1. Introduction
Global warming is projected to have major consequences on food security worldwide, exacerbating the expected increase in food demand by 70% to 100% by 2050 due to the population growth [
1,
2,
3]. Anthropogenic greenhouse gas (GHG) emissions, particularly CH
4, are major contributors to global warming. Methane has a global warming potential approximately 28 times greater than CO
2 [
2]. The agricultural sector is considered to be one of the major sources of CH
4 emissions, with ruminant animals, particularly domestic ruminants being significant contributors [
4,
5]. Ruminal methanogens are responsible for over 87% of total CH
4 emissions from ruminants and about 26% in comparison to other sources of CH
4 production in the environment [
3,
6]. Methane is produced in the rumen during the normal fermentation process by methanogenic archaea which use either CO
2 and hydrogen (H
2), methylamines or methanol, or acetate and H
2 to produce CH
4 [
7]. Other microorganisms residing within the rumen such as bacteria, protozoa, and fungi can provide methanogens with excessive H
2, either directly or indirectly, and thereby promote methanogenic activity [
8,
9]. Although utilizing excess H
2 benefits ruminal fermentation by preventing H
2 build-up and feedback inhibition, ruminal CH
4 production represents 2%- 12% of gross energy loss [
10]. Therefore, there is an impetus need for developing approaches to mitigate CH
4 emissions from ruminant livestock to reduce energy loss from animals while improving environmental health.
Over the last five decades, ruminal methanogens and anti-methanogenic intervention strategies have been extensively explored as a means of mitigating CH
4 emissions [
11]. These strategies involve alterations in animal management, dietary composition, and ruminal fermentation, as well as direct inhibition of the growth and metabolic activity of methanogens using anti-methanogenic compounds and substances [
12,
13]. However, most of these approaches have shown limited efficacy due to the complex nature of animal management and ruminal physiology [
14,
15]. Additionally, recent research has focused on reducing CH
4 emissions from ruminants by genetic selection and manipulation of the ruminal microbiota, and the latter has become an active area of research due to advances in next-generation sequencing technologies [
16]. While genomic selection could provide a long-term solution to CH
4 emissions [
17,
18,
19], the impact of the selected anti-methanogenic traits on ruminal nutrient metabolism, fermentation, and the microbial community is yet to be defined. Recent identification of a distinctive ruminal microbiota between cattle and sheep with high and low CH
4 emitting phenotypes [
20] suggest that the manipulation of the ruminal microbiota to mitigate livestock CH
4 production may provide long-lasting solutions.
While most of the current research has focused on characterizing the taxonomic diversity and abundance of methanogenic archaea in the rumen and the potential role of the ruminal microbiome in methanogenesis, emerging evidence suggests that microbial communities associated with extra-ruminal sites of animals including the reproductive and respiratory tracts and mammary glands may harbor methanogenic archaeal species [
7,
21,
22,
23,
24] and these extra-gastrointestinal methanogens may interact with ruminal methanogens. Some of the methanogenic taxa (e.g.,
Methanobrevibacter spp.) have been reported to be shared as core taxa across ruminal, respiratory, and reproductive tract-associated microbial communities in cattle [
21,
25]. This, coupled with increased appreciation of the microbiome-gut-organ (respiratory/reproductive) axis [
25,
26] highlight the possible existence of interactions between methanogenic archaea in the rumen with methanogens and microbiomes present in extra-gastrointestinal organs. Such interactions between the rumen and other organs may be responsible for seeding the rumen or other organs with methanogenic species and/or influencing metabolic activities of the ruminal methanogens. The potential seeding of the rumen with methanogens by methanogens present in the reproductive tract is further supported by the recent identification of methanogenic archaeal species in fetal fluid and intestines of bovine fetuses [
21,
27]. Thus, these new developments point out that focusing solely on the methanogens present in the rumen and developing CH
4 mitigation strategies targeted at only ruminal methanogens could be too narrow of an approach. The ruminal and extra-gastrointestinal methanogens and their interactions on ruminal CH
4 emissions should be considered. In this review, we first provide a holistic survey of the methanogenic archaea present in different anatomical sites of cattle. We then discuss potential seeding sources of the ruminal methanogenic archaea in cattle. In addition, we highlight some challenges and future research directions associated with studying ruminal and extra-gastrointestinal methanogens in cattle.
