho J-C. Granulosicoccus marinus sp. nov., isolated from Antarctic seawater, and emended description of the genus Granulosicoccus. Int J Syst Evol Microbiol. 2014;64(Pt 12):4103–8. pmid:25238763
  72. 72. Montes MJ, Bozal N, Mercadé E. Marinobacter guineae sp. nov., a novel moderately halophilic bacterium from an Antarctic environment. Int J Syst Evol Microbiol. 2008;58(Pt 6):1346–9. pmid:18523176
  73. 73. Shivaji S, Sathyanarayana Reddy G, Sundareswaran VR, Thomas C. Description of Thalassospira lohafexi sp. nov., isolated from Southern Ocean, Antarctica. Arch Microbiol. 2015;197(5):627–37. pmid:25702315
  74. 74. Denner EB, Mark B, Busse HJ, Turkiewicz M, Lubitz W. Psychrobacter proteolyticus sp. nov., a psychrotrophic, halotolerant bacterium isolated from the Antarctic krill Euphausia superba Dana, excreting a cold-adapted metalloprotease. Syst Appl Microbiol. 2001;24(1):44–53. pmid:11403398
  75. 75. Hwang CY, Zhang GI, Kang S-H, Kim HJ, Cho BC. Pseudomonas pelagia sp. nov., isolated from a culture of the Antarctic green alga Pyramimonas gelidicola. Int J Syst Evol Microbiol. 2009;59(Pt 12):3019–24. pmid:19643900
  76. 76. Oh H-M, Lee K, Cho J-C. Lewinella antarctica sp. nov., a marine bacterium isolated from Antarctic seawater. Int J Syst Evol Microbiol. 2009;59(Pt 1):65–8. pmid:19126725
  77. 77. Bozal N, Montes MJ, Tudela E, Jiménez F, Guinea J. Shewanella frigidimarina and Shewanella livingstonensis sp. nov. isolated from Antarctic coastal areas. Int J Syst Evol Microbiol. 2002;52(Pt 1):195–205. pmid:11837303
  78. 78. Collins MD, Jones D. Distribution of isoprenoid quinone structural types in bacteria and their taxonomic implication. Microbiol Rev. 1981;45(2):316–54. pmid:7022156
  79. 79. Amesz J. The function of plastoquinone in photosynthetic electron transport. Biochim Biophys Acta. 1973;301(1):35–51. pmid:4574766
  80. 80. Ducklow HW, Baker K, Martinson DG, Quetin LB, Ross RM, Smith RC, et al. Marine pelagic ecosystems: the west Antarctic Peninsula. Philos Trans R Soc Lond B Biol Sci. 2007;362(1477):67–94. pmid:17405208
  81. 81. Kawaguchi S, Yoshida T, Finley L, Cramp P, Nicol S. The krill maturity cycle: a conceptual model of the seasonal cycle in Antarctic krill. Polar Biol. 2006;30(6):689–98.
  82. 82. Siegel V. Krill stocks in high latitudes of the Antarctic Lazarev Sea: seasonal and interannual variation in distribution, abundance and demography. Polar Biol. 2012;35(8):1151–77.
  83. 83. Meyer B, Auerswald L, Siegel V, Spahic c, Pape C, Fach B, et al. Seasonal variation in body composition, metabolic activity, feeding, and growth of adult krill Euphausia superba in the Lazarev Sea. Mar Ecol Prog Ser. 2010;398:1–18.
  84. 84. Quetin LB, Ross RM. Behavioral and physiological characteristics of the antarctic krill, Euphausia superba. Am Zool. 1991;31(1):49–63.
  85. 85. Maiti A, Erimban S, Daschakraborty S. Extreme makeover: the incredible cell membrane adaptations of extremophiles to harsh environments. Chem Commun (Camb). 2024;60(75):10280–94. pmid:39190300