2. General Overview of Methanogens
Methanogens are a diverse group of microorganisms that produce CH
4 as a metabolic byproduct of their energy conservation processes [
28,
29]. They are commonly present in a variety of environments including the digestive tracts of animals, predominantly ruminants, wetlands, and other anaerobic environments [
11,
30]. Methanogens are classified in the domain archaea and are phylogenetically diverse [
31]. Methane production is an essential part of the global carbon cycle, accounting for approximately 18% of anthropogenic GHG emissions [
32].
Methanogens are classified within the archaeal phyla
Euryarchaeota, Crenarchaeota, and
Korarchaeota. They are further subdivided into several orders and families based on their phylogenetic relationships and metabolic pathways [
33,
34]. Recent research has revealed the diversity of methanogens in different environments, with new genera and species being identified through metagenomic analysis and other non-culture based techniques [
35,
36]. High-throughput sequencing techniques have enabled the discovery of novel methanogen species and lineages from diverse environments, such as the animal gut and reproductive tracts, rice paddies, and deep-sea sediments [
11,
37,
38]. For example, a recent study using metagenomic analysis identified a new genus of methanogen from the digestive tract of a giant panda, which was found to be closely related to
Methanobrevibacter smithii, a common human gut methanogen [
39,
40,
41].
Methanogens are believed to be one of the earliest forms of life on Earth, with evidence suggesting that they were present over 3.5 billion years ago [
42]. Their unique metabolic capabilities are thought to have evolved in response to the anaerobic conditions of the early Earth, where they played a significant role in the carbon cycle [
43]. Based on the substrates used to produce CH
4, methanogens can be classified as hydrogenotrophic, acetoclastic and methylotrophic methanogens [
44,
45]. The hydrogenotrophic class uses H
2 for the reduction of CO
2 into CH
4. Examples of such methanogens are
Methanobrevibacter,
Methanobacterium, and
Methanomicrobiales. The rumen is mainly inhabited by hydrogenotrophic methanogens [
46]. The second class, acetoclastic methanogens which are most commonly present in freshwater sediments and anaerobic digestors, but use alcohols such as ethanol or 2-propanol as electron donors to produce CH
4 [
41,
42,
47,
48,
49]. The methylotrophic class which is predominant in freshwater and wetland soils [
50,
51,
52] relies on methyl groups such as methanol and methylamines to produce CH
4, and encompasses the order
Methanococcales and
Methanosarcinales. Of note, hydrogenotrophic methanogens are the focus of the present review as they are the main class of methanogens involved in enteric CH
4 emissions from cattle. The other two classes of methanogens will be briefly discussed as potential environmental sources that could seed ruminal methanogens in cattle.
3. Main Methanogenic Species in the Rumen
The methanogenic community in the rumen of ruminant animals is dominated by two main phyla: Euryarchaeota and Crenarchaeota [
53]. The Euryarchaeota phylum is the most abundant and taxonomically diverse group of methanogens in the rumen. This phylum includes the orders
Methanobacteriales,
Methanomicrobiales, Methanosarcinales, and
Methanocellales. The Crenarchaeota phylum contains the order
Thermoproteales and is present in some ruminants but is less abundant as compared to the Euryarchaeota phylum [
54] (
Table 1).
Methanobrevibacter is the most abundant genus of ruminal methanogens in cattle and it belongs to Euryarchaeota phylum [
54]. Multiple species of
Methanobrevibacter including
M. ruminantium, M. smithii, and
M. gottschalkii have been reported in the rumen of cattle other ruminant species (
Table 1). The
Methanobrevibacter spp. produce CH
4 from H
2 and CO
2, and they can also utilize formate and acetate as alternative substrates [
55]. Another common archaeal genus found in the rumen is
Methanosphaera [
56], and species within this genus consume H
2 and CO
2, as well as methanol and methylamines to produce CH
4 [
56]. Multiple species within
Methanosphaera (e.g.,
M. stadtmanae and
M. cuniculi) have also been detected in the rumen, and believed to contribute to the ruminal CH
4 production [
57,
58]. Guzman and colleagues identified
Methanomicrobiales mobile,
Methanoccocales votae, and
Methanobrevibacter spp. from the gastrointestinal tract of neonatal dairy calves sampled within five minutes of birth [
59].
Methanomassiliicoccus, within the phylum Euryarchaeota, is a relatively recent discovered genus from the rumen and feces of ruminants [
57]. This genus is unique in a way that it produces CH
4 through the reduction of methanol and methylamines, rather than H
2 and CO
2 [
57].
Methanomassiliicoccushas been suggested as a potential target for inhibiting ruminal CH
4 emissions due to its ability to outcompete hydrogenotrophic methanogens [
60]. Also,
Methanospirillum, classified within the order
Methanomicrobiales and the phylum Euryarchaeota, has been found in the rumen and feces of cattle and sheep [
61]. Additionally,
Methanospirillum hungatei and
Methanospirillum lacunae are also present in the rumen [
62]. Overall, the rumen is home to taxonomically and metabolically diverse methanogenic archaeal species.
4. Pro-and Anti-Methanogenic Ruminal Microorganisms
Methanogens undergo methanogenesis; an energy-intensive process that requires specific substrates and environmental conditions [
63]. Syntrophic bacteria are among the most extensively studied microorganisms that enhance the activity of methanogens in the rumen. Syntrophic bacteria, such as
Syntrophomonas spp. and
Smithella spp., form symbiotic associations with methanogens, by degrading complex organic matter to simpler compounds that methanogens can utilize [
57,
64]. Examples of syntrophic bacteria are
Syntrophomonas wolfei,
Syntrophobacter fumaroxidans, and
Pelotomaculum thermopropionicum. In this relationship, syntrophic bacteria oxidized short chain fatty acids (SCFAs) to produce H
2 and CO
2, both of which are used by methanogens to produce CH
4 [
65].
In addition to syntrophic bacteria, some other bacterial species may enhance the activity of methanogens through various mechanisms in the rumen. For example, exopolysaccharide-producing bacterial species can promote the aggregation of methanogens, creating microenvironments favoring methanogenesis [
55]. Other bacteria species that produce secondary metabolites including formic acid and ethanol can facilitate methanogenesis [
66]. Furthermore,
Pelobacter spp. and
Bacteroides spp. can promote methanogenesis by enhancing the growth of specific methanogenic species [
67].
While some bacteria promote methanogens, there are some bacteria in the rumen that can inhibit methanogenesis. Sulfate-reducing bacteria (SRB) such as
Desulfovibrio spp. consume organic matter and produce hydrogen sulfide (H
2S). Both SRB and methanogens compete for H
2, as SRB require it to reduce sulfate to sulfide; while methanogens need H
2 to reduce CO
2 for CH
4 production. Because of this competition, the presence of SRB indirectly decreases methane production in the rumen [
20]. Ruminal SRB utilize various forms of sulfur (S), including sulfate, sulfite, thiosulfate, and elemental S, as optional H
2 sinks [
68]. As the end-product of the sulfate reduction pathway, H
2S can inhibit methanogenic activity, consequently reducing ruminal CH
4 production [
69]. In addition, abundance of bacterial genera such as
Prevotella,
Fibrobacter, and
Ruminococcuswere found to be negatively correlated with methanogenic activity in dairy cows [
14]. These bacteria that are involved in the degradation of fiber and the production of propionate can compete with methanogenesis for H
2. Fumarate-reducing and lactate-producing bacteria may also inhibit methanogens, which was suggested by a study where nitrate supplementation reduced CH
4 emission in grazing steers by promoting fumarate-reducing and lactate-producing bacteria [
70]. Jenayathan and colleagues [
12] also reported that direct-fed microbials comprising of
Propionibacterium and
Lactobacillus spp. were able to mitigate CH
4 emissions in sheep. The genus
Lactobacillus has a long history of being used as a probiotic and has recently been proposed to mitigate ruminal CH
4 emissions [
71]. Other genera such as
Prevotella and
Succinivibrio have been negatively associated with ruminal methanogenesis [
56,
72,
73]. The family
Succinivibrionaceae is a key gut microbial member in the Tammar wallaby that produce only 20% of the CH
4 emissions of cattle [
74]. This is because
Succinivibrionaceae produce succinate through the fumarate-succinate pathway, which is an intermediate product of propionate, that are easily absorbed by the animal for energy [
75].
Certain viral species can infect methanogens, called methanogenic viruses or methanophages. Methanophages against
Methanosarcina,
Methanococcus, and
Methanobacterium [
76,
77,
78] have been reported in methanogen abundant anoxic environments. Viruses that infect bacterial species can compete with methanogens for substrates [
76] and have also been reported in methanogenic environments. Accordingly, it is plausible that viruses infecting methanogenic archaea or anti-methanogenic bacteria are present in the bovine rumen.
Methane produced in the rumen can be utilized by other ruminal community members. Methanotrophic archaea, also known as methanotrophs, are a group of archaea that can utilize CH
4 as the sole source of carbon and energy [
79]. Under aerobic conditions, methanotrophs combine O
2 and CH
4 to form formaldehyde, which is then incorporated into organic compounds via the ribulose monophosphate pathway by type I methanotrophs (γ -proteobacteria) or the serine pathway by type II methanotrophs (α proteobacteria) [
79]. The methanotrophic bacteria including
Methylobacterium,
Methylomonas and
Methylomicrobium genera have been detected in the bovine rumen and have been shown to influence methanogens [
80].
Fungi species have been shown to promote methanogenic activity by producing various enzymes such as cellulases and hemicellulases, and these enzymes can break down complex polysaccharides (cellulose and hemicellulose) into simpler compounds that can be utilized by methanogens [
81]. Anaerobic fungi, such as
Neocallimastix spp., and
Piromyces spp., have been extensively studied for their ability to enhance the activity of methanogens in the rumen [
81]. These fungi species are commonly found in the rumen and play a crucial role in the degradation of plant biomass [
82]. As discussed above, it is apparent that the activities of methanogens in the rumen are interdependent on other microbes and their respective activities in the ruminal environment. Thus, understanding the interactions between the methanogens and other microorganisms within the rumen is important as such interactions could be harnessed for enteric methane mitigations from cattle.
5. Methanogens in the Reproductive Tract: Vagina, Uterus and Semen
Methanogen presence has been reported in both the lower and upper reproductive tracts of cattle (
Figure 1,
Table 2). The microbial community associated with the bovine vaginal tract has been relatively well characterized as compared to the cervical and uterine microbiota [
83]. Overall, there is less species richness and community diversity in the vaginal microbiota as compared to the bovine gut, and this community has been shown to influence reproductive health and fertility of female cattle [
83,
84]. Although the archaeal members of the vaginal microbiome have not yet been as extensively characterized as the bacterial members, the presence of some methanogens in the cattle vagina have been reported from 16S rRNA gene amplicon-based studies. The
Methanobrevibacter genus has been reported to be the predominant methanogen genus in the vaginal samples of Nellore cows [
85]. We recently reported 6 amplicon sequence variants (ASVs) that were classified as
Methanobrevibacter spp. (5 of these taxa were unclassified at species level and the remaining one was
M. ruminantium) present from vaginal swabs of both virgin yearling heifers and pregnant beef heifers [
21]. The
Methanobrevibacter ruminantium taxa was most frequently identified from the vaginal swab samples with greater abundance than the other
Methanobrevibacter taxa [
21].
While there are no culture-based studies reporting the isolation and identification of methanogens in the vaginal tract of cattle, methanogenic archaeal species have been cultured and isolated from the vaginal swabs [
86] and urine specimens [
87] of women with urinary tract infections. Belay et al. [
86] cultured two different
Methanobrevibacter smithii strains from the vaginal swabs of women diagnosed with bacterial vaginosis using traditional anaerobic culturing technique. Briefly, vaginal swabs were enriched in a medium containing various salts and additives, and yeast extract and tryptone in anaerobic serum tubes pressurized with H
2-CO
2 and supplemented with cysteine hydrochloride and Na
2S. 9H
20. Methane production in the serum tube was monitored using gas chromatography. Following enrichment, the cultures that produced CH
4 gas were plated on medium with 1% Gelrite to isolate methanogens. Two methanogen isolates were isolated and taxonomically identified as
Methanobrevibacter smithii PS and ALI based on the morphological, cultural, and immunological features. Likewise, Grine and colleagues [
87] isolated
Methanobrevibacter smithii strains from the urine samples of women suffering from urinary tract infections using a Hungate culture tube containing SAB medium, a versatile medium that supports the growth of most of methanogen species [
88]. Based on their methanogenic archaeal culturing results from 383 urine specimens (61% of them from women) prospectively collected for diagnosing urinary tract infection, these authors suggest that
M. smithii is part of the urinary microbiota of some individuals. Thus, both sequencing and culturing-based results obtained from bovine and human studies discussed above highlight that the microbial community in the bovine lower reproductive tract could harbor methanogenic archaea. The physiological function of methanogens in the lower reproductive tract of cattle remains to be explored even though some studies have suggested potential association of methanogens with reproductive health [
21,
85,
89,
90]. In the human vaginal tract, methanogens are known to play a significant role in prevention of acid accumulation (increase in vaginal pH) which disrupts the vaginal microbiota in bacterial vaginosis patients [
86,
87,
91].
The
in-utero environment has long been viewed as sterile as the cervix was thought to prevent ascending bacteria from the lower reproductive tract into the uterus (Wang et al., 2018). However, culture-independent high-throughput sequencing technologies have enabled the identification of commensal microbiota presence in the bovine uterus during both pregnancy and after parturition [
93]. The potential role of the uterine microbiome in reproductive health, conception, and embryo development is increasingly appreciated [
83,
94,
95]. Within the bovine uterine microbial community, methanogenic archaeal species have been reported. A sequencing-based study identified several methanogens in both pregnant and non-pregnant cows, including
Methanosphaera stadtmanae,
Methanobrevibacter ruminantium, and
Methanobacterium congolense [
85] (
Table 2;
Figure 1). Our lab has also identified
Methanobrevibacter ruminantium and
Methanobrevibacter wolini, which accounted for 0.05% of the total microbiota present in the uterus of virgin beef heifers (21-months old) [
25]. We also observed greater abundance of
Methanobrevibacter ruminantium (ASV330) in the uterine microbiota of beef cows that became pregnant than those remained open following artificial insemination, suggesting positive association of
Methanobrevibacter ruminantium with fertility [
96]. In contrary, methanogens have been shown to be present in uterus of cows with uterine infections, suggesting a potential role in pathogenesis [
97]. The functional and taxonomic characteristics of methanogens in the bovine uterus, like those found in the vagina, are yet to be fully explored.
Recent sequencing-based studies revealed that there are diverse and dynamic microbial communities residing within the bull reproductive tract [
98]. Methanogenic archaeal species are identified as commensal microbiota associated with bull semen and the abundance of methanogens in the semen may have an association with bull fertility. For example, Koziol and colleagues identified
Methanobrevibacter, Methanosphaera, and
Methanomassiliicoccus as the predominant methanogens present in the semen of breeding beef bulls [
99] using 16S rRNA gene amplicon sequencing. Likewise,
Methanocorpusculum spp. was identified in bovine bull semen, and the relative abundance of this methanogenic genus was inversely correlated with seminal commensal genera
Ruminoccoceae and
Rikenellaceae RC9 Gut group [
100]. Our research group detected more than a dozen methanogenic archaeal taxa (Listed in
Figure 1;
Table 2) from semen samples collected at three different stages of yearling beef bull development [
101]. These studies together demonstrated that the male reproductive tract is colonized by methanogens.
Although the functional features of the seminal microbiota including methanogenic archaeal members are yet to be characterized, a negative correlation of methanogenic archaeal abundance with bull fertility has been reported [
99,
100]. The bulls with low fertility had greater abundance of seminal
Methanocorpusculum as compared to bulls with high fertility [
100]. Semen samples with greater abundance of methanogens had significantly lower sperm motility compared to semen samples with lower levels of methanogens, suggesting a potential negative correlations between methanogens and sperm motility and development [
99].
6. Methanogens in the Respiratory Tract
Bovine respiratory microbial communities, particularly bacterial microbiota in the upper and lower respiratory tracts have been well studied using both culturing and sequencing-based methods due to their role in protecting or predisposing animal to bovine respiratory disease (BRD), which is one of the costliest diseases affecting commercial feedlot cattle [
102,
103,
104,
105]. While most of these sequencing methods used to characterize bovine respiratory microbiota are mainly limited to the 16S rRNA amplicon (V4) and (V3-V4) sequencing (which is more specific to bacterial populations), several studies have reported the presence of methanogenic archaea in the upper respiratory tract (
Table 2;
Figure 1). Amat and colleagues reported the presence of the
Methanobrevibacter genus in the nasopharynx of feedlot steers [
21]. Several taxa within the Methanobrevibacter, including
Methanobrevibacter ruminantium, have also been detected in the nasopharynx of virgin and pregnant beef cattle [
21]. Two
Methanobrevibacter species (
wolinii and
ruminantium) have also been reported in the nasopharyngeal microbiota of finishing feedlot heifers [
25]. The lower airway is also colonized by a microbial community and bacterial microbiota associated with the trachea [
103,
106,
107] and lung tissue have been relatively well documented in cattle. However, presence of archaeal species in the lower airway has not been reported in any of these studies. Since the 16S rRNA gene (V4 region) was used by most of these studies and neither archaeal targeted amplicon sequencing nor shotgun metagenomic sequencing approaches have been employed to characterize the lung tissue samples, it is challenging to make a conclusive statement on the presence or absence of methanogenic archaea in the bovine lower respiratory tract.
Figure 1.
Presence (purple color) or absence (blue) of methanogenic archaeal species reported in different anatomical sites of cattle. This figure was generated based on the data presented in the references listed in
Table 1 and
Table 2.
Figure 1.
Presence (purple color) or absence (blue) of methanogenic archaeal species reported in different anatomical sites of cattle. This figure was generated based on the data presented in the references listed in
Table 1 and
Table 2.
However, evidence derived from human studies suggests that the lower respiratory tract may harbor methanogenic archaea.
Methanobrevibacter spp.
(oralis and smithii) have been cultured and isolated from sputum, trachea-bronchial, and broncho-alveolar samples collected from humans [
108].
Methanogenic archaeal cell presence in the upper respiratory tract of cattle raises an important question about the survival mechanisms of methanogens in such an O
2 rich environment given that archaeal species involved in methanogenesis are believed to be strict anaerobes. It is not uncommon to identify anaerobic bacterial species some of which are associated with the ruminal commensal microbiota such as
Ruminococcus and
Thermodesulfovibrio (sulfate reducing bacteria) in the upper respiratory tract of cattle [
109]. Anaerobic bacteria are predominant components of the upper respiratory tract, and mixed anaerobic-aerobic agents are often responsible for respiratory infections in humans[
110]. Thus, despite that some of the methanogenic species in the nasopharyngeal and lung tissue samples of cattle can be transient and from eructation and inhalation of ruminal gas cap, the aerosols generated from the dust and soil particles [
106,
111,
112], the airway mucosal surface of the cattle can harbor methanogens as part of their commensal microbiota. These airway specific methanogens could have evolved to adapt and survive in the microenvironments along the respiratory tract, especially those parts with reduced O
2 levels. One of the potential methanogen-promoting factors in the airway can be associated with biofilm forming bacterial cells, as biofilms can provide localized anaerobic conditions. Biofilms can form in different areas of the respiratory tract [
113]. In addition, the presence of oxygen-utilizing bacteria in the respiratory tract may support the growth of methanogens by consuming O
2 and thereby creating anaerobic pockets where methanogens can persist [
114,
115]. Future culture-dependent studies are needed to isolate methanogens from the respiratory tract and explore metabolic features of these methanogens, and their interactions with the methanogens present in the rumen.
7. Methanogens in the Udder
The mammary gland is another site that has been reported to harbor relatively diverse and rich microbial communities [
116]. Distinctive and site-specific microbial communities are present in various niches of the udder including the teat apex, teat canal, milk, and colostrum [
116]. Some of these communities encompass archaeal members (
Table 2;
Figure 1). Guo and colleagues characterized the archaeal community shared between the maternal rumen and milk in grazing yak calves. They identified two archaeal phyla and 11 different common archaeal genera [
60]. The primary archaeal phyla found on the skin of the teat were
Euryarchaeota (76.8%) and
Thaumarchaeota (23.1%) with dominant genera being
Methanobrevibacter (61.7%) and
Candidatus nitrocosmicus (12.5%). Similar findings have been reported for the skin of dairy cows, where
Methanobrevibacter and
Methanosphaera were identified as the primary genera [
117]. Species within
Methanobrevibacter, including
M. ruminantium, M. smithii, M. millerae, and some
Methanocorpusculum spp. have also been detected in the bovine milk [
23,
60,
117]. No data is available regarding the presence of methanogenic archaea in bovine colostrum. However,
Methanobrevibacter oralis and
M. smithii species have been found in human colostrum [
118], suggesting that methanogenic archaea may also be present in the cattle colostrum.
Similar to the respiratory tract, the presence of methanogens on teat skin and udder raises an important question regarding the strict anaerobic nature of these methanogens.
Methanobrevibacter and
Candidatus nitrocosmicus are known to be strict anaerobes and are typically unable to survive with exposure to ambient air for more than 10 minutes [
119]. Therefore, their survival on the teat skin would be unlikely unless there is a wound present that creates an anaerobic environment suitable for methanogens. Further, research is needed to investigate the mechanisms and conditions that allow for the presence of methanogens on the skin and explore their potential role in the overall microbial ecology of the teat as related to milk production.
9. Challenges Associated with the Ruminal Methanogens and Future Directions
In vitro culturing techniques allow researchers to isolate and study specific microorganisms in a controlled environment and can provide insights into the physiology and ecology of these organisms. Isolation and culturing of methanogens from the rumen is a particularly challenging task due to their strict anaerobic nature and growth requirements for special culturing media, culturing apparatus, and H
2 gas supplementation, all of which have hindered the progress of isolation, and metabolic and genomic characterization of the methanogenic archaea associated with ruminal CH
4 production [
138,
139]. While recent advances in culture-independent high-throughput sequencing techniques have enabled characterization of ruminal microbiota and the potential involvement in methanogenic activity, the information is mostly limited to the bacterial population of the ruminal microbial ecosystem as most of the sequencing is based on 16S rRNA gene amplicon sequencing, which is more specific to bacteria and captures only a small fraction of the archaeal population. Thus, to understand the complete taxonomic characterization of the methanogens and other archaeal populations in the rumen, and other extra-gastrointestinal sites of the bovine body, archaea targeting amplicon sequencing such as 16S rRNA V2-V3 primers and
mcrA gene-based primers should be applied. To gain insights beyond the taxonomic properties of bovine methanogens, the metabolic features, and their interactions with other microorganisms such as fungi, bacteria and viruses, shotgun metagenomic sequencing should be performed. Also, comparative genomics on methanogenic isolates from different cattle body sites (e.g., respiratory, reproductive, ruminal and udder) should be performed to understand the genomic adaptative features of the methanogens from different anatomical sites and identify the seeding sources of the ruminal methanogens. Given the several external sources including the feed, soil and water consumed by cattle, and other farm animals and farmers who could exchange methanogens with cattle rumen and other body sites, comprehensive survey of the methanogens present in these external sources and their interactions with ruminal methanogens in cattle warrants further research.
While these culture-independent sequencing methods can provide taxonomic composition and functional features of the methanogenic archaeal members and their interactions with other microbial partners in a particular niche, one of the limitations of these sequencing techniques is that they could not provide information on the viability of the methanogenic archaeal cells. Considering the anaerobic nature of methanogens and their presence in non-anaerobic body sites including respiratory and lower reproductive tracts of cattle, it is critical to use culture- dependent techniques to isolate methanogens from these sites and verify findings from metagenomic sequencing. It is plausible that some of the genomic DNA extracted from the samples associated with nasopharynx, lung tissue and vagina of cattle might be originated from transient and dead methanogens. Nevertheless, identification of methanogenic archaeal genera and species with relatively high abundance, and consistently over multiple sampling timepoints in bovine respiratory and reproductive tracts presented above highlights that the methanogenic archaea could colonize and survive aerobic mucosal surfaces along the airway and urogenital tract of cattle. Thus, further research is warranted to isolate methanogens from extra-gastrointestinal tracts of cattle and explore the survival mechanisms of the methanogens in the environment where oxygen is present. Some anaerobic bacterial species can have evolved mechanisms that can either minimize the extent to which oxygen disrupts their metabolism [
140,
141] and/or rely on potential anaerobic and aerobic species co-existence mechanisms [
142].
Emerging evidence from humans [
141], bovine fetal fluids [
21,
27], the fetal intestine [
21,
27,
143], as well as the human fetal lung [
144], suggests that microbial colonization of calves may begin
in utero. This, coupled with rodent studies which demonstrate that fetal metabolic and nervous system development is impacted by the maternal microbiota during pregnancy [
145,
146], highlight the potential and extended role, of the maternal microbiome in calf microbiome development. Recent studies reported the presence of methanogenic archaeal species in fetal fluids and fetal intestine at 4-8 months of gestation. Thus, these recent developments warrant a re-consideration of the timing and mechanisms involved in the first colonization of calf ruminal methanogens.
10. Conclusions
Methanogens are responsible for enteric CH4 emissions in cattle, which contributes to a significant amount of dietary energy loss to the host and GHG emissions. The species associated with ruminal CH4 production are not only present in the cattle rumen, but they could also present in extra-gastrointestinal organs of cattle such as the reproductive and respiratory tracts, udder, eye, and hoof. Recent sequencing-based studies revealed that certain methanogenic taxa are shared by the ruminal, respiratory, and reproductive tracts of cattle as core taxa, suggesting potential interactions between the ruminal and extra-intestinal methanogens. The seeding of the rumen with methanogenic archaea could be from many possible sources within the bovine body (e.g., reproductive and respiratory tracts, and other microbial communities) and external sources such as pasture, soil, water, and farm animals. Therefore, a singular focus on the methanogens in the rumen may not be sufficient and a holistic approach which takes into consideration the transfer of methanogens between ruminal, extra-gastrointestinal, and environmental microbial communities. Taxonomic, genomic, and metabolic characteristics of the methanogenic archaeal species in the rumen and other bovine body sites should be investigated to gain more holistic insights into the methanogens in cattle. It is anticipated that the holistic understanding of the methanogens in the rumen and their interactions with the extra-gastrointestinal methanogens, and identification of the seeding sources (both within and external), and the colonization timing of the ruminal methanogens are important for the development of more effective CH4 mitigation strategies in cattle